The collisions of plates occur at "convergent boundaries". Convergent boundaries include "subduction zones" (where one goes under the other) and "continental collisions".
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The exact name of where two plates collide is called a convergent bounday.
The Subduction zone
a convergent boundery
subduction zone
It is called a earthquake
convergence
When two plates collide one pushes the other one down. Then the magma goes through the gaps between the plates and then the volcano erupts. Volcanoes can also erupt by the plates spreading apart.
Mountains form where continental and oceanic plates collide by the actions of the plates upon one another. Often one plate pushes up and over the other one, and the upper one creates a row of mountains.
The more dense plate subducts (goes under) the less dense plate. For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
The reason alot of volacanoes are around the plate boundaries is because the plates are floating on magma. They float around and sometimes they collide(or hit) eachother, causing the parts that hit to rise and form mountains or folds on the surface. The magma underneath also goes up into the volcano.
The subduction zone.
subduction boundrary. thanks for looking :)
The plates in the earth collide and one goes under the other
Subduction.
convergence
Best Answer:When two plates carrying oceanic crust collide, the resultis that one goes underneath the other - probably causinga tsunami - or an underwater earthquake.
the contintinental plate goes below the other and lava floating from the center of the earth creates a ridge
When two plates collide one pushes the other one down. Then the magma goes through the gaps between the plates and then the volcano erupts. Volcanoes can also erupt by the plates spreading apart.
Mountains form where continental and oceanic plates collide by the actions of the plates upon one another. Often one plate pushes up and over the other one, and the upper one creates a row of mountains.
Two tectonic plates collide, one goes under and the other goes over. Usually this forms an earthquake and is how most mountains are formed eg: the great dividing range. :D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D:D
The more dense plate subducts (goes under) the less dense plate. For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
When two plates collide directly (versus sliding along each other) they typically form a mountain range. For example, the Himalayan Mountains are are formed by the collision of the Eurasian Plate and the Indo-Australian Plate. As John McPhee says in "Annals of the Former World", the most amazing thing is that the summit of Mount Everest, the worlds tallest mountain, is marine limestone.