Earth Systems Science
An oceanic trench is a deep, narrow depression in the ocean floor that forms where one tectonic plate is being subducted beneath another. These trenches are typically associated with convergent plate boundaries and play a critical role in the recycling of the Earth's crust, influencing seafloor spreading and the evolution of ocean basins. They are often the deepest parts of the ocean and are characterized by their steep sides and unique geological features.
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