The most common cause of a tsunami is a large earthquake below or near the ocean floor. Landslides, volcanic activity, weather, and asteroids can also generate tsunami.
Not all earthquakes generate tsunami. Whether an earthquake generates a tsunami depends on its location, size, and depth. In general, earthquakes that generate tsunami:
- Occur under or very near the ocean
- Have magnitudes over 7.0
- Are less than 62 miles below Earth’s surface.
An earthquake may cause the ocean floor to suddenly rise or fall. This sudden vertical movement of the ocean floor is what typically sets a tsunami in motion.
Tsunami can also occur when a landslide displaces ocean water. A landslide-generated tsunami may be larger than a tsunami generated by an earthquake and can affect nearby coasts within minutes. These tsunami usually lose energy quickly and rarely travel great distances.