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How they are formed

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There are all kinds of fault lines and here are a couple

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There are all kinds of fault lines and here are a couple

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Two things. One make sure that whatever you put on your page deals with how earthquakes are formed and two that everything is in your own words. 

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Two things. One make sure that whatever you put on your page deals with how earthquakes are formed and two that everything is in your own words. 

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USGS Earthquake Hazards Program, responsible for monitoring, reporting, and researching earthquakes and earthquake hazards

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Before and After a desistating earthquake

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Before and After a desistating earthquake

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Fault- a crack in Earths crust

Epicenter-the point on the Earth's surface directly above the focus of an earthquake

Focus- the center of intensity

Transform Boundary- when two tectonic plates slide along each others

S Wave- the secondary wave

P Wave-first wave to arrive at the seismograph

After Shock-a smaller earthquake following the main shock of a large earthquake

Richtor Scale- which defines magnitude as the logarithm of the ratio of the amplitude of the seismic waves to an arbitrary, minor amplitude

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Some people don't know what to do during an earthquake so here are some quick to do and not to do.

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Some people don't know what to do during an earthquake so here are some quick to do and not to do.

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The plate boundaries are made up of many faults, and most of the earthquakes around the world occur on these faults. Since the edges of the plates are rough, they get stuck while the rest of the plate keeps moving. Finally, when the plate has moved far enough, the edges unstick on one of the faults and there is an earthquake.

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An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter.