Why do scientists today accept the movement of continents but did not accept this theory back in weg

Look at a world map. After burying Wegener, Villumsen had resumed his journey to West camp, but was never seen again. In addition to rich dinosaur fossils, there are also plant fossils that illustrate the reduction in plant species across the K—Pg boundary.

In Wegener was appointed to a professorship in meteorology and geophysics in Grazwhich finally provided him with a secure position for himself and his family.

Proposing a feasible mechanism was something Wegener himself had failed to do, he had only proposed some evidence complementary coastlines and fossil distributions across continents. This is atheory that has been established by Wegener and did not get goodsupport initially. Besides the coast of west Africa and eastern South America, what are some other regions of the world that look as they could be closely fit together?

The continents also have an almost jigsaw fit. The relatively low levels of extinction seen among amphibians probably reflect the low extinction rates seen in freshwater animals.

Another was the fact that the same types of fossil are found inboth places.

Cretaceous–Paleogene extinction event

Many families of terrestrial squamates became extinct at the boundary, such as monstersaurians and polyglyphanodontsand fossil evidence indicates they suffered very heavy losses in the KT event, only recovering 10 million years after it.

Cynognathus and Lystrosaurus were reptiles that lived on land. Success depended on enough provisions being transferred from West camp to Eismitte "mid-ice" for two men to winter there, and this was a factor in the decision that led to his death.

He found a way. How can the locations where ancient fossils are found be used as evidence for continental drift? Villumsen had buried the body with great care, and a pair of skis marked the grave site. Wegener also looked at evidence from ancient glaciers.

Wegeners theory was that the tectonic plates in the earth were moving and colliding with each other due to temperature changes and convection currents at the core of the earth….

High School Earth Science/Continental Drift

Mid-latitude, deep-water echinoderms were much less affected at the K—Pg boundary. Although his proposed mechanism was wrong, he was the first to realize the insight that one of the effects of continental motion would be the formation of mountains, and attributed the formation of the Himalayas to the collision between the Indian subcontinent with Asia.

However scientific studies showed that these animals and plants could not have survived in all of these different climates. Although he presented much evidence for continental drift, he was unable to provide a convincing explanation for the physical processes which might have caused this drift.

Also, at the time, they had no evidence that the continents were or even possibly cou…ld move, and the majority of people thought he was potty. TyrannosaurusAnkylosaurusPachycephalosaurusTriceratopsand Torosaurus[] which suggests food was plentiful immediately prior to the extinction.

These characteristics have been linked to crocodilian survival at the end of the Cretaceous. At the ocean borders, the heavy oceanic crust is subducted under the continental plates, which imparts motion to the continents. Archosaurs[ edit ] The archosaur clade includes two surviving groups, crocodilians and birdsalong with the various extinct groups of non-avian dinosaurs and pterosaurs.

The super-continent eventually broke into the smaller continental. Review Questions[ edit ] Why can paper cutouts of the continents including the continental margins be pieced together to form a single whole?

Worse, the most viable forms of the theory predicted the existence of convection cell boundaries reaching deep into the earth that had yet to be observed.

But gravitational measurements showed that many areas are not in isostatic equilibrium. He analyzed both sides of the Atlantic Ocean for rock type, geological structures and fossils. As the marine microbiota recovered, however, it is thought that increased speciation of benthic foraminifera resulted from the increase in food sources.

He suggested that at one time, all of the continents had been united into a single super continent. The theory of continental drift was originated by Abraham Ortelius in and further developed by Alfred Wegener, a German geophysicist and meteorologist, around Be able to explain the continental drift hypothesis.

Any burrowing or semiaquatic mammal would have had additional protection from K—Pg boundary environmental stresses.The Cretaceous–Paleogene (K–Pg) extinction event, also known as the Cretaceous–Tertiary (K–T) extinction, was a sudden mass extinction of some three-quarters of the plant and animal species on Earth, approximately 66 million years ago.

With the exception of some ectothermic species such as the leatherback sea turtle and crocodiles, no tetrapods weighing more than 25 kilograms (55 lb. In art, a study is a drawing, sketch or painting done in preparation for a finished piece, or as visual notes. A study can have more impact than a more-elaborately planned work, due to the fresh insights the artist is gaining while exploring his/her subject.

Fossils and geologic evidence show that most of the continents used to have startlingly different climates than they do today. Wegener thought continental drift was the key to these climatic puzzles, so he and Vladimir Koppen plotted ancient deserts, jungles, and ice sheets on paleogeographic maps based on Wegener's theory.

Wegener proposed the continental drift theory, and provided scientific evidences for such, but couldn't explain the mechanism or processes behind the movement of continents. scientist did not accept the hypothesis of continental driftbecause they could not figure out how continents moved.

Alfred Lothar Wegener (/ ˈ v eɪ ɡ ən ər /; German: [ˈveːgənɐ]; 1 November – November ) was a German polar researcher, geophysicist and meteorologist.

Continental drift

During his lifetime he was primarily known for his achievements in meteorology and as a pioneer of polar research, but today he is most remembered as the originator of the theory of continental drift by hypothesizing in

Why do scientists today accept the movement of continents but did not accept this theory back in weg
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