about theory of continental drift
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Answer:
Arthur Holmes later proposed mantle convection for that mechanism. The idea of continental drift has since been subsumed by the theory of plate tectonics, which explains that the continents more by riding on plates of the Earth's lithosphere.
Explanation:
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Answer:
Alfred Wegener 1880-1930 a German meteorologist and geologist, was the first person to propose the theory of continental drift. In his book, Origin of Continents and Oceans, he calculated that 200 million years ago the continents were originally joined together, forming large supercontinent. He named this supercontinent Pangaea, meaning All-earth.
The Earth's crust is not a single continuous layer. It is made up of a number of gigantic pieces like a huge jigsaw puzzle.
Each piece is called a crustal plate. Currents of molten rock rise up through the mantle like boiling water in a saucepan.
These form convection cells that drive the movement of the plates so that they are continuously moving away or towards each other. Geologically, the most important things happen at the plate boundaries, including most of the earthquakes, volcanoes, igneous rocks, major metamorphism, and mountain building processes.