Q:

Where does subduction take place?

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Quick Answer

Subduction is a geological process that takes place at the boundaries between tectonic plates in which one plate is forced underneath another. Subduction occurs when the massive pressures of entire continental or oceanic tectonic plates collide, over the course of millennia, and one slowly is subsumed underneath the other.

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Full Answer

Subduction often results in spectacular natural geographic phenomena. Geological subduction is exemplified by the Himalayan Mountains, the earthquakes of the American Pacific coast and the volcanic activity that gave rise to the island of Japan. Subduction is one of the most immense physical processes on Earth, shaping the face of the Earth itself.

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Related Questions

  • Q:

    What are the boundaries of the lithospheric plate?

    A:

    Three types of boundaries, divergent, convergent and transform fault boundaries, occur in the lithosphere plate. As the plates diverge or pull apart from each other and converge or come together, tremendous amounts of energy are released, resulting in the transformation of the Earth's surface.

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  • Q:

    What kinds of plate boundaries are there?

    A:

    The three types of plate boundaries are divergent plate boundaries, convergent plate boundaries and transform plate boundaries. Divergent plate boundaries occur in places where two plates are moving away from each other. When two plates are being forced together, they are called convergent plate boundaries. Finally, transform plate boundaries occur in places where two plates are moving in opposite directions and rubbing against each other.

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  • Q:

    What is the place where two plates move together?

    A:

    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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  • Q:

    What happens at a divergent boundary?

    A:

    At divergent boundaries, the Earth's tectonic plates pull apart from each other. This contrasts with convergent boundaries, where the plates are colliding, or converging, with each other. Divergent boundaries exist both on the ocean floor and on land.

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