Fossils, rocks, and the Theory of continental drift are all connected because when the continents moved apart from each other, the spreading actually moves the rocks and fossils to another area, resulting in rocks that fit perfectly together but were separated and many similar fossils in different areas. hOPE IT HELPS ;)
Yes, fossils are evidence of continental drift because similar fossils have been found on different continents that are now far apart. This suggests that these continents were once connected, supporting the theory of continental drift.
It supports the continental drift.
Fossils found on different continents with similar characteristics suggest that these landmasses were once connected millions of years ago. As continents drift apart, similar fossils can only be explained by the movement of landmasses over time, supporting the theory of continental drift. This provides evidence that different continents were once part of a single supercontinent, such as Pangaea.
continental drift. This is because the presence of similar fossils on opposite sides of the ocean suggests that the landmasses were once connected and have since drifted apart. This phenomenon supports the theory 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.
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.
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.
Yes, the presence of the same organisms on multiple continents suggests that at some point in the past, those continents were connected. This supports the theory of continental drift, which explains how landmasses have moved over time. The distribution of these similar organisms across different continents provides additional evidence for this theory.
Fossils found on separate continents that were once connected suggest that landmasses have moved over time. Identical or closely related species of plants and animals found on different continents indicate that they were once part of the same landmass and have since drifted apart. This evidence supports the theory of continental drift proposed by Alfred Wegener.
He used evidence from landform, climate, and fossils to support his theory of the 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.