1949 Eastern Guatemalan Floods | |
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| Total costs | N/A |
| Deaths | 40000 |
The 1949 Eastern Guatemalan floods were a series of violent and devastating floods, following a particularly destructive Atlantic Ocean Hurricane season. Death toll estimates range from 1000 to 40,000, placing the floods as some of the deadliest in recorded history. Apart from the direct deadly consequences of the floods, the disaster had a huge impact in many other spheres of life in Guatemala. It is estimated that the financial consequences of the floods ranged from $15,000,000 to $40,000,000.Landslides and road blockages affected communications within the country, and also impacted distribution of foods and other resources. As news of the floodings in Guatemala broke international headlines, Foreign governments pledged aid to the recovery of the country accordingly. The neighbouring countries of The United States and Cuba rushed to provide immediate aid by plane to victims of the disaster.
Source: Wikipedia 1362 Grote Mandraenke | |
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| Total costs | N/A |
| Deaths | 40000 |
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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