.

Monday, October 14, 2013

Geology And Continental Drift

RUNNING HEAD: CONTINENTAL DRIFT DISCUSSION association Instructor Student The theory of Continental Drift was commencement exercise hypothesized by Alfred Wegener, a meteorologist and geologist from Germany, was officially tell in 1912. natural in Berlin, in the 1880s he was not ascribe with the discovery until after his death. It was assumed that Continental Drift was unaccepted because there was no hard turn up to apologise how the continents of the world could be freestandingd. It would take a ramp of slap-up magnitude to cause such an aggressive switching of transaction mass. Wegeners theory called Pangaea or all reality (Weil, 1997), proposed that the undefiled earth had at angiotensin converting enzyme time been one bulky land mass. His reasoning was based on land semblance, meteoric conditions, and fossils from continents separated by oceans having similar characteristics (Weil, 1997). Fossils at that place was the familiarity of the adopt sam e plant, (Glossopteris Fern) and living creature (Lystrosaurus, reptile) fossils existing during the same age on continents such as India and Madagascar. The Glossopteris fern was also found on continents of Australia and Antartica, Antarctica and India, as well as South the States and Africa (See code 1).
Ordercustompaper.com is a professional essay writing service at which you can buy essays on any topics and disciplines! All custom essays are written by professional writers!
Additionally, other animal fossils that shared continents were the Mesosaurus and Cynognathus from both South America and Africa (Figure 1). Couple that with the intelligible understanding that the plants and animals did not traverse the oceans to lie in these separate lands. Yet they existed at the same t ime in nonuple locations. Continental Dr! ift Evidence. Figure 1 (Watson. J. 1999). meteorologic Conditions The certainty for Continental Drift later called Plate architectonics in meteorology lies in the existence of plants and coral reefs requiring warming temperatures to wax and flourish, existing in Antarctica and other colder regions (Wagner, 2008). Land Semblance there are features of land in both Europe and northernmost America such as the coal flora fossils from the Coal...If you penury to get a full essay, order it on our website: OrderCustomPaper.com

If you want to get a full essay, visit our page: write my paper

No comments:

Post a Comment