Lemezszubdukció
Lemezszubdukció is a Hungarian term that translates to "plate subduction" in English. It refers to the geological process where one tectonic plate slides beneath another and sinks into the Earth's mantle. This phenomenon is a fundamental aspect of plate tectonics, the scientific theory that describes the large-scale motion of Earth's lithosphere.
Subduction occurs at convergent plate boundaries, where two plates collide. Typically, denser oceanic crust will subduct
The process of subduction is responsible for many of Earth's most dramatic geological events, including earthquakes