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Diamond Gift Ulta - It was Boxing Day 2004, and thousands of European and American tourists had flocked to the beaches of Thailand, Sri Lanka and Indonesia to escape the winter cold in a tropical paradise. At 7.59am, a magnitude 9.1 earthquake - one of the strongest on record - tore through an undersea fault in the Indian Ocean, sending a huge column of water towards unsuspecting shores.

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The Boxing Day tsunami would be the deadliest in history, killing an incredible 230,000 people in a matter of hours. The town of Banda Aceh, on the northern tip of Sumatra, was closest to the epicenter of the powerful quake, and the first waves hit in just 20 minutes.

It's almost impossible to imagine the 30-meter-high mountain of water that engulfed the coastal city of 320,000 people, instantly killing more than 100,000 men, women and children. Buildings, trees and automobiles bent like houses of cards were swept away by the oil-black rapids, and virtually none survived the deluge.

The next stop was Thailand. With waves rolling through the Indian Ocean at 800 km/h, the tsunami hit the coastal provinces of Phang Nga and Phuket an hour and a half later. Despite the time lapse, locals and tourists were completely unaware of the impending destruction.

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Curious beach-goers even strolled between the oddly receding waves, only to be chased by a churning wall of water. The death toll in Thailand stands at nearly 5,400, including 2,000 foreign tourists. An hour later, across the Indian Ocean, waves hit India's southeast coast near the city of Chennai, pushing miles of debris-choked water inland

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land and killing more than 10,000 people, mostly women and children, since the men were out fishing. But some of the worst devastation was reserved for the island nation of Sri Lanka, where more than 30,000 people were swept away by the waves and hundreds of thousands were left homeless.

A testament to the tsunami's record strength, the last victims of the Boxing Day disaster died nearly eight hours later as swollen seas and rogue waves stunned swimmers in South Africa, 5,000 miles from the epicenter of the earthquake. Vasily Titov is a tsunami researcher and forecaster at the National Oceanic and Atmospheric Administration Center for Tsunami Research.

He attributes the relentless destructiveness of the 2004 Indian Ocean tsunami to the sheer force of the earthquake that produced it. The quake originated in a so-called mega-thrust fault, in which heavy oceanic plates were submerged beneath lighter continental plates. “These are the biggest faults in the world and they are all under water,” says Titov.

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The 2004 earthquake ruptured a 900-mile stretch along the Indian and Australian plates 31 miles below the seafloor. Instead of causing a violent jolt, the quake lasted 10 minutes unabated and released as much pent-up energy as several thousand nuclear bombs. America The Story of Us is an epic 12-hour television event that tells the extraordinary story of America's invention.

In the process, massive segments of the seafloor were pushed up about 30 or 40 meters (up to 130 feet). The effect was like the world's largest rock falling into the Indian Ocean, with mountain-sized waves spreading in all directions. Titov points out that tsunamis are not like the giant surf waves that many of us imagine.

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It's a wave, but from the observer's perspective, you wouldn't recognize it as a wave," says Titov. "It's more like the ocean turning into a river of living water and flooding everything in its path." Once you get caught in the raging waters and the current doesn't drag you underwater, the debris will finish the job.

“Earthquakes kill a number of people, but many more are injured. With tsunamis, it's completely the opposite,” says Titov. "Almost no injuries because it's such a difficult disaster to survive." Earthquakes and tsunamis of the magnitude of 2004 are so rare that catastrophic tsunamis are virtually unheard of in the long cultural history of India and Sri Lanka, says Jose Borrero, a tsunami researcher at the University of California du

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South and director of eCoast. a maritime consultancy firm based in New Zealand. "[The Indian Ocean tsunami] made landfall in these places, which also had no natural warning because they were far enough away not to feel the quake," Borrero said. "With no natural warning, no official warning, and no history of tsunamis hitting coasts full of people, it's the perfect combination to cause a lot of death and destruction."

Geological Survey to measure the full extent of the tsunami that hit Sumatra. During these expeditions, scientists have confirmed maximum wave heights of over 131 feet at the northwest tip of the island. Borrero remembers encountering a colossal freighter loaded with bags of cement that had been thrown on its back and its propeller hovering in the air.

It was the most extreme tsunami since 1960," Borrero said, referring to the Chilean earthquake and 8.6 magnitude tsunami that struck the Pacific, including the devastation of Hilo, Hawaii, 15 hours later. the earthquake. Titov will never forget the scene of widespread devastation he witnessed months after the tsunami waters subsided in Sumatra.

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“We took a boat from the center of the island to Banda Aceh, the hardest hit area, and for hundreds of miles it was like someone taking an eraser and erasing everything below the 20-meter line," he said. "The scale of the destruction was simply staggering."

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Dave Roos is a freelance writer based in the United States and Mexico. A longtime contributor to HowStuffWorks, Dave has also published in The New York Times, Los Angeles Times and Newsweek. We seek accuracy and fairness. But if you see something wrong, click here to contact us!

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