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2010 Yushu earthquake vs. 1960 Agadir earthquake -...
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2010 Yushu earthquake vs 1960 Agadir earthquake

2010 Yushu earthquake
1960 Agadir earthquake
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2010 Yushu earthquake

Total costsN/A
Deaths 2968

Informations

The 2010 Yushu earthquake struck on April 14 and registered a magnitude of 6.9 Mw (USGS, EMSC) or 7.1 Ms (CEA, CENC). It had a maximum felt intensity of IX (Violent) on the Mercalli intensity scale. It originated in Yushu, Qinghai, China, at 7:49 am local time (23:49 April 13 UTC). According to the Xinhua News Agency, 2,698 people were confirmed dead, 270 missing and 12,135 injured, 1,434 of them severely. The epicenter was located in Rima village (日玛村/日麻村), Upper Laxiu township (上拉秀乡) of Yushu County, in remote and rugged terrain, near the border of Tibet Autonomous Region, about 30 km from Gyêgu town or Jyekundo, the seat of Yushu County, and about 240 km from Qamdo. The epicenter was in a sparsely populated area on the Tibetan plateau that is regularly hit by earthquakes.The 12th century Thrangu Monastery and surrounding villages were severely damaged and many monks and villagers were killed.

Source: Wikipedia
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1960 Agadir earthquake

Total costsN/A
Deaths 12000

Informations

The 1960 Agadir earthquake occurred 29 February at 23:40 Western European Time near the city of Agadir, located in western Morocco on the shore of the Atlantic Ocean. Despite the earthquake's moderate Mw scale magnitude of 5.8, its relatively shallow depth (15.0 km) resulted in strong surface shaking, with a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Between 12,000 and 15,000 people (about a third of the city's population of the time) were killed and another 12,000 injured with at least 35,000 people left homeless, making it the most destructive and deadliest earthquake in Moroccan history. Particularly hard hit were Founti, the Kasbah, Yachech (iḥšaš) and the Talbordjt area. The earthquake's shallow focus, close proximity to the port city of Agadir, and unsatisfactory construction methods were all reasons declared by earthquake engineers and seismologists as to why it was so destructive.

Source: Wikipedia

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