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The lithosphere and sea floor spreading are both factors in the movement of tectonic plate movement. As there is no foreseeable reason for the currents to stop, there is also no foreseeable reason for all tectonic plate movement to stop.
A soft collision between two plates could possibly stop the plates from moving for a time. But if subduction occurs, when one plate is forced down into the magma, movement would begin once more.
If the asthenosphere beneath the plates cooled and solidified, the plates would no longer be able to move freely as they do now. This would likely result in decreased tectonic activity and potentially decrease in the movement of the plates over time.
Trenches form where plates are moving towards each other in a convergent plate boundary, not where they are moving apart. At divergent boundaries, such as mid-ocean ridges, plates are moving apart, creating new crust.
Moving of tectonic plates causes earthquakes, volcanic activity, and the formation of mountain ranges when plates collide or pull apart. These movements also contribute to the creation of ocean basins and continents over long periods of time.
Friction causes plates to stop moving temporarily. The motion of the magma under the plates will cause the plates to move again.
It will stop moving in 200 million years.
no
earth plates stop moving
The Almighty God.
They'd stop moving.
The lithosphere and sea floor spreading are both factors in the movement of tectonic plate movement. As there is no foreseeable reason for the currents to stop, there is also no foreseeable reason for all tectonic plate movement to stop.
Moving Gelatine Plates was created in 1968.
To stop your best friend from moving if you really want it that bad confront that bitch and stop him/her if u don't usually talk to each other just deal with it.
A soft collision between two plates could possibly stop the plates from moving for a time. But if subduction occurs, when one plate is forced down into the magma, movement would begin once more.
moving plates
No, both the continental and oceanic plates are always moving. Moving slowly, but always moving.