Continental drift

Alfred Wegener gave many facts that help prove his Continental Drift theory. Wegener’s supporting facts include fossil evidence, land features, climate evidence, and sea floor spreading. In the beginning of Wegener’s research to prove his Continental Drift theory, he found clues from fossil evidence from millions of years ago. Different animals, such as the Cynognathus, Lystrasaurus, and Mesosaurus gave proof that the continents have moved. The Cynognathus was a land animal, whose fossils where

Alfred Wegener was a meteorologist and astronomer. He was the first scientist to introduce the theory of the continental drift. Wegener theorized that at one time the continents were one large landmass or Pangaea that had drifted apart. His ideas were initially rejected by other scientists. It was not until long after Wegener’s death that proof was obtained and his theory verified. The Life of Alfred Wegener Alfred was born in Germany in 1880 and led a very busy life. He received a PhD in astronomy

1. What is continental drift? Continental drift is the gradual movement of the continents across the earth’s surface through geological time. The theory of plate tectonics, which use to be called continental drift, is described as the movement of the continents and sea floor across the surface of the Earth. The theory explains many odd facts about Earth’s geology, such as the present arrangement of landmasses which have stated that the Earth’s crust slowly drifts atop a liquid core. 2. What was

Continental Drift Should the Fixists have accepted Alfred Wegeners’ idea of continental drift more quickly? I personally have more sympathy on Wegeners’ part, having some very sound evidence to support an exceedingly well claim. The idea that Pangea, a supercontinent consisting of all the landmasses on earth, existed 300 million years ago, was all Wegeners’. In this essay, I will give evidence to support Wegeners’ claim such as plate boundaries, glacial scratches, mountain ranges, and fossil evidence

One line of evidence used to support continental drift is the discovery of similar fossils on different continents. Both fossil plants and animals found in India, South Africa, Australia, Antarctica, and South America are very similar. This supports the idea that the continents were once one because it suggests that the animals roamed the land, were fossilized where they were when they died, and then we discovered the fossils after the supercontinent had separated. Another line of evidence that

Continental drift has helped create the diversity we see present in modern day plants and animals. Through a process of speciation, the movement of the continents has had a generous role throughout evolution, effecting and distributing flora and fauna. The Earth’s continents were once one, a large supercontinent called Pangea that later separated into two smaller ones known as Gondwana and Laurasia. The separation and collision of continents has not only created some of the valleys and mountain ranges

Continental Drift and Plate Tectonics Theory (Part 1a) Introduction: The Beginning of the “Continental Drift Theory” In the middle of the eighteenth century, James Hutton proposed a theory, uniformitarianism; “the present is the key to the past”. It held that processes such as geologic forces- gradual and catastrophic-occurring in the present were the same that operated in the past. (Matt Rosenberg, 2004) This theory coincides with the theory of Continental Drift that was first proposed by Abraham

Alfred Wegener suggested that the continents have moved about the earth. Wegener carefully compiled evidence for continental drift that eventually became universally accepted in the scientific community. This lab also helped support the theory of continental drift. In this lab, we created a map of Earth 225 million years ago. This map indicates that South America, Africa, India, Antarctica, and Australia all used to be a part of a landmass called pangaea. Both the fossil evidences and the shape

of astronomy. Wegener believed he could make a greater impact and contribution in meteorology, and he did. Wegener achieved several great accomplishments throughout his life but, the one we're focusing on is the theory of continental drift. Continental Drift? Continental Drift was a groundbreaking scientific theory developed in the years 1910-1912 by Alfred Wegener , a German

There are many differences between continental drift and sea-floor spreading and plate tectonics. there are also lots of differences between continental drift and sea-floor spreading and plate tectonics. They all have different factors that makes them different or the same. Sea-floor spreading is an important part of the world. Plate tectonics and continental drift are all also an important part of the world. There is a lot of ways to tell you about the differences and similar traits like showing