a trench is develop due to the sliding of the plates
subduction
earthquake
Destructive/convergent
Mount Vesuvius is the result of a subduction zone, where one tectonic plate slides under another. In this case the portion of the African Plate that is under the Mediterranean is sliding under the Eurasian Plate. This generates magma tha allows volcanoes to form.
it formed by one plate sliding under another
The 2004 and 2011 tsunamis were the result of something called megathrust earthquakes. Off the coasts of Sumatra and Japan, where the tsunamis originated, there are subduction zones, places where one tectonic plate pushes into and slides under another. For the 2004 tsunami it was the Indian Plate sliding under the Eurasian Plate. For the 2011 tsunami it was the Pacific Plate sliding under the Okhotsk Plate. As this happens the plates become snagged on one another and distort under the force of it, building up tension over the course of a few hundred years. Eventually the plates snap back into place, triggering a major earthquake. This results in part of one plate being thrust upward, displacing an enormous column of water and creating a tsunami.
it has transform boundary
It is where one plate slides past another plate, rubbing against it. One slides right, the other left. An example would be North America. Your Welcome.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
A transformed plate margin is the plate that slides past each other
collision
An earthquake or tremmor may happen if the slide is strong enough.
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This happens at a plate boundary. The oceanic plate subducts (sinks) under the continental plate, because it is heavier. (the oceanic plate is made of basalt and the continental plate is made of granite.) This happens at a destructive plate margin. it is called this because part if the oceanic plate is destroyed, because it melts as it sinks.
one plate of earth crust sliding under another plate
are stuff and the front edge of the left plate is sliding under the front edge of the right plate as the left plate slides down into the earth, it enters the hot mante
Mountains and earth quakes.
Where a tectonic plate slides past another.