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What is the theory of the moveable plates on earth?
The theory is called plate tectonics.
What do you call a scientific theory that earts crust is made up of moving plates?
The scientific theory is called plate tectonics, which describes the movement and interaction of Earth's lithosphere plates. This theory explains phenomena such as earthquakes, volcanoes, and mountain formation.
What is the Theory earth divided into moving plates?
The place where tectonic plates touch
How does the motion of the tectonic plates relate to continental drift?
Continental drift is the theory that "plates" on the Earth are constantly in motion and have been for millions of years. Tectonic plates are the actual moving plates.
What Is the theory that the earths lithosphere is divided into tectonic plates that move around on top of the asthenosphere?
A theory that says the lithosphere is divided into plates that move around on top of the asthenosphere is called '' plate tectonics''
Which scientific theory is not shown by the world map of earth's plates?
the theory of plate tectonics
What is the theory that the lithosphere is divided into tectonic plates that move around?
That would be the theory of plate tectonics.
How is a mountain formed by colliding continental plates?
In theory, tectonic plates. http://www.ucmp.berkeley.edu/geology/tectonics.html
THEORY OF PLATE TECHTONIC?
When the Continental Drift Theory applies; when two plates either collide, smash, or slide to move plate techtonics.
What do scientists call the theory that describe the motion of the plates?
Scientists call the theory that describes the motion of tectonic plates "plate tectonics." This theory explains how the Earth's lithosphere is divided into several large plates that move and interact with each other, leading to processes like earthquakes, volcanic activity, and mountain building.
What is the theory that explains why you have earthquakes?
Due to the disturbances in tectonic plates
What theory that plates move around on the asthenosphere?
It is plate tectonics.
