Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similarities in rock formations and fossils across continents, and the matching of ancient climate indicators like glaciation patterns. Despite facing initial skepticism, Wegener's evidence paved the way for the development of the theory of plate tectonics.
Alfred Wegener did not use direct geological evidence, such as rock samples or detailed seismic data, to support his theory of continental drift. Instead, he relied on indirect evidence like the fit of continental coastlines, the distribution of fossils across continents, and the similarities in rock formations and mountain ranges on different continents.
Alfred Wegener's theory of continental drift was supported by several lines of evidence, including the matching coastlines of different continents, similarities in rock formations and mountain ranges across continents, and the distribution of fossils of similar species on different continents. He also observed the fit of the continents like pieces of a jigsaw puzzle and the presence of ancient glacial deposits in regions that are now at different latitudes.
Alfred Wegener is pronounced as "AL-fret VEG-ner."
Alfred Wegener presented several pieces of evidence to support his theory of continental drift, including the jigsaw-like fit of continents, particularly South America and Africa. He also noted the similarity of fossil remains, such as the Mesosaurus, found on widely separated continents, and similarities in rock formations and mountain ranges across continents. Additionally, he observed climatic evidence, like glacial deposits in now-tropical regions, which suggested that continents had once been positioned differently.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
human remains
Alfred Wegener's proclamation of continental drift was initially considered a hypothesis because it lacked substantial empirical evidence to fully support it. A theory requires a well-established body of evidence and confirmed predictions, which were not present at the time of Wegener's proposal.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
Alfred Wegener used various pieces of evidence to support his theory of continental drift, including the fit of the continents, rock and fossil similarities across continents, glacial evidence, and similar geological features on different continents.
Alfred Wegener used fossil evidence, geological evidence, and paleoclimatic evidence to support his theory of Continental Drift. Fossils of the same species found on different continents, similar rock formations and mountain ranges across continents, and matching ancient climate patterns were key pieces of evidence that he presented.
Alfred Wegener had several lines of evidence to support his idea of Pangaea, including the fit of the continents, similarities in rock formations and fossils across continents, and the presence of past glacial evidence in regions that are now separated by large distances. Additionally, Wegener noted similarities in climate and geological features that suggested the continents were once connected.
Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similar rock formations and mountain ranges across continents, and the distribution of plants and animals. He also looked at evidence from fossils and ancient climate data to support his hypothesis.
No, Alfred Wegener proposed the theory of continental drift, not a shrinking earth. He used evidence from matching coastlines, fossils, rock types, and climate to support his idea that the continents were once joined in a single supercontinent called Pangaea.
Frederick J. Vine helped Alfred Wegener by providing important evidence to support the theory of continental drift. Vine's research on magnetic anomalies in the ocean floor provided crucial support for Wegener's idea of plate tectonics. This collaboration helped to further validate Wegener's revolutionary theory in the field of geology.
Alfred Wegener had discovered pangaea in the year of 1912.
Alfred Wegener used evidence such as the apparent fit of the continents, similarities in rock formations and mountain ranges across continents, and the distribution of fossils of identical species in continents that are now separated by vast oceans to support his theory of the breakup of Pangaea. He also cited geological and paleontological evidence from different continents that suggested they were once connected.