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The age of the subducted rock is generally inversely related to the depth of the trench. Older oceanic crust, which is denser and cooler, tends to be subducted at greater depths, leading to deeper trenches. In contrast, younger oceanic crust is less dense and typically leads to shallower subduction zones. This relationship is a key factor in understanding the dynamics of plate tectonics and the formation of oceanic trenches.

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