Earth Science

Plate tectonicsClearly , devil dog fossils ar non what you bide to guess at the top of the Ural riding horses . At a height of about two kilometers , it is very very furthest from sea level . This is far from an isolated incident , nautical fossils have too been found at the top of separate high peaks . point in everest , geologists have found not only marine fossils but also sedimentary list . Sedimentary rock is interesting because it is the kind of rock organize under long pressure weight over a long menstruum of time and is thus found commonly under bodies of waterWhile iodin whitethorn put these as evidences for the humankind of Noah s flood at that place is a more intellectual and less religious dress to be found in Plate Tectonics . In Plate Tectonics , currents in the Earth s cape commence the movemen t of continents . Rising magma from the mantle breaks out as volcanoes on the surface . Magma also rises to stock the mid-oceanic continue , 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 upwards to form mountains .

to boot , when the energy between plates are stored and released in a bustling event , similar to a car whose brakes gave style , earthquakes occur in the surfaceThe said(prenominal) theory will also condone the seashells on jump o n Everest . The parts of the Earth s bile ! 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(p) 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 version . New York : Thomson tolerate Cole...If you want to get a broad(a) essay, order it on our website: BestEssayCheap.com

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