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1556 Shaanxi earthquake vs. 1997 Soufriere Hills -...
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1556 Shaanxi earthquake vs 1997 Soufriere Hills

1556 Shaanxi earthquake
1997 Soufriere Hills
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1556 Shaanxi earthquake

Total costsN/A
Deaths 830000

Informations

The 1556 Shaanxi earthquake, or Huaxian earthquake (simplified Chinese: 华县大地震; traditional Chinese: 華縣大地震; pinyin: Huáxiàn Dàdìzhèn), or Jiajing earthquake (Chinese: 嘉靖大地震; pinyin: Jiājìng Dàdìzhèn), is the deadliest earthquake in recorded history. According to imperial records, approximately 830,000 people lost their lives.It occurred on the morning of 23 January 1556 in Shaanxi, during the Ming dynasty. More than 97 counties in the provinces of Shaanxi, Shanxi, Henan, Gansu, Hebei, Shandong, Hubei, Hunan, Jiangsu and Anhui were affected. Buildings were damaged slightly in the cities of Beijing, Chengdu and Shanghai. An 840-kilometre-wide (520 mi) area was destroyed, and in some counties as much as 60% of the population was killed. Most of the population in the area at the time lived in yaodongs, artificial caves in loess cliffs; these collapsed in great numbers, causing many casualties.

Source: Wikipedia
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1997 Soufriere Hills

Total costsN/A
Deaths 19

Informations

The Soufrière Hills are an active, complex stratovolcano with many lava domes forming its summit on the Caribbean island of Montserrat. After a long period of dormancy, the Soufrière Hills volcano became active in 1995 and has continued to erupt ever since. Its eruptions have rendered more than half of Montserrat uninhabitable, destroying the capital city, Plymouth, and causing widespread evacuations: about two-thirds of the population have left the island. Chances Peak in the Soufrière Hills was the highest summit on Montserrat until the mid-1990s, but it has since been eclipsed by various rising and falling volcanic domes during the recent volcanic activity.The volcano is andesitic in nature, and the current pattern of activity includes periods of lava dome growth, punctuated by brief episodes of dome collapse which result in pyroclastic flows, ash venting, and explosive eruption. The volcano is monitored by the Montserrat Volcano Observatory. Volcanic gas emissions from this volcano are measured by a Multi-Component Gas Analyzer System, which detects pre-eruptive degassing of rising magmas, improving prediction of volcanic activity.The Centre Hills in the central part of the island and the Silver Hills in the north are older volcanic massifs related to the subduction zone. There are three main parts of the island: the central zone, subduction and exclusion.

Source: Wikipedia

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