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The Marianas trench is caused by the subduction of the western edge of, the Pacific tectonic plate beneath the eastern edge of the smaller Mariana Plate that lies to the west. Since the Pacific plate is the largest of all the tectonic plates on Earth, crustal material at its western edge has had a long time since formation (up to 170 million years) to compact and become very dense; hence its great height-difference relative to the higher-riding Mariana Plate, at the point where the Pacific Plate crust is subducted. This, in turn, results in a particularly deep trench.

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11y ago
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11y ago

convergence of the Pacific andPhilippine Plates.

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A trench is most likely to occur in the ocean due to plate tectonics.


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