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When two continents collide, their tectonic plates push against each other, causing intense pressure to build up. This pressure can force rocks to deform and fold, leading to the formation of mountain ranges. The collision may also cause crustal uplift and the thickening of the Earth's crust, further contributing to mountain formation.
The theory of plate tectonics explains that the Earth's lithosphere is divided into large plates that float on the semi-fluid asthenosphere. These plates move due to the heat-driven convective currents in the mantle. Continental drift is the movement of the continents across the Earth's surface over geologic time. The continents have shifted over time due to the movement of these tectonic plates, leading to the formation of supercontinents like Pangaea, which later broke apart into the continents we see today.
The theory that explains why and how continents move is called plate tectonics. It states that Earth's outer shell is divided into several large plates that float on the semi-fluid asthenosphere below, and these plates move and interact with each other, leading to phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Wegener proposed the theory of continental drift, suggesting that the continents were once connected in a single landmass called Pangaea. He proposed that the continents drifted apart over time due to the movement of the Earth's crustal plates.
Wegener believed that all continents were once part of a supercontinent called Pangaea, which began breaking apart about 200 million years ago. He proposed the theory of continental drift to explain the movement of the continents over time.
The current shape and position of continents provide evidence for the theory of plate tectonics, which suggests that continents were once part of a supercontinent called Pangaea that has since drifted apart. This movement helps explain the similarities between the geology and fossils of now widely separated continents, as well as the presence of matching coastlines and mountain ranges.