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Newforex indonesia earthquake
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Meanwhile, It caused by the Indian plate and the Burma plate drifted, coincide with each other, and finally shake the affected area with a strength of approximately 9. Then, the biggest disaster called Tsunami occurred. Giant waves arise as high as 30 meters and hit several areas such as Aceh, Thailand, Sri Lanka, India, the Maldives, even the east coast of Africa.
Tsunami waves reached 9 meters. On the other hand, the duration of the earthquake before the tsunami is the longest in history. At that time the earth shocked approximately 8 to 10 minutes. After that, the sea water was receding from the shoreline in several areas. According to the U.
Geological Survey, the death toll reached up to Then,Indonesia became country that suffered damage and most casualties. It claimed more than , victims. Mostly the people lived in Aceh. Moreover, dozens of buildings were destroyed, especially in Meulaboh and Banda Aceh.
So, Aceh earthquake in is the third most powerful earthquake ever recorded. Java Island The next island with most of earthquake happened is Java. There are several cities ever experienced the biggest earthquake. Such as: 1. Jogjakarta Earthquake in 6. The epicenter was 38 km in south Jogjakarta at a depth reached 33 km above sea level.
Earthquake happened at dawn approximately in pm for only 57 seconds. A finite fault model by the ANSS indicate rupture along a fault measuring 90 km by 15 km with a maximum coseismic slip of 4. Coseismic slip might have been 2. This region of Indonesia is also not as seismically active, hence many expert seismologists did not expect a large earthquake to occur. The strike-slip mechanism was also unusual as thrust faulting is the dominant mechanism for earthquakes in the area.
In , the fault generated a magnitude 5. Earthquakes were also triggered on the Selayar Fault, a prominent normal fault located west of the Kalaotoa Fault, believed to be the result of stress transfer. Tsunami[ edit ] Tsunami warnings were issued to coastal communities of the Flores region, causing panic among residents. Videos posted on social media showed panicked residents running to higher ground to avoid the anticipated waves.
The Flores region lie at the complex tectonic boundary between the Australian and Sunda plates , as well as several microplates. Among the major active faults are the Flores Back Arc Thrust Fault and Sunda megathrust to accommodate the complex convergence between the tectonic plates.
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It occurred at 2,31 Northern longitude and 92,67 eastern longitude. Then, the epicenter was at 29 km Northwest of North Bengkulu. So, it was the biggest earthquake ever happened in Indonesia. On the other hand, earthquake felt strong enough even the shock occurred approximately for 10 minutes.
It caused by the movement of the strike-slip-fault. So, it gave a big impacts in several countries. Aceh earthquake in 9,1 — 9,3 SR The devastating earthquake occurred in Indian ocean, the west coast of Aceh in December Without prediction and warning, Indonesia and several Southeast Asia regions struck by a terrifying shock.
Meanwhile, It caused by the Indian plate and the Burma plate drifted, coincide with each other, and finally shake the affected area with a strength of approximately 9. Then, the biggest disaster called Tsunami occurred. Giant waves arise as high as 30 meters and hit several areas such as Aceh, Thailand, Sri Lanka, India, the Maldives, even the east coast of Africa. Tsunami waves reached 9 meters. On the other hand, the duration of the earthquake before the tsunami is the longest in history.
At that time the earth shocked approximately 8 to 10 minutes. After that, the sea water was receding from the shoreline in several areas. According to the U. Geological Survey, the death toll reached up to Then,Indonesia became country that suffered damage and most casualties. It claimed more than , victims. Mostly the people lived in Aceh. Coseismic slip might have been 2. This region of Indonesia is also not as seismically active, hence many expert seismologists did not expect a large earthquake to occur.
The strike-slip mechanism was also unusual as thrust faulting is the dominant mechanism for earthquakes in the area. In , the fault generated a magnitude 5. Earthquakes were also triggered on the Selayar Fault, a prominent normal fault located west of the Kalaotoa Fault, believed to be the result of stress transfer. Tsunami[ edit ] Tsunami warnings were issued to coastal communities of the Flores region, causing panic among residents.
Videos posted on social media showed panicked residents running to higher ground to avoid the anticipated waves. The Flores region lie at the complex tectonic boundary between the Australian and Sunda plates , as well as several microplates. Among the major active faults are the Flores Back Arc Thrust Fault and Sunda megathrust to accommodate the complex convergence between the tectonic plates.
The Flores Back Arc Thrust formed due to the convergence between the Sunda and Australian plates, accommodating compression.
