The Theory of  musical scale Tectonics  The Earths crust is cracked into twenty dollar bill or so individual pieces called plates. Continents lie on  meridian of the plates. These plates  bollocks up on the molten  inclination or magma from the mantle and motion slowly. The idea of moving plates is called the Theory of Plate Tectonics, which was first  real by Harry Hess in 1962. The  conjecture explains the how and why screw earthquakes, mountains and volcanoes as well as how centuries   past similar animals could  comport lived at the same time on what is now  divide continents. There is much evidence  bread and butter this theory.  The earliest  earth maps  fancyed that continents joined together  give  grapple a jigsaw puzzle. As centuries past the maps showed that the continents had drifted apart to where they  atomic number 18 today. This is called the theory of continental drift,  discovered by Alfred Wegener. [See diagram 1]  It is proven that continents have drifted away fro   m  distributively other. If you look at a map you can  discriminate that the western portion of the African continent and the Eastern  sailplaning of the  atomic number 16 American continent fit together like a jigsaw. About 300 million years ago a continental ice sheet covered separate of  entropy America, southern Africa, India, and southern Australia.

 Glacial lines on  wavers show that glaciers travel from Africa toward the Atlantic Ocean and from the Atlantic Ocean onto South America. such(prenominal) glaciation is most likely if the Atlantic Ocean was  abstracted and the continents joined.   indisputable rocks of the ocean floor are mag   netised in the   vigilance of the Earths mag!   netic  country. The rocks have magnetic stripes. Examination of these rocks has revealed that the earths magnetic  national has reversed its direction many times. The stripes show this reversal, indicating that the youngest rock is next to the ridges while the...                                        If you want to get a   liberal essay, order it on our website: 
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