A tsunami is a series of ocean waves with very long wavelengths (typically hundreds of kilometers) caused by large-scale disturbances of the ocean, such as earthquakes, volcanic eruptions, or underwater landslides. Tsunamis can travel across entire ocean basins, and when they reach shallow coastal waters, they can grow in height and cause widespread destruction.
Tsunamis can be caused by a variety of natural events, including:
When a tsunami is generated, it forms a series of waves that travel outward in all directions from the source area. These waves can travel at speeds of up to 500-600 miles per hour in deep ocean water, but their amplitudes (heights) are often less than a meter, making them difficult to detect in deep water.
As the waves approach shallow coastal areas, the water gets shallower, causing the waves to slow down and increase in height. This can result in devastating waves that inundate coastlines and cause widespread damage to coastal communities.
When studying tsunamis, it's important to understand the following key points:
By understanding the science behind tsunamis and their potential impact, we can better prepare for and respond to these natural hazards.
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