How where the fossil symbols and mountain belts helpful in deciding where to move to move the continents.
The fossil symbols were helpful in deciding where to move the continents because it showed where land and water dinosaurs could and could not live, especially with the non-swimmers in Africa and South America. There is also proof of some mountains matching in Western Europe and Greenland.
Glossopteris is a fossil plant that has been found on multiple continents, including South America, Africa, Australia, Antarctica, and India. It is an important indicator of the past connections between these landmasses when they were part of the supercontinent Gondwana.
Yes, fossil evidence supports the theory of continental drift. Fossils of similar plants and animals have been found on continents that are now separated by oceans, suggesting they were once connected. This provides evidence that continents have indeed moved over time.
Glossopteris is a plant fossil that was found in multiple continents that were once part of the supercontinent Gondwana. The widespread distribution of Glossopteris across these continents suggests that they were once connected, providing evidence for the existence of Gondwana.
The geologist is applying the principle of superposition, which states that in an undisturbed sequence of rock layers, the oldest rocks are at the bottom and the youngest are at the top. This helps geologists determine the relative ages of fossils found in different layers of sedimentary rock.
The fossil symbols were helpful in deciding where to move the continents because it showed where land and water dinosaurs could and could not live, especially with the non-swimmers in Africa and South America. There is also proof of some mountains matching in Western Europe and Greenland.
Fossil symbols and mountain belts were helpful in deciding the theory of plate tectonics because they provided evidence of past connections between continents and the movement of tectonic plates. Fossil similarities between continents suggested that they were once connected, and asymmetric mountain belts indicated the direction of plate movement. These pieces of evidence supported the idea that continents move and drift on the Earth's surface.
Fossil symbols and similarities in mountain belts across different continents provided evidence for the theory of continental drift, suggesting that the continents were once connected. By looking at the distribution of fossils and rocks across continents, scientists were able to piece together the historical movement and eventual arrangement of the continents.
Fossil symbols were helpful in showing that similar fossils were found on continents that are now separated by oceans, suggesting they were once joined. Mountain belts provided evidence of past tectonic activity where continents collided and moved, supporting the theory of plate tectonics and continental drift. By mapping these features, scientists could determine the movements and positions of continents over time.
Fossil symbols found in different continents can help determine the locations where these continents were once connected based on shared species. Mountain belts can also aid in identifying past plate boundaries and understanding the movement of continents. By studying these features, geologists can trace the historical positions of continents and reconstruct the process of plate tectonics.
Fossil symbols helped in determining the past connections between continents by showing similarities in species that were now separated by large distances. Mountain belts provided geological evidence of past tectonic activity, such as where two continents may have collided. By studying these clues, scientists were able to infer the movement of continents and reconstruct past supercontinents.
Fossil symbols were used to correlate similar ancient life forms found on distant continents, providing evidence of past connections. Mountain belts were important because they showed where continental crusts had collided and formed mountain ranges, indicating potential past plate boundaries and movement of continents. By studying these features, scientists were able to piece together the theory of plate tectonics and use it to determine the movement of continents over time.
Fossil symbols and mountain belts were important because they provided geologic evidence of past connections between continents and helped to support the theory of plate tectonics. Fossils of similar organisms found on different continents suggested that these landmasses were once connected. Mountain belts formed through tectonic collisions of continents gave clues about the movement and positions of landmasses over time. This information helped geologists determine the past positions of continents and how they have shifted over millions of years.
In no way at all is burning fossil fuels (coal, oil and natural gas) helpful to wildlife.
Fit of the continents: The coastlines of continents such as South America and Africa appear to fit together like puzzle pieces. Fossil evidence: Similar fossils of plants and animals have been found on continents that are now widely separated by oceans. Geological features: Matching rock formations and mountain ranges across different continents suggest they were once connected.
True
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