Tsunami are a series of long and wide ocean waves (like a ripple effect), caused by large-scale disturbances of the ocean, such as earthquakes, landslide, volcanic eruptions, explosions, or meteorites.
Tsunami waves travel fast across oceans, generally with little impact. It is when these waves approach shallow and coastal areas they slow down and increase in height. Being wide and long series of waves, there is a large volume of water behind each wave. Unlike normal ocean waves, which roll and break quickly, tsunami waves can roll onto shore and continue inland, for long periods of time. Sometimes it is not the first tsunami wave which is the largest. The ripple effect of tsunami waves impacting coastal areas can often be exaggerated in areas like harbours, where these ripples can bounce around in more closed water areas linked to the ocean.
Tsunamis can be classified as either local, regional, or distant, depending on the distance of generation from the coastline.