How tall did the 2004 tsunami get?

Some locations reported that the waves had reached a height of 30 feet (9 metres) or more when they hit the shoreline. The tsunami killed at least 225,000 people across a dozen countries, with Indonesia, Sri Lanka, India, Maldives, and Thailand sustaining massive damage.

What caused the tsunami that killed approximately 230000 people on December 26 2004 * Your answer?

A powerful undersea earthquake that struck off the coast of Sumatra island, Indonesia, set off the 2004 Indian Ocean tsunami, also known as the Christmas or Boxing Day tsunami, on Sunday morning, Dec. 26, 2004.

Did Thailand know the tsunami was coming?

There was no warning of the first wave so people had no idea it was coming. These days, Thailand is better prepared for tsunamis as they are 2 hours away from being hit again if there is a new tsunami.

Where did the tsunami hit on December 26, 2004?

The Dec. 26, 2004, earthquake ruptured 250 kilometers offshore of Sumatra, Indonesia; tsunami waves traveled thousands of kilometers with enough power to kill hundreds of people and destroy villages as far away as the east coast of Africa.

How tall was the tsunami in the Indian Ocean?

Over the past decade, the Indian Ocean tsunami and its aftermath have driven researchers and governments worldwide to improve tsunami warning systems and led to the creation of the Indian Ocean Tsunami Warning and Mitigation System. The tsunami reached heights of more than 30 meters in some places around the Indian Ocean.

How did the tsunami in Japan compare to the 2004 tsunami?

The tsunami was only recently rivaled by the 2011 tsunami in Japan. “The foremost impact, of course, is the loss of life in both cases,” said Eric Geist, USGS research geophysicist. “For the 2004 tsunami, the loss of life far outweighed damage to infrastructure, whereas for the 2011 tsunami, there was significant damage to infrastructure in Japan.”

Why did scientists study the Indian Ocean tsunami?

The tsunami effects were studied in an effort to develop techniques to improve the identification of paleotsunami deposits in the geologic record.