Continental drift
Fossils, rock layers, and mountain ranges were some of the land features that provided evidence for Wegener's hypothesis of continental drift.
Fossils found on separate continents that are now far apart provide evidence for continental drift. Similar fossil species found on continents that were once connected suggest that these landmasses were once united. Additionally, matching rock formations and paleoclimate evidence from fossils support the hypothesis of continental drift.
Fossil evidence supporting Wegener's hypothesis of continental drift included identical fossils found on separate continents, showing that these landmasses were once connected. This supported the idea that continents had drifted apart over time. Additionally, the presence of ancient glacial deposits in regions that are now too warm for glaciers to form suggested that these areas were once located closer to the South Pole.
Evidence supporting the hypothesis of continental drift includes the fit of continental coastlines, matching rock formations and fossils across continents, and the alignment of mountain ranges. Additionally, the distribution of ancient glacial deposits and paleoclimate data further support the idea that continents were once connected.
Fossil evidence: the discovery of identical fossils on continents separated by vast oceans supports the idea that these landmasses were once joined together. Matching geological features: the alignment of mountain ranges and rock formations on different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, provide evidence of past connections.
Fossils support his hypothesis.
Tropical fossils in Antarctica.
Well it wasn't so much climate as the fossils that have been found. Fossils have been found in Antarctica of plants that only occur in tropical climates so at one point it must have had a tropical climate. That is the most dramatic example but there are more subtle ones that led him to believe that the continents, at one point, must have been in different locations on the Earth and then moved to where they currently are.
The continental Coastlines fit together like puzzle pieces, fossils, and glacier Grover in warm places
Fossils, rock layers, and mountain ranges were some of the land features that provided evidence for Wegener's hypothesis of continental drift.
Fossils found on separate continents that are now far apart provide evidence for continental drift. Similar fossil species found on continents that were once connected suggest that these landmasses were once united. Additionally, matching rock formations and paleoclimate evidence from fossils support the hypothesis of continental drift.
Fossil evidence supporting Wegener's hypothesis of continental drift included identical fossils found on separate continents, showing that these landmasses were once connected. This supported the idea that continents had drifted apart over time. Additionally, the presence of ancient glacial deposits in regions that are now too warm for glaciers to form suggested that these areas were once located closer to the South Pole.
One key piece of evidence that supports Alfred Wegener's hypothesis of continental drift is the similarity of fossil remains found on widely separated continents. For instance, fossils of the Mesosaurus, a freshwater reptile, have been discovered in both South America and Africa, suggesting that these continents were once joined. Additionally, the matching geological formations and rock types on either side of the Atlantic Ocean further bolster his theory by indicating a shared geological history.
Evidence supporting the hypothesis of continental drift includes the fit of continents like South America and Africa, matching geological features and rock formations across continents, and similar fossil records found on separate continents. Additionally, the presence of ancient glacial deposits and the alignment of mountain ranges between continents provide further support for the movement of continents over time.
Yes, because he found fossils from a fresh water lizard, in two different continents separated by salt water.
The theory for fossils of tropical plants found on an island in the Arctic Ocean is that the island was once situated in a tropical or subtropical region, and through the movement of tectonic plates, it shifted to its current location in the Arctic. This suggests that the climate of the island has significantly changed over time due to the shifting of the Earth's landmasses.
It is any trace of an ancient organism that has been preserved in rock.Fossils provided evidence for continental drift by Wegener's hypothesis. Wegener studied land features, fossils, and evidence of climate change.