Plate Tectonics.
continental drift
Another name for the Continental Drift theory is "Plate Tectonics." This theory explains the movement of Earth's lithosphere plates over the asthenosphere.
Pangia
continental drift
Pangaea .
continental drift theory
Alfred wegener came up with the theory of continental drift, when all of the continents were together as one the landmass was called Pangea
The theory that led to the theory of plate tectonics is called continental drift. Proposed by Alfred Wegener in the early 20th century, continental drift suggested that continents were once joined together and have since drifted apart to their current positions on Earth's surface.
Alfred Wegener's support of continental drift was known as the theory of "continental drift," which proposed that the continents were once joined together as a single supercontinent called Pangaea and have since drifted apart.
The theory that the continents were once joined and then slowly drifted apart is called "continental drift." This theory was proposed by Alfred Wegener in the early 20th century and later developed into the theory of plate tectonics.
Continental Drift is an obsolete name for the theory of Plate Tectonics and yes, it is true. It has been proved in many ways, by comparing the composition of oceanic crust and its ages with that of the continental crust, by plotting the reversals of magnetism in the oceanic crust and many other ways.
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.