Subduction is a geological process in which one tectonic plate moves beneath another tectonic plate at a convergent boundary. This occurs when two tectonic plates collide, and the denser oceanic plate is forced underneath the less dense continental plate. Subduction zones are characterized by intense geological activity, including earthquakes, volcanic eruptions, and the formation of deep ocean trenches.
To gain a comprehensive understanding of subduction, consider the following study guide:
By thoroughly exploring these key concepts and engaging with the study guide, you can build a solid foundation of knowledge about subduction and its significance in the field of geology and plate tectonics.
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