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In this video, we explain how tectonic plates and underwater earthquakes causes tsunami. Deep beneath the ocean waves, powerful forces are always at work. Today, we are going on an underwater adventure to discover how tsunami really begins!. Beneath the ocean floor, massive pieces of earth called tectonic plates are always moving. sometimes they bump, slide or push under each other. This slow movement builds pressure. When the pressure becomes too much. Snap. The seafloor suddenly shifts. This causes a powerful undersea earthquake. And that moment can set a tsunami in motion. When the ocean floor jumps. It pushes a huge mass of water above it. That water has to go somewhere - and it spreads out in all directions. Fun fact: a tsunami can travel as fast as a jet, that's over 800 kilometer an hour! but the waves are so long and low that ships might not even feel them. As the tsunami reaches shallow waters near the coast, something dramatic happens. The bottom of the wave slows down. But the top keeps going. The waves grows taller and taller like it's standing up. One of the first warning signs is the drop back. The water suddenly pulls away from the shore, leaving the beach strangely dry. If you ever seen this - run to high ground immediately!. Fun fact: Tsunamis aren't just one wave. They often come in a series, each one powerful. When the waves finally reach land, it crashes forward with incredible force. That's why many countries have warning systems, evacuation plans and ocean sensors to detect tsunami early so we can stay safe. So let's recap!. Tsunamis are caused when the ocean floor suddenly moves - usually from an underwater earthquake. That movement pushes water into giant waves that can travel across entire oceans. And when they reach the coast... They can become huge. But with science and early mornings, we can protect people and save lives. The ocean is powerful but knowledge is stronger!.