the breaking down of pangea
The theory of plate tectonics supports the idea of continental drift. It suggests that the Earth's lithosphere is divided into large plates that move over the asthenosphere, which explains the movement of continents over time.
the theory would be called Continental drift.
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.
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The idea of continental drift has been subsumed by the theory of plate tectonics.
A German scientist Alfred Wegener first proposed the idea of Continental Drift.
Before the theory of Continental Drift was widely accepted, scientists believed in the concept of stationary continents. They thought that the continents were fixed in place and did not move over time. This idea was known as the theory of continental permanence.
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.
The idea of continental drift was first proposed by Alfred Wegener in 1912. Wegener's theory suggested that the continents were once joined together in a single landmass called Pangaea and had drifted apart over time.
Alfred Wegener proposed the theory of continental drift at the beginning of the 20th century. His idea was that the Earth's continents were once joined together, but gradually moved apart over millions of years. The idea was rejected at first as he was a Meteorologist and not regarded as a proper scientist.
The plate tectonic theory expands on the idea of continental drift by incorporating the movement of the Earth's lithosphere into rigid plates. This theory also explains how these plates interact at their boundaries, causing phenomena like earthquakes and volcanic activity. In contrast, continental drift primarily focused on the movement of continents across the Earth's surface without explaining the mechanism behind it.
plate tectonics