Javascript must be enabled to use all features of this site and to avoid misfunctions
2010 Yushu earthquake vs. 1973 Eldfell - Comparison...
HOME
Select category:
Disasters
Select category
NEW

Advertising

Cancel

Search in
Close

2010 Yushu earthquake vs 1973 Eldfell

2010 Yushu earthquake
1973 Eldfell
Change

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
Change

1973 Eldfell

Total costsN/A
Deaths 1

Informations

Eldfell is a volcanic cone just over 200 metres (660 ft) high on the Icelandic island of Heimaey. It formed in a volcanic eruption, which began without warning on the eastern side of Heimaey, in the Westman Islands, on 23 January 1973. The name means Hill of Fire in Icelandic. The eruption caused a major crisis for the island and led to its temporary evacuation. Volcanic ash fell over most of the island, destroying around 400 homes, and a lava flow threatened to close off the harbour, the island's main income source via its fishing fleet. An operation was mounted to cool the advancing lava flow by pumping sea water onto it, which was successful in preventing the loss of the harbour. After the eruption, the islanders used heat from the cooling lava flows to provide hot water and to generate electricity. They also used some of the extensive tephra, fall-out of airborne volcanic material to extend the runway at the island's small airport and as landfill on which 200 new houses were built.

Source: Wikipedia

More intresting stuff