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the plates are moving away from each other.
Convergent plates move towards each other, leading to the collision and subduction of one plate beneath the other. This movement often results in the formation of mountain ranges, deep ocean trenches, and volcanic activity.
plate tectonics=D
Mountains are formed by plate tectonics when tectonic plates collide or move past each other. This movement can cause the Earth's crust to fold, buckle, or uplift, creating mountain ranges.
The four main types of plate tectonics are divergent boundaries, where plates move away from each other; convergent boundaries, where plates collide; transform boundaries, where plates slide past each other horizontally; and subduction zones, where one plate is forced beneath another.
an earth quake
Earthquakes
But plate tectonics is the theory which suggests that the Earth's crust is made up of solid plates moving relative to each other. Plate tectonics and the plate tectonics theory aren't really two separate things. However plates are pieces of the Earth's crust which are moving.
it shows that the polarity was switched and they push away from each other.
Plate tectonics are what each continent is on. They move and are continuing to move today. It has to do with the earth's shape because the plate tectonics move the continents around.
I think it is plate tectonics
Plate tectonics create mountains by shifting. They ran into each other and the crashes created solid mountains. Mountains are like wrinkles in the earth.
No, plate tectonics refers to the theory that Earth's outer shell is divided into several plates that move and interact with each other. These plates are not flat but constantly shifting and changing due to the forces beneath the Earth's surface.
the plates are moving away from each other.
Convergent plates move towards each other, leading to the collision and subduction of one plate beneath the other. This movement often results in the formation of mountain ranges, deep ocean trenches, and volcanic activity.
plate tectonics=D
Plate tectonics.