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Convergent plate bondary

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Economic loss: 360 billion USD

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360

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15896 deaths
6157 injured
2537 people missing

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15896

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There are compressional force produce by convergent plate boundary.
Earthquakes are usually caused when rock underground suddenly breaks along a fault. This sudden release of energy causes the seismic waves that make the ground shake. When two blocks of rock or two plates are rubbing against each other, they stick a little. They don't just slide smoothly; the rocks catch on each other. The rocks are still pushing against each other, but not moving. After a while, the rocks break because of all the pressure that's built up. When the rocks break, the earthquake occurs. During the earthquake and afterward, the plates or blocks of rock start moving, and they continue to move until they get stuck again. The spot underground where the rock breaks is called the focus of the earthquake. The place right above the focus (on top of the ground) is called the epicenter of the earthquake.

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Haiti sits above two tectonic plates, the Caribbean plate and the North American plate. These plates are rigid parts of the Earth’s crust that slide separately on the planet’s molten core. They were sliding past each other. When the two jagged edges catch, they hold at first. The mounting pressure eventually forces them to grind past each other. That’s what causes an earthquake.

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Transform plate boundary

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2011 Tohoku Tsunami

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The Caribbean Plate & the North American Plate

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2018 Osaka Earthquake

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Mount Merapi in Indonesia

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Molten lava burn houses

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Magma produced rises up to the earth's surface through vents

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In the middle of Pacific Plate

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Type of plate boundaries or Distribution

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Type of plate boundaries or Distribution

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A series of big sea waves

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Lava, hot rock debris, ashes and gases are ejected or emitted from an opening in the earth's surface

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Sudden shaking of the land