A tsunami is a very large, powerful wave (or set of waves) that can race across the whole ocean and crash onto land.
It is not made by wind like normal beach waves.
Something has to push a huge amount of seawater all at once. Let's find out what! 🔎
Tap Next to begin your adventure.
Earth's surface is made of giant slabs of rock called tectonic plates. They fit together like puzzle pieces — and they slowly push against each other under the sea.
The plates get stuck and squeeze, building up energy — like bending a ruler more and more. 🔧
When the stuck plates suddenly slip, the seafloor jolts up. That sudden jump is an earthquake under the ocean — the most common cause of a tsunami.
When the seafloor jumps up, it shoves the water above it upward too. This makes a giant bulge of water on the ocean surface. 💧
Drag the slider to push the seafloor up and watch the water rise.
That bulge of water can't stay still — it spreads out in all directions as fast as a jet plane. ✈️ In deep water the wave is low, so ships barely feel it.
Speed in deep water can be over 700 km/h — about as fast as a plane!
As the wave reaches shallow water near the coast, it slows down and the water piles up — so the wave grows much taller before it hits land.
Quick check — why does the wave get taller near the beach?
You learned the 4 steps! Drag the cards into the right order — from first to last. 🧩
If you are ever at a beach, these clues can warn you a tsunami may be coming. Tap each card to reveal what to do. 🛟
Here's the whole story in 4 steps:
Great job learning how tsunamis form. Stay curious and stay safe! 🌟