Seismology
In the context of subduction zone seismology, trenches are deep, narrow depressions in the ocean floor formed where one tectonic plate is being forced beneath another. These geological features are significant as they indicate the locations where intense seismic activity occurs, due to the movement of plates interacting at convergent boundaries. The presence of trenches provides insights into the dynamics of plate tectonics and the associated risks of earthquakes and tsunamis in nearby regions.
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