One key piece of evidence supporting Wegner's theory of continental drift was the striking geometric fit of the continents on either side of the Atlantic Ocean. Additionally, the distribution of identical plant and animal fossils on opposite sides of the Atlantic further suggested that the continents were once connected. Finally, the discovery of matching geological features, such as mountain chains and rock formations, across different continents provided further evidence for his theory.
Wegner needed evidence of a mechanism by which continents could move, data supporting the idea of past and present continental positions, geological similarities between continents, and paleoclimatic evidence to strengthen his argument for continental drift.
Two main pieces of evidence that support Wegner's theory of continental drift are the fit of the continents' coastlines, indicating they were once connected, and the distribution of similar fossils and rock formations across separate continents, suggesting a shared geological history.
Wegner used evidence from fossil distributions, rock formations, and the fit of continents like puzzle pieces to support his theory of continental drift. He also noted similarities in plant and animal species found on different continents, suggesting they were once connected.
Geological evidence such as the matching of rock formations and mountain ranges across continents Fossil evidence, specifically the presence of identical fossils on different continents separated by vast oceans Paleoclimatic evidence, including glacial deposits and coal seams found in regions where they shouldn't be if the continents were positioned differently Wegner was particularly interested in the matching of geological features across continents, as this provided strong evidence for his theory of continental drift. Additionally, the distribution of fossils on different continents intrigued him due to the implications for how species could have migrated and evolved.
Four pieces of evidence used by Alfred Wegener to support his theory of continental drift were the fit of the continents, matching geological formations across continents, similar fossil distributions, and glacial evidence in tropical regions.
yes
Wegner needed evidence of a mechanism by which continents could move, data supporting the idea of past and present continental positions, geological similarities between continents, and paleoclimatic evidence to strengthen his argument for continental drift.
Tropic plants in Greenland.
Wegner
Fossil evidence showing similar plant and animal species in regions that are now widely separated provides support for Wegner's hypothesis of continental drift. This suggests that the continents were once connected in a single landmass.
it was a dino and more things added to his list but he did'nt add it to the list.
Two main pieces of evidence that support Wegner's theory of continental drift are the fit of the continents' coastlines, indicating they were once connected, and the distribution of similar fossils and rock formations across separate continents, suggesting a shared geological history.
In Africa there are scratch marks that could only have been caused by glaciers but Africa is by a hot place by the equate so once it was colder there
He used evidence from landform, climate, and fossils to support his theory of the continental drift.
Erik Wegner's birth name is Erik Otto Wegner.
Erik Wegner is 5' 9".
Lyndsey Wegner is 5' 4".