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2005 Kashmir earthquake vs. 1219 St.'s Marcellus...
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2005 Kashmir earthquake vs 1219 St.'s Marcellus Flood

2005 Kashmir earthquake
1219 St.'s Marcellus Flood
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2005 Kashmir earthquake

Total costsN/A
Deaths 87351

Informations

The 2005 Kashmir earthquake occurred at 08:50:39 Pakistan Standard Time on 8 October in Pakistani-administered Azad Kashmir. It was centred near the city of Muzaffarabad, and also affected nearby Balakot in Khyber Pakhtunkhwa and some areas of Indian-administered Jammu and Kashmir. It registered a moment magnitude of 7.6 and had a maximum Mercalli intensity of VIII (Severe) or XI (Extreme). The earthquake also affected countries in the surrounding region where tremors were felt in Afghanistan, Tajikistan, India and the Xinjiang region. The severity of the damage caused by the earthquake is attributed to severe upthrust. Over 86,000 people died, a similar number were injured, and millions were displaced. It is considered the deadliest earthquake to hit South Asia, surpassing the 1935 Quetta earthquake.

Source: Wikipedia
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1219 St.'s Marcellus Flood

Total costsN/A
Deaths 36000

Informations

Saint Marcellus's flood or Grote Mandrenke (Low Saxon: /ɣroːtə mandrɛŋkə/; Danish: Den Store Manddrukning, 'Great Drowning of Men') was an intense extratropical cyclone, coinciding with a new moon, which swept across the British Isles, the Netherlands, northern Germany, and Denmark (including Schleswig/Southern Jutland) around 16 January 1362 (OS), causing at least 25,000 deaths. The storm tide is also called the 'Second St. Marcellus flood' because it peaked 16 January, the feast day of St. Marcellus. A previous 'First St. Marcellus flood' drowned 36,000 people along the coasts of West Friesland and Groningen on 16 January 1219. An immense storm tide of the North Sea swept far inland from England and the Netherlands to Denmark and the German coast, breaking up islands, making parts of the mainland into islands, and wiping out entire towns and districts such as: Rungholt, said to have been located on the island of Strand in North Frisia; Ravenser Odd in East Yorkshire; and, the harbour of Dunwich.This storm tide, along with others of like size in the 13th century and 14th century, played a part in the formation of the Zuiderzee, and was characteristic of the unsettled and changeable weather in northern Europe at the beginning of the Little Ice Age.

Source: Wikipedia

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