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The first wave came 5 minutes after the earthquake, preceded by a recession of the sea up to 600–700 m (2,000–2,300 ft). [citation needed]. The second and third waves came in 10 minutes intervals after the first wave. The third wave was the strongest, with a maximum tsunami wave height of 11 m (36 ft).
The earthquake itself, with a moment magnitude of around 9.2-9.3, devastated Aceh Province, Indonesia, while the tsunami affected countries all around the Indian Ocean. Nations which were affected are listed below in alphabetical order. For detailed information about each country affected by the earthquake and tsunami, see their individual ...
UTC time: 2010-10-25 14:42:22: ISC event: 15264887: USGS-ANSSComCat: Local date: 25 October 2010 (): Local time: 21:42:22: Magnitude: 7.8 M w: Depth: 12.8 miles (20.6 km) Epicenter: 1] [2]: Fault: Sunda megathrust: Type: Thrust fault: Areas affected: Indonesia: Max. intensity: MMI V (Moderate) [1]: Casualties: 408 dead + 303 missing [3]: The 2010 Mentawai earthquake occurred with a moment ...
Although the meanings of "tidal" include "resembling" [16] or "having the form or character of" [17] tides, use of the term tidal wave is discouraged by geologists and oceanographers. A 1969 episode of the TV crime show Hawaii Five-O entitled "Forty Feet High and It Kills!" used the terms "tsunami" and "tidal wave" interchangeably. [18]
Landing Craft Air Cushion (LCAC) Hovercraft from USS Bonhomme Richard (LHD 6) is delivering materials and supplies needed by the citizens of Meulaboh, Indonesia. The town of Meulaboh , which had a population of 120,000 before the tsunami, was struck by a series of waves, killing an estimated 40,000 and destroying most parts of the city ...
M7.7 – south of Java, Indonesia – United States Geological Survey; In pictures: Indonesian tsunami – BBC News 'Stealth' Tsunami That Killed 600 In Java Last Summer Had 65 Foot High Wave – ScienceDaily; A comparison study of 2006 Java earthquake and other Tsunami earthquakes – University of California, Santa Barbara
It was the first detailed documentation of a tsunami in Indonesia and the largest ever recorded in the country. [1] The exact fault which produced the earthquake has never been determined, but geologists postulate either a local fault, or a larger thrust fault offshore. The extreme tsunami was likely the result of a submarine landslide.
The river originates in the Barisan Mountains of West Sumatra and flows to the island's eastern coast, emptying into the Malacca Strait, directly opposite Singapore.It is the confluence of two tributaries of almost equal size: the Kampar Kanan River (or Right Kampar) and the Kampar Kiri River (or Left Kampar).