1) Earthquakes regularly occur at plate boundaries in the oceans, such as at subduction zones where one tectonic plate slides under another.
2) Major earthquakes can generate destructive tsunamis by displacing large volumes of water very quickly. These tsunami waves travel across the ocean and grow in height as they reach shorelines.
3) Studying areas like the Nankai Trough off Japan, where great earthquakes repeatedly occur, can provide insights into why and how these quakes happen, and help determine areas at risk for future seismic events.