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January 21, 2010

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There are three main types of fault that may cause an earthquake: normal, reverse(thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other ; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.

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i like this part of the post:"Residents of the capital city of more than two million cried and prayed, their hands bloody from digging through rubble as they searched for loved ones. Bodies, some partially charred, lay beside roads. Hungry and thirsty, crowds massed at the airport gate hoping for some of the food, water and medical supplies coming in on transport planes." is very good

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I frankly hope that not repeat disaster from previous hurricanes.

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