Plate Boundaries
In space and astronautical engineering, plate boundaries refer to the regions where two or more tectonic plates meet. These boundaries are characterized by intense geological activity, including earthquakes, volcanic eruptions, and the formation of mountains. There are three main types of plate boundaries: divergent, convergent, and transform. Divergent boundaries occur where plates move away from each other, creating new crust and causing seafloor spreading. Convergent boundaries occur where plates collide, resulting in subduction zones, mountain building, and volcanic activity. Transform boundaries occur where plates slide past each other, causing earthquakes and faulting. The study of plate boundaries is important for understanding the dynamics of the Earth's crust and for predicting natural disasters such as earthquakes and volcanic eruptions.
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