#tsunami #naturaldisaster #tectonicplate a tsunami is a series of large ocean waves caused by disturbances such as underwater earthquakes, volcanic eruptions, landslides, or even asteroid impacts. These waves can travel at high speeds across the ocean and cause devastating flooding when they reach coastal areas.

Underwater Earthquake: Most tsunamis are caused by subduction zone earthquakes, where one tectonic plate is forced under another, suddenly displacing a large volume of water.
Volcanic Eruptions: Explosive eruptions or the collapse of a volcano into the ocean can displace water and generate a tsunami.
Landslides: Large landslides, either from coastal cliffs or underwater slopes, can push water and trigger a tsunami.
Asteroid Impact: Though rare, a large asteroid hitting the ocean could create massive waves.
The displaced water forms a series of waves that spread outward from the source in all directions.
These waves travel at high speeds (up to 800 km/h or 500 mph) in deep water but are barely noticeable because they have long wavelengths and low heights.
When the tsunami reaches land, it can cause massive flooding, destroy buildings, and lead to loss of life.
Tsunamis can come in multiple waves, and the first wave is not always the largest.


Tsunami waves vs normal waves

சுனாமி உருவாக காரணம் இதுதான் | How Tsunami are Formed | Tsunami Explained in Tamil | Sunami Wave

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