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The 2010 Haiti earthquake caused complete and total devastation of communication systems—including destroying the control tower of the Toussaint Louverture International Airport, and the main seaports.

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.

Watch "Deadly Disasters" Tuesdays and Tuesdays on EarthX.

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Transcript
00:00What is the definition of a disaster for professionals like myself?
00:06It is an event that is of such magnitude
00:09that the local or the national government cannot face it alone.
00:14Efforts to get food, medical aid and water to the survivors
00:18were hindered by the breakdown in communication systems.
00:30Although the runways at the Toussaint Louverture International Airport were intact,
00:35damage to the control tower meant that planes couldn't take off or land safely.
00:42At the main seaport, piers had collapsed and cranes had been knocked over,
00:47so ships were not able to unload urgently needed supplies.
00:51Almost all paved roads were blocked due to severe surface damage,
00:55fallen trees and debris from collapsed buildings.
01:01In the hours following the quake, survivors dug through rubble,
01:05often with their bare hands, to rescue family and friends.
01:12Dusk fell just two hours after the earthquake.
01:16In the eerie darkness, rescuers had to use flashlights
01:20as they continued to claw at the rubble, trying to reach those trapped beneath.
01:25Everywhere is dark.
01:26She's just like an incredible bright star in the middle of this, you know, darkness
01:30and it's a wonderful feeling.
01:34That night, many people in Haiti were forced to sleep on the streets,
01:38either because their homes had been destroyed
01:41or because they were terrified of aftershocks.
01:45When a fault moves and causes an earthquake,
01:47it changes the distribution of the stresses around the fault.
01:51So aftershocks are generated, they're usually smaller than the main shock,
01:56but there have been cases where they're almost as large as the main shock.

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