1. An undersea earthquake causes the seabed to be displaced
2. A large volume of water is lifted, forming waves of great wavelength and low height of less than 1 metre
3. The waves travel towards land at high speeds around 800km/h
4. On approaching the coast, greater friction with the shallower seabed slows the waves down
5. The waves get closer together and increase in height. Waves can reach up to a height of 15m or more, travel at a speed of 30 - 50km/h and devastate shorelines the waves hit
6. Before a tsunami occurs, the sea may recede from the shore because the sea water fills in the void caused by displacement of the seabed