It is the theory that continents are connected to the lithosphere, and whenever the lithosphere moves, so do the continents. Also, continents collide, seperate, and grind past each other at boundaries known as Transform Fault Boundaries( Plates grinding past each other), Convergent Boundaries(colliding plates), and Divergent Boundaries(Plates separating). At Convergent Boundaries, either the oceanic plate(if there is one) goes under the other plate and melts in the lithosphere, or 2 land plates collide and create mountains. At Divergent Boundaries, underwater, a space forms called a rift. Above water on land, volcanoes form, no matter what way the plates move. At Convergent Boundaries underwater, mid-ocean ridges form. Above on land, mountains form. At Transform Fault Boundaries, plates grinding past each other usually don't create volcanoes. They create earthquakes.
I think that continetal drift replaced his theory
The continental drift theory was replaced by the theory of plate tectonics.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
kantot
Another name for the Continental Drift theory is "Plate Tectonics." This theory explains the movement of Earth's lithosphere plates over the asthenosphere.
I think that continetal drift replaced his theory
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.
The continental drift theory was replaced by the theory of plate tectonics.
the Continental Drift Theory is the slow movement of the Earths continents. A.K.A the continents drift
No, only Continental Drift Theory.
Continental Drift
continental drift is caused by plate tectonics
The theory of continental drift did originate in the 1930s. Continental drift asserts that the continents were once a single landmass called Pangaea that drifted apart over time.
The main problem with Wegners theory of continental drift was that at the time he proposed it he had no real proof.
Continental drift
k
1912