Q:

What is the place where two plates move together?

A:

Quick Answer

Areas where tectonic plates make contact with each other are known as convergent boundaries. Collisions between two plates are very slow, with movement of only a few centimeters per year occurring at the convergent boundaries.

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Full Answer

There are many types of plate boundaries depending on the density and type of plate involved. Continental and oceanic plates that meet at a convergent boundary form a subduction zone, with the heavier oceanic plate forced under the less dense continental plate. Mountains, earthquakes and volcanoes are formed by the movement of tectonic plates and are often found close to the convergent boundaries where plates meet.

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Related Questions

  • Q:

    What happens at a transform boundary?

    A:

    Tectonic plates move horizontally past one another at transform boundaries in either strike-slip or aseismic motions. Earthquakes and tsunamis occur when the pressure locking plates in a strike-slip boundary releases suddenly. Volcanic activity, while common at convergent and divergent plate boundaries, is rare at transform borders.

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  • Q:

    What are the three types of plate boundaries?

    A:

    There are three types of plate boundaries: convergent, when tectonic plates come together; divergent, when tectonic plates are moving away from each other; and transform, when two plates are sliding past one another. Each boundary serves a different purpose, and mountains are also the result of activity on these boundaries.

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  • Q:

    What happens at plate boundaries?

    A:

    Three major events take place at plate boundaries: the formation of volcanoes and mountains, and a greater occurrence of earthquakes. There are also three main types of plate boundaries: divergent, convergent and transform.

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  • Q:

    How does the movement of tectonic plates cause earthquakes?

    A:

    The movement of tectonic plates causes earthquakes when two plates that are in contact with each other move in opposite directions and release built-up stress. For example, one plate may move north, while the other may move south. Stress can build up to a significant amount while the plates are held stationary, but trying to move, which can then be released as an earthquake.

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