The uplift is so slow that the stream will usually eventually cut down into the uplifted area to resume its course.
Convection currents (the movement of magma beneath the plates)
This kind of boundary is mountainous.
There is land beneath the oceans, tectonic plate boundaries separate land masses.
the tectonic plates start to collide which causes shearing, so the epicenter is forces to move farther down the path of the fault.
Frequency of Earth Quake depends on the formation /thickness/ fault / movements of tectonic plates beneath the earth's surface in that region. It varies from place to place.
subduction, which is when one tectonic plate is pushed down beneath another tectonic plate.
The tectonic plates, part of the lithosphere, move around and float on the top of the asthenosphere.
The asthenosphere lies beneath the lithosphere, which is where the tectonic plates lie. Because of the high temperature, the asthenosphere has the property to flow (plasticity); the tectonic plates "float" on this flow.
The subduction of the Nazca plate beneath the South America plate.
Convection currents (the movement of magma beneath the plates)
Due to the tectonic plates beneath the ocean moving and creating magma.
Santorini is on the Eurasian Plate near where the African Plate subducts beneath it.
This kind of boundary is mountainous.
When tectonic plates move and grind against each other, this is an earthquake. If the moving of tectonic plates were to occur beneath the ocean's surface, the result would be a tsunami.
The answer is tectonic plates floating on the lithosphere. Does that answer your question? LOL :)
subduction, which is when one tectonic plate is pushed down beneath another tectonic plate.
The tectonic plates beneath the earth's crust are shifting away or towards each other.