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Just as the front ends of cars fold and bend in a collision, so do the "front ends" of colliding plates. The edge of the continental plate in the drawing has folded into a huge mountain range, while the edge of the oceanic plate has bent downward and dug deep into the Earth. A trench has formed at the bend. All that folding and bending makes rock in both plates break and slip

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Where a divergent boundary crosses the land, the rift valleys which form are typically 30 to 50 kilometers wide.

Ex: the East Africa rift in Kenya and Ethiopia, and the Rio Grande rift in New Mexico.

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the San Andrea fault the strongest and most famous earthquake hit San Francisco in 1906. Many buildings were shaken to pieces by the quake, and much of the rest of the city was destroyed by the fires that followed.

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I picked Brentwood, California to live and in the city of bentwood an earthquake occurred.It had a magnitude of

2.6 which means I would be able to feel the earthqake.

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M2.8 - 21km

-measured with the Richter scale

-no afterschocks or damages

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-1960 San Francisco

-Haiti 2010

-1923 Tokyo

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at least 52 after measuring 4.5 or greater had been recorded.e government of Haiti estimated that 250,000 residence and 30,000  had collapsed or were severely damaged

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Has a magnitude 7.9.Brought extreme destruction in the Tokyo-Yokohama area, both from the temblor and subsequent firestorms.

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The San Andreas Fault is a continental transform fault.The plates slide past one another.

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Is a smaller earthquake that occurs after a previous large earthquake,

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Straight through the surface and first to reach the seismograph

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This is the wave that second to reach the seismograph.Moves through the bodys

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This the scale that measures a earthquake magnitude

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cause earthquakes with it sliding of the plates.

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This is where the explosion starts.

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It where the earthquake beings and the ground erupts at this part.

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Transform boundary

epicenter

focus

Richter scale

fault
S-wave P-wave
Aftershock Epicenter

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1. 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.