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, and underwater landslides. These waves can travel across entire ocean basins and cause widespread destruction when they reach the coast.
Tsunamis are commonly caused by:
When a tsunami is generated, it propagates outward from its source in the form of a series of waves. These waves can travel at speeds of up to 500-600 miles per hour in deep ocean water, but their amplitudes (heights) are usually small. As the tsunami waves approach shallow coastal areas, their energy is compressed, causing the waves to grow in height and become more destructive.
Tsunamis can cause devastating impacts on coastal communities, leading to loss of life, destruction of infrastructure, and environmental damage. The most destructive effects of tsunamis are usually felt near the coast, where the waves can inundate low-lying areas and cause widespread flooding.
To understand tsunamis in more detail, it is important to study the following topics: