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The German scientist, Alfred Wegener first proposed the continental drift theory.
Alfred Wegener was the scientist who first proposed the theory of continental drift, which later developed into the theory of plate tectonics. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart.
The scientist who proposed the theory of continental drift was Alfred Wegener, a German meteorologist and geophysicist. He suggested that the continents were once joined together in a single supercontinent called Pangea and have since moved apart to their current positions.
Alfred Wegener
A German scientist Alfred Wegener first proposed the idea of Continental Drift.
Alfred Wegener, a German meteorologist and geophysicist, proposed the theory of continental drift in 1912. He suggested that thermal convection currents in the mantle cause the movement of continents over time.
The scientist who proposed the continental drift theory was Alfred Wegener, a German meteorologist and geophysicist. In the early 20th century, he suggested that the continents were once part of a supercontinent called Pangaea and have since 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.
Alfred Wegener, a German meteorologist, proposed the first formal theory of continental drift in 1912. He suggested that the continents were once joined together in a single landmass called Pangaea, which later broke apart and drifted to their current positions.
Alfred Wegener, a German meteorologist and geophysicist, proposed the theory of continental drift in the early 20th century after observing cracks in the continents and similarities in rock formations and fossils across different continents.
Alfred Wegener, a German meteorologist, proposed the theory of continental drift in 1912. He suggested that the thermal convection currents in the mantle were responsible for the movement of continents across the Earth's surface.
German scientist Alfred Wegener (1880-1930) first proposed the theory of continental drift in 1912, but it was not widely accepted until the 1950s.