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The mechanics behind the devastating 7.0-magnitude earthquake that rocked Haiti in 2010.

This clip comes from "Deadly Disasters," Season 01, Episode 01: Earthquakes.

About "Deadly Disasters:"
Explore some of the most terrifying, destructive natural disasters to ever strike the planet. With jaw-dropping footage and expert insight, uncover fascinating new details about these deadly disasters.

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Transcript
00:00Just before five o'clock in the evening, on the 12th of January 2010,
00:06Haiti was suddenly rocked by a magnitude 7 earthquake.
00:21It was the most powerful earthquake to hit the area in more than 200 years.
00:26Basically earthquakes are the result of the movement of the earth's plates.
00:32The plates move because of the internal heat of the earth which moves them around and the plate
00:38boundaries where the plates meet each other, that's where you can generate earthquakes because
00:43you've got giant fractures in the earth's crust. Those are moving very slowly, they're only moving
00:48about the same rate as your fingernails grow, which is from millimeters to centimeters per year,
00:53but eventually the stress is so high that it overcomes the friction and then the fault moves
00:58very rapidly, a couple of meters per second, and that will then generate earthquakes which
01:04travel as waves through the solid part of the earth.
01:14The epicenter of this cataclysmic event was below the city of Leogane,
01:19about 25 kilometers from the capital Port-au-Prince. The earthquake was unusually near the surface,
01:26occurring at a depth of only 13 kilometers. This dramatically increased the level of shaking above.
01:34Port-au-Prince in Haiti is very close to plate boundary of what's called the Ganave microplate,
01:41and that southern boundary stretches all the way from Jamaica, in fact it goes all the way through
01:46the center of Jamaica and then goes all along the southern peninsula of Haiti and passes very
01:53close to Port-au-Prince. Shocks quickly spread throughout Haiti and the neighboring Dominican
01:59Republic, as well as to parts of the nearby Caribbean islands of Cuba, Jamaica and Puerto Rico.
02:06Roughly three million people were affected by intense shaking that was strong enough to cause damage to buildings.
02:23The closer they were to the epicenter, the more destruction occurred around them.
02:36you

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