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Monday, January 28, 2013

Earth Science

Plate tectonicsClearly , devil dog fossils ar not what you expect to guess at the top of the Ural riding horses . At a height of about two kilometers , it is very very far from sea level . This is far from an isolated incident , marine fossils have too been found at the top of other high peaks . point in everest , geologists have found not only marine fossils but also sedimentary careen . Sedimentary rock is interesting because it is the kind of rock formed under long pressure weight over a long menstruum of time and is thus found usually under bodies of waterWhile iodin may put these as evidences for the existence of Noah s flood at that place is a more rational and less religious dress to be found in Plate Tectonics . In Plate Tectonics , currents in the Earth s mantle commence the movement of continents . Rising magma from the mantle breaks out as volcanoes on the surface . Magma also rises to form the mid-oceanic ridge , an undersea sess range . The expansion of the mid-oceanic ridge pushes the plates apart . At places where plates conflict , one plate may subduct (force one plate to go underneath it ) another or both plates may go upward to form mountains .
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Additionally , when the energy between plates are stored and released in a quick event , similar to a car whose brakes gave way , earthquakes occur in the surfaceThe said(prenominal) theory will also explain the seashells on jump on Everest . The parts of the Earth s crust which form Mount Everest and the Ural mountains were erstwhile under the ocean . In there , they accumulated the respective(a) fossils and sedimentary rocks we see today . Due to Plate Tectonics , these underwater rocks were then forced upward to form the mountain ranges we see today , carrying along the millions of years of fossils and rocks from the ocean floorBibliographyThompson , G Turk , J (2007 ) and the Environment 4th edition . New York : Thomson tolerate Cole...If you want to get a full essay, order it on our website: Ordercustompaper.com

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