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a volcanoe! hope you found this helpfull! :)
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.
They are geologic features because when the crustal plates move its makes cracks on earth the the mountains are one because everytime the crustal plates move it breaks the earths surface and the dirt and rocks start gathering together
When two oceanic plates collide, one may be pushed under the other and cause magma from the mantle to rise, forming a volcanoe or volcanoes. When two continential plates collide at a reverse fault tectonic earthquakes occur.
A subduction zone, that includes a ocean trench. This is only possible if one of the plates are oceanic, because if two continental plates collide a mountain range is formed.
yes
collide
mountain
tectonic movement can cause tectonic plates to collide, drift apart, or slide across one another
Tectonic plates can cause harm, when they collide with, plunge under one another etc. This is a cause of earthquakes
When the two plates collide, they fold. causing both plates to move upwards trying to get around one another. Over time when the plates move upwards, mountains form. This is exactly how Everest was formed.
When the two plates collide, they fold. causing both plates to move upwards trying to get around one another. Over time when the plates move upwards, mountains form. This is exactly how Everest was formed.
Continents are basically floating on their own tectonic plates. They collide into one another, separate from one another, etc. So if they separate, the plates are basically moving in opposing directions.
I am going to make this easy. The answer is DIVIDE!
They can slide past each other, they can collide, or they can pull apart.
a volcanoe! hope you found this helpfull! :)
A convergent boundary is one where two plates are grinding into each other, so the plates are moving toward each other. If one plate more dense than the other, (say a continent and an oceanic plate collide) then the denser plate (the oceanic plate) may be subducted. If two plates of similar or the same density collide, then neither plate will subduct, and crustal thickening may occur. This is the process which formed the Himalayas, resulting from the pressure of two continental plates, the Indian and the Asian.