Geology+Illustrations


 * ...[[image:http://i.stack.imgur.com/1qxMW.jpg width="604" height="482"]] ||  ||
 * [[image:http://www.eoearth.org/files/120601_120700/120672/Mountain_building_diagram.gif caption="ISOSTATIC UPLIFTWhen erosion removes materials from the surface of the Earth,the crust rises (uplifted) from the lower crust as an effect of rebound."]] ||  ||
 * [[image:http://content.answcdn.com/main/content/img/McGrawHill/Encyclopedia/images/CE356500FG0010.gif width="559" height="766"]] ||  ||
 * [[image:http://xenon.colorado.edu/spotlight/data/chur/eo/scienceImage1.png width="448" height="495"]] ||  ||
 * [[image:http://images.wisegeek.com/sandstone.jpg width="448" height="495" caption="NUMBER 1"]] || [[image:https://sp.yimg.com/xj/th?id=OIP.Mc9a73107b73108594ba118c8b5970044o0&pid=15.1&P=0&w=214&h=162 width="390" height="357" caption="NUMBER 2"]] ||
 * [[image:http://img.geocaching.com/cache/22ccc501-cd61-4f43-b050-50a2d0a86d29.jpg width="448" height="495" caption="NUMBER 3"]] || [[image:http://upload.wikimedia.org/wikipedia/commons/d/dd/Mongol_rock_salt_Edit.jpg width="524" height="393" caption="NUMBER 4"]] ||
 * ......[[image:https://encrypted-tbn3.gstatic.com/images?q=tbn:ANd9GcRuXnPynpei6R4FOosFiMCTALGyqZBT3r2F1sSt2RQ2rE0qzxzc0GXSFe2m width="360" height="337" caption="NUMBER 5"]] || [[image:http://www.adn.com/sites/default/files/styles/ad_slideshow_940/public/IMG_2646_oiled-rock_Kiukpalik_Carson_2011.jpg?itok=pFFyy0R0 width="589" height="393" caption="NUMBER 6"]] ||
 * [[image:http://rockingaroundwithrocks.files.wordpress.com/2012/03/dsc01189.jpg width="448" height="495" caption="NUMBER 7"]] || [[image:http://www.ocean.odu.edu/%7Espars001/common/graphics/figures/sedimentary_procedure.jpg]] ||
 * || [[image:http://crystal-information.com/wp-content/uploads/bfi_thumb/obsidian-1920x1080-mcwx4s4h8kf6u99ock73ces2g68dlnnh1nreno7shs.jpg width="699" height="393" caption="NUMBER 8"]] ||
 * || [[image:http://www.pitt.edu/%7Ecejones/GeoImages/2IgneousRocks/IgneousCompositions/7Rhyolite/Rhyolite.jpg width="523" height="393" caption="Number 9 is an extrusive igneous rock(silica-rich) compositionThe mineral assemblage is usually quartz, sanidine and plagioclase.It is the extrusive equivalent to granite.Contents"]] ||
 * || [[image:https://www.earth.ox.ac.uk/%7Eoesis/rocks/medium/ign8a-m.jpg width="483" height="393" caption="NUMBER 10"]] ||
 * [[image:http://www.virtualmicroscope.org/sites/default/files/at616-Syenite1_Rob.jpg width="402" height="393" caption="NUMBER 11"]] ||  ||
 * .....[[image:https://upload.wikimedia.org/wikipedia/commons/a/a1/Qtz_porphyry.JPG width="524" height="393" caption="Number 12 .Its texture resembles extrusive and intrusive rock because it has large quartz crystals (phenocrystals)surrounded by  a fine-grained matrix, usually of micro-crystalline or felsitic structure."]] ||   ||
 * [[image:https://i.ytimg.com/vi/7q3O9cbDy8U/maxresdefault.jpg width="654" height="343" caption="Number 13"]] ||  ||
 * || [[image:https://www.earth.ox.ac.uk/%7Eoesis/rocks/medium/ign8a-m.jpg width="483" height="393" caption="NUMBER 10"]] ||
 * [[image:http://www.virtualmicroscope.org/sites/default/files/at616-Syenite1_Rob.jpg width="402" height="393" caption="NUMBER 11"]] ||  ||
 * .....[[image:https://upload.wikimedia.org/wikipedia/commons/a/a1/Qtz_porphyry.JPG width="524" height="393" caption="Number 12 .Its texture resembles extrusive and intrusive rock because it has large quartz crystals (phenocrystals)surrounded by  a fine-grained matrix, usually of micro-crystalline or felsitic structure."]] ||   ||
 * [[image:https://i.ytimg.com/vi/7q3O9cbDy8U/maxresdefault.jpg width="654" height="343" caption="Number 13"]] ||  ||
 * [[image:https://i.ytimg.com/vi/7q3O9cbDy8U/maxresdefault.jpg width="654" height="343" caption="Number 13"]] ||  ||