<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-969896454889667372</id><updated>2011-10-11T06:01:50.966-07:00</updated><title type='text'>ॐ*·Glossary of  Geological Engineering Terms·*ॐ</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>23</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5080041176217010136</id><published>2009-03-05T15:46:00.005-08:00</published><updated>2009-05-11T11:29:14.350-07:00</updated><title type='text'></title><content type='html'>&lt;p style="FONT-STYLE: italic" align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="WIDTH: 389px; HEIGHT: 216px" src="http://img155.imageshack.us/img155/3726/73ds2.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;br /&gt;&lt;br /&gt;&lt;p style="FONT-STYLE: italic"&gt;&lt;span style="FONT-WEIGHT: bold;font-size:180%;" &gt;"&lt;span style="font-family:arial;"&gt;Hi there!...Wait a few minutes in order to carge the page. you will find words, meanings, images and videos. in the left side you will find a translator and a virtual radius in order to let you listen the music in english. Thank you for visiting&lt;/span&gt;!&lt;/span&gt;&lt;span style="font-size:180%;"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-STYLE: italic"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="WIDTH: 87px; HEIGHT: 83px" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/ccschoolread3.gif" /&gt;&lt;/span&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img height="125" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/grdcl1r.gif" width="189" /&gt;&lt;/span&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="WIDTH: 87px; HEIGHT: 83px" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/ccschoolread3.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: left"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: left"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="WIDTH: 57px; HEIGHT: 75px" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/panda.gif" /&gt;&lt;/span&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="WIDTH: 88px; HEIGHT: 88px" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/A_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="WIDTH: 57px; HEIGHT: 75px" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/panda.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;br /&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;&lt;strong&gt;ADJECTIVE:&lt;/strong&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;The part of speech that modifies a noun or other sustantive. it is a word used tu describe people, animal and objects&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;Example: big- small&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;&lt;img style="WIDTH: 124px; HEIGHT: 230px" height="788" src="http://www.goethe-verlag.com/book2/_bilder/068.jpg" width="584" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;strong&gt;ADVERB:&lt;/strong&gt; It is a word that changes the verb and/or the adjective&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://myword.info/images/adverb_1d.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Alkali metal&lt;/span&gt;: A strongly basic metal like potassium or sodium.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.chem4kids.com/files/art/elem_alkalimetal1.gif" src="http://www.chem4kids.com/files/art/elem_alkalimetal1.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Alluvium&lt;/span&gt;: Unconsolidated terrestrial sediment composed of sorted or unsorted sand, gravel, and clay that has been deposited by water&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.showme.net/%7Efkeller/quake/images3/alluvium.gif" src="http://www.showme.net/~fkeller/quake/images3/alluvium.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Angular unconformity:&lt;/span&gt; An unconformity in which the bedding planes of the rocks above and below are not parallel.&lt;/span&gt;&lt;span style="font-size:130%;color:black;"&gt;ular unconformity&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.winona.edu/geology/mrw/mrwimages/Earth%20History/angular_uncof.JPG" src="http://www.winona.edu/geology/mrw/mrwimages/Earth%20History/angular_uncof.JPG" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Anthracite&lt;/span&gt;: The most highly metamorphosed form of coal, containing 92 to 98 percent of fixed carbon. It is black, hard, and glassy. &lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.matternetwork.com/images/Matter/300px-Coal_anthracite.jpg" src="http://www.matternetwork.com/images/Matter/300px-Coal_anthracite.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Aquifer&lt;/span&gt;: A permeable formation that stores and transmits groundwater in sufficient quantity to supply wells.&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://library.thinkquest.org/04oct/01590/humans/aquifer.jpg" src="http://library.thinkquest.org/04oct/01590/humans/aquifer.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;ARCHIMIDES&lt;/span&gt;&lt;span style="FONT-WEIGHT: normal;font-size:130%;" &gt;:was a Greek mathematician, physicist,engineer, inventor, and astronomer. Although few details of his life are known, he is regarded as one of the leading scientist in classical antiquity&lt;/span&gt;&lt;span style="FONT-WEIGHT: normal;font-size:130%;" &gt;.&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="WIDTH: 248px; HEIGHT: 269px" alt="http://www.barilochenyt.com.ar/arquimides.jpg" src="http://www.barilochenyt.com.ar/arquimides.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;object height="405" width="500"&gt;&lt;param name="movie" value="http://www.youtube.com/v/h3GIhfyLXwc&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/h3GIhfyLXwc&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;Arkose: A variety of sandstone containing abundant feldspar and quartz, frequently in angular, poorly sorted grains.&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.eserc.stonybrook.edu/terryville/Rocks/Arkose.jpg" src="http://www.eserc.stonybrook.edu/terryville/Rocks/Arkose.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Artesian well&lt;/span&gt;: A well that penetrates an aquiclude to reach an aquifer containing water under pressure. Thus water in the well rises above the surrounding water table&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.bartleby.com/images/A4images/A4artwel.jpg" src="http://www.bartleby.com/images/A4images/A4artwel.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="FONT-WEIGHT: bold; FONT-STYLE: italic; TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;strong&gt;ARTICLES: word used before nouns.In English the definite article is the, the indefinite article is a or an, and their force is generally to impart specificity to the noun or to single out the referent from the class named by the noun.&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;strong style="FONT-WEIGHT: bold"&gt;&lt;img height="65" src="http://educatecenter.com/images/Todos-hombre_29.jpg" width="52" border="0" /&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="TEXT-ALIGN: center"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Atmosphere &lt;/span&gt;: A unit of pressure equal to 101,325 newtons per square meter, or about 14.7 pounds per square inch.&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;img alt="http://iln.cite.hku.hk/com/1238/users/wkho2/Atmosphere/atmosphere-couche_f.jpg" src="http://iln.cite.hku.hk/com/1238/users/wkho2/Atmosphere/atmosphere-couche_f.jpg" /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;ATOLL&lt;/span&gt;: A continuous or broken circle of coral reef and low coral islands surrounding a central lagoon&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;img style="WIDTH: 318px; HEIGHT: 209px" alt="http://www.com.univ-mrs.fr/IRD/atollpol/ecorecat/images/atoll2.jpg" src="http://www.com.univ-mrs.fr/IRD/atollpol/ecorecat/images/atoll2.jpg" /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style="FONT-WEIGHT: bold;font-size:130%;" &gt;AXIS&lt;/span&gt;&lt;span style="font-size:130%;"&gt;:The line, real or imaginary, passing through the center of an object about which it could rotate; a point of reference.&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span lang="EN-GB"   style="font-family:Arial;font-size:130%;"&gt;&lt;img id="_x0000_i1038" height="320" alt="AppleMark " src="http://www.jensplanet.com/mathcourse/images/section4part2pic1.jpg" width="440" /&gt;&lt;/span&gt;&lt;br /&gt;&lt;/div&gt;&lt;p align="center"&gt;&lt;strong&gt;&lt;/strong&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5080041176217010136?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5080041176217010136/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_574.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5080041176217010136'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5080041176217010136'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_574.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/th_ccschoolread3.gif' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-1972985364427391867</id><published>2009-03-05T15:46:00.003-08:00</published><updated>2009-04-04T08:50:05.412-07:00</updated><title type='text'></title><content type='html'>&lt;p style="text-align: center;"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="width: 56px; height: 56px;" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/cutecolorskoala5a.gif" /&gt;&lt;/span&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 83px; height: 83px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/B_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;img style="width: 58px; height: 58px;" src="http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/cutecolorskoala5a.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Banded iron ore&lt;/span&gt;: A sediment consisting of layers of chert alternating with bands of ferric iron oxides (hematite and limonite) in valuable concentrations.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Barchan&lt;/span&gt;: A crescent-shaped sand dune moving across a clean surface with its convex face upwind and its concave slip face downwind.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 414px; height: 325px;" alt="http://www.indiana.edu/%7Eg103/G103/Week8/dune1.jpg" src="http://www.indiana.edu/%7Eg103/G103/Week8/dune1.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;h4 style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;BARREL:&lt;/span&gt;&lt;span style="font-weight: normal;font-size:130%;" &gt;A volumetric unit of measure for crude oil and petroleum products.&lt;br /&gt;&lt;/span&gt;&lt;/h4&gt;&lt;h4 style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 169px; height: 299px;" alt="https://www.eleconomista.es/imag/_v2/ilustraciones/barril-petroleo.jpg" src="https://www.eleconomista.es/imag/_v2/ilustraciones/barril-petroleo.jpg" /&gt;&lt;/span&gt;&lt;/h4&gt;&lt;div style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Basalt:&lt;/span&gt; A fine-grained, dark, mafic igneous rock composed largely of plagioclase feldspar and pyroxene.&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 267px; height: 193px;" alt="http://z.about.com/d/geology/1/0/R/K/basalt.jpg" src="http://z.about.com/d/geology/1/0/R/K/basalt.jpg" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Base-level&lt;/span&gt;: The level below which a stream cannot erode; usually sea level sometimes locally the level of a lake or resistant formation. &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 445px; height: 192px;" src="http://strata.geol.sc.edu/images/06FigBaseLevel.jpg" /&gt;&lt;/span&gt;&lt;span style=";font-family:Arial,Helvetica,sans-serif;font-size:130%;"  &gt;&lt;img style="width: 418px; height: 134px;" src="http://strata.geol.sc.edu/images/07FigBaseLevel.jpg" /&gt;&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Basement&lt;/span&gt;: The oldest rocks recognized in a given area, a complex of metamorphic and igneous rocks that underlies all the sedimentary formations. Usually Precambrian or Paleozoic in age.&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;img alt="http://www.yankalilla.sa.gov.au/webdata/resources/images/Our_Rocky_Foundation_02.jpg" src="http://www.yankalilla.sa.gov.au/webdata/resources/images/Our_Rocky_Foundation_02.jpg" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Basic rock&lt;/span&gt;: Any igneous rock containing mafic minerals rich in iron and magnesium, but containing no quartz and little sodium rich plagioclase feldspar.&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/Y6zpC3rPuzY&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/Y6zpC3rPuzY&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Basin:&lt;/span&gt; In tectonics, a circular, syncline-like depression of strata. In sedimentology, the site of accumulation of a large thickness of sediments. &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.shale-mudstone-research-schieber.indiana.edu/images/shale%20general/belt-shale-mudstone-s9.jpg" src="http://www.shale-mudstone-research-schieber.indiana.edu/images/shale%20general/belt-shale-mudstone-s9.jpg" /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Batholith:&lt;/span&gt; A great irregular mass of coarse-grained igneous rock with an exposed surface of more than 100 square kilometers, which has either intruded the country rock or been derived from it through metamorphism.&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;img alt="No se puede mostrar la imagen “http://www.tulane.edu/%7Esanelson/images/batholith.gif” porque contiene errores." src="http://www.tulane.edu/%7Esanelson/images/batholith.gif" /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Bauxite:&lt;/span&gt; A rock composed primarily of hydrous aluminum oxides and formed by weathering in tropical areas with good drainage; a major ore of aluminum.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.mii.org/Minerals/Minpics1/Bauxite.jpg" src="http://www.mii.org/Minerals/Minpics1/Bauxite.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Bedding&lt;/span&gt;: A characteristic of sedimentary rocks in which parallel planar surfaces separating different grain sizes or compositions indicate successive depositional surfaces that existed at the time of sedimentation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 457px; height: 347px;" alt="http://www.nhm.ac.uk/research-curation/research/projects/martian-met/images/2abedding.jpg" src="http://www.nhm.ac.uk/research-curation/research/projects/martian-met/images/2abedding.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Bed-load: &lt;/span&gt;The sediment that a stream moves along the bottom of its channel by rolling and bouncing.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/GeoBytes/Fieldwork/Snowdonia%20(A2)/Large%20angular%20bedload.jpg" src="http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/GeoBytes/Fieldwork/Snowdonia%20%28A2%29/Large%20angular%20bedload.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Beta-particle&lt;/span&gt;: An electron emitted with high energy and velocity from a nucleus undergoing radioactive decay.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://images.encyclopedia.com/getimage.aspx?id=2793144&amp;amp;hero=yes" src="http://images.encyclopedia.com/getimage.aspx?id=2793144&amp;amp;hero=yes" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;B-horizon: &lt;/span&gt;The intermediate layer in a soil, situated below the A-horizon and consisting of clays and oxides. Also called the zone of accumulation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 387px; height: 515px;" alt="http://www-markinfo.slu.se/eng/soilche/baskat/images/alb2.gif" src="http://www-markinfo.slu.se/eng/soilche/baskat/images/alb2.gif" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Biochemical precipitate: &lt;/span&gt;A sediment, especially of limestone or iron, formed from elements extracted from seawater by living organisms.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.microgenbioproducts.com/images/0004.jpg" src="http://www.microgenbioproducts.com/images/0004.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Bituminous coal: &lt;/span&gt;A soft coal formed by an intermediate degree of metamorphism and containing 15 to 20 percent volatiles. The most common grade of coal.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 534px; height: 364px;" alt="http://www.geoinfo.amu.edu.pl/wpk/pe/a/harbbook/c_xii/images/Bituminous1.jpg" src="http://www.geoinfo.amu.edu.pl/wpk/pe/a/harbbook/c_xii/images/Bituminous1.jpg" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Block fault&lt;/span&gt;&lt;span style="font-weight: bold;"&gt;:&lt;/span&gt; A structure formed when the crust is divided into blocks of different elevation by a set of normal faults.&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.uwgb.edu/DutchS/graphic0/seismol/faultblk.gif" src="http://www.uwgb.edu/DutchS/graphic0/seismol/faultblk.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Blowout:&lt;/span&gt; A shallow circular or elliptical depression in sand or dry soil formed by wind erosion.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="https://www.countyofsb.org/energy/images/blowoutOverhead.jpg" src="https://www.countyofsb.org/energy/images/blowoutOverhead.jpg" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;h3 style="text-align: center; font-weight: normal;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Bore:&lt;/span&gt; To enlarge and finish the surface of a cylindrical hole by the action of a rotating boring bar (cutting tool) or by the action of a stationary tool pressed (fed) against the surface as the part is rotated. &lt;/span&gt;&lt;/h3&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 189px; height: 244px;" alt="http://www.kalipedia.com/kalipediamedia/matematicas/media/200709/26/aritmetica/20070926klpmatari_89.Ges.SCO.png" src="http://www.kalipedia.com/kalipediamedia/matematicas/media/200709/26/aritmetica/20070926klpmatari_89.Ges.SCO.png" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;st1:city style="font-weight: bold;"&gt;&lt;st1:place&gt;&lt;span style="color:black;"&gt;Butte&lt;/span&gt;&lt;/st1:place&gt;&lt;/st1:city&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;:&lt;/span&gt; A steep sided and flat topped hill formed by erosion of flat laying strata where remnants of a resistant layer protect the softer rocks underneath.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt; &lt;/div&gt;&lt;div style="text-align: center;"&gt; &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;BYTE:&lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt;Eight related bits of data or an eight-bit binary number. Also denotes the amount of memory required to store one byte of data&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;a href="http://isis.astrogeology.usgs.gov/IsisWorkshop/index.php/Image:Bit-byte-word.jpg" class="internal" title="There are 8 bits in 1 byte, and 16 bits in 2 bytes. A 16-bit value is called a word."&gt;&lt;img alt="uploaded image: There are 8 bits in 1 byte, and 16 bits in 2 bytes. A 16-bit value is called a word." longdesc="/IsisWorkshop/index.php/Image:Bit-byte-word.jpg" class="thumbimage" src="http://isis.astrogeology.usgs.gov/IsisWorkshop/images_off/0/0d/Bit-byte-word.jpg" width="600" height="300" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-1972985364427391867?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/1972985364427391867/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_6101.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1972985364427391867'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1972985364427391867'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_6101.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://i11.photobucket.com/albums/a168/evelynregly/cutecolors/th_cutecolorskoala5a.gif' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-6001228906574608986</id><published>2009-03-05T15:46:00.001-08:00</published><updated>2009-04-04T09:07:46.821-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img src="file:///C:/DOCUME%7E1/JOSE/CONFIG%7E1/Temp/moz-screenshot-2.jpg" alt="" /&gt;&lt;img style="width: 83px; height: 96px;" alt="imagen" src="http://galeon.hispavista.com/animadosparati/img/de" vspace="5" border="0" hspace="5" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 82px; height: 82px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/C_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img style="width: 83px; height: 95px;" alt="imagen" src="http://galeon.hispavista.com/animadosparati/img/de" vspace="5" border="0" hspace="5" /&gt;&lt;img src="file:///C:/DOCUME%7E1/JOSE/CONFIG%7E1/Temp/moz-screenshot-3.jpg" alt="" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Caldera:&lt;/span&gt; A large, circular depression in a volcanic terrain, typically originating in collapse, explosion, or erosion.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 337px; height: 700px;" alt="http://earthsci.org/education/teacher/basicgeol/igneous/caldera1.gif" src="http://earthsci.org/education/teacher/basicgeol/igneous/caldera1.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;CALCULUS&lt;/span&gt;&lt;span style="font-size:130%;"&gt;: The branch of mathematics that deals with limits and the differentiation and integration of functions of one or more variables.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 292px; height: 188px;" alt="http://blog.beliefnet.com/moviemom/calculus.JPG" src="http://blog.beliefnet.com/moviemom/calculus.JPG" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Carbonate ion&lt;/span&gt;: The anion group CO3 with a charge of minus two.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.uwgb.edu/DutchS/GRAPHIC0/ROCKMIN/ATOM-STRUCT/Calcite0.gif" src="http://www.uwgb.edu/DutchS/GRAPHIC0/ROCKMIN/ATOM-STRUCT/Calcite0.gif" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Carbonate platform:&lt;/span&gt; A submarine or intertidal shelf whose elevation is maintained by active shallow water carbonate deposition.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://strata.geol.sc.edu/thinsections/images/fig61.jpg" src="http://strata.geol.sc.edu/thinsections/images/fig61.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Carbonate rock:&lt;/span&gt; A rock composed of carbonate minerals, especially limestone and dolomite.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 401px; height: 401px;" alt="http://upload.wikimedia.org/wikipedia/commons/f/fc/Silica_Carbonate_Rock_-_Metamorphic_Rock_San_Benito_County_California_1622.jpg" src="http://upload.wikimedia.org/wikipedia/commons/f/fc/Silica_Carbonate_Rock_-_Metamorphic_Rock_San_Benito_County_California_1622.jpg" /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Cataclastic rock&lt;/span&gt;: A breccia of powdered rock formed by crushing and shearing during tectonic movements.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 297px; height: 191px;" alt="http://www.taskgeoscience.co.uk/images/cataclasis/Fig7.jpg" src="http://www.taskgeoscience.co.uk/images/cataclasis/Fig7.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;Cation: Any ion with a positive electric charge. &lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://mediateca.educa.madrid.org/imagen/imagenes/publicas/tam4/gr/gr6kcm9kbnrl3h6q.jpg" src="http://mediateca.educa.madrid.org/imagen/imagenes/publicas/tam4/gr/gr6kcm9kbnrl3h6q.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Central vent:&lt;/span&gt; The largest vent of a volcano, situated at the center of its cone.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 306px; height: 332px;" alt="http://cache.eb.com/eb/image?id=72249&amp;amp;rendTypeId=35" src="http://cache.eb.com/eb/image?id=72249&amp;amp;rendTypeId=35" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Chemical engineering&lt;/b&gt; is the branch of engineering that deals with the application of physical science with mathematics, to the process of converting raw material or chemicals into more useful or valuable forms. In addition to producing useful materials, chemical engineering is also concerned with pioneering valuable new materials and techniques, an important form of research and development. A person employed in this field is called a chamical engineer&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 275px; height: 183px;" alt="http://www.grupoconexant.com.ar/imagenes/quimica.jpg" src="http://www.grupoconexant.com.ar/imagenes/quimica.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;h1 style="text-align: center;" id="firstHeading" class="firstHeading"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/h1&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Chemical weathering&lt;/span&gt;: The total set of all chemical reactions that act on rock exposed to water and atmosphere and so change it minerals to stable forms.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 414px; height: 310px;" alt="http://www.earth.ox.ac.uk/%7Eoesis/field/medium/granite1.jpg" src="http://www.earth.ox.ac.uk/%7Eoesis/field/medium/granite1.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;CHEMISTRY&lt;/span&gt;&lt;span style="font-size:130%;"&gt;:is the science concerned with the composition, structure, and properties of matter, as well as the changes it undergoes during chemical reactions.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt; &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 273px; height: 254px;" alt="http://www.oaklandcc.edu/asc/ASCAH/images/metalcomplex.gif" src="http://www.oaklandcc.edu/asc/ASCAH/images/metalcomplex.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt; &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Chert&lt;/span&gt;: A sedimetary form of amorphous or extremely fine-grained silica, partially hydrous, found in concretions and beds.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.uky.edu/KGS/rocksmn/images/chert_var.jpg" src="http://www.uky.edu/KGS/rocksmn/images/chert_var.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Cinder cone&lt;/span&gt;: A steep, conical hill built up about a volcanic vent and composed of coarse pyroclasts expelled from the vent by escaping gases.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 328px; height: 239px;" alt="http://www.k12.hi.us/%7Ekapunaha/student_projects/volc_blowout/images/chad%27s_cinder_cone.gif" src="http://www.k12.hi.us/%7Ekapunaha/student_projects/volc_blowout/images/chad%27s_cinder_cone.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Civil engineering:&lt;/b&gt;is the branch of engineering hat deals with the design, and construction of public and private works, such as infrastructure ( water supply,treatment etc.), bridges and buildings.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;a href="http://en.wikipedia.org/wiki/File:Torres_Petronas_Mayo_2004.jpg" class="image" title="The Petronas Twin Towers, designed by Thornton-Tomasetti and Ranhill Bersekutu Sdn Bhd engineers, and Cesar Pelli, were the world's tallest buildings from 1998 to 2004."&gt;&lt;img style="width: 205px; height: 307px;" alt="" src="http://upload.wikimedia.org/wikipedia/commons/thumb/f/f1/Torres_Petronas_Mayo_2004.jpg/300px-Torres_Petronas_Mayo_2004.jpg" class="thumbimage" border="0" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;    &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Clastic rock:&lt;/span&gt; A sedimentary rock formed from mineral particles (clasts) that were mechanically transported.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 455px; height: 313px;" alt="http://www.dkimages.com/discover/previews/796/5103775.JPG" src="http://www.dkimages.com/discover/previews/796/5103775.JPG" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Clay: &lt;/span&gt;Any of a number of hydrous aluminosilicate minerals formed by weathering and hydration of other silicates; also, any mineral fragment smaller than 1/255 mm.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 306px; height: 218px;" alt="http://www.dep.state.fl.us/geology/geologictopics/rocks/common_clay.jpg" src="http://www.dep.state.fl.us/geology/geologictopics/rocks/common_clay.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Coal:&lt;/span&gt; The metamorphic product of stratified plant remains. It contains more than 50 percent carbon compounds and burns readily.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 366px; height: 243px;" alt="http://www.astecindustries.com/images/photos/Coal_Hands.jpg" src="http://www.astecindustries.com/images/photos/Coal_Hands.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Coastal plain&lt;/span&gt;: A low plain of little relief adjacent to the ocean and covered with gently dipping sediments.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.alaska-in-pictures.com/data/media/6/arctic-coastal-plain_7967.jpg" src="http://www.alaska-in-pictures.com/data/media/6/arctic-coastal-plain_7967.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Composite cone:&lt;/span&gt; The volcanic cone of a stratovolcano, composed of both cinders and lava flows.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 378px; height: 343px;" alt="http://cache.eb.com/eb/image?id=62705&amp;amp;rendTypeId=4" src="http://cache.eb.com/eb/image?id=62705&amp;amp;rendTypeId=4" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;computer&lt;/b&gt; is a machine  that manipulates data according to a list of instructions.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 232px; height: 232px;" alt="http://maternal.cesfam.vmf.googlepages.com/computadora-ninos-3.jpg/computadora-ninos-3-full.jpg" src="http://maternal.cesfam.vmf.googlepages.com/computadora-ninos-3.jpg/computadora-ninos-3-full.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Construction&lt;/b&gt;:The systematic act or process of building or erecting buildings, roads or other structures.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 320px; height: 226px;" alt="http://www.dreamhouse.lt/foto/constructions/main.jpg" src="http://www.dreamhouse.lt/foto/constructions/main.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;color:black;"&gt;&lt;span style="font-weight: bold;"&gt;Contact metamorphism:&lt;/span&gt; Mineralogical and textural changes and deformation of rock resulting from the head and pressure of an igneous intrusion in the near vicinity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 419px; height: 287px;" alt="http://academic.brooklyn.cuny.edu/geology/grocha/monument/images/metheat.gif" src="http://academic.brooklyn.cuny.edu/geology/grocha/monument/images/metheat.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/div&gt;&lt;br /&gt;&lt;p align="center"&gt;&lt;img src="file:///C:/DOCUME%7E1/JOSE/CONFIG%7E1/Temp/moz-screenshot.jpg" alt="" /&gt;&lt;img src="file:///C:/DOCUME%7E1/JOSE/CONFIG%7E1/Temp/moz-screenshot-1.jpg" alt="" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-6001228906574608986?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/6001228906574608986/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9049.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/6001228906574608986'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/6001228906574608986'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9049.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5764877322890881235</id><published>2009-03-05T15:45:00.005-08:00</published><updated>2009-04-04T09:09:05.577-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img style="width: 97px; height: 97px;" alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/anibfly4.gif" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 84px; height: 84px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/D_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img style="width: 98px; height: 98px;" alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/anibflyf3.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Datum plane:&lt;/span&gt; An artificially established, well surveyed horizontal plane against which elevations, depths, tides, etc. are measured (for example mean sea-level).&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 338px; height: 253px;" alt="http://farm4.static.flickr.com/3163/2678638123_f1a4b49e29.jpg" src="http://farm4.static.flickr.com/3163/2678638123_f1a4b49e29.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Daughter element:&lt;/span&gt; Also "daughter product". An element that occurs in a rock as end product of the radioactive decay of another element.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 320px; height: 187px;" alt="http://www.istockanalyst.com/images/articles/HAI_01132009_Fig1.jpg2009148352.jpg" src="http://www.istockanalyst.com/images/articles/HAI_01132009_Fig1.jpg2009148352.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Debris avalanche&lt;/span&gt;: A fast downhill mass movement of soil and rock.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 332px; height: 246px;" alt="http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_33/PublishingImages/33-debav.gif" src="http://www.conservation.ca.gov/cgs/information/publications/cgs_notes/note_33/PublishingImages/33-debav.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Declination:&lt;/span&gt; At any place on Earth, the angle between the magnetic and rotational poles.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://astronomy.swinburne.edu.au/cms/imagedb/albums/userpics/declination1.gif" src="http://astronomy.swinburne.edu.au/cms/imagedb/albums/userpics/declination1.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Deflation:&lt;/span&gt; The removal of clay and dust from dry soil by strong winds.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 221px; height: 112px;" alt="http://www.fhsu.edu/biology/Eberle/PacificNW/DeflationPlainME99.JPG" src="http://www.fhsu.edu/biology/Eberle/PacificNW/DeflationPlainME99.JPG" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Delta&lt;/span&gt;: A body of sediment deposited in an ocean or lake at the mouth of a stream.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 349px; height: 518px;" alt="http://www.vegueries.com/reportatges/deltaFmap.gif" src="http://www.vegueries.com/reportatges/deltaFmap.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Delta kame:&lt;/span&gt; A deposit having the form of a steep, flat topped hill, left at the front of a retreating continental glacier.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.earth.rochester.edu/ees274/EBNApage/kamedelta2.gif" src="http://www.earth.rochester.edu/ees274/EBNApage/kamedelta2.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Dendritic drainage:&lt;/span&gt; A stream system that branches irregularly and resembles a branching tree in plan.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.tulane.edu/%7Esanelson/images/drainpat.gif" src="http://www.tulane.edu/%7Esanelson/images/drainpat.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Density&lt;/span&gt;: The mass per unit volume of a substance, commonly expressed in grams/ cubic centimeter.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 175px; height: 196px;" alt="http://static.howstuffworks.com/gif/science-projects-for-kids-density-and-volume-2.jpg" src="http://static.howstuffworks.com/gif/science-projects-for-kids-density-and-volume-2.jpg" /&gt;&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Density current&lt;/span&gt;: A s&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;ubaqueous current that flows on the bottom of a sea or lake because entering water is denser due to temperature or suspended sediments.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 316px; height: 200px;" alt="http://www.cst.com/CMS/images/article205/fields.jpg" src="http://www.cst.com/CMS/images/article205/fields.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Deposition&lt;/span&gt;: A general term for the accumulation of sediments by either physical or chemical sedimentation.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 380px; height: 248px;" alt="http://www.pacificislandtravel.com/nature_gallery/geomorpohology3.gif" src="http://www.pacificislandtravel.com/nature_gallery/geomorpohology3.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Desert pavement:&lt;/span&gt; A residual deposit produced by continued deflation, which removes the fine grains of a soil and leaves a surface covered with closely packed cobbles.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www2.mcdaniel.edu/Biology/wildamerica/desert/DesertPavement.jpg" src="http://www2.mcdaniel.edu/Biology/wildamerica/desert/DesertPavement.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Detrital sediment:&lt;/span&gt; A sediment deposited by a physical process.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 326px; height: 242px;" alt="http://spot.pcc.edu/%7Eksutton/GEO207/Images/witwatersrand_conglomerate.jpg" src="http://spot.pcc.edu/%7Eksutton/GEO207/Images/witwatersrand_conglomerate.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Diagenesis:&lt;/span&gt; The physical and chemical changes undergone by a sediment during lithification and compaction, excluding erosion and metamorphism.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.cnsm.csulb.edu/departments/geology/images/monterey.jpg" src="http://www.cnsm.csulb.edu/departments/geology/images/monterey.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Diatom&lt;/span&gt;: A one celled plant that has a siliceous framework and grows in oceans and lakes.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.micrographia.com/specbiol/alg/diato/diat0200/diatom05.jpg" src="http://www.micrographia.com/specbiol/alg/diato/diat0200/diatom05.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Diatomite:&lt;/span&gt; A siliceous chert-like sediment formed from the hard parts of diatoms.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 308px; height: 239px;" alt="http://www.mine-engineer.com/mining/mineral/Diatomite-small.jpg" src="http://www.mine-engineer.com/mining/mineral/Diatomite-small.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Diatom ooze:&lt;/span&gt; A fine muddy sediment consisting of the hard parts of diatoms.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 225px; height: 517px;" alt="http://www-odp.tamu.edu/publications/202_IR/chap_12/images/12_f21.jpg" src="http://www-odp.tamu.edu/publications/202_IR/chap_12/images/12_f21.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Diatreme:&lt;/span&gt; A volcanic vent filled with breccia by the explosive escape of gases.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.eos.ubc.ca/research/diamonds/kopylova/pics/Maar_xsect1.gif" src="http://www.eos.ubc.ca/research/diamonds/kopylova/pics/Maar_xsect1.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;strong&gt;DICTIONARY&lt;/strong&gt;:It is a reference book.You can be found: meaning of words, translation, synonyms, tenses, grammatical information, pronunciation, abbreviations, examples, images, derivations and grossed reference.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;A book giving information on particular subjects or on a particular class of words, names, or facts, usually arranged alphabetically: a biographical dictionary; a dictionary of mathematics.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt; &lt;span style="font-size:130%;"&gt;&lt;img src="http://www.ucmp.berkeley.edu/glossary/glossary.gif" width="215" height="196" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;differential&lt;/b&gt;: &lt;/span&gt;&lt;span style="font-size:130%;"&gt;is a device, usually but not necessarily employing gears, capable of transmitting torque and rotation through three shafts, almost always used in one of two ways. In one way, it receives one input and provides two outputs; this is found in most automobiles. In the other way, it combines two inputs to create an output that is the sum, difference, or average, of the inputs.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://stockcarscience.com/blog/media/blogs/scs/differential.gif" src="http://stockcarscience.com/blog/media/blogs/scs/differential.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;    &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Dip&lt;/span&gt;: The angle by which a stratum or other planar feature deviates from the horizontal. The angle is measured in a plane perpendicular to the strike.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 337px; height: 334px;" alt="http://www.uwm.edu/Course/geosci697/stereo/dip-angle%20direction.jpg" src="http://www.uwm.edu/Course/geosci697/stereo/dip-angle%20direction.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Divide:&lt;/span&gt; A ridge of high ground separating two drainage basins emptied by different streams. &lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 498px; height: 400px;" alt="http://www.noaanews.noaa.gov/stories2006/images/southern-ocean-divide.jpg" src="http://www.noaanews.noaa.gov/stories2006/images/southern-ocean-divide.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Dome&lt;/span&gt;: In structural geology, a round or elliptical upwarp of strata resembling a short anticline.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 333px; height: 250px;" alt="http://media-2.web.britannica.com/eb-media/07/125907-004-8EB5F2E2.jpg" src="http://media-2.web.britannica.com/eb-media/07/125907-004-8EB5F2E2.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Drainage basin&lt;/span&gt;: A region of land surrounded by divides and crossed by streams that eventually converge to one river or lake.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.uwsp.edu/geO/faculty/ritter/images/lithosphere/fluvial/drainage_basin.jpg" src="http://www.uwsp.edu/geO/faculty/ritter/images/lithosphere/fluvial/drainage_basin.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Drift (glacial):&lt;/span&gt; A collective term for all the rock, sand, and clay that is transported and deposited by a glacier either as till or as outwash.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 381px; height: 255px;" alt="http://pubs.usgs.gov/dds/dds-39/images/JPG/large_screen/fig51.jpg" src="http://pubs.usgs.gov/dds/dds-39/images/JPG/large_screen/fig51.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Drumlin:&lt;/span&gt; A smooth, streamlined hill composed of till.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 366px; height: 215px;" alt="http://www.fettes.com/lothian/images/drumlin.jpg" src="http://www.fettes.com/lothian/images/drumlin.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Dry wash: &lt;/span&gt;An intermittent streambed in an arroyo or canyon that carries water only briefly after a rain.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 419px; height: 298px;" alt="http://pubs.usgs.gov/of/2008/1100/images/coverphoto.jpg" src="http://pubs.usgs.gov/of/2008/1100/images/coverphoto.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="color:black;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Dune:&lt;/span&gt; An elongated mound of sand formed by wind or water.&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 235px; height: 176px;" alt="http://chgblog.com/images/dune.jpg" src="http://chgblog.com/images/dune.jpg" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5764877322890881235?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5764877322890881235/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_1983.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5764877322890881235'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5764877322890881235'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_1983.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://farm4.static.flickr.com/3163/2678638123_f1a4b49e29_t.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5558523668297633080</id><published>2009-03-05T15:45:00.003-08:00</published><updated>2009-04-04T09:10:12.663-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img style="width: 89px; height: 62px;" alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/faebutterflybush.gif" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 71px; height: 71px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/E_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img style="width: 85px; height: 59px;" alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/faebutterflybush.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Earthflow:&lt;/span&gt; A detachment of soil and broken rock and its subsequent downslope movement at slow or moderate rates in a stream- or tongue like form.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://pubs.usgs.gov/fs/2004/3072/images/slump-earth%20flow_opt.jpg" src="http://pubs.usgs.gov/fs/2004/3072/images/slump-earth%20flow_opt.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Earthquake&lt;/span&gt;: The violent oscillatory motion of the ground caused by the passage of seismic waves radiating from a fault along which sudden movement has taken place.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/4Y-62Ti5_6s&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/4Y-62Ti5_6s&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Ebb tide&lt;/span&gt;: The part of the tide cycle during which the water level is falling.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 455px; height: 341px;" alt="http://i.pbase.com/u34/selvin/upload/31162513.EbbTide.jpg" src="http://i.pbase.com/u34/selvin/upload/31162513.EbbTide.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Echo-sounder&lt;/span&gt;: An oceanographic instrument that emits sound pulses into the water and measures its depth by the time elapsed before they return.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in;" alt="http://upload.wikimedia.org/wikipedia/commons/3/3c/Sediment_echo-sounder_hg.png" src="http://upload.wikimedia.org/wikipedia/commons/3/3c/Sediment_echo-sounder_hg.png" width="590" height="845" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Ecliptic&lt;/span&gt;: The plane that contains the Earth's orbit around the Sun.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.astro.virginia.edu/class/oconnell/astr121/im/CS-ecliptic-2-CK.jpg" src="http://www.astro.virginia.edu/class/oconnell/astr121/im/CS-ecliptic-2-CK.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eclogite&lt;/span&gt;: An extremely high-pressure metamorphic rock containing garnet and pyroxene.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 534px; height: 631px;" alt="http://www.geol.ucsb.edu/faculty/hacker/photos/petrology/eclogiteFoldsNordfjord.jpg" src="http://www.geol.ucsb.edu/faculty/hacker/photos/petrology/eclogiteFoldsNordfjord.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Ecology&lt;/span&gt;: The science of the life cycles, populations, and interactions of various biological species as controlled by their physical environment, including also the effect of life forms upon the environment.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 124px; height: 137px;" src="http://www.mi-direccion.com/gifsanimados/NATURALEZA/arboles/1360_animado.gif" border="0" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Elastic rebound theory&lt;/span&gt;: A theory of fault movement and earthquake generation that holds that faults remain locked while strain energy accumulates in the country rock, and then suddenly slip and release this energy.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://alancolville.com/quakes/elastic_rebound.jpg" src="http://alancolville.com/quakes/elastic_rebound.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Electrical engineering&lt;/span&gt;: &lt;/span&gt;&lt;span style="font-size:130%;"&gt; referred to as &lt;/span&gt;&lt;span style="font-size:130%;"&gt;electrical and electronic engineering&lt;/span&gt;&lt;span style="font-size:130%;"&gt;, is a field of &lt;/span&gt;&lt;span style="font-size:130%;"&gt;engineering&lt;/span&gt;&lt;span style="font-size:130%;"&gt; that deals with the study and application of electricity,electronics and electrimagnetism&lt;/span&gt;&lt;span style="font-size:130%;"&gt;.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 229px; height: 198px;" alt="http://acalzonquitao.files.wordpress.com/2008/09/electricidad.jpg" src="http://acalzonquitao.files.wordpress.com/2008/09/electricidad.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Electron&lt;/span&gt;: A negatively charged particle with negligible mass orbiting around the nucleus of an atom.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/2IGIyA57Brc&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/2IGIyA57Brc&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Elevation&lt;/span&gt;: The vertical height of one point on the Earth above a given datum plane, usually sea level.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 647px; height: 457px;" alt="http://upload.wikimedia.org/wikipedia/commons/3/3c/Earth_elevation_histogram_fr.jpg" src="http://upload.wikimedia.org/wikipedia/commons/3/3c/Earth_elevation_histogram_fr.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Elliptical orbit: An orbit with the shape of a geometrical ellipse. All orbits are elliptical or hyperbolic, with the Sun occupying one focus.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 570px; height: 250px;" alt="http://www.uwsp.edu/geo/faculty/ritter/images/atmosphere/energy/elliptical_orbit.jpg" src="http://www.uwsp.edu/geo/faculty/ritter/images/atmosphere/energy/elliptical_orbit.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eolian&lt;/span&gt;: Pertaining to or deposited by wind.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://energiaeoliana.files.wordpress.com/2008/05/harta_potentialului_eolian.jpg" src="http://energiaeoliana.files.wordpress.com/2008/05/harta_potentialului_eolian.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt; &lt;span style="font-weight: bold;font-size:130%;" &gt;EMPLOY&lt;/span&gt;&lt;span style="font-size:130%;"&gt;:to hire or engage the services of (a person or persons); provide employment for; have or keep in one's service&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 211px; height: 140px;" alt="http://www.uthm.edu.my/ppi/images/employ.jpg" src="http://www.uthm.edu.my/ppi/images/employ.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;&lt;span style="font-style: italic;"&gt;ENGINEER&lt;/span&gt;&lt;/span&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;:&lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt;person professionally engaged in a field of engineering&lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt;. Engineers are concerned with developing economical and safe solutions to practical problems, by applying mathematics &lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt;and scientific knowledge &lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt;while considering technical constraints&lt;/span&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://www.burkett.org/portfolio/fall07/MickeyMouseEngineer.jpg" width="220" border="0" height="226" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: center;"&gt;&lt;span style="font-weight: bold; font-style: italic;font-size:130%;" &gt;Engineering&lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt;:is the discipline  &lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt; of applying scientific knowledge&lt;/span&gt;&lt;span style="font-style: italic;font-size:130%;" &gt; and utilizing natural laws and physical resources in order to design and implement, materials,structures,machines,devices,systems and processes that safely realize a desired objective and meet specified criteria.&lt;/span&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 339px; height: 328px;" alt="http://www.nww.usace.army.mil/html/offices/ed/c/images/c4.jpg" src="http://www.nww.usace.army.mil/html/offices/ed/c/images/c4.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eon:&lt;/span&gt; The largest division of geologic time, embracing several Eras, for example, the Phanerozoic, 600 m.y. ago to present); also any span of one billion years.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://gsc.nrcan.gc.ca/paleochron/images/timechart.gif" src="http://gsc.nrcan.gc.ca/paleochron/images/timechart.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Epicenter:&lt;/span&gt; The point on the Earth's surface directly above the focus or hypocenter of an Earthquake.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://www.glynn.k12.ga.us/BHS/Juniorprojects/Hopkins01/miguelo23724/Epicenter.gif" src="http://www.glynn.k12.ga.us/BHS/Juniorprojects/Hopkins01/miguelo23724/Epicenter.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Epoch&lt;/span&gt;: One subdivision of a geologic period, often chosen to correspond to a stratigraphic series. Also used for a division of time corresponding to a paleomagnetic interval.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://images.chron.com/blogs/sciguy/archives/EPOCH-0_lores.jpg" src="http://images.chron.com/blogs/sciguy/archives/EPOCH-0_lores.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Era&lt;/span&gt;: A time period including several periods, but smaller than an eon. Commonly recognized eras are Precambrian, Paleozoic, Mesozoic, and Cenozoic.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.indiana.edu/%7Egeol105b/images/gaia_chapter_6/timescale.jpg" src="http://www.indiana.edu/%7Egeol105b/images/gaia_chapter_6/timescale.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Erosion:&lt;/span&gt; The set of all processes by which soil and rock are loosened and moved downhill or downwind.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 641px; height: 405px;" alt="http://drake.marin.k12.ca.us/stuwork/rockwater/Beach%20Erosion%20-%20Water%20Project/Erosion%20for%20title%20page%202.jpg" src="http://drake.marin.k12.ca.us/stuwork/rockwater/Beach%20Erosion%20-%20Water%20Project/Erosion%20for%20title%20page%202.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eskar&lt;/span&gt;: A glacial deposit in the form of a continuous, winding ridge, formed from the deposits of a stream flowing beneath the ice.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://img.sparknotes.com/figures/3/31ebea601a7d05e9ec8d0854cec9b406/earthscience_f17.jpg" src="http://img.sparknotes.com/figures/3/31ebea601a7d05e9ec8d0854cec9b406/earthscience_f17.jpg" /&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Ethics&lt;/b&gt; is a branch of philosophy which seeks to address questions about morality, such as how a moral outcome can be achieved in a specific situation, how moral values should be determined , what moral values people actually.&lt;/span&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://4.bp.blogspot.com/_SUGxQ6MZbyQ/RuU9aeSbo9I/AAAAAAAAAGk/IbkHk4DcN0s/s320/ETICAS.JPG" src="http://4.bp.blogspot.com/_SUGxQ6MZbyQ/RuU9aeSbo9I/AAAAAAAAAGk/IbkHk4DcN0s/s320/ETICAS.JPG" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="color: rgb(0, 0, 0); text-align: left;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eugeosyncline&lt;/span&gt;: The seaward part of a geosyncline; characterized by clastic sediments and volcanism.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 455px; height: 195px;" alt="http://www.uwsp.edu/geo/projects/geoweb/participants/dutch/graphic0/platetec/geosyn4.gif" src="http://www.uwsp.edu/geo/projects/geoweb/participants/dutch/graphic0/platetec/geosyn4.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eustatic change&lt;/span&gt;: Sea level changes that affect the whole Earth.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.homepage.montana.edu/%7Egeol445/hyperglac/eustasy1/eustasyloop.gif" src="http://www.homepage.montana.edu/%7Egeol445/hyperglac/eustasy1/eustasyloop.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Eutrophication:&lt;/span&gt; A superabundance of algal life in a body of water; caused by an unusual influx of nitrate, phosphate, or other nutrients.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://library.thinkquest.org/04oct/01590/pollution/culturaleutroph.jpg" src="http://library.thinkquest.org/04oct/01590/pollution/culturaleutroph.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Evaporite: A chemical sedimentary rock consisting of minerals precipitated by evaporating waters, especially salt and gypsum.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://media-2.web.britannica.com/eb-media/11/2711-004-3FC05D3A.gif" src="http://media-2.web.britannica.com/eb-media/11/2711-004-3FC05D3A.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Exfoliation&lt;/span&gt;: A physical weathering process in which sheets of rock are fractured and detached from an outcrop.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://ougseurope.org/rockon/surface/img/exfoliation.jpg" src="http://ougseurope.org/rockon/surface/img/exfoliation.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Exobiology&lt;/span&gt;: The study of life outside the Earth.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.molvray.com/sf/images/dinoman_neoteny.jpg" src="http://www.molvray.com/sf/images/dinoman_neoteny.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5558523668297633080?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5558523668297633080/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_1795.html#comment-form' title='1 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5558523668297633080'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5558523668297633080'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_1795.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_SUGxQ6MZbyQ/RuU9aeSbo9I/AAAAAAAAAGk/IbkHk4DcN0s/s72-c/ETICAS.JPG' height='72' width='72'/><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-2909823833818102201</id><published>2009-03-05T15:45:00.001-08:00</published><updated>2009-04-04T09:11:02.105-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/fairyani10.gif" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 84px; height: 84px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/F_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/fairyani10.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Facies: &lt;/span&gt;The set of all characteristics of a sedimentary rock that indicates its particular environment of deposition and which distinguish it from other facies in the same rock.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.museumwales.ac.uk/media/2/2/4/2/thumb_500/facies.jpg" src="http://www.museumwales.ac.uk/media/2/2/4/2/thumb_500/facies.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fault&lt;/span&gt;: A planar or gently curved fracture in the Earth's crust across which there has been relative displacement.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.geo.wvu.edu/%7Ejtoro/Petroleum/petroleum_figs/review2/traps/faults.jpg" src="http://www.geo.wvu.edu/%7Ejtoro/Petroleum/petroleum_figs/review2/traps/faults.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fault-block mountain:&lt;/span&gt; A mountain or range formed as a horst when it was elevated between parallel normal faults.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://upload.wikimedia.org/wikipedia/commons/6/6a/Teton_fault_block.jpg" src="http://upload.wikimedia.org/wikipedia/commons/6/6a/Teton_fault_block.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fault plane&lt;/span&gt;: The plane that best approximates the fracture surface of a fault.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.bhrc.ac.ir/ISMN/SHABAKEH/faq/files/Fault%20plane_files/image001.jpg" src="http://www.bhrc.ac.ir/ISMN/SHABAKEH/faq/files/Fault%20plane_files/image001.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Faunal succession&lt;/span&gt;: The evolutionary sequence of life forms, especially as recorded by the fossil remains in a stratigraphic sequence.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in;" alt="http://www.soton.ac.uk/%7Eimw/jpg-Lulworth/5LC-lullog-succession.jpg" src="http://www.soton.ac.uk/%7Eimw/jpg-Lulworth/5LC-lullog-succession.jpg" width="845" height="845" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Felsic&lt;/span&gt;: An adjective used to describe a light-colored igneous rock poor in iron and magnesium content, abundant in feldspars and quartz.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.mongolia.cratertocirque.com/images/pages/medium/mg-347-felsic-mafic-blobs.jpg" src="http://www.mongolia.cratertocirque.com/images/pages/medium/mg-347-felsic-mafic-blobs.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fiord&lt;/span&gt;: A former glacial valley with steep walls and a U-shaped profile now occupied by the sea.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://www.pitt.edu/%7Ecejones/GeoImages/3IntrusiveBodies/1Plutonsz/FelsicEnclaves.JPG" src="http://www.pitt.edu/%7Ecejones/GeoImages/3IntrusiveBodies/1Plutonsz/FelsicEnclaves.JPG" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fissure:&lt;/span&gt; An extensive crack, break, or fracture in the rocks.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.phoenixrealestateguy.com/BlogImages/blogimagesearth-20fissure.png" src="http://www.phoenixrealestateguy.com/BlogImages/blogimagesearth-20fissure.png" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fissure vein:&lt;/span&gt; A cleft or crack in the rock material of the earth's crust, filled with mineral matter different from the walls and precipitated therin from aqueous solution.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.geologywales.co.uk/dgb/banded.jpg" src="http://www.geologywales.co.uk/dgb/banded.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Flood basalt&lt;/span&gt;: A plateau basalt extending many kilometers in flat, layered flows originating in fissure eruptions.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://upload.wikimedia.org/wikipedia/commons/thumb/0/07/3-Devils-grade-Moses-Coulee-Cattle-Feed-Lot-PB110016.JPG/721px-3-Devils-grade-Moses-Coulee-Cattle-Feed-Lot-PB110016.JPG" src="http://upload.wikimedia.org/wikipedia/commons/thumb/0/07/3-Devils-grade-Moses-Coulee-Cattle-Feed-Lot-PB110016.JPG/721px-3-Devils-grade-Moses-Coulee-Cattle-Feed-Lot-PB110016.JPG" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Flood plain&lt;/span&gt;: A level plain of stratified alluvium on either side of a stream; submerged during floods and built up silt and sand carried out of the main channel.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.bbc.co.uk/schools/riversandcoasts/images/alt_stills/flood-plain1.gif" src="http://www.bbc.co.uk/schools/riversandcoasts/images/alt_stills/flood-plain1.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Flood tide&lt;/span&gt;: The part of the tide cycle during which the water is rising or leveling off at high water&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://www.mabernierfinearts.com/images/gallery/FebruaryFloodTide.JPG" src="http://www.mabernierfinearts.com/images/gallery/FebruaryFloodTide.JPG" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Flow cleavage&lt;/span&gt;: In a metamorphic rock, the parallel arrangement of all planar or linear crystals as a result of rock flowage during metamorphism.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://ic.ucsc.edu/%7Ecasey/eart150/Lectures/1classIntro/APClvgNovaScta.jpg" src="http://ic.ucsc.edu/%7Ecasey/eart150/Lectures/1classIntro/APClvgNovaScta.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fluid inclusion&lt;/span&gt;: A small body of fluid that is entrapped in a crystal and has the same composition as the fluid from which the crystal formed.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.nuigalway.ie/nanoscale/images/Inclus01.jpg" src="http://www.nuigalway.ie/nanoscale/images/Inclus01.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Flume:&lt;/span&gt; A laboratory model of stream flow and sedimentation consisting of a rectangular channel filled with sediment and running water.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.egr.msu.edu/%7Ephani/microadv_flume.jpg" src="http://www.egr.msu.edu/%7Ephani/microadv_flume.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Focus (earthquake)&lt;/span&gt;: The point at which the rupture occurs; synonymous with hypocenter.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://alancolville.com/quakes/focus_epicenter.jpg" src="http://alancolville.com/quakes/focus_epicenter.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fold:&lt;/span&gt; A planar feature, such as a bedding plane, that has been strongly warped, presumably by deformation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Foliation&lt;/span&gt;: Any planar set of minerals or banding of mineral concentrations including cleavage, found in a metamorphic rock.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://www.indiana.edu/%7Egeol105/images/gaia_chapter_5/foliation.jpg" src="http://www.indiana.edu/%7Egeol105/images/gaia_chapter_5/foliation.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Foraminifera:&lt;/span&gt; A class of oceanic protozoa most of which have shells composed of calcite.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://strata.geol.sc.edu/thinsections/images/fig3.jpg" src="http://strata.geol.sc.edu/thinsections/images/fig3.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Foraminiferal ooze:&lt;/span&gt; A calcareous sediment composed of the shells of dead Foraminifera.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://chestofbooks.com/animals/Manual-Of-Zoology/images/Fig-15-Organisms-in-the-Atlantic-ooze-chiefly-Foraminif.jpg" src="http://chestofbooks.com/animals/Manual-Of-Zoology/images/Fig-15-Organisms-in-the-Atlantic-ooze-chiefly-Foraminif.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;FORCE:&lt;/span&gt;An influence that if applied to a free body results chiefly in an acceleration of the body and sometimes in elastic deformation and other effects.&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 378px; height: 216px;" alt="http://www.starbaseca.org/images/mud2.jpg" src="http://www.starbaseca.org/images/mud2.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Forset bed: &lt;/span&gt;One of the inclined beds found in crossbedding; also an inclined bed deposited on the outer front of a delta.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www-personal.umich.edu/%7Ehoaglund/TwoCreek/northend.jpg" src="http://www-personal.umich.edu/%7Ehoaglund/TwoCreek/northend.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Formation: The basic unit for the naming of rocks in stratigraphy: a set of rocks that are or once were horizontally continuous, that share some distinctive feature of lithology, and are large enough to be mapped.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://media-cdn.tripadvisor.com/media/photo-s/01/03/1f/72/red-rock-formation.jpg" src="http://media-cdn.tripadvisor.com/media/photo-s/01/03/1f/72/red-rock-formation.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fossil:&lt;/span&gt; An impression, cast, outline, or track of any animal or plant that is preserved in rock after the original organic material is transformed or removed.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/SEDfRy6DQns&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/SEDfRy6DQns&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fossil fuel: &lt;/span&gt;A general term for combustible geologic deposits of carbon in reduced (organic) form and of biological origin, including coal, oil, natural gas, oil shales, and tar sands. &lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Friction breccia:&lt;/span&gt; A breccia formed in a fault zone or volcanic pipe by the relative motion of two rock bodies.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://depthome.brooklyn.cuny.edu/geology/core332/images/breccia.jpg" src="http://depthome.brooklyn.cuny.edu/geology/core332/images/breccia.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fringing reef:&lt;/span&gt; A coral reef that is directly attached to a landmass not made of coral.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 632px; height: 474px;" alt="http://www.albion.edu/geology/Geo210_Hawaii/Coastal/images/fringing_reefs.jpg" src="http://www.albion.edu/geology/Geo210_Hawaii/Coastal/images/fringing_reefs.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Fumarole: &lt;/span&gt;A small vent in the ground from which volcanic gases and heated groundwater emerge, but not lava.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.skimountaineer.com/Trips/LassenSki99/LassenFumarole.jpg" src="http://www.skimountaineer.com/Trips/LassenSki99/LassenFumarole.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-2909823833818102201?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/2909823833818102201/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_122.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/2909823833818102201'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/2909823833818102201'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_122.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-7522463205862010006</id><published>2009-03-05T15:44:00.004-08:00</published><updated>2009-04-04T09:13:09.362-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img style="width: 52px; height: 87px;" alt="imagen" src="http://galeon.hispavista.com/animadosparati/img/shdg" vspace="5" border="0" hspace="5" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 79px; height: 79px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/G_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img style="width: 52px; height: 87px;" alt="imagen" src="http://galeon.hispavista.com/animadosparati/img/shdg" vspace="5" border="0" hspace="5" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Gabbro: &lt;/span&gt;A black, coarse-grained, intrusive igneous rock, composed of calcic feldspars and pyroxene. The intrusive equivalent of basalt.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.indiana.edu/%7Eg103/G103/wk3/gabbro.jpg" src="http://www.indiana.edu/%7Eg103/G103/wk3/gabbro.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;GAS:&lt;/span&gt;&lt;span style="font-size:130%;"&gt; is A fluid (such as air) that has neither independent shape nor volume, but tends to expand indefinitely.&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt; &lt;span style="font-size:130%;"&gt;&lt;img style="width: 235px; height: 235px;" alt="http://www.earrese.es/images/gas.jpg" src="http://www.earrese.es/images/gas.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Geochronology&lt;/span&gt;: The science of absolute dating a&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;nd relative dating of geologic formations and events, primarily through the measurement of daughter elements produced by radioactive decay in minerals.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.ansto.gov.au/__data/assets/image/0012/7203/Geochronology_core.jpg" src="http://www.ansto.gov.au/__data/assets/image/0012/7203/Geochronology_core.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Geologic cycle&lt;/span&gt;: The sequence through which rock material passes in going from its sedimentary form, through diastrophism and deformation of sedimentary rock, then through metamorphism and eventual melting and magma formation, then through volcanism and plutonism to igneous rock formation, and finally through erosion to form new sediments.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.earth.rochester.edu/ees119/fig1_5.jpg" src="http://www.earth.rochester.edu/ees119/fig1_5.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Geomorphology: The science of surface landforms and their interpretation on the basis of geology and climate.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 686px; height: 641px;" alt="http://bullard.esc.cam.ac.uk/%7Erwalker/pictures/gowk_geomorph.jpg" src="http://bullard.esc.cam.ac.uk/%7Erwalker/pictures/gowk_geomorph.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Geosyncline&lt;/span&gt;: A major downwarp in the Earth's crust, usually more than 1000 kilometers in length, in which sediments accumulate to thicknesses of many kilometers. The sediments may eventually be deformed and metamorphosed during a mountain-building episode.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.yankalilla.sa.gov.au/webdata/resources/images/The_End_of_the_Geosyncline_02.jpg" src="http://www.yankalilla.sa.gov.au/webdata/resources/images/The_End_of_the_Geosyncline_02.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Geotherm:&lt;/span&gt; A curving surface within Earth along which the temperature is constant.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.solarserver.de/lexikon/images/geotherm.jpg" src="http://www.solarserver.de/lexikon/images/geotherm.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Glacial rebound&lt;/span&gt;: Epeirogenic uplift of the crust that takes place after the retreat of a continental glacier, in response to earlier subsidence under the weight of the ice.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://bprc.osu.edu/education/rr/webex/Images%20WebEx/glacial%20rebound.jpg" src="http://bprc.osu.edu/education/rr/webex/Images%20WebEx/glacial%20rebound.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Glacier:&lt;/span&gt; A mass of ice and surficial snow that persists throughout the year and flows downhill under its own weight. The size range is from 100 meters to 10,000 kilometers.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.pocketpicks.co.uk/latest/wp-content/uploads/2007/06/glacier1.jpg" src="http://www.pocketpicks.co.uk/latest/wp-content/uploads/2007/06/glacier1.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Glass&lt;/span&gt;: A rock formed when magma is too rapidly cooled (quenched) to allow crystal growth.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 232px; height: 232px;" alt="http://www.lakewoodconferences.com/direct/dbimage/50222982/Reflective_Glass.jpg" src="http://www.lakewoodconferences.com/direct/dbimage/50222982/Reflective_Glass.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Gneiss: A coarse-grained regional metamorphic rock that shows compositional banding and parallel alignment of minerals.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 471px; height: 413px;" alt="http://www.gc.maricopa.edu/earthsci/imagearchive/KINKED_GNEISS_big.jpg" src="http://www.gc.maricopa.edu/earthsci/imagearchive/KINKED_GNEISS_big.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Graben&lt;/span&gt;: A downthrown block between two normal faults of parallel strike but converging dips; hence a tensional feature. See also horst.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/study/Images/HorstGraben.gif" src="http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/study/Images/HorstGraben.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Graded bedding&lt;/span&gt;: A bed in which the coarsest particles are concentrated at the bottom and grade gradually upward into fine silt, the whole bed having been deposited by a waning current.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://media-2.web.britannica.com/eb-media/07/2707-004-EF56DCEB.gif" src="http://media-2.web.britannica.com/eb-media/07/2707-004-EF56DCEB.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Graded stream: A stream whose smooth profile is unbroken by resistant ledges, lakes, or waterfalls, and which maintains exactly the velocity required to carry the sediment provided to it.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 401px; height: 581px;" alt="http://myweb.cwpost.liu.edu/vdivener/notes/gradation.gif" src="http://myweb.cwpost.liu.edu/vdivener/notes/gradation.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;Granite: A coarse-grained, intrusive igneous rock composed of quartz, orthoclase feldspar, sodic plagioclase feldspar, and micas. Also sometimes a metamorphic product.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 270px; height: 270px;" alt="http://www.global-b2b-network.com/direct/dbimage/50343312/Granite.jpg" src="http://www.global-b2b-network.com/direct/dbimage/50343312/Granite.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Granitization&lt;/span&gt;: The formation of metamorphic granite from other rocks by recrystallization with or without complete melting.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Granular snow&lt;/span&gt;: Snow that has been metamorphosed into small granules of ice.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 396px; height: 297px;" alt="http://farm1.static.flickr.com/155/358306874_d58bc3bf86.jpg?v=0" src="http://farm1.static.flickr.com/155/358306874_d58bc3bf86.jpg?v=0" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Granulite&lt;/span&gt;: A metamorphic rock with coarse interlocking grains and little or no foliation.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;a href="http://www.monanneeaucollege.com/minerauxphoto/granulite.1.net2.jpg"&gt;&lt;img src="http://www.monanneeaucollege.com/minerauxphoto/granulite.1.net1.jpg" alt="zoom" width="369" border="1" height="281" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Gravel&lt;/span&gt;: The coarsest of alluvial sediments, containing mostly particles larger than 2 mm in size and including cobbles and boulders.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.davidcopeland.com/Gravel.jpg" src="http://www.davidcopeland.com/Gravel.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;Gravitation:&lt;/span&gt;&lt;span style="font-size:130%;"&gt; is a natural phenomenon  by which objects with mass attract one another. In everyday life, gravitation is most commonly thought of as the agency which lends weight to objects with mass.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;a href="http://en.wikipedia.org/wiki/File:Solar_sys.jpg" class="image" title="Gravitation keeps the planets in orbit about the Sun. (Not to scale)"&gt;&lt;img alt="" src="http://upload.wikimedia.org/wikipedia/commons/thumb/c/c2/Solar_sys.jpg/350px-Solar_sys.jpg" class="thumbimage" width="350" border="0" height="220" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Gravity anomaly&lt;/span&gt;: The value of gravity left after subtracting from a gravity measurement the reference value based on latitude, and possibly the free-air and Bouguer corrections.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.geologyrocks.co.uk/system/files/u2/subgravanom.gif" src="http://www.geologyrocks.co.uk/system/files/u2/subgravanom.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Gravity survey&lt;/span&gt;: The measurement of gravity at regularly spaced grid points with repetitions to control instrument drift.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.gravitationalsystems.org/world_gravity.jpg" src="http://www.gravitationalsystems.org/world_gravity.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Greenhouse effect:&lt;/span&gt; The heating of the atmosphere by the absorption of infrared energy re-emitted by the Earth as it receives light energy in the visible band from the Sun.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.myclimatechange.net/UserImage/3/Definition/GreenhouseEffect.jpg" src="http://www.myclimatechange.net/UserImage/3/Definition/GreenhouseEffect.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Greenschist&lt;/span&gt;: A metamorphic schist containing chlorite and epidote (which are green) and formed by low-temperature, low-pressure metamorphism.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://z.about.com/d/geology/1/0/8/W/actinstone.jpg" src="http://z.about.com/d/geology/1/0/8/W/actinstone.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Ground moraine&lt;/span&gt;: A glacial deposit of till with no marked relief, interpreted as having been transported at the base of the ice.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.geographyhigh.connectfree.co.uk/s3glacgeoghigh35c.gif" src="http://www.geographyhigh.connectfree.co.uk/s3glacgeoghigh35c.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Groundwater:&lt;/span&gt; The mass of water in the ground below the phreatic zone, occupying the total pore space in the rock and moving slowly downhill where permeability allows.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://bottledh20.files.wordpress.com/2008/03/groundwater_1.jpg" src="http://bottledh20.files.wordpress.com/2008/03/groundwater_1.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Gully&lt;/span&gt;: A small steep-sided valley or erosional channel from 1 meter to about 10 meters across.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="cursor: -moz-zoom-in;" alt="http://plantandsoil.unl.edu/croptechnology2005/UserFiles/Image/siteImages/GullyErosionPasture-NRCS-LG.jpg" src="http://plantandsoil.unl.edu/croptechnology2005/UserFiles/Image/siteImages/GullyErosionPasture-NRCS-LG.jpg" width="603" height="845" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Guyot&lt;/span&gt;: A flat-topped submerged mountain or seamount found in the ocean.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://nsdl.sdsc.edu/projects/CapricornModule/guyot-formation.jpeg" src="http://nsdl.sdsc.edu/projects/CapricornModule/guyot-formation.jpeg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-7522463205862010006?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/7522463205862010006/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_3715.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/7522463205862010006'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/7522463205862010006'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_3715.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-4242553461096959786</id><published>2009-03-05T15:44:00.003-08:00</published><updated>2009-03-27T10:07:11.343-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-4242553461096959786?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/4242553461096959786/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9856.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/4242553461096959786'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/4242553461096959786'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9856.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-1669429921476163098</id><published>2009-03-05T15:44:00.001-08:00</published><updated>2009-04-04T09:13:54.450-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/faetwinkle.gif" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 79px; height: 79px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/H_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/faetwinkle.gif" /&gt;&lt;/p&gt;  &lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hanging valley:&lt;/span&gt; A former glacial tributary valley that enters a larger glacial valley above its base, high up on the valley wall.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.scalloway.org.uk/images/uvalley.gif" src="http://www.scalloway.org.uk/images/uvalley.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hard water&lt;/span&gt;: Water that contains sufficient dissolved calcium and magnesium to cause a carbonate scale to form when the water is boiled or to prevent the sudsing of soap.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img style="cursor: -moz-zoom-in; width: 616px; height: 683px;" alt="http://www.watersoftening.org/Blocked%20Pipe1.jpg" src="http://www.watersoftening.org/Blocked%20Pipe1.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;HEAT&lt;/span&gt;:If a temperature difference exists between two points heat will flow from the point at the higher temperature to the point at the lower temperature. This flow will continue until equilibrium has been reached&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 262px; height: 182px;" alt="http://www.iesmarquesdelozoya.net/111/calor.jpg" src="http://www.iesmarquesdelozoya.net/111/calor.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Heat conduction:&lt;/span&gt; The transfer of the rapid vibrational energy of atoms and molecules, which constitutes heat energy, through the mechanism of atomic or molecular impact.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.beodom.com/assets/images/blog/principles-thermal-insulation/heat-transmittance-means.jpg" src="http://www.beodom.com/assets/images/blog/principles-thermal-insulation/heat-transmittance-means.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Heat engine&lt;/span&gt;: A device that transfers heat from a place of high temperature to a place of lower temperature and does mechanical work in the process.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.chemistry.wustl.edu/%7Ecourses/genchem/Tutorials/Fridge/images/HeatEng.jpg" src="http://www.chemistry.wustl.edu/%7Ecourses/genchem/Tutorials/Fridge/images/HeatEng.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hill: &lt;/span&gt;A natural land elevation, usually less than 1000 feet above its surroundings, with a rounded outline. The distinction between hill and mountain depends on the locality.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hogback&lt;/span&gt;: A formation similar to a Cuesta in that it is a ridge formed by slower erosion of hard strata, but having two steep, equally inclined slopes.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 617px; height: 462px;" alt="http://upload.wikimedia.org/wikipedia/commons/5/58/Garden_of_the_Gods_Hogback_Formations.jpg" src="http://upload.wikimedia.org/wikipedia/commons/5/58/Garden_of_the_Gods_Hogback_Formations.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hooke's Law: &lt;/span&gt;The principle that the stress within a solid is proportional to the strain. It holds only for strains of a few percent or less.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://www.4physics.com/phy_demo/HookesLaw/InitialSetUp.gif" src="http://www.4physics.com/phy_demo/HookesLaw/InitialSetUp.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hornfels&lt;/span&gt;: A high-temperature, low-pressure metamorphic rock of uniform grain size showing no foliation. Usually formed by contact metamorphism.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://geology.com/rocks/pictures/hornfels.jpg" src="http://geology.com/rocks/pictures/hornfels.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Horst: &lt;/span&gt;An elongate, elevated block of crust forming a ridge or plateau, typically bounded by parallel, outward-dipping normal faults.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://earthquake.usgs.gov/learning/glossary/images/horst_graben.jpg" src="http://earthquake.usgs.gov/learning/glossary/images/horst_graben.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hot spring&lt;/span&gt;: A spring whose waters are above both human body and soil temperature as a result of plutonism at depth.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img src="http://www.usatourist.com/slideshows/yellowstone/images/Rimmed%20Hot%20Spring.jpg" alt="Rimmed Hot Spring" border="0" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Humus: &lt;/span&gt;The decayed part of the organic matter in a soil.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt; &lt;/span&gt;&lt;img alt="http://www.quick-compost.com/organicgardensoil/images/humus_hands1.jpg" src="http://www.quick-compost.com/organicgardensoil/images/humus_hands1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hydration&lt;/span&gt;: A chemical reaction, usually in weathering, which adds water or OH to a mineral structure.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://records.viu.ca/%7Eearles/kerrick-dehydration-earthquakes.gif" src="http://records.viu.ca/%7Eearles/kerrick-dehydration-earthquakes.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hydraulic conductivity&lt;/span&gt;: A measure of the permeability of a rock or soil: the volume of flow through a unit surface in unit time with unit hydraulic pressure difference as the driving force.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 544px; height: 407px;" alt="http://soils.usda.gov/technical/technotes/note6fig2.jpg" src="http://soils.usda.gov/technical/technotes/note6fig2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hydrocarbon: &lt;/span&gt;An organic chemical compound made up of ca&lt;/span&gt;&lt;span style=";font-size:130%;color:black;"  &gt;rbon and hydrogen atoms arranged in chains or rings.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 402px; height: 349px;" alt="http://www.energy.gov.ab.ca/NaturalGas/graphics/NGC_Molecule.jpg" src="http://www.energy.gov.ab.ca/NaturalGas/graphics/NGC_Molecule.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hydrologic cycle&lt;/span&gt;: The cyclical movement of water from the ocean to the atmosphere, through rain to the surface, through runoff and groundwater to streams, and back to the sea.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/vYBjPE0wekw&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/vYBjPE0wekw&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Hydrology&lt;/span&gt;: The science of that part of the hydrologic cycle between rain and return to the sea; the study of water on and within the land.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.ldeo.columbia.edu/%7Emartins/hydro/Hydro_cycle.gif" src="http://www.ldeo.columbia.edu/%7Emartins/hydro/Hydro_cycle.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-1669429921476163098?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/1669429921476163098/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_861.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1669429921476163098'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1669429921476163098'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_861.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-7110403821856143121</id><published>2009-03-05T15:43:00.007-08:00</published><updated>2009-04-04T09:14:42.636-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/angel2.gif" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 74px; height: 74px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/I_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img alt="Animated fairies at dragondropland.com" src="http://www.dragondropland.com/FAE/angel1.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Igneous rock&lt;/span&gt;: A rock formed by congealing rapidly or slowly from a molten state.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/Y4HOOvtvH9Q&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/Y4HOOvtvH9Q&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Ignimbrite&lt;/span&gt;: An igneous rock formed by the lithification of volcanic ash and volcanic breccia.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Inclination&lt;/span&gt;: The angle between a line in the Earth's magnetic field and the horizontal plane; also a synonym for dip.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.tpub.com/content/neets/14189/img/14189_124_2.jpg" src="http://www.tpub.com/content/neets/14189/img/14189_124_2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Index of refraction:&lt;/span&gt; The ratio of the speed of light in a vacuum to the speed in a material; this ratio determines the amount that light is refracted as it passes into a crystal.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://sol.sci.uop.edu/%7Ejfalward/refraction/airglassrefract.jpg" src="http://sol.sci.uop.edu/%7Ejfalward/refraction/airglassrefract.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Infiltration:&lt;/span&gt; The movement of groundwater or hydrothermal water into rock or soil through joints and pores.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 455px; height: 356px;" alt="http://www.clw.csiro.au/mar/images/mar_infiltration.gif" src="http://www.clw.csiro.au/mar/images/mar_infiltration.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Interfacial angle&lt;/span&gt;: The angle between two crystal faces of a crystal, characteristic of a mineral's symmetry.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.esrf.eu/UsersAndScience/Publications/Highlights/2000/scmatter/SCMFig-38.gif" src="http://www.esrf.eu/UsersAndScience/Publications/Highlights/2000/scmatter/SCMFig-38.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Interior drainage&lt;/span&gt;: A system of streams that converge in a closed basin and evaporate without reaching the sea.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.permanentwaterproofing.com/images/Interior%20Drainage%20System.gif" src="http://www.permanentwaterproofing.com/images/Interior%20Drainage%20System.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Intermontane basin&lt;/span&gt;: A basin between mountain ranges, often formed over a graben.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 610px; height: 401px;" alt="http://www.geomorph.org/gal/mslattery/IAG7.jpg" src="http://www.geomorph.org/gal/mslattery/IAG7.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Intrusion:&lt;/span&gt; An igneous rock body that has forced its way in a molten state into surrounding country rock.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.lenntech.com/images/gw-sewater-intrusion2.gif" src="http://www.lenntech.com/images/gw-sewater-intrusion2.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Intrusive rock&lt;/span&gt;: Igneous rock that is interpreted as a former intrusion from its cross-cutting contacts, chilled margins, or other field relations.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 390px; height: 202px;" alt="http://www.uwsp.edu/geo/faculty/ritter/images/lithosphere/Earth_Structure/igenous%20landforms.jpg" src="http://www.uwsp.edu/geo/faculty/ritter/images/lithosphere/Earth_Structure/igenous%20landforms.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Ion&lt;/span&gt;: An atom or group of atoms that has gained or lost electrons and so has a net electric charge.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://porpax.bio.miami.edu/%7Ecmallery/150/memb/ion_channel2_sml.jpg" src="http://porpax.bio.miami.edu/%7Ecmallery/150/memb/ion_channel2_sml.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Isograd:&lt;/span&gt; A line or curved surface connecting rocks that have undergone an equivalent degree of metamorphism.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.webpages.uidaho.edu/%7Edgeist/isograd.jpg" src="http://www.webpages.uidaho.edu/%7Edgeist/isograd.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Isostasy&lt;/span&gt;: The mechanism whereby areas of the crust rise or subside until the mass of their topography is buoyantly supported or compensated by the thickness of crust below, which "floats" on the denser mantle. The theory that continents and mountains are supported by low-density crustal "roots."&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.physicalgeography.net/fundamentals/images/isostasy.jpg" src="http://www.physicalgeography.net/fundamentals/images/isostasy.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style=";font-size:130%;color:black;"  &gt;&lt;span style="font-weight: bold;"&gt;Isotope&lt;/span&gt;: One of several forms of one element, all having the same number of protons in the nucleus, but differing in their number of neutrons and thus atomic weight.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://education.jlab.org/glossary/isotope.gif" src="http://education.jlab.org/glossary/isotope.gif" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-7110403821856143121?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/7110403821856143121/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_2851.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/7110403821856143121'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/7110403821856143121'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_2851.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-7028053893027772178</id><published>2009-03-05T15:43:00.005-08:00</published><updated>2009-04-04T09:22:40.378-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span id="ctl00_MainContentPlaceholder_ctl01_ctl00_lblEntry"&gt;&lt;/span&gt;&lt;img src="http://www.scjfrayluis.com/gifsanimados/hadas/013.gif" width="91" height="80" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 81px; height: 81px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/J_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img src="http://www.scjfrayluis.com/gifsanimados/hadas/013.gif" width="91" height="80" /&gt;&lt;/p&gt;  &lt;p&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Juvenile gas&lt;/span&gt;: Gases that come to the surface for the first time from the deep interior. &lt;/span&gt;&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://z.about.com/d/geology/1/0/A/7/1/saltonmudvolcs11.jpg" src="http://z.about.com/d/geology/1/0/A/7/1/saltonmudvolcs11.jpg" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-7028053893027772178?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/7028053893027772178/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_7245.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/7028053893027772178'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/7028053893027772178'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_7245.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-1249634981685689298</id><published>2009-03-05T15:43:00.003-08:00</published><updated>2009-04-04T09:37:48.223-07:00</updated><title type='text'></title><content type='html'>&lt;p style="font-style: italic;" align="center"&gt;&lt;img style="width: 103px; height: 103px;" src="http://www.castelldeferro.info/gif/hadas1/036.gif" border="0" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 85px; height: 85px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/L_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img style="width: 103px; height: 103px;" src="http://www.castelldeferro.info/gif/hadas1/036.gif" border="0" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Laccolith: A sill-like igneous intrusion that forces apart two strata and forms a round, lens-shaped body many times wider than it is thick.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://upload.wikimedia.org/wikipedia/commons/thumb/4/4f/Laccolith.svg/512px-Laccolith.svg.png" src="http://upload.wikimedia.org/wikipedia/commons/thumb/4/4f/Laccolith.svg/512px-Laccolith.svg.png" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lahar: A mudflow of unconsolidated volcanic ash, dust, breccia, and boulders mixed with rain or the water of a lake displaced by a lava flow.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://mail.colonial.net/%7Ehkaiter/earth_science_images/MSH82_lahar_from_march_82_eruption_03-21-82_med.jpg" src="http://mail.colonial.net/%7Ehkaiter/earth_science_images/MSH82_lahar_from_march_82_eruption_03-21-82_med.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Landslide: The rapid downslope movement of soil and rock material, often lubricated by groundwater, over a basal shear zone; also the tongue of stationary material deposited by such an event.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.geology.enr.state.nc.us/Landslide%20web%20version/Geologic_hazards_landslides/Fig-4_General_landslide.jpg" src="http://www.geology.enr.state.nc.us/Landslide%20web%20version/Geologic_hazards_landslides/Fig-4_General_landslide.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lapilli: A fragment of volcanic rock formed when magma is ejected into the air by expanding gases. The size of the fragments ranges from sand- to cobble-size.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 376px; height: 268px;" alt="http://www.swisseduc.ch/stromboli/glossary/icons/lapilli.jpg" src="http://www.swisseduc.ch/stromboli/glossary/icons/lapilli.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lateral moraine: A moraine formed along the side of a valley glacier and composed of rock scraped off or fallen from the valley sides.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.fettes.com/Cairngorms/images/lateral_moraine_Patagonia.jpg" src="http://www.fettes.com/Cairngorms/images/lateral_moraine_Patagonia.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lava: Magma or molten rock that has reached the surface.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.fukubonsai.com/images/Lava_4_exploding.jpg" src="http://www.fukubonsai.com/images/Lava_4_exploding.jpg" /&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Leaching: The removal of elements from a soil by dissolution in water moving downward in the ground.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.rpi.edu/dept/chem-eng/Biotech-Environ/LEACH/leach3.gif" src="http://www.rpi.edu/dept/chem-eng/Biotech-Environ/LEACH/leach3.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;LEVER:&lt;/span&gt;&lt;span style="font-size:130%;"&gt;  is a rigid object that is used with an appropriate fulcrum or pivot point to multiply the mechanical force that can be applied to another object.&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 423px; height: 178px;" alt="http://visual.merriam-webster.com/images/science/physics-mechanics/lever.jpg" src="http://visual.merriam-webster.com/images/science/physics-mechanics/lever.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Limestone: A sedimentary rock composed principally of calcium carbonate (CaCO2), usually as the mineral calcite.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.beg.utexas.edu/mainweb/publications/graphics/limestone400.jpg" src="http://www.beg.utexas.edu/mainweb/publications/graphics/limestone400.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lineation: Any linear arrangement of features found in a rock.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.geol.ucsb.edu/faculty/hacker/geo102C/lectures/MariposaSl.jpg" src="http://www.geol.ucsb.edu/faculty/hacker/geo102C/lectures/MariposaSl.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Liquid:&lt;/b&gt;A fluid (such as water) that has no independent shape but has a definite volume and does not expand indefinitely and that is slightly compressible.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 327px; height: 228px;" alt="http://www.andaluciaimagen.com/Liquido_13422.jpg" src="http://www.andaluciaimagen.com/Liquido_13422.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lithification: The processes that convert a sediment into a sedimentary rock.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 497px; height: 398px;" alt="http://www.indiana.edu/%7Eg103/G103/wk4/sedproc%20copy.jpg" src="http://www.indiana.edu/%7Eg103/G103/wk4/sedproc%20copy.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lithology: The systematic description of rocks, in terms of mineral composition and texture.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 522px; height: 460px;" alt="http://www.taganov.com/lithology/images/riggins_lithology_high.jpg" src="http://www.taganov.com/lithology/images/riggins_lithology_high.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lithosphere: The outer, rigid shell of the Earth, situated above the asthenosphere and containing the crust, continents, and plates.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.ngdir.ir/sitelinks/kids/Image/erathquake%20-en/glossary/image015-mm.jpg" src="http://www.ngdir.ir/sitelinks/kids/Image/erathquake%20-en/glossary/image015-mm.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lopolith: A large laccolith that is bowl-shaped and depressed in the center, possibly by subsidence of an emptied magma chamber beneath the intrusion.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://images.suite101.com/80253_lopolith.png" src="http://images.suite101.com/80253_lopolith.png" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Lowland: Land of general low relief at the lower levels of regional elevation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 611px; height: 367px;" alt="http://www.lancashire.gov.uk/environment/photographs/landscapes/Gallery1/images/lowland_JPG_jpg_jpg.jpg" src="http://www.lancashire.gov.uk/environment/photographs/landscapes/Gallery1/images/lowland_JPG_jpg_jpg.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Low-velocity zone: A region in the Earth, especially a planar layer that has lower seismic-wave velocities than the region immediately above it.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.geologyrocks.co.uk/system/files/u2/earthstruc.gif" src="http://www.geologyrocks.co.uk/system/files/u2/earthstruc.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Luster: The general textural impression of a mineral surface, given by the light reflected from it. Terms such as metallic, submetallic are standardized but subjective.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 366px; height: 391px;" alt="http://mocoloco.com/upload/2008/02/luster/ridgely_luster_light.jpg" src="http://mocoloco.com/upload/2008/02/luster/ridgely_luster_light.jpg" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-1249634981685689298?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/1249634981685689298/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_5324.html#comment-form' title='1 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1249634981685689298'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1249634981685689298'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_5324.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-735422183657185214</id><published>2009-03-05T15:43:00.001-08:00</published><updated>2009-04-04T10:07:28.634-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img style="width: 74px; height: 74px;" src="http://www.castelldeferro.info/gif/mariposas1/4.gif" border="0" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 83px; height: 83px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/M_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img style="width: 80px; height: 80px;" src="http://www.castelldeferro.info/gif/mariposas1/4.gif" border="0" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Maar volcano: A volcanic crater without a cone, believed to have been formed by an explosive eruption of trapped gases.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://abob.libs.uga.edu/bobk/cerrocol.JPG" src="http://abob.libs.uga.edu/bobk/cerrocol.JPG" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mafic mineral: A dark-colored mineral rich in iron and magnesium, especially a pyroxene, amphibole, or olivine.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://csmres.jmu.edu/geollab/fichter/RockMin/Pyrox-70.JPG" src="http://csmres.jmu.edu/geollab/fichter/RockMin/Pyrox-70.JPG" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Magma: Molten rock material that forms igneous rocks upon cooling. Magma that reaches the surface is referred to as lava.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 582px; height: 389px;" alt="http://fuentesdeciencia.files.wordpress.com/2008/12/magma.jpg" src="http://fuentesdeciencia.files.wordpress.com/2008/12/magma.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Magmatic water: Water that is dissolved in a magma or that is derived from such water.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://oceanexplorer.noaa.gov/explorations/06fire/background/chemistry/media/arcvolcano_600.jpg" src="http://oceanexplorer.noaa.gov/explorations/06fire/background/chemistry/media/arcvolcano_600.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Magnetic stratigraphy: The study and correlation of polarity epochs and events in the history of the Earth's magnetic field as contained in magnetic rocks.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www-odp.tamu.edu/publications/185_SR/synth/images/14_f03.gif" src="http://www-odp.tamu.edu/publications/185_SR/synth/images/14_f03.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Magnetometer: An instrument for measuring either one orthogonal component or the entire intensity of the Earth's magnetic field at various points.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 288px; height: 366px;" alt="http://www.trifieldmeter.com/EarthMagnetometer.jpg" src="http://www.trifieldmeter.com/EarthMagnetometer.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Magnitude: A measure of earthquake size, determined by taking the common logarithm base 10) of the largest ground motion observed during the arrival of a P-wave or seismic surface wave and applying a standard correction for distance to the epicenter.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://sci.esa.int/science-e-media/img/20/apparent-magnitude.jpg" src="http://sci.esa.int/science-e-media/img/20/apparent-magnitude.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mantle: The main bulk of the Earth, between the crust and core, ranging from depths of about 40 to 3480 kilometers. It is composed of dense mafic silicates and divided into concentric layers by phase changes that are caused by the increase in pressure with depth.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/3xLiOFjemWQ&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/3xLiOFjemWQ&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Massive rock: A rock that is little or not at all broken by joints, cracks, foliation, or bedding, tending to present a homogeneous appearance.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span class="outline"&gt;&lt;img class="media" id="fullSizedImage" src="http://i65.photobucket.com/albums/h219/rubbermeatheadman/massive-rock-in-huge-dump-truck.jpg" alt="massive-rock-in-huge-dump-truck.jpg image by rubbermeatheadman" galleryimg="no" style="width: 600px; height: 450px;" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mass movement: A downhill movement of soil or fractured rock under the force of gravity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://earthsci.org/processes/geopro/massmov/creep2.jpg" src="http://earthsci.org/processes/geopro/massmov/creep2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mass spectrometer: An instrument for separating ions of different mass but equal charge (mainly isotopes in geology) and measuring their relative quantities.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://upload.wikimedia.org/wikipedia/commons/thumb/b/b8/Mass_spectrometer_schematics.png/300px-Mass_spectrometer_schematics.png" src="http://upload.wikimedia.org/wikipedia/commons/thumb/b/b8/Mass_spectrometer_schematics.png/300px-Mass_spectrometer_schematics.png" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Maturity&lt;/span&gt;: A stage in the geomorphic cycle in which maximum relief and well-developed drainage are both present.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Meander: Broad, semicircular curves in a stream that develop as the stream erodes the outer bank of a curve and deposits sediment against the inner bank.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.uwsp.edu/gEo/faculty/ritter/images/lithosphere/fluvial/meander_GSC_large.jpg" src="http://www.uwsp.edu/gEo/faculty/ritter/images/lithosphere/fluvial/meander_GSC_large.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mechanical weathering: The set of all physical processes by which an outcrop is broken up into small particles.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 619px; height: 405px;" alt="http://www.geology.wisc.edu/%7Eqlab/sipfolder/o16-1.jpg" src="http://www.geology.wisc.edu/%7Eqlab/sipfolder/o16-1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Medical geology: The application of geologic science to problems of health, especially those relating to mineral sources of toxic or nutritious elements and natural dispersal of toxic pollutants.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.medicalgeology.org/images/BOOKcover.jpg" src="http://www.medicalgeology.org/images/BOOKcover.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mesosphere: The lower mantle.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.chem.leeds.ac.uk/JMCP/images/mesosphere.jpg" src="http://www.chem.leeds.ac.uk/JMCP/images/mesosphere.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Metamorphism: The changes of mineralogy and texture imposed on a rock by pressure and temperature in the Earth's interior. Meteoric water: Rainwater, snow, hail, and sleet.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.tulane.edu/%7Esanelson/images/lowgradeassembl.gif" src="http://www.tulane.edu/%7Esanelson/images/lowgradeassembl.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Meteorite: A stony or metallic object from inter-planetary space that penetrates the atmosphere to impact on the surface.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.cherrycoloured.com/wordpress/wp-content/uploads/2006/06/meteorite.jpg" src="http://www.cherrycoloured.com/wordpress/wp-content/uploads/2006/06/meteorite.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Micrometeorite: A meteorite less than 1 millimeter in diameter.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://astro.wsu.edu/worthey/astro/html/im-meteor/micrometeorite.jpg" src="http://astro.wsu.edu/worthey/astro/html/im-meteor/micrometeorite.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Microseism: A weak vibration of the ground that can be detected by seismographs and which is caused by waves, wind, or human activity, but not by an earthquake.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://img.tfd.com/wn/6C/6673E-microseism.jpg" src="http://img.tfd.com/wn/6C/6673E-microseism.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Migmatite: A rock with both igneous and metamorphic characteristics that shows large crystals and laminar flow structures. Probably formed metamorphically in the presence of water and without melting.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 367px; height: 226px;" alt="http://www.stubotics.com/rocks/bpo1.jpg" src="http://www.stubotics.com/rocks/bpo1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mineral: A naturally occurring element or compound with a precise chemical formula and a regular internal lattice structure. Organic products are usually not included.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://geology.com/articles/tucson/mineral.jpg" src="http://geology.com/articles/tucson/mineral.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mineralogy: The study of mineral composition, structure, appearance, stability, occurrence, and associations.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in;" alt="http://upload.wikimedia.org/wikipedia/commons/e/e4/Mineral_illustration_-_James_Sowerby_-_in_Familiar_Lessons_on_Mineralogy_and_Geology.jpg" src="http://upload.wikimedia.org/wikipedia/commons/e/e4/Mineral_illustration_-_James_Sowerby_-_in_Familiar_Lessons_on_Mineralogy_and_Geology.jpg" width="449" height="845" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Miogeosyncline: A Geosyncline that is situated near a craton and receives chemical and well-sorted elastic sediments from the continent.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.uwsp.edu/geo/projects/geoweb/participants/dutch/graphic0/platetec/geosyn0.gif" src="http://www.uwsp.edu/geo/projects/geoweb/participants/dutch/graphic0/platetec/geosyn0.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mohorovic discontinuity: The boundary between crust and mantle, marked by a rapid increase in seismic wave velocity to more than 8 kilometers per second. Depth: 5 to 45 kilometers. Abbreviated "Moho" or "M-discontinuity."&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://geology.com/articles/images/moho-mohorovicic.gif" src="http://geology.com/articles/images/moho-mohorovicic.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Monocline: The S-shaped fold connecting two horizontal parts of the same stratum at different elevations. Its central limb is usually not overturned.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/study/Images/Monocline.gif" src="http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/study/Images/Monocline.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Moraine: A glacial deposit of till left at the margin of an ice sheet. See specifically by name, ground moraine, longitudinal moraine, medial moraine, and terminal moraine.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.outreach.canterbury.ac.nz/resources/geology/glossary/moraine.jpg" src="http://www.outreach.canterbury.ac.nz/resources/geology/glossary/moraine.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mountain: A steep-sided topographic elevation larger than a hill; also a single prominence forming part of a ridge or mountain range.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.3d-screensaver-jam.com/images/free/freemountain/big2.jpg" src="http://www.3d-screensaver-jam.com/images/free/freemountain/big2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mudflow: A mass movement of material finer than sand, lubricated with large amounts of water. Mudstone: The citified equivalent of mud, a fine grained sedimentary rock similar to shale but more massive. &lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 470px; height: 308px;" alt="http://www.nsf.gov/news/mmg/media/images/mudflow1_h.jpg" src="http://www.nsf.gov/news/mmg/media/images/mudflow1_h.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Mylonite: A very fine lithified fault breccia commonly found in major thrust faults and produced by shearing and rolling during fault movement.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 431px; height: 281px;" alt="http://maps.unomaha.edu/Maher/GEOL3300/week6/NGS_myloniteUSGS.jpg" src="http://maps.unomaha.edu/Maher/GEOL3300/week6/NGS_myloniteUSGS.jpg" /&gt;&lt;/p&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;MACHINE&lt;/span&gt;&lt;span style="font-size:130%;"&gt;: is any device that uses energy  to perform some activity.A simple machine  is a device that transforms the direction or magnitude of a force without consuming any energy&lt;/span&gt;&lt;/p&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.sindominio.net/singuerra/petroleo2.jpeg" src="http://www.sindominio.net/singuerra/petroleo2.jpeg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;MAGNITUDE&lt;/span&gt;&lt;span style="font-size:130%;"&gt;: a number characteristic of a quantity and forming a basis for comparison with similar quantities, as length.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 461px; height: 463px;" alt="http://www.holoborodko.com/pavel/wp-content/uploads/second_order_snrd_n4_magnitude_response_1.gif" src="http://www.holoborodko.com/pavel/wp-content/uploads/second_order_snrd_n4_magnitude_response_1.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Materials&lt;/b&gt; &lt;/span&gt;&lt;span style="font-style: italic; color: rgb(0, 0, 0);font-size:130%;" &gt;are substance or components  &lt;/span&gt;&lt;span style="font-style: italic; color: rgb(0, 0, 0);font-size:130%;" &gt;with certain physical properties which are used as inputs to production or manufacturing&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-style: italic; color: rgb(0, 0, 0);font-size:130%;" &gt; &lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.bancoimagenes.com/cd642/cd642f3_a.jpg" src="http://www.bancoimagenes.com/cd642/cd642f3_a.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Mechanical Engineering&lt;/b&gt;: is an engineering  discipline that involves the application of principes of physics  for analysis,design, manufacturing , and maintenance of mechanical systems . Mechanical engineering is one of the oldest and broadest engineering disciplines.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 336px; height: 180px;" alt="http://www.itcm.edu.mx/itcm06/html/licenciaturas/imag/mecanica.jpg" src="http://www.itcm.edu.mx/itcm06/html/licenciaturas/imag/mecanica.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;dl style="text-align: center;"&gt;&lt;dt&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Mineral&lt;/b&gt;: is A solid homogeneous crystalline chemical element or compound that results from the inorganic processes of nature.&lt;br /&gt;&lt;/span&gt;&lt;/dt&gt;&lt;dt&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 362px; height: 271px;" alt="http://depthome.brooklyn.cuny.edu/geology/core332/images/mineral.jpg" src="http://depthome.brooklyn.cuny.edu/geology/core332/images/mineral.jpg" /&gt;&lt;/span&gt;&lt;/dt&gt;&lt;/dl&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Mining and geological engineers, including mining safety engineers&lt;/b&gt; find, extract, and prepare coal, metals, and minerals for use by manufacturing industries and utilities. They design open-pit and underground mines, supervise the construction of mine shafts and tunnels in underground operations, and devise methods for transporting minerals to processing plants.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt; &lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;a href="http://images.google.co.ve/imgres?imgurl=http://media.epi.es/www.lne.es/media/fotos/noticias/318x200/2008-12-10_IMG_2008-12-03_01.51.05__1111647.jpg&amp;amp;imgrefurl=http://www.lne.es/secciones/noticia.jsp%3FpRef%3D2008120300_38_702924__Cuencas-estudiante-hibrido-Mieres&amp;amp;usg=__X6y3ukd_3Q1gv6rql8jshNhZZhc=&amp;amp;h=759&amp;amp;w=318&amp;amp;sz=47&amp;amp;hl=es&amp;amp;start=53&amp;amp;sig2=KMj6X6J1M6rFxLh6UvkAyQ&amp;amp;um=1&amp;amp;tbnid=Q89KzWSDMcpdSM:&amp;amp;tbnh=142&amp;amp;tbnw=59&amp;amp;prev=/images%3Fq%3Dingeniero%2Bgeologo%26ndsp%3D18%26hl%3Des%26client%3Dfirefox-a%26channel%3Ds%26rls%3Dorg.mozilla:es-ES:official%26sa%3DN%26start%3D36%26um%3D1&amp;amp;ei=2AbFScOFFoWGtgfdscjNCg"&gt;&lt;img style="border: 1px solid ; width: 68px; height: 155px;" src="http://tbn2.google.com/images?q=tbn:Q89KzWSDMcpdSM:http://media.epi.es/www.lne.es/media/fotos/noticias/318x200/2008-12-10_IMG_2008-12-03_01.51.05__1111647.jpg" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://www.castelldeferro.info/gif/mariposas1/30.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 73px; height: 73px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/N_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://www.castelldeferro.info/gif/mariposas1/30.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Native metal: A natural deposit of a metallic element in pure metallic form, neither oxidized nor combined with sulfur or other elements.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://z.about.com/d/geology/1/0/L/B/gold.jpg" src="http://z.about.com/d/geology/1/0/L/B/gold.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Neap tide: A tide cycle of unusually small amplitude, which occurs twice monthly when the lunar and solar tides are opposed-that is, when the gravitational pull of the Sun is at right angles to that of the Moon.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://users.manchester.edu/facstaff/gwclark/NASC103/tfigure_1.jpg" src="http://users.manchester.edu/facstaff/gwclark/NASC103/tfigure_1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Nebula: An immense, diffuse body of interstellar gas and dust that has not condensed into a star.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://asymptotia.com/wp-images/2007/02/Helix_Nebula.jpg" src="http://asymptotia.com/wp-images/2007/02/Helix_Nebula.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Nebular hypothesis: A theory of the formation of the planets that states that a rotating nebula contracted and was then torn into fragments by centrifugal forces, with planets condensing from the fragments.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/jhYEQgLW5NM&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/jhYEQgLW5NM&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Neutron: An electrically neutral elementary particle in the atomic nucleus having the mass of one proton.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;img alt="http://lc.brooklyn.cuny.edu/smarttutor/core3_22/images/Atom_structure_neutron2.gif" src="http://lc.brooklyn.cuny.edu/smarttutor/core3_22/images/Atom_structure_neutron2.gif" /&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;strong&gt;NOUN&lt;/strong&gt;:&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;The part of speech that is used to name a person, place, thing, quality, or action and can function as the subject or object of a verb, the object of a preposition, or an appositive&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span class="Estilo8"  style="font-size:130%;"&gt;&lt;span class="Estilo7"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img src="http://myword.info/images/proper_noun_1aa.gif" width="155" height="122" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt; &lt;span style="font-weight: bold;font-size:130%;" &gt;NUMBER&lt;/span&gt;&lt;span style="font-size:130%;"&gt;:a word or symbol, or a combination of words or symbols, used in counting or in noting a total.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 219px; height: 219px;" alt="http://x.couver.us/images/wristband/numbered_black_sweatband_number11_orange.jpg" src="http://x.couver.us/images/wristband/numbered_black_sweatband_number11_orange.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-735422183657185214?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/735422183657185214/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_5866.html#comment-form' title='1 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/735422183657185214'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/735422183657185214'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_5866.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5163382431473204195</id><published>2009-03-05T15:42:00.005-08:00</published><updated>2009-04-03T17:36:07.347-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/O_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Obsidian: Dark volcanic glass of felsic composition.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.es.ucl.ac.uk/schools/Glossary/obsidian.jpg" src="http://www.es.ucl.ac.uk/schools/Glossary/obsidian.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Octahedral coordination: The packing of six ions around an ion of opposite charge to form an octahedron.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://folk.ntnu.no/krill/mineralogee/11-filer/naclstruct.gif" src="http://folk.ntnu.no/krill/mineralogee/11-filer/naclstruct.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Oil field: An underground accumulation of oil and gas concentrated beneath an impermeable trap, preventing its escape upward.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.theflyinggoose.com/blog1/wp-content/uploads/2008/11/oil-field-tmr.jpg" src="http://www.theflyinggoose.com/blog1/wp-content/uploads/2008/11/oil-field-tmr.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Oil shale: A dark-colored shale containing organic material that can be crushed and heated to liberate gaseous hydrocarbons.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 371px; height: 261px;" alt="http://geology.fullerton.edu/whenderson/F2007201/greenriver/images/geooil.jpg" src="http://geology.fullerton.edu/whenderson/F2007201/greenriver/images/geooil.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Oolite: A sedimentary carbonate particle composed of spherical grains precipitated from warm ocean water on carbonate platforms. Also a rock composed of such particles.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 336px; height: 201px;" alt="http://www.beachfamily.net/Martin/oolite.jpg" src="http://www.beachfamily.net/Martin/oolite.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Opaque mineral: A mineral which transmits no light through a thin section under a microscope. Usually a native metal, sulfide, or metallic oxide mineral.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 383px; height: 423px;" alt="http://z.about.com/d/chemistry/1/0/R/c/turquoise.jpg" src="http://z.about.com/d/chemistry/1/0/R/c/turquoise.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Ophiolite suite: An assemblage of mafic and ultra-mafic igneous rocks with deep-sea sediments supposedly associated with divergence zones and the sea-floor environment.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 415px; height: 318px;" alt="http://upload.wikimedia.org/wikipedia/commons/6/6a/Ophiolite_suite_scheme.jpg" src="http://upload.wikimedia.org/wikipedia/commons/6/6a/Ophiolite_suite_scheme.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Orbit: The elliptical or hyperbolic path traced by a planet or meteorite or satellite in the presence of a more massive body.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 492px; height: 255px;" alt="http://www.astro.uni.wroc.pl/vt-2004/mt-2003/mt-mercury-orbit.jpg" src="http://www.astro.uni.wroc.pl/vt-2004/mt-2003/mt-mercury-orbit.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;st1:state&gt;&lt;st1:place&gt;Ore&lt;/st1:place&gt;&lt;/st1:state&gt;: A natural deposit in which a valuable metallic element occurs in high enough concentration to make mining economically feasible.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;st1:state&gt;&lt;st1:place&gt;Ore&lt;/st1:place&gt;&lt;/st1:state&gt; mineral: The mineral of an ore that contains the useful element.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.seshat.ch/home/ore.JPG" src="http://www.seshat.ch/home/ore.JPG" /&gt;&lt;/p&gt; &lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Orogenic belt: A linear region, often a former geo-syncline, that has been subjected to folding, and other deformation in a mountain-building episode.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.uwsp.edu/geo/projects/geoweb/participants/Dutch/graphic0/platetec/strzone.gif" src="http://www.uwsp.edu/geo/projects/geoweb/participants/Dutch/graphic0/platetec/strzone.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Orogeny: The tectonic process in which large areas are folded, thrust-faulted, metamorphosed, and subjected to plutonism. The cycle ends with uplift and the formation of mountains.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 239px; height: 479px;" alt="http://www.nvcc.edu/home/cbentley/shenandoah/app_orogeny.jpg" src="http://www.nvcc.edu/home/cbentley/shenandoah/app_orogeny.jpg" /&gt;&lt;span style="font-size:130%;"&gt;.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Outgassing: The release of juvenile gases to the atmosphere and oceans by volcanism.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt; &lt;/span&gt;&lt;img style="width: 500px; height: 380px;" alt="http://www.drbateman.net/gcse2003/gcsesums/chemsums/earth/VolcanoOutgassing.jpg" src="http://www.drbateman.net/gcse2003/gcsesums/chemsums/earth/VolcanoOutgassing.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Outwash: A glaciofluvial sediment that is deposited by meltwater streams emanating from a glacier. Overturned fold: A fold in which a limb has tilted past vertical so that the older strata are uppermost. Oxbow lake: A long, broad, crescent-shaped lake formed when a stream abandons a meander and takes a new course.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;a href="http://www.uwsp.edu/geO/faculty/ritter/images/lithosphere/glacial/outwash_plain_DDS21_Cooper_river_region_Alaska.jpg"&gt;&lt;img src="http://www.uwsp.edu/geO/faculty/ritter/images/lithosphere/glacial/outwash_plain_DDS21_Cooper_river_region_Alaska_small.jpg" alt="outwash plain" width="296" border="0" height="225" /&gt;&lt;/a&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Oxidation: A chemical reaction in which electrons are lost from an atom and its charge becomes more positive.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 428px; height: 321px;" alt="http://members.chello.nl/r.kuijt/images/en_oxidation_reduction.jpg" src="http://members.chello.nl/r.kuijt/images/en_oxidation_reduction.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Oxidized element: An element occurring in the more positively charged of two common ionic forms.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.globalchange.umich.edu/gctext/Inquiries/Inquiries_by_Unit/Unit_10_files/image013.gif" src="http://www.globalchange.umich.edu/gctext/Inquiries/Inquiries_by_Unit/Unit_10_files/image013.gif" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5163382431473204195?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5163382431473204195/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_4443.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5163382431473204195'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5163382431473204195'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_4443.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-9163025621514922705</id><published>2009-03-05T15:42:00.003-08:00</published><updated>2009-04-04T10:28:21.938-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img src="http://www.castelldeferro.info/gif/flores2/cfl140.gif" width="99" border="0" height="125" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 82px; height: 82px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/P_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img src="http://www.castelldeferro.info/gif/flores2/cfl140.gif" width="99" border="0" height="125" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pahoehoe: A basaltic lava flow with a glassy, smooth, and undulating, or ropy, surface.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://library.thinkquest.org/J001393/volcanoes/images/pahoehoe.jpg" src="http://library.thinkquest.org/J001393/volcanoes/images/pahoehoe.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Paleoclimate: The average state or typical conditions of climate during some past geologic period.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 594px; height: 297px;" alt="http://www.johnstonsarchive.net/spaceart/earthicemap.jpg" src="http://www.johnstonsarchive.net/spaceart/earthicemap.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Paleomagnetism: The science of the reconstruction of the Earth's ancient magnetic field and the positions of the continents from the evidence of remnant magnetization in ancient rocks.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://stloe.most.go.th/volcano/lo401/images/Eng/4_2.jpg" src="http://stloe.most.go.th/volcano/lo401/images/Eng/4_2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Paleontology: The science of fossils, of ancient life-forms, and their evolution.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.paleoportal.org/kiosk/sample_site/images/nautilus_home.jpg" src="http://www.paleoportal.org/kiosk/sample_site/images/nautilus_home.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Paleowind: A prevailing wind direction in an area, inferred from dune structure or the distribution of volcanic ash for one particular time in geologic history.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.aapg.org/explorer/2008/11nov/conjugate1.jpg" src="http://www.aapg.org/explorer/2008/11nov/conjugate1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pangaea: According to some theories, a great proto-continent from which all present continents have broken off by the mechanism of sea-floor spreading and continental drift..&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 380px; height: 430px;" alt="http://bprc.osu.edu/education/rr/plate_tectonics/pangea_diagram.jpg" src="http://bprc.osu.edu/education/rr/plate_tectonics/pangea_diagram.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Panthalassa: A hypothetical primeval ocean covering two-thirds of the world except for the continent of Pangaea.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 421px; height: 392px;" alt="http://www.estrellamountain.edu/faculty/farabee/biobk/aPerm.jpg" src="http://www.estrellamountain.edu/faculty/farabee/biobk/aPerm.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Peat: A marsh or swamp deposit of water-soaked plant remains containing more than 50 percent carbon.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.wsgs.uwyo.edu/coalweb/images/peat4.jpg" src="http://www.wsgs.uwyo.edu/coalweb/images/peat4.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pedalfer: A common soil type in humid regions, characterized by an abundance of iron oxides and clay minerals deposited in the B-horizon by leaching.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.gly.fsu.edu/%7Esalters/GLY1000/10Weathering_Erosion/Slide32.jpg" src="http://www.gly.fsu.edu/%7Esalters/GLY1000/10Weathering_Erosion/Slide32.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pediment: A planar, sloping rock surface forming a ramp up to the front of a mountain range in an arid region. It may be covered locally by thin alluvium.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.geocities.com/scott_cotter/pediment1.jpg" src="http://www.geocities.com/scott_cotter/pediment1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pedocal: A common soil type of arid regions, characterized by accumulation of calcium carbonat&lt;/span&gt;&lt;span style="font-size:130%;"&gt;e in the A-horizon.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 387px; height: 605px;" alt="http://hays.outcrop.org/images/weathering/press4e/figure-07-16-5.jpg" src="http://hays.outcrop.org/images/weathering/press4e/figure-07-16-5.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pegmatite: An igneous rock with extremely large grains, more than a centimeter in diameter. It may be of any composition but most frequently is granitic.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;&lt;img style="width: 497px; height: 463px;" alt="http://www.gc.maricopa.edu/earthsci/imagearchive/PEGMATITE_big.jpg" src="http://www.gc.maricopa.edu/earthsci/imagearchive/PEGMATITE_big.jpg" /&gt;&lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Perched groundwater&lt;/span&gt;: An isolated body of ground-water that is perched above and separated from the main water table by an aquiclude.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.co.portage.wi.us/Groundwater/undrstnd/Images/perch2.jpg" src="http://www.co.portage.wi.us/Groundwater/undrstnd/Images/perch2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Peridotite: A coarse-grained mafic igneous rock composed of olivine with accessory amounts of pyroxene and amphibole but little or no feldspar.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 343px; height: 257px;" alt="http://geology.com/rocks/pictures/peridotite.jpg" src="http://geology.com/rocks/pictures/peridotite.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Potable water: Water that is agreeable to the taste and not dangerous to the health.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.akvadon.ru/images/PicDrink.jpg" src="http://www.akvadon.ru/images/PicDrink.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pothole: A semispherical hole in the bedrock of a stream bed, formed by abrasion of small pebbles and cobbles in a strong current.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 326px; height: 215px;" alt="http://media.torontolife.com/dynimages/pothole.jpg" src="http://media.torontolife.com/dynimages/pothole.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pratt isostatic compensation: The mechanism in which variations in crustal density act to counterbalance the varying weight of topographic features. The crust is here assumed to be of approximately uniform thickness, thus a mountain range would be underlain by li&lt;/span&gt;&lt;img alt="http://content.answers.com/main/content/img/McGrawHill/Encyclopedia/images/CE356500FG0010.gif" src="http://content.answers.com/main/content/img/McGrawHill/Encyclopedia/images/CE356500FG0010.gif" /&gt;&lt;span style="font-size:130%;"&gt;ghter rocks.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;strong&gt;PREPOSITION:&lt;/strong&gt;it es a word used before nouns, pronouns, or other substantives to form phrases functioning as modifiers of verbs, nouns, or adjectives, and that typically express a spatial, temporal, or other relationship, as in, on, by, to, since.&lt;/span&gt;&lt;/p&gt;&lt;p style="font-style: italic; text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://www.enchantedlearning.com/bgifs/behind.GIF" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-style: italic; font-weight: bold;font-size:130%;" &gt;PROCESS&lt;/span&gt;&lt;span style="font-weight: bold; font-style: italic;font-size:130%;" &gt; (&lt;/span&gt;&lt;span style="font-size:130%;"&gt;&lt;b style="font-style: italic;"&gt;engineering&lt;/b&gt;): refers to engineering which is collaborative and concerned with completing a project as a whole.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;strong&gt;PRONOUN:&lt;/strong&gt;The part of speech that substitutes for nouns or noun phrases and designates persons or things asked for, previously specified, or understood from the context. &lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://myword.info/images/pronoun_1ac.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Proto-sun: A large cloud of dust and gas gradually coalescing into a star under the force of gravity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://physicalsciences.ucsd.edu/news/releases/2005/SolarNebula_lg.jpg" src="http://physicalsciences.ucsd.edu/news/releases/2005/SolarNebula_lg.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Proven reserves&lt;/span&gt;: Deposits of fossil fuels whose location and extent are known, as opposed to potential but unproved ('*discovered") deposits.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;pulley&lt;/b&gt; is a mechanism composed of a wheel  with a groove  &lt;/span&gt;&lt;span style="font-size:130%;"&gt;between two flanges  around the wheel's circumference. A rope cable or belt  usually runs inside the groove. Pulleys are used to change the direction of an applied force, transmit rotational motion, or realize a mechanical advantage in either a linear or rotational system of motion.&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 176px; height: 308px;" alt="http://etc.usf.edu/clipart/25700/25757/fixed_pulley_25757_lg.gif" src="http://etc.usf.edu/clipart/25700/25757/fixed_pulley_25757_lg.gif" /&gt;&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pumice: A form of volcanic glass, usually of silicic composition, so filled with vesicles that it resembles a sponge and is very light.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 403px; height: 295px;" alt="http://www.swisseduc.ch/stromboli/glossary/icons/pumice_2.jpg" src="http://www.swisseduc.ch/stromboli/glossary/icons/pumice_2.jpg" /&gt;&lt;/p&gt;&lt;br /&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pyroclastic rock: A rock formed by the accumulation of fragments of volcanic rock scattered by volcanic explosions.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.es.ucl.ac.uk/schools/Glossary/tuff.jpg" src="http://www.es.ucl.ac.uk/schools/Glossary/tuff.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Pyroxene granulite: A coarse-grained contact metamorphic rock containing pyroxene, formed at high temperatures and low pressures.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.nhm.ac.uk/resources-rx/images/beacon-sandstone-with-sun-cracks-20321-1.jpg" src="http://www.nhm.ac.uk/resources-rx/images/beacon-sandstone-with-sun-cracks-20321-1.jpg" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-9163025621514922705?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/9163025621514922705/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9340.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/9163025621514922705'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/9163025621514922705'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9340.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5036483065216520558</id><published>2009-03-05T15:42:00.001-08:00</published><updated>2009-04-05T09:06:43.204-07:00</updated><title type='text'></title><content type='html'>&lt;p style="text-align: center;"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/R_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Ray: A linear landform of the lunar surface emanating from a large crater and extending as much as 100 kilometers outward, probably consisting of fine ejecta thrown out by the impact of a meteorite.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.sciencebits.com/files/pictures/climate/crcFig4.jpg" src="http://www.sciencebits.com/files/pictures/climate/crcFig4.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Reaction series: A series of chemical reactions occurring in a cooling magma by which a mineral formed at high temperature becomes unstable in the melt and reacts to form another mineral (see also Discontinuous reaction series).&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.georgiacenter.uga.edu/idl/webid/portfolio/graphics/illustrations/bowdens_reaction.jpg" src="http://www.georgiacenter.uga.edu/idl/webid/portfolio/graphics/illustrations/bowdens_reaction.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Recharge: In hydrology, the replenishment of ground-water by infiltration of meteoric water through the soil.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.state.nj.us/dep/njgs/enviroed/aqfrchrg.gif" src="http://www.state.nj.us/dep/njgs/enviroed/aqfrchrg.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rectangular drainage: A system of streams in which each straight segment of each stream takes one of two characteristic perpendicular directions, with right-angle bends between. The streams are usually following two perpendicular sets of joints.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://rst.gsfc.nasa.gov/Sect17/TrellisDrainage.jpg" src="http://rst.gsfc.nasa.gov/Sect17/TrellisDrainage.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Recumbent fold: An overturned fold with both limbs nearly horizontal.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://dnowlan.ca/VM/science7/planetearth/syasyovt.jpg" src="http://dnowlan.ca/VM/science7/planetearth/syasyovt.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Regional metamorphism: Metamorphism occurring over a wide area and caused by deep burial and high internal temperatures of the Earth.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.indiana.edu/%7Egeol105/images/gaia_chapter_5/regmeta.jpg" src="http://www.indiana.edu/%7Egeol105/images/gaia_chapter_5/regmeta.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Regolith: Any solid material lying on top of bedrock. Includes soil, alluvium, and rock fragments weathered from the bedrock.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://ceng.calpoly.edu/media/uploads/news_releases/070511_regolithRumble_vlg10a_widec.jpg" src="http://ceng.calpoly.edu/media/uploads/news_releases/070511_regolithRumble_vlg10a_widec.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Relief: The maximum regional difference in elevation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 456px; height: 353px;" alt="http://www.mymapman.com/images/ReliefEurope.jpg" src="http://www.mymapman.com/images/ReliefEurope.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Remote sensing: The study of Earth surface conditions and materials from airplanes and satellites by means of photography, spectroscopy, or radar.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 319px; height: 260px;" alt="http://www.etsu.edu/cas/geosciences/pictures/remote_sensing.jpg" src="http://www.etsu.edu/cas/geosciences/pictures/remote_sensing.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Replacement deposit: A deposit of ore minerals by hydrothermal solutions that have first dissolved the original mineral to form a small cavity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 434px; height: 187px;" alt="http://www.magsilver.com/i/photos/CincoMayoHeader.jpg" src="http://www.magsilver.com/i/photos/CincoMayoHeader.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Respiration: The chemical reaction by which carbohydrates are oxidized and by which all animals and plants convert their food into energy. Carbon dioxide is released and oxygen used up.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://bioweb.wku.edu/courses/BIOL115/Wyatt/Metabolism/Respiration.gif" src="http://bioweb.wku.edu/courses/BIOL115/Wyatt/Metabolism/Respiration.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Reversible reaction: A chemical reaction which can proceed in either direction, depending on the concentration of reacting materials.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://image.wetpaint.com/image/1/6SlDaIisv3Is9IWV0y_xwA27045/GW453H149" src="http://image.wetpaint.com/image/1/6SlDaIisv3Is9IWV0y_xwA27045/GW453H149" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rheidity: (1) The ability of a substance to yield to viscous flow under large strains. (2) One thousand times the time required for a substance to stop changing shape when stress is no longer applied.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 290px; height: 135px;" alt="http://www.geotech.org/survey/geotech/geotslum.gif" src="http://www.geotech.org/survey/geotech/geotslum.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rhyolite: The fine-grained volcanic or extrusive equivalent of granite, light brown to gray and compact. Richter magnitude scale: See Magnitude.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 291px; height: 268px;" alt="http://www.mii.org/Minerals/Minpics1/Rhyolite.jpg" src="http://www.mii.org/Minerals/Minpics1/Rhyolite.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rift valley: A fault trough formed in a divergence zone or other area of tension.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.instablogsimages.com/images/2007/07/27/rift-valley-formation-leads-to-earthquakes_5106.jpg" src="http://www.instablogsimages.com/images/2007/07/27/rift-valley-formation-leads-to-earthquakes_5106.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Right-lateral fault: A strike-slip fault on which the displacement of the far block is to the right when viewed from either side.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 336px; height: 224px;" alt="http://pangea.stanford.edu/courses/GP4/lecture_slides/faulttype/FaultTypes-ImageF.00001.jpeg" src="http://pangea.stanford.edu/courses/GP4/lecture_slides/faulttype/FaultTypes-ImageF.00001.jpeg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Ring dike: A dike in the form of a segment of a cone or cylinder, having an arcuare outcrop.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.indiana.edu/%7Egeol105/images/gaia_chapter_5/dike&amp;amp;sill.jpg" src="http://www.indiana.edu/%7Egeol105/images/gaia_chapter_5/dike&amp;amp;sill.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rip current: A current that flows strongly away from the sea shore through gaps in the surf zone at intervals along the shoreline.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.loving-long-island.com/image-files/calm-rip-current.jpg" src="http://www.loving-long-island.com/image-files/calm-rip-current.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Ripple: A very small dune of sand or silt whose long dimension is formed at right angles to the current. River order: See Stream order.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 266px; height: 364px;" alt="http://strongerteams.files.wordpress.com/2007/02/ripple-crop.jpg" src="http://strongerteams.files.wordpress.com/2007/02/ripple-crop.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rock cycle: The geologic cycle, with emphasis on the rocks produced; sedimentary rocks are metamorphosed to metamorphic rocks, or melted to create igneous rocks, and all rocks may be uplifted and eroded to make sediments, which lithify to sedimentary rocks.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.teachnet-lab.org/ps101/bglasgold/rocks/EFCycleP2.gif" src="http://www.teachnet-lab.org/ps101/bglasgold/rocks/EFCycleP2.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rock flour: A glacial sediment of extremely fine (silt-and clay-size) ground rock formed by abrasion of rocks at the base of the glacier.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 287px; height: 431px;" alt="http://www.celestialfireworks.com/tmp/images/PeytoLake-RockFlour.jpg" src="http://www.celestialfireworks.com/tmp/images/PeytoLake-RockFlour.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rock glacier: A glacier-like mass of rock fragments or talus with interstitial ice that moves downhill under the force of gravity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 181px; height: 179px;" alt="http://nsidc.org/glaciers/gallery/thumbnails/rockglacier_tmbA.jpg" src="http://nsidc.org/glaciers/gallery/thumbnails/rockglacier_tmbA.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Rockslide: A landslide involving mainly large blocks of detached bedrock with little or no soil or sand. Rounding: The degree to which the edges and corners of a particle become worn and rounded as a result of abrasion during transportation. Expressed as angular, subrounded, well-rounded, etc.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.ac-nancy-metz.fr/enseign/anglais/Henry/rockslide.gif" src="http://www.ac-nancy-metz.fr/enseign/anglais/Henry/rockslide.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Runoff: The amount of rain water directly leaving an area in surface drainage, as opposed to the amount that seeps out as groundwater.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.animalwaste.okstate.edu/images/Runoff.jpg" src="http://www.animalwaste.okstate.edu/images/Runoff.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Rupture strength:&lt;/span&gt; The greatest stress that a material can sustain without fracturing at one atmosphere pressure.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5036483065216520558?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5036483065216520558/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_4508.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5036483065216520558'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5036483065216520558'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_4508.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-8666099450618988453</id><published>2009-03-05T15:41:00.006-08:00</published><updated>2009-04-04T11:05:44.366-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/S_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Safety engineering&lt;/b&gt; is an applied science strongly related to systems engineering and the subset System Safety Engineering. Safety engineering assures that a life-critical system behaves as needed even when pieces fail.&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 274px; height: 279px;" alt="http://www.gwinto.co.uk/Booklet/Aroon%20Parmar1.jpg" src="http://www.gwinto.co.uk/Booklet/Aroon%20Parmar1.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Saltation: The movement of sand or fine sediment by short jumps above the ground or stream bed under the influence of a current too weak to keep it permanently suspended.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 534px; height: 159px;" alt="http://www.co.mendocino.ca.us/aqmd/images/Saltation.jpg" src="http://www.co.mendocino.ca.us/aqmd/images/Saltation.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Sandblasting: A physical weathering process in which rock is eroded by the impact of sand grains carried by the wind, frequently leading to ventifact formation of pebbles and cobbles.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.truckrefinishers.com.au/images/sandblasting.jpg" src="http://www.truckrefinishers.com.au/images/sandblasting.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Sandstone: A detrital sedimentary rock composed of grains from 1/16 to 2 millimeters in diameter, dominated in most sandstones by quartz, feldspar, and rock fragments, bound together by a cement of silica, carbonate, or other minerals or a matrix of clay minerals.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img src="http://www.beg.utexas.edu/mainweb/publications/graphics/sandstone400.jpg" width="400" border="1" height="300" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;&lt;br /&gt;&lt;/b&gt;&lt;/span&gt;&lt;/p&gt;&lt;br /&gt;&lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;SCALE NODEL&lt;/b&gt;:is a representation or copy of an object that is larger or smaller than the actual size of the object . Very often the scale model is smaller than the original and used as a guide to making the object in full size. Scale models are built or collected for many reasons.Engineers who require scale models to test the likely performance of a particular design at an early stage of development without incurring the full expense of a full-sized prototype.&lt;/span&gt;&lt;br /&gt;&lt;/div&gt; &lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 371px; height: 296px;" src="http://www.howardmodels.com/architectural-models-07/reston/reston1.jpg" alt="Architectural Scale Model, Reston VA Real Estate - Howard Architectural Models " border="0" /&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Schist: A metamorphic rock characterized by strong foliation or schistosity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://csmres.jmu.edu/geollab/Fichter/MetaRx/Rkimage/P0000737.s.jpg" src="http://csmres.jmu.edu/geollab/Fichter/MetaRx/Rkimage/P0000737.s.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Schistosity: The parallel arrangement of shaly or prismatic minerals like micas and amphiboles resulting from nonhydrostatic stress in metamorphism.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.miracosta.cc.ca.us/home/cmetzler/GeolDayTrip/Julian_schist_a.jpg" src="http://www.miracosta.cc.ca.us/home/cmetzler/GeolDayTrip/Julian_schist_a.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;font-size:130%;" &gt;SCIENCE:&lt;/span&gt;&lt;span style="font-size:130%;"&gt;refers to any systematic knowledge or practice . In its more usual restricted sense, science refers to a system of acquiring knowledge based on scientific method , as well as to the organized body of knowledge gained through such research.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 196px; height: 248px;" alt="http://3.bp.blogspot.com/_xJ7R8Znjvis/SbTp1Vsfk-I/AAAAAAAAASM/cIkgPFiNPS4/s400/ciencia.jpg" src="http://3.bp.blogspot.com/_xJ7R8Znjvis/SbTp1Vsfk-I/AAAAAAAAASM/cIkgPFiNPS4/s400/ciencia.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;&lt;br /&gt;&lt;/b&gt;&lt;/span&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Scoria: Congealed lava, usually of mafic composition, with a large number of vesicles formed by gases coming out of solution.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;a href="http://www.ux1.eiu.edu/%7Ecfjps/1300/scoria.jpg"&gt;&lt;img src="http://www.ux1.eiu.edu/%7Ecfjps/1300/scoria.jpg" width="300" border="1" height="196" /&gt;&lt;/a&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Seamount: An isolated tall mountain on the sea floor that may extend more than 1 kilometer from base to peak (see also Guyot).&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.mar-eco.no/__data/page/54/seamount_big.jpg" src="http://www.mar-eco.no/__data/page/54/seamount_big.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;br /&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Sedimentary rock: A rock formed by the accumulation and cementation of mineral grains transported by wind, water, or ice to the site of deposition or chemically precipitated at the depositional site.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 543px; height: 407px;" alt="http://www.wellcollc.com/images/glossary/sedimentary%20rocks.jpg" src="http://www.wellcollc.com/images/glossary/sedimentary%20rocks.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Sedimentation: The process of deposition of mineral grains or precipitates in beds or other accumulations. Seif dune: A longitudinal dune that shows the sculpturing effect of cross-winds not parallel to its axis.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;img style="width: 531px; height: 347px;" alt="http://www.pacificislandtravel.com/nature_gallery/geomorpohology3.gif" src="http://www.pacificislandtravel.com/nature_gallery/geomorpohology3.gif" /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Seismicity: The world-wide or local distribution of earthquakes in space and time; a general term for the number of earthquakes in a unit of time.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://earthquake.usgs.gov/regional/states/alaska/images/seismicity.gif" src="http://earthquake.usgs.gov/regional/states/alaska/images/seismicity.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Stratification: A structure of sedimentary rocks, which have recognizable parallel beds of considerable lateral extent. &lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.fishsniffer.com/guest/images/041103lakezones.gif" src="http://www.fishsniffer.com/guest/images/041103lakezones.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Stratigraphy: The science of the description, correlation, and classification of strata in sedimentary rocks, including the interpretation of the depositional environments of those strata.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://micropress.org/stratigraphy/graphics/vol1.jpg" src="http://micropress.org/stratigraphy/graphics/vol1.jpg" /&gt; &lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Stratovolcano: A volcanic cone consisting of both lava and pyroclastic rocks, often conical.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://explorevolcanoes.com/volcanoimages/stratovolcano%20volcano_hazards%20USGS.gif" src="http://explorevolcanoes.com/volcanoimages/stratovolcano%20volcano_hazards%20USGS.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Streak: The fine deposit of mineral dust left on an abrasive surface when a mineral is scraped across it; especially the characteristic color of the dust.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;img alt="http://geology.csupomona.edu/alert/mineral/streak.jpg" src="http://geology.csupomona.edu/alert/mineral/streak.jpg" /&gt;&lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Stromatolite: A fossil form representing the growth habit of an algal mat: concentric spherules, stacked hemispheres, or flat sheets of calcium carbonate and trapped silt encountered in limestones.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 406px; height: 324px;" alt="http://www.rockhounds.com/grand_hikes/images/phantom_ranch/stromatolite_hakatai4.jpg" src="http://www.rockhounds.com/grand_hikes/images/phantom_ranch/stromatolite_hakatai4.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Subduction zone: A dipping planar zone descending away from a trench and defined by high seismicity, interpreted as the shear zone between a sinking oceanic plate and an overriding plate.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 375px; height: 280px;" alt="http://sio.ucsd.edu/volcano/about/images/recycle.gif" src="http://sio.ucsd.edu/volcano/about/images/recycle.gif" /&gt; &lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Sublimation: A phase change from the solid to the gaseous state, without passing through the liquid state.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 374px; height: 314px;" alt="http://beckerantarctica.crustal.ucsb.edu/images/sublimation_cartoon.gif" src="http://beckerantarctica.crustal.ucsb.edu/images/sublimation_cartoon.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Submarine canyon: An underwater canyon in the continental shelf.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.dkimages.com/discover/previews/851/20117924.JPG" src="http://www.dkimages.com/discover/previews/851/20117924.JPG" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Subsidence: A gentle epeirogenic movement where a broad area of the crust sinks without appreciable deformation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;img alt="http://dnr.state.il.us/mines/lrd/images/subpit.jpg" src="http://dnr.state.il.us/mines/lrd/images/subpit.jpg" /&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Supersaturation: The unstable state of a solution that contains more solute than its solubility allows.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;&lt;img alt="http://www-tc.pbs.org/kcet/wiredscience/assets/story/88.jpg" src="http://www-tc.pbs.org/kcet/wiredscience/assets/story/88.jpg" /&gt;&lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Swash: The landward rush of water from&lt;/span&gt;&lt;span style="font-size:130%;"&gt; a breaking wave up the slope of the beach.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.diam.unige.it/%7Ebrocchin/swash1.gif" src="http://www.diam.unige.it/%7Ebrocchin/swash1.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Swell: An oceanic water wave with a wavelength on the order of 30 meters or more and a height of perhaps 2 meters or less that may travel great distances from its source.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt; &lt;/span&gt;&lt;img style="width: 337px; height: 209px;" alt="http://www.artshole.co.uk/arts/artists/01dec06/tracey%20Betts/Neutral-Swell.jpg" src="http://www.artshole.co.uk/arts/artists/01dec06/tracey%20Betts/Neutral-Swell.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Symbiosis: The interaction of two mutually supporting species that do not compete with or prey upon each other.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 448px; height: 298px;" alt="http://qarrtsiluni.files.wordpress.com/2007/12/asmyth4_dsc_9821-symbiosis.jpg" src="http://qarrtsiluni.files.wordpress.com/2007/12/asmyth4_dsc_9821-symbiosis.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Syncline: A large fold whose limbs are higher than its center; a fold with the youngest strata in the center.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://z.about.com/d/geology/1/0/F/F/syncline.jpg" src="http://z.about.com/d/geology/1/0/F/F/syncline.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-8666099450618988453?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/8666099450618988453/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_3530.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/8666099450618988453'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/8666099450618988453'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_3530.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_xJ7R8Znjvis/SbTp1Vsfk-I/AAAAAAAAASM/cIkgPFiNPS4/s72-c/ciencia.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-8400346580116723694</id><published>2009-03-05T15:41:00.005-08:00</published><updated>2009-04-03T17:21:32.972-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/T_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tableland: A large elevated region with a relatively low relief surface.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 435px; height: 326px;" alt="http://www.100megsfree3.com/wordsmith/backpacking/tableland1700.jpg" src="http://www.100megsfree3.com/wordsmith/backpacking/tableland1700.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tar sand: A sandstone containing the densest asphaltic components of petroleum - the end-product of evaporation of volatile components or of some thickening process.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://climateprogress.org/wp-content/uploads/2007/10/tar_sands.jpg" src="http://climateprogress.org/wp-content/uploads/2007/10/tar_sands.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Talus: A deposit of large angular fragments of physically weathered bedrock, usually at the base of a cliff or steep slope.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;a href="http://3dparks.wr.usgs.gov/landslide/big/3.htm"&gt;&lt;img style="width: 470px; height: 484px;" src="http://3dparks.wr.usgs.gov/landslide/images/arroyo_seco4.jpg" alt="Cliff with talus slope with human for scale" border="0" /&gt;&lt;/a&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;TECHNOLOGY:refer to material objects of use to humanity, such as machines,hardware or utensils but can also encompass broader themes, including systems, methods of organitation and&lt;/span&gt;&lt;span style="text-decoration: underline;font-size:130%;" &gt; techniques&lt;/span&gt;&lt;span style="font-size:130%;"&gt;. The term can either be applied generally or to specific areas&lt;/span&gt;&lt;/p&gt; &lt;div style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 376px; height: 300px;" alt="http://portal.educ.ar/debates/eid/tecnologia/img/Laautoridadmaxima.jpg" src="http://portal.educ.ar/debates/eid/tecnologia/img/Laautoridadmaxima.jpg" /&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tectonics: The study of the movements and deformation of the crust on a large scale, including epeirogeny, metamorphism, folding, faulting, and plate tectonics.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 373px; height: 144px;" alt="http://apollo.lsc.vsc.edu/classes/met130/notes/chapter16/graphics/plate_tectonics.jpg" src="http://apollo.lsc.vsc.edu/classes/met130/notes/chapter16/graphics/plate_tectonics.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Terminal moraine: A sinuous ridge of unsorted glacial till deposited by a glacier at the line of its farthest advance.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 456px; height: 293px;" src="http://www.swisseduc.ch/glaciers/glossary/icons/terminal-moraine.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Terrestrial planet: A planet similar in size and composition to the Earth; especially Mars, Earth, Venus, and Mercury.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/kw_9pdqGiXQ&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/kw_9pdqGiXQ&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Terrestrial sediment: A deposit of sediment that accumulated above sea level in lakes, alluvial fans, floodplains, moraines, etc., regardless of its present elevation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.ozcoasts.org.au/geom_geol/case_studies/images/cs_figure-3.jpg" src="http://www.ozcoasts.org.au/geom_geol/case_studies/images/cs_figure-3.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Texture (rock): The rock characteristics of grain or crystal size, size variability, rounding or angularity, and preferred orientation.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/u6FoUgU_W_o&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/u6FoUgU_W_o&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Thermonuclear reaction: A reaction in which atomic nuclei fuse into new elements with a large release of heat; especially a reaction that is self-sustaining. Occasionally used to include fission reactions as well.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.atomeromu.hu/tortenelem/kepek/napkitor.jpg" src="http://www.atomeromu.hu/tortenelem/kepek/napkitor.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Thrust fault: A dip-slip fault in which the upper block above the fault plane moves up and over the lower block, so that older strata are placed over younger.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 281px; height: 385px;" alt="http://www.dukelabs.com/Abstracts%20and%20Papers/1CManual0209_files/image004.jpg" src="http://www.dukelabs.com/Abstracts%20and%20Papers/1CManual0209_files/image004.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tidal current: A horizontal displacement of ocean water under the gravitational influence of Sun and Moon, causing the water to pile up against the coast at high tide and move outward at low tide.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.racerocks.com/racerock/rrcom/rrjantrip/poolgroup.jpg" src="http://www.racerocks.com/racerock/rrcom/rrjantrip/poolgroup.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tidal flat: A broad, flat region of muddy or sandy sediment, covered and uncovered in each tidal cycle.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 304px; height: 463px;" alt="http://www.heinzle.org/alaska/bears/images/websize/beachfissures.jpg" src="http://www.heinzle.org/alaska/bears/images/websize/beachfissures.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Till: An unconsolidated sediment containing all sizes of fragments from clay to boulders deposited by glacial action, usually unbedded.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://pubs.usgs.gov/of/2004/1216/tz/images/till1.gif" src="http://pubs.usgs.gov/of/2004/1216/tz/images/till1.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Time scale: The division of geologic history into eras, periods, and epochs accomplished through stratigraphy and paleontology.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="cursor: -moz-zoom-in; width: 371px; height: 630px;" alt="http://3dparks.wr.usgs.gov/coloradoplateau/images/timescale.jpg" src="http://3dparks.wr.usgs.gov/coloradoplateau/images/timescale.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Topographic map: See Contour map; also a schematic drawing of prominent landforms indicated by conventionalized symbols, such as hachures or contours.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.compassdude.com/i/topographic-map.jpg" src="http://www.compassdude.com/i/topographic-map.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Topography: The shape of the Earth's surface, above and below sea level; the set of landforms in a region; the distribution of elevations.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.topography-maps.com/front-flip-topography-300.gif" src="http://www.topography-maps.com/front-flip-topography-300.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Transgression: A rise in sea level relative to the land which causes areas to be submerged and marine deposition to begin in that region.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 519px; height: 307px;" alt="http://higheredbcs.wiley.com/legacy/college/levin/0471697435/chap_tut/images/nw0048-nn.jpg" src="http://higheredbcs.wiley.com/legacy/college/levin/0471697435/chap_tut/images/nw0048-nn.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Transition element: Elements of atomic number 21 to 29, 38 to 46, and 71 to 78, whose second outermost electron shell is only partially filled.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 530px; height: 347px;" alt="http://www.elementsdatabase.com/Images/periodic_table1.gif" src="http://www.elementsdatabase.com/Images/periodic_table1.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Transpiration: The removal of water from the ground into plants, ultimately to be evaporated into the atmosphere by them.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 388px; height: 448px;" alt="http://techalive.mtu.edu/meec/module01/images/transpiration.jpg" src="http://techalive.mtu.edu/meec/module01/images/transpiration.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Transverse dune: A dune that has its axis transverse to the prevailing winds or to a current. The upwind or upcurrent side has a gentle slope, and the downwind side lies at the angle of repose.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 472px; height: 239px;" alt="http://www.indiana.edu/%7Eg103/G103/Week8/dunes2.jpg" src="http://www.indiana.edu/%7Eg103/G103/Week8/dunes2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Trap (oil): A sedimentary or tectonic structure that impedes the upward movement of oil and gas and allows it to collect beneath the barrier.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.cartografareilpresente.org/local/cache-vignettes/L348xH249/Various_traps.jpg" src="http://www.cartografareilpresente.org/local/cache-vignettes/L348xH249/Various_traps.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Travertine: A terrestrial deposit of limestone formed in caves and around &lt;st1:city&gt;&lt;st1:place&gt;hot   springs&lt;/st1:place&gt;&lt;/st1:city&gt; where cooling, carbonate-saturated groundwater is exposed to the air.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 357px; height: 262px;" src="http://www.njminerals.org/travertine.jpg" alt="Travertine showing layering" border="0" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Trellis drainage: A system of streams in which tributaries tend to lie in parallel valleys formed in steeply dipping beds in folded belts.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.mhhe.com/earthsci/geology/mcconnell/streams/images/drain_basins.gif" src="http://www.mhhe.com/earthsci/geology/mcconnell/streams/images/drain_basins.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Trench: A long and narrow deep trough in the sea floor; interpreted as marking the line along which a plate bends down into a subduction zone.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://z.about.com/d/goeurope/1/0/e/D/trench_death_2.jpg" src="http://z.about.com/d/goeurope/1/0/e/D/trench_death_2.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Triple junction: A point that is common to three plates and which must also be the meeting place of three boundary features, such as divergence zones, convergence zones, or transform faults.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.aps.org/publications/apsnews/200504/images/fig2_triple_junction_cell.jpg" src="http://www.aps.org/publications/apsnews/200504/images/fig2_triple_junction_cell.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tsunami: A large destructive wave caused by sea-floor movements in an earthquake.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;object width="500" height="405"&gt;&lt;param name="movie" value="http://www.youtube.com/v/eAkijDDS61A&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/eAkijDDS61A&amp;amp;hl=es&amp;amp;fs=1&amp;amp;color1=0x234900&amp;amp;color2=0x4e9e00&amp;amp;border=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="500" height="405"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Tuff: A consolidated rock composed of pyroclastic fragments and fine ash. If particles are melted slightly together from their own heat, it is a "welded tuff."&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://z.about.com/d/geology/1/0/t/W/tuff_grnvly1.jpg" src="http://z.about.com/d/geology/1/0/t/W/tuff_grnvly1.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Turbulent flow: A high-velocity flow in which streamlines are neither parallel nor straight but curled into small tight eddies (compare Laminar flow).&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.healthyhouseinstitute.com/images/Turbulent-Flow-Precipitation-Principle.gif" src="http://www.healthyhouseinstitute.com/images/Turbulent-Flow-Precipitation-Principle.gif" /&gt;&lt;/p&gt;&lt;br /&gt;&lt;p align="center"&gt;&lt;xml&gt;&lt;w:worddocument&gt;&lt;w:punctuationkerning&gt;&lt;w:validateagainstschemas&gt;&lt;w:alwaysshowplaceholdertext&gt;&lt;/w:alwaysshowplaceholdertext&gt;   &lt;w:compatibility&gt;    &lt;w:breakwrappedtables&gt;    &lt;w:snaptogridincell&gt;    &lt;w:wraptextwithpunct&gt;    &lt;w:useasianbreakrules&gt;    &lt;w:dontgrowautofit&gt;   &lt;/w:dontgrowautofit&gt;&lt;/w:useasianbreakrules&gt;&lt;/w:wraptextwithpunct&gt;&lt;/w:snaptogridincell&gt;&lt;/w:breakwrappedtables&gt;&lt;/w:compatibility&gt;&lt;/w:validateagainstschemas&gt;&lt;/w:punctuationkerning&gt;&lt;/w:worddocument&gt;&lt;/xml&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-8400346580116723694?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/8400346580116723694/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9093.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/8400346580116723694'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/8400346580116723694'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9093.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-620094655173638747</id><published>2009-03-05T15:41:00.003-08:00</published><updated>2009-04-03T16:37:53.743-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/U_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;Ultramafic rock&lt;/span&gt;: An igneous rock consisting dominantly of mafic minerals, containing less than 10 percent feldspar. Includes dunite, peridotite, amphibolite, and pyroxenite.&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 375px; height: 314px;" title="Hydrothermally Altered Ultramafic Rock Grayson County" src="http://www.varockhound.com/rs/dm/dmr-36.jpg" alt="Hydrothermally Altered Ultramafic Rock Grayson County" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;Unconformity:&lt;/span&gt; A surface that separates two strata. It represents an interval of time in which deposition stopped, erosion removed some sediments and rock, and then deposition resumed (see also Angular unconformity ).&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;Unconsolidated material&lt;/span&gt;: Nonlithified sediment that has no mineral cement or matrix binding its grains.&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 564px; height: 321px;" alt="http://www.sinkhole.org/assets/pic_003f.jpg" src="http://www.sinkhole.org/assets/pic_003f.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;br /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;Unit cell&lt;/span&gt;: The smallest contiguous group of atomic structural units in a mineral that can be repeated in three directions to form a crystal.&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.ctcms.nist.gov/wulffman/docs_1.2/unit_cell.gif" src="http://www.ctcms.nist.gov/wulffman/docs_1.2/unit_cell.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;Uplift&lt;/span&gt;: A broad and gentle epeirogenic increase in the elevation of a region without a eustatic change of sea level.&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.mantleplumes.org/images2/DeccanUpliftFig6_550.gif" src="http://www.mantleplumes.org/images2/DeccanUpliftFig6_550.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;Upwelling current&lt;/span&gt;: The upward movement of cold bottom water in the sea, which occurs when wind or currents displace the lighter surface water.&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://hypnea.botany.uwc.ac.za/marbot/images/upwell.gif" src="http://hypnea.botany.uwc.ac.za/marbot/images/upwell.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-weight: bold;"&gt;U-shaped valley&lt;/span&gt;: A deep valley with steep upper walls that grade into a flat floor, usually eroded by a glacier.&lt;br /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://pubs.usgs.gov/of/2004/1216/tz/images/ushapedvalley3.gif" src="http://pubs.usgs.gov/of/2004/1216/tz/images/ushapedvalley3.gif" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-620094655173638747?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/620094655173638747/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9668.html#comment-form' title='1 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/620094655173638747'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/620094655173638747'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_9668.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5339638204727140006</id><published>2009-03-05T15:41:00.001-08:00</published><updated>2009-03-31T11:26:28.299-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/V_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Vadose zone:&lt;/span&gt; The region in the ground between the surface and the water table in which pores are not filled with water. Also called the unsaturated zone.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://geology.er.usgs.gov/eespteam/brass/ground/art/fig10_6.gif" src="http://geology.er.usgs.gov/eespteam/brass/ground/art/fig10_6.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Valence electron:&lt;/span&gt; An electron of the outermost shell of an atom; one of those most active in bonding.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://hyperphysics.phy-astr.gsu.edu/Hbase/solids/imgsol/valen.gif" src="http://hyperphysics.phy-astr.gsu.edu/Hbase/solids/imgsol/valen.gif" /&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Van der Waals bond&lt;/span&gt;: A bond much weaker than the ionic or covalent, which bonds atoms by small electrostatic attraction.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.ndt-ed.org/EducationResources/CommunityCollege/Materials/Graphics/VanderWaals1.gif" src="http://www.ndt-ed.org/EducationResources/CommunityCollege/Materials/Graphics/VanderWaals1.gif" /&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Varve:&lt;/span&gt; A thin layer of sediment grading upward from coarse to fine and light to dark, found in a lake bed and representing one year's deposition of glacial outwash.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 228px; height: 248px;" alt="http://soconnell.web.wesleyan.edu/ees106/field_trips/ct_tectonics/images/stop%20_1_east_berlin_fm/image3-ebf.gif" src="http://soconnell.web.wesleyan.edu/ees106/field_trips/ct_tectonics/images/stop%20_1_east_berlin_fm/image3-ebf.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Vector: &lt;/span&gt;A mathematical element that has a direction and magnitude, but no fixed position. Examples are force and gravity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://portales.educared.net/wikiEducared/images/3/3e/Vector_desplazamiento.gif" src="http://portales.educared.net/wikiEducared/images/3/3e/Vector_desplazamiento.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Ventifact:&lt;/span&gt; A rock that exhibits the effects of sand-blasting or "snowblasting" on its surfaces, which become fiat with sharp edges in between.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.marine.maine.edu/%7Ewellsm/Gallery/Ventifact%20small.gif" src="http://www.marine.maine.edu/%7Ewellsm/Gallery/Ventifact%20small.gif" /&gt;&lt;/p&gt;&lt;p style="text-align: right;"&gt;&lt;span style="font-size:130%;"&gt;&lt;strong&gt;VERB:&lt;/strong&gt;The part of speech that expresses existence, action, events and states.&lt;/span&gt;&lt;/p&gt; &lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img src="http://www.rocketlanguages.com/spanish/images/grammar/spanish_verbs_er.gif" width="388" height="533" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Vertical exaggeration: The ratio of the horizontal scale (for example, 100,000: 1) to the vertical scale (for example, 500: 1) in an illustration.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.cct.nrcan.gc.ca/resource/tutor/stereo/images/geom_e.gif" src="http://www.cct.nrcan.gc.ca/resource/tutor/stereo/images/geom_e.gif" /&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Viscosity:&lt;/span&gt; A measure of resistance to flow in a liquid.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://syntheticperformanceoil.com/spo/images/cold-temp-hot-temp-viscosity.jpg" src="http://syntheticperformanceoil.com/spo/images/cold-temp-hot-temp-viscosity.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Volcanic ash:&lt;/span&gt; A volcanic sediment of rock fragments, usually glass, less than 4 millimeters in diameter that is formed when escaping gases force out a fine spray of magma.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 248px; height: 365px;" alt="http://upload.wikimedia.org/wikipedia/commons/thumb/b/bc/Pompeii_Garden_of_the_Fugitives_02.jpg/408px-Pompeii_Garden_of_the_Fugitives_02.jpg" src="http://upload.wikimedia.org/wikipedia/commons/thumb/b/bc/Pompeii_Garden_of_the_Fugitives_02.jpg/408px-Pompeii_Garden_of_the_Fugitives_02.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Volcanic cone: &lt;/span&gt;The deposit of lava and pyroclastic materials that has settled close to the volcano's central vent.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt; &lt;/span&gt;&lt;img style="width: 358px; height: 568px;" alt="http://www.ifremer.fr/drogm_uk/Realisation/Vulgar/Volcanisme/index.6.gif" src="http://www.ifremer.fr/drogm_uk/Realisation/Vulgar/Volcanisme/index.6.gif" /&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;br /&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Volcanic pipe&lt;/span&gt;: The vertical chamber along which magma and gas ascend to the surface; also, a formation of igneous rock that cooled in a pipe and remains after the erosion of the volcano. &lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://www.marketoracle.co.uk/images/MAM683-IMG2.jpg" src="http://www.marketoracle.co.uk/images/MAM683-IMG2.jpg" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Volcano:&lt;/span&gt; Any opening through the crust that has allowed magma to reach the surface, including the deposits immediately surrounding this vent.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img alt="http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/GeoBytes%20GCSE%20Blog%20Resources/Images/Plate%20Tectonics/Plate%20Tectonics/VolcanoStructure.jpg" src="http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/GeoBytes%20GCSE%20Blog%20Resources/Images/Plate%20Tectonics/Plate%20Tectonics/VolcanoStructure.jpg" /&gt;&lt;/p&gt;&lt;div style="text-align: right;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;V-shaped valley: &lt;/span&gt;A valley whose walls have a more-or-less uniform slope from top to bottom, usually formed by stream erosion. &lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;img style="width: 318px; height: 424px;" alt="http://www.nelsonthornes.com/secondary/geography/key_geography/html/images/vshaped_valley.jpg" src="http://www.nelsonthornes.com/secondary/geography/key_geography/html/images/vshaped_valley.jpg" /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5339638204727140006?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5339638204727140006/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_7671.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5339638204727140006'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5339638204727140006'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_7671.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-1374102502035824785</id><published>2009-03-05T15:40:00.003-08:00</published><updated>2009-03-27T15:23:54.320-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/W_clr.gif" width="60" border="0" height="60" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Wadi: A steep-sided valley containing an intermittent stream in an arid region.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://z.about.com/d/cruises/1/0/m/V/3/wadi_rum04.jpg" src="http://z.about.com/d/cruises/1/0/m/V/3/wadi_rum04.jpg" /&gt;&lt;/span&gt; &lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Warping: In tectonics, refers to the gentle, regional bending of the crust, which occurs in epeirogenic movements.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 335px; height: 203px;" alt="http://www.mathworks.com/matlabcentral/fx_files/11343/1/MATLAB%202006-05-25%2016-09-04-98.jpg" src="http://www.mathworks.com/matlabcentral/fx_files/11343/1/MATLAB%202006-05-25%2016-09-04-98.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Water mass: A mass of water that fills part of an ocean or lake and is distinguished by its uniform physical and chemical properties, such as temperature and salinity.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.eng.warwick.ac.uk/staff/gpk/Teaching-undergrad/es427/rice.glacier.edu-oceans/GLACIER%20Oceans-%20--%20Densitydriven_files/4_pacificmasses.gif" src="http://www.eng.warwick.ac.uk/staff/gpk/Teaching-undergrad/es427/rice.glacier.edu-oceans/GLACIER%20Oceans-%20--%20Densitydriven_files/4_pacificmasses.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Water table: A gently-curved surface below the ground at which the vadose zone ends and the phreatic zone begins; the level to which a well would fill with water.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 470px; height: 251px;" alt="http://geoscape.nrcan.gc.ca/h2o/bowen/images/watertable_e.jpg" src="http://geoscape.nrcan.gc.ca/h2o/bowen/images/watertable_e.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Wave-cut terrace: A level surface formed by wave erosion of coastal bedrock to the bottom of the turbulent breaker zone. May appear above sea level if uplifted.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://coastal.er.usgs.gov/coasts-colombia/caribbean/images/fig-18.jpg" src="http://coastal.er.usgs.gov/coasts-colombia/caribbean/images/fig-18.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Wavelength: The distance between two successive peaks, or between troughs, of a cyclic propagating disturbance.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://dwb.unl.edu/Teacher/NSF/C11/C11Links/gened.emc.maricopa.edu/bio/bio181/BIOBK/wavelength.gif" src="http://dwb.unl.edu/Teacher/NSF/C11/C11Links/gened.emc.maricopa.edu/bio/bio181/BIOBK/wavelength.gif" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Wave steepness: The maximum height or amplitude of a wave divided by its wavelength.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 459px; height: 263px;" alt="http://worldtidesandcurrents.com/Longwavefig1.jpg" src="http://worldtidesandcurrents.com/Longwavefig1.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;  &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;b&gt;Watt steam engine:&lt;/b&gt;was the first type of steam engine to make use of steam at a pressure just above atmospheric to drive the piston helped by a partial vacuum.&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;a href="http://en.wikipedia.org/wiki/File:Maquina_vapor_Watt_ETSIIM.jpg" class="image" title="A late version of a Watt double-acting steam engine, the steam engine that propelled the Industrial Revolution in Britain and the world, located in the lobby of the Superior Technical School of Industrial Engineers of the UPM (Madrid)."&gt;&lt;img alt="" src="http://upload.wikimedia.org/wikipedia/commons/thumb/9/9e/Maquina_vapor_Watt_ETSIIM.jpg/300px-Maquina_vapor_Watt_ETSIIM.jpg" class="thumbimage" width="300" border="0" height="223" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;Weathering: The set of all processes that decay and break up bedrock, by a combination of physically fracturing or chemical decomposition.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 453px; height: 306px;" alt="http://upload.wikimedia.org/wikipedia/commons/f/fc/YehliuTaiwan-HoneycombWeathering.jpg" src="http://upload.wikimedia.org/wikipedia/commons/f/fc/YehliuTaiwan-HoneycombWeathering.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-1374102502035824785?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/1374102502035824785/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_2578.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1374102502035824785'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/1374102502035824785'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_2578.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-3019319724023475709</id><published>2009-03-05T15:40:00.001-08:00</published><updated>2009-04-04T10:09:40.699-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img src="http://www.castelldeferro.info/gif/flores4/51.gif" width="106" border="0" height="85" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 80px; height: 80px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/Y_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img src="http://www.castelldeferro.info/gif/flores4/51.gif" width="106" border="0" height="85" /&gt;&lt;/p&gt;&lt;p style="text-align: left;"&gt;&lt;span style="font-size:130%;"&gt;Youth (geomorphology): A stage in the geomorphic cycle in which a landscape has just been uplifted and is beginning to be dissected by canyons cut by young streams.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.canaanvi.org/canaanvi_web/uploadedImages/Education/rosgen_fge_2008.JPG" src="http://www.canaanvi.org/canaanvi_web/uploadedImages/Education/rosgen_fge_2008.JPG" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-3019319724023475709?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/3019319724023475709/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_05.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/3019319724023475709'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/3019319724023475709'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos_05.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-969896454889667372.post-5664142761907346914</id><published>2009-03-05T15:31:00.000-08:00</published><updated>2009-04-04T10:08:50.580-07:00</updated><title type='text'></title><content type='html'>&lt;p align="center"&gt;&lt;img src="http://www.castelldeferro.info/gif/mariposas1/87.gif" width="113" border="0" height="113" /&gt;&lt;span class="Estilo8"&gt;&lt;span class="Estilo7"&gt;&lt;img style="width: 89px; height: 78px;" alt="Gif Letras, Numeros y Simbolos en Rombos" src="http://elrinconcito.net/Imagenes/Letras-y-Numeros/Estilo/Z_clr.gif" border="0" /&gt;&lt;/span&gt;&lt;/span&gt;&lt;img src="http://www.castelldeferro.info/gif/mariposas1/87.gif" width="113" border="0" height="113" /&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Zeolite&lt;/span&gt;: A class of silicates containing H=O in cavities within the crystal structure. Formed by alteration at low temperature and pressure of other silicates, often volcanic glass.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img alt="http://www.bojistones.com/crystals/Zeolite-5.jpg" src="http://www.bojistones.com/crystals/Zeolite-5.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="text-align: center;"&gt;   &lt;/div&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-weight: bold;"&gt;Zoned crystal&lt;/span&gt;: A single crystal of one mineral that has a different chemical composition in its inner and outer parts. Formed from minerals belonging to a solid-solution series, and caused by the changing concentration of elements in a cooling magma that results from crystals settling out. &lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: center;"&gt;&lt;span style="font-size:130%;"&gt;&lt;img style="width: 474px; height: 315px;" alt="http://www.wordcraft.net/Fluorescent/961apatite.jpg" src="http://www.wordcraft.net/Fluorescent/961apatite.jpg" /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;br /&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/969896454889667372-5664142761907346914?l=ana20cristina.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://ana20cristina.blogspot.com/feeds/5664142761907346914/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos.html#comment-form' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5664142761907346914'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/969896454889667372/posts/default/5664142761907346914'/><link rel='alternate' type='text/html' href='http://ana20cristina.blogspot.com/2009/03/gif-letras-numeros-y-simbolos-en-rombos.html' title=''/><author><name>Ana Henández</name><uri>http://www.blogger.com/profile/15069615070112112062</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='29' height='32' src='http://2.bp.blogspot.com/_gG0sJErOSDo/SbBnRJjXGhI/AAAAAAAAAA0/8KjI1nqf_yg/S220/Copia_de_Copia_de_Copia_de_Copia_de_mi_011.jpg'/></author><thr:total>0</thr:total></entry></feed>
