what evidence did alfred wegener use to support continental drift
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Continental Drift Wegener gathered evidence from different scientific fields to support his ideas about continental drift. He studied land features, fossils, and evidence of climate change. In 1915, Wegener published his evidence for continental drift in a book called The Origin of Continents and Oceans.egener gathered evidence from different scientific fields to support his ideas about continental drift. He studied land features, fossils, and evidence of climate change. In 1915, Wegener published his evidence for continental drift in a book called The Origin of Continents and Oceans.
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Alfred Wegener 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 1912 that the continents are slowly drifting around the Earth (German: Kontinentalverschiebung).
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- Deep-sea mountain ranges had caught his attention. Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangaea.Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions. people found this useful. 1  The Land Bridge Theory and Continental Drift Land bridge theory began as an effort to counter Alfred Wegener's theory of continental drift (which was ultimately proven correct anyway), yet survived in a modified form as….
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- Evidence. Alfred Wegener collected diverse pieces of evidence to support his theory, including geological “fit” and fossil evidence. It is important to know that the following specific fossil evidence was not brought up by Wegener to support his theory.vidence. Alfred Wegener collected diverse pieces of evidence to support his theory, including geological “fit” and fossil evidence. It is important to know that the following specific fossil evidence was not brought up by Wegener to support his theory.
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What observation led albert wegener to develop the hypothesis of a centental drift? Confidence votes 331. Wegener first noticed that it looked like South America coastline could fit into Africa's. After that he analysed both their continental shelve's and this showed an even closer fit.The thrid observation that brought about his theory of continental drift was that he found fossils of the same animals (can't remember any names off the top of my head sorry) in both Argentina and east Somalia, Africa.onfidence votes 331. Wegener first noticed that it looked like South America coastline could fit into Africa's. After that he analysed both their continental shelve's and this showed an even closer fit.
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- Draw Conclusion. What conclusions did Alfred Wegener draw about Pangaea? He concluded that it split apart and that the continents “drifted” to their present positions. QUICK CHECK
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- The concept was first proposed by Alfred Wegener, the originator of the theory of continental drift, in his 1912 publication The Origin of Continents (Die Entstehung der Kontinente).
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wegener's theory Alfred Wegener (1880 - 1930). Alfred Wegener proposed the theory of continental drift at the beginning of the 20th century. His idea was that the Earth's continents were once joined together, but gradually moved apart over millions of years.egener’s evidence for continental drift was that: 1  the same types of fossilised animals and plants are found in South America and Africa. 2  the shape of the east coast of South America fits the west coast of Africa, like pieces in a jigsaw puzzle.
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When Continental Drift Was Considered Pseudoscience Wegener published his idea in an article that April to no great notice. Later, recovering from wounds he suffered while fighting for Germany during World War I, he developed his idea in a book, The Origin of Continents and Oceans, published in German in 1915.
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Continental Drift: Theory & Definition Continental drift was a theory that explained how continents shift position on Earth's surface. Set forth in 1912 by Alfred Wegener, a geophysicist and meteorologist, continental drift also explained why look-alike animal and plant fossils, and similar rock formations, are found on different continents.lthough Wegener's continental drift theory was discarded, it did introduce the idea of moving continents to geoscience. And decades later, scientists would confirm some of Wegener's ideas, such as the past existence of a supercontinent joining all the world's landmasses as one.
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Alfred Wegener plate tectonics: Alfred Wegener and the concept of continental drift. In 1912 German meteorologist Alfred Wegener, impressed by the similarity of the geography of the Atlantic coastlines, explicitly presented the concept of continental drift.
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Wegener and Continental Drift Theory Wegener needed a mechanism for Continental Drift. Galileo needed an explanation for the lack of stellar parallax and the poor performance of his model (see Galileo's Battle for the Heavens) . It is not only the community that requires faith.
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Alfred Wegener Alfred Wegener, in full Alfred Lothar Wegener (born November 1, 1880, Berlin, Germany—died November 1930, Greenland), German meteorologist and geophysicist who formulated the first complete statement of the continental drift hypothesis.
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- Wegener's drift theory seemed more plausible than land bridges connecting all of the continents. But that in itself was not enough to support his idea. Another observation favoring continental drift was the presence of evidence for continental glaciation in the Pensylvanian period. Striae left by the scraping of glaciers over the land surface indicated that Africa and South America had been close together at the time of this ancient ice age.
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- Many people believe that Alfred Wegener invented the theory of continental drift. Wegener had been struck by the remarkable fit of the coastlines of South America and Africa.
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Alfred Wegener Continental drift theory. Alfred Wegener first thought of this idea by noticing that the different large landmasses of the Earth almost fit together like a jigsaw puzzle. The Continental shelf of the Americas fit closely to Africa and Europe, and Antarctica, Australia, India and Madagascar fitted next to the tip of Southern Africa.
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Chapter 5 Plate Tectonics Section 3 Drifting Continents Although scientist rejected his theory, Wegener continued to collect evidence on continental drift and to update his book. He died in 1930 on an expedition to explore Greenland's continetal glacier.
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- Click Here to return to the search form. Alfred Wegener brought together several lines of evidence to support his theory of continental drift. One is quite simple -- that the continents look like they could fit together, much like puzzle pieces that have drifted apart.lick Here to return to the search form. Alfred Wegener brought together several lines of evidence to support his theory of continental drift. One is quite simple -- that the continents look like they could fit together, much like puzzle pieces that have drifted apart.
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What observation led albert wegener to develop the hypothesis of a centental drift? Making the world better, one answer at a time. the observation of finding the fossil of the reptile Mesosaurus in both Africa and South America. wegener also found the fossil of the fern Glossopteris in Africa,Australia, india, south america, and antarctica.he thrid observation that brought about his theory of continental drift was that he found fossils of the same animals (can't remember any names off the top of my head sorry) in both Argentina and east Somalia, Africa. The animal is the Mesosaurus, a fossil known to live 270 million years ago.
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Wegener and Continental Drift Theory In spite of all the criticism, Wegener was able to keep Continental Drift part of the discussion until his death. He knew that any argument based simply on the jigsaw fit of the continents could easily be explained away. To strengthen his case he drew from the fields of geology, geography, biology and paleontology.
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Continental Drift Quiz This is evidence of ancient swamps and glaciers that Wegener used to prove continental drift Rocks and Mountains Wegener used bands of these solid objects that seamed to connect between continents as proof of continental drift Fossils Wegener used these remains of the same animals found on distance continents to prove contiental drift
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- Although Wegener's continental drift theory was discarded, it did introduce the idea of moving continents to geoscience. And decades later, scientists would confirm some of Wegener's ideas, such as the past existence of a supercontinent joining all the world's landmasses as one.et forth in 1912 by Alfred Wegener, a geophysicist and meteorologist, continental drift also explained why look-alike animal and plant fossils, and similar rock formations, are found on different continents.
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Alfred Wegenerâs Continental Drift Hypothesis Wegener's main interest was meteorology, and he wanted to join the Denmark-Greenland expedition scheduled for mid-1912. He presented his Continental Drift hypothesis on January 6, 1912. He analyzed either side of the Atlantic Ocean for rock type, geological structures and fossils.
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Continental Drift He studied land features, fossils, and evidence of climate change. In 1915, Wegener published his evidence for continental drift in a book called The Origin of Continents and Oceans. Evidence From Land Features. As shown in Figure 12, mountains and other features on
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Wegener and Continental Drift Theory The reaction to Alfred Wegener's Continental Drift Theory demonstrates that new ideas threaten the establishment, regardless of the century. Alfred Wegener was the scientist who proposed the Continental Drift Theory in the early twentieth century.Simply put, his hypothesis proposed that the continents had once been joined, and over time had drifted apart.he reaction to Alfred Wegener's Continental Drift Theory demonstrates that new ideas threaten the establishment, regardless of the century. Alfred Wegener was the scientist who proposed the Continental Drift Theory in the early twentieth century.