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They move because of the heat in the earth's core that makes molten rock in the mantle to move. It moves in a pattern called a convection cell that gets made when warm stuff rises, cools and then sinks down. They cause volcanoes.

Oceanic and Continental crusts are some examples of some plates at their boundary.

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A destructive plate boundary is sometimes called a convergent or tensional plate margin.

A destructive plate boundary happens where an oceanic and continental plate move towards each other.

A destructive plate boundary is sometimes called a convergent or tensional plate margin.

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A destructive plate boundary is sometimes called a convergent or tensional plate margin. This occurs when oceanic and continental plates move together

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destructive plate

this is what happens when oceanic and continental plates crash together. The oceanic plate is forced under the lighter continental plate. Friction causes the destruction of the oceanic plate and may trigger earthquakes.

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An example of a destructive plate boundary is where the Nazca plate is forced under the South American Plate.

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The Destructive plate happens the oceanic plate and the continental plate move together and friction is caused when they move and  this can cause earthquakes. Magma rises up through the cracks and erupts to the surface. An example of this is when the Nazca plate is forced under the South American plate. Collision zones form when two continental plates collide, neither plate is forced under the other and both are forced up and create fold mountains.

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A destructive plate boundary is caused when and oceanic and Continental plate move towards each other. The oceanic plate is more dense than the continental plate.
The destructive plate boundary can cause earthquakes, when friction makes the oceanic plate melt it can, cause earthquakes.

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A destructive plate boundary happens where an oceanic and continental plate move towards each other. Destructive plate boundaries can cause earthquakes and other natural hazards.

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A destructive boundary is also known as convergent.This happens when oceanic and continental plates collide. The oceanic plate is forced underneath the lighter continental plate. Friction melts the oceanic plate causing earthquakes. Volcanoes can also be formed as magma rises through the cracks and erupts. The Nazca plate is forced under the South American Plate

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The oceanic plate goes under the lighter continental plate. Friction causes melting of the oceanic plate and may trigger earthquakes.

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A destructive plate boundary happens when the more dense  Oceanic plate is forced under the Continental plate. Examples of this include the Pacific, Nazca, Eurasian and South American plates