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Tsunami
When large earthquake, landslide, or volcanic eruption happens under the ocean a tsunami wave can be made. Tsunami waves usually come from a long distance away, thousands of miles. The wave starts out very small, but grows to huge heights as it comes near land. Tsunami waves a very powerful and can cause a lot of damage to the land.
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Surface Faulting

A surface fault is a crack in the crust that reaches the surface of the Earth. It happens when an earthquake occurs just under the surface and if the epicenter is less than 20 kilometers.
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Ground Shaking

Waves of energy that are released during an earthquake causes the land to make waves like water does. Ground shaking happens when a fault moves suddenly. The waves travel across the surface of the earth and through the earth under the surface too.

Landslide
USGS image A landslide happens when land on a slope is weakened by an earthquake or heavy rain. The land along the slope slides down to the land below it.
Liquifaction

When the ground is full of water it becomes weak and acts like a fluid. Sand near the seashore is a good example of this. Shaking ground can make water from under the ground saturate the ground above it. The dirt becomes more like a sediment and can drain away.

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Tectonic Deformation
The Earth's crust sits on top of tectonic plates. Millions of years ago the tectonic plates were in a different position and the continents were too. When the continental plates move or change it is called tectonic deformation.
Seiches

If you have ever sloshed a bowl of water, then you understand what a seiche is. When you move a bowl back and forth the water spills out. The same think happens to lakes when the earth shakes back and forth during an earthquake. The water goes side-to-side and some of the water spills out onto the land.

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