There are four things that are used for evidence for the continental drift. The four continental drift was Shape of continents, fossil evidence, glacial evidence and similar rocks found in different continents.
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Fossil evidence, such as identical species found on opposite continents that were once connected, and geological evidence like matching mountain ranges and rock formations suggest that continents were once joined together and have drifted apart over time. Additionally, paleoclimatic evidence, such as glacial deposits in regions that are now near the equator, also support the theory of continental drift.
Mesosaurus fossils
Alfred Wegener used evidence from the fit of continents, distribution of fossils, rock types, and ancient climate data to support his theory of continental drift.
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.
Wegener used the fit of the continents, matching rock formations and mountain ranges across continents, and the distribution of fossils as evidence to support his theory of continental drift.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
Evidence for continental drift includes the fit of the continents like a puzzle, similarities in rock formations and fossils across continents, and matching mountain ranges and geologic structures on different landmasses. Additionally, the distribution of certain species and climate indicators supports the theory of continental drift. These pieces of evidence suggest that the continents were once connected and have since moved apart over millions of years.