1931 China Flood | |
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| Total costs | N/A |
| Deaths | 4000000 |
The 1931 China floods, or the 1931 Yangtze–Huai River floods, occurred from June to August 1931 in China, hitting major cities such as Wuhan, Nanjing and beyond, which eventually culminated into a dike breach along Lake Gaoyou on 25 August 1931. Fatality estimates vary widely. A field survey by the University of Nanking led by John Lossing Buck immediately after the flood found '150,000 people had drowned, and that this number represented less than a quarter of all fatalities during the first 100 days of the flood.' The official report found 140,000 drowned and claims that '2 million people died during the flood, having drowned or died from lack of food'. A cholera epidemic in the subsequent year, from May 1932, was officially reported to have 31,974 deaths and 100,666 cases. A popular high-end estimate of 3.7 to 4.0 million fatalities 'enjoys great currency online, helping the 1931 flood to secure its position on sensationalist lists of the world’s deadliest disasters.'
Source: Wikipedia 1219 St.'s Marcellus Flood | |
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| Total costs | N/A |
| Deaths | 36000 |
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.
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