For many of years geologists submit been searching for ways to shew the Continental Drive scheme to the world. Yet the lack great(p) consequence, rather have a collection of theories and semi-relevant evidence. If one takes a step back and observes all item closely, it is obvious that Continental Drift is more(prenominal) than than a theory. It very sound could be a feature. The evidence is there. The patently coincidental score of Continental shapes, fossil correlation, paleomagnetism, paleoglaciation, and paleoclimatology evidence all are genuine pieces of evidence that the p youngs on the domain are in incident drifting. Close examination of a world often results in the manifestation that most of the continents seem to fit to bulgeher like a jigsaw puzzle: the double-u African coastline seems to snuggle nicely into the east coast of confederation America and the Caribbean sea; and a similar fit appears cross-section(prenominal) the Pacific. The fit is even more striking when the submerged Continental shelves are compared rather than the coastlines. In 1912, Alfred Wegener (1880-1930) noticed the equivalent social occasion and proposed that the continents were one magazine flavourless into a single topnotch continent, which he called Pangaea, and over meter they have drifted apart into their on-line(prenominal) position. He believed that Pangaea was intact until the late carbonous period, about ccc million years ago, when it began to prisonbreak up and drift apart.

However, Wegeners system lacked a geological chemical mechanism to inform how the continents could drift crossways the earths surface as he proposed. scrutinizing for evidence to further fail his theory of continental drift, Wegener came crossways a paper suggesting that a land twain had in one case connected Africa with Brazil. This proposed land bridge was an attempt to explain the hygienic known observation that the same fossilized plants and animals from the same conviction period were found... If you want to get a full essay, describe it on our website:
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