Fossils can provide a more direct link between rock layers on different continents because they represent a specific time period and can be used for relative dating. Rock types can vary widely and may not provide as clear of a correlation between different continents. By comparing the presence and distribution of similar fossils in different rock layers, researchers can establish connections between geological formations on different continents more accurately.
Fossils are more useful than rock types in correlating rock layers on different continents because they provide direct evidence of ancient life forms that can be compared and matched across continents. Fossils can also help determine the relative ages of rock layers, which is crucial for understanding the timing and sequence of events in Earth's history. In contrast, rock types can vary widely between continents, making direct correlations more challenging.
Wegener used evidence from the fit of the continents, the distribution of fossils, and similarities in rock formations and mountain ranges across different continents to support his theory of drifting continents.
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.
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.
Index fossils are used to correlate rocks of similar age in different locations. By studying index fossils found in rock layers from different continents, scientists can determine which layers are of similar age and potentially infer how these continents were once connected. This information helps in reconstructing past continental configurations, such as during the time of Pangea.
Fossils are more useful than rock types in correlating rock layers on different continents because they provide direct evidence of ancient life forms that can be compared and matched across continents. Fossils can also help determine the relative ages of rock layers, which is crucial for understanding the timing and sequence of events in Earth's history. In contrast, rock types can vary widely between continents, making direct correlations more challenging.
The same rocks and minerals from the same batch, dinosaur fossils dating back to the same time periods, natural landforms and structures can be found on completely separate continents. This evidence supports the Plate Techtonics and Continental Drift theories.
By boook
because if the same fossils were found in the same spot but on two different continents and if you put the continents together like a puzzle and the fossils were in the same spot, it would mean the continents drifted apart.
By boook
It can help show that continental drift happened, if you find the same fossils on different continents. This would mean that the continents had to be close together if the fossils are found on land.
fossils
Wegener used evidence from the fit of the continents, the distribution of fossils, and similarities in rock formations and mountain ranges across different continents to support his theory of drifting continents.
Because, similar fossils could be found on different continents, in rocks of the same age.
The inference is that both continents were once one single land-mass.
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, 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.