Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός "pertaining to building")[1] is a scientific theory that describes the large scale motions of Earth's lithosphere. The theory builds on the concepts of continental drift, developed during the first decades of the 20th century, and accepted by the majority of the geoscientific community when the concepts of seafloor spreading were developed in the late 1950s and early 1960s.
30%
continental drift
Its Tectonic Activity
due to volcanics effects and movement of earth which affect the earth surface
crust
the movement and formation of the plates or continents is caused by conduction under the crust.
the movement and formation of the plates or continents is caused by conduction under the crust.
it is water cycle
30%
the earths plates shifted....
In great detail
the Continental Drift Theory is the slow movement of the Earths continents. A.K.A the continents drift
Just under 30%
continental drift
Its Tectonic Activity
One third is surface and the rest is the sea.
The continents have moved, Volcanoes and mountains have made hige changes in the earths suface too.