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.
200 million years ago
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.
Yes, fossil evidence such as similar plant and animal species found on separate continents has been used to support the continental drift hypothesis. The distribution of fossils across continents suggests that these land masses were once connected and later moved apart.
The fossil that was found on different continents and used to support the theory of continental drift is the Mesosaurus. This extinct freshwater reptile had limited swimming abilities, making it unlikely that it could have crossed vast oceans. Its distribution on both sides of the Atlantic Ocean provided evidence of land connections that later formed the basis for the theory of continental drift.
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.
The name of the floral fossils Wegner used for the idea of continental drift was glossopteris. Alfred Wegner used the continental drift as a way to explain the continental shapes.
He used evidence from landform, climate, and fossils to support his theory of the continental drift.
Alfred Wegener used evidence such as the fit of continents like puzzle pieces, matching rock formations and fossils across continents, and similarities in geological features to support his theory of continental drift. These pieces of evidence suggested that the continents were once joined together in a single supercontinent, which later drifted apart to their current positions.
Alfred Wegener used a variety of evidence to support his theory of continental drift, including the fit of the continents, matching geological features across continents, similar fossils found on different continents, and matching rock formations and mountain ranges across continents. These lines of evidence formed the basis for his argument that the continents were once connected in a single supercontinent called Pangaea.
their roots
Evidence such as the puzzle-like fit of continents, matching geological formations across continents, and similar fossil distributions on different continents convinced scientists that Wegener's theory of continental drift was true. Additionally, the discovery of mid-ocean ridges and the mechanism of plate tectonics further supported the idea of continental drift.
composition of meteorites
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.
Continental drift is the theory that continents move over the Earth's surface over long periods of time, explaining the changing positions of landmasses and geological features.
Alfred Wegener proposed the idea of continental drift, suggesting that the continents of South America and Africa fit together like a puzzle. He used geological and fossil evidence to support his theory of the supercontinent Pangaea.
Continental drift is a concept relating to the movement of the Earth's continents. The proving of the continental drift theory came from evidence found around the world. Foremost, scientists had discovered that similar plants and animal fossils were found in or around different continents, suggesting that they were once joined. The theory of plate tectonics also supported continental drift. If one were to look at a global map, the complementary arrangements between South America and Africa can be easily seen.