Want this question answered?
material from the Earth's surface is returned to the interior.
In a subduction zone an oceanic plate slides under a continental plate or another oceanic plate. The subduction plate introduces water into the mantle, lowering melting temperatures and generating magma. This causes volcanoes, usually stratovolcanoes, to form on the overriding plate. If the overriding plate is continental a mountain range may develop.
When one plate slides beneath another it is said to subduct. This is called a subduction zone. However, a continental plate cannot subduct, only an oceanic plate can. When two continental plates collide the land between them is squeezed horizontally, forming mountain ranges. Eventually the continental land masses will fuse together.
NO that would mean we are making heaps of tetonic plates although this scenario can cause an earthquake and for rocks to slide under or above the plates and the mantle
Earthquakes
material from the Earth's surface is returned to the interior.
Unlike deep sea trenches which are found in areas where one tectonic plate slides beneath another undersea canyons are found along the slopes of most continental margins the submarine canyons for example tend to have steeper side slopes much higher gradients and considerably narrower floors. thats how they different
In a subduction zone an oceanic plate slides under a continental plate or another oceanic plate. The subduction plate introduces water into the mantle, lowering melting temperatures and generating magma. This causes volcanoes, usually stratovolcanoes, to form on the overriding plate. If the overriding plate is continental a mountain range may develop.
When one plate slides beneath another it is said to subduct. This is called a subduction zone. However, a continental plate cannot subduct, only an oceanic plate can. When two continental plates collide the land between them is squeezed horizontally, forming mountain ranges. Eventually the continental land masses will fuse together.
Unlike deep sea trenches which are found in areas where one tectonic plate slides beneath another undersea canyons are found along the slopes of most continental margins the submarine canyons for example tend to have steeper side slopes much higher gradients and considerably narrower floors. thats how they different
Deep ocean trenches can be formed by undersea earthquakes, land-slides, but also by the movement along the edges of tectonic plates.
the oceanic plate is less bouyant so it slides under the continental plate
When oceanic plates slide under continental plates they form subduction zones. Subduction zones always occur at convergent boundaries where one plate slides beneath another plate.
Tsunami and/or Earthquake. I'm not 100% about some of the other stuff.
A subduction zone is formed.
The movement of one tectonic plate under another occurs at convergent boundaries. For example, at this boundary denser oceanic crust slides under the lighter continental crust.
Word doesn't have slides of its own. You can copy slides from another program, such as Powerpoint or Impress, and paste them into Word.