Intro to Geology
Benioff zones are areas of seismic activity that occur in subduction zones where one tectonic plate is being forced beneath another. They are characterized by the inclined plane of earthquakes that forms at the interface between the descending plate and the overlying plate, indicating the depth and angle of the subduction process. This concept is essential in understanding how tectonic plates interact and has contributed significantly to the development of plate tectonic theory.
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