same fossils in diferent places show that they were all connected once.
Wegener used the presence of Glossopteris fossils, a type of fern-like plant, to support his idea of continental drift. These fossils were found across multiple continents that currently have widely separated coastlines, suggesting they were once part of a single landmass.
Fossils found on different continents that were once connected support the idea of continental drift. The similarities in fossilized plants and animals found on separate continents suggest these landmasses were once part of the same supercontinent. This evidence helps corroborate the hypothesis of continental drift proposed by Alfred Wegener.
The presence of the same fossils or geological formations on different continents can provide evidence to support the theory of continental drift. This suggests that the continents were once connected and have since drifted apart over geological time scales.
Fossils found on separated continents provide evidence that those landmasses were once connected. Similar fossils on continents that are now far apart suggest a shared history and support the idea of continental drift. Additionally, the distribution of fossils across continents can help reconstruct the movement of landmasses over geological time.
Fossils found on separate continents that were once connected suggest that those current landmasses were once part of a single landmass. As continents drifted apart, the fossils remained in place, providing evidence for the theory of continental drift. This phenomenon supports the idea that the Earth's continents were once part of a supercontinent called Pangaea.
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.
Wegener used the presence of Glossopteris fossils, a type of fern-like plant, to support his idea of continental drift. These fossils were found across multiple continents that currently have widely separated coastlines, suggesting they were once part of a single landmass.
Name a fossil that was found on different continents and was used to support the theory of continental drift.
Fossils found on different continents that were once connected support the idea of continental drift. The similarities in fossilized plants and animals found on separate continents suggest these landmasses were once part of the same supercontinent. This evidence helps corroborate the hypothesis of continental drift proposed by Alfred Wegener.
The presence of the same fossils or geological formations on different continents can provide evidence to support the theory of continental drift. This suggests that the continents were once connected and have since drifted apart over geological time scales.
Fossils found on separated continents provide evidence that those landmasses were once connected. Similar fossils on continents that are now far apart suggest a shared history and support the idea of continental drift. Additionally, the distribution of fossils across continents can help reconstruct the movement of landmasses over geological time.
True. Alfred Wegener, the scientist who proposed the theory of continental drift, used the distribution of fossils of tropical plants across continents as evidence to support his idea that the continents were once connected. This was one of the key pieces of evidence Wegener used to support his theory.
yeah yeah sure sure
The same fossils found on different sides of the ocean.
i nned the answer to
Cynognathus is a good candidate for providing evidence for the continental drift theory because its fossil has been found in both South America and Africa, which were once connected in the supercontinent Gondwana. This distribution pattern supports the idea of continental drift, as it suggests that these continents were once joined together and later drifted apart.
Fossils found on separate continents that were once connected suggest that those current landmasses were once part of a single landmass. As continents drifted apart, the fossils remained in place, providing evidence for the theory of continental drift. This phenomenon supports the idea that the Earth's continents were once part of a supercontinent called Pangaea.