A deep-sea trench is a narrow, elongated depression in the ocean floor that reaches extreme depths, often formed at convergent plate boundaries where one tectonic plate is forced beneath another. These trenches are some of the deepest parts of the Earth's oceans and play a significant role in the recycling of materials between the Earth's surface and its interior. They are associated with intense geological activity, including earthquakes and volcanic activity, highlighting their importance in understanding plate tectonics and the dynamic processes shaping our planet.
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