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. These waves can travel across entire ocean basins and cause widespread destruction when they reach coastal areas.
When a tsunami is generated, it produces a series of waves that can travel at high speeds across the ocean, sometimes reaching speeds of over 500 miles per hour (800 kilometers per hour). These waves can have wavelengths of up to 200 kilometers and may appear as a rapidly advancing wall of water when they approach shallow coastal areas.
When a tsunami reaches the coast, it can cause devastating flooding and widespread destruction of coastal communities, infrastructure, and ecosystems. The force of the waves can erode shorelines, demolish buildings, and cause loss of life and property.
To better understand tsunamis, consider the following study guide:
By studying these aspects of tsunamis, you can gain a comprehensive understanding of this natural hazard and its implications for coastal regions.
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