1570 All Saints Flood | |
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| Total costs | N/A |
| Deaths | 20000 |
The All Saints' Flood (Dutch: Allerheiligenvloed) of 1570 was a disaster which happened on November 1, on the Dutch and German coast. Affected cities include Egmond, Bergen op Zoom and Saeftinghe. On 1 November 1570, the Domeinraad council in Bergen op Zoom had warned the dijkgraafs of the south and north quarters of a 'very excessive high flood' 'considering those big storms of wind starting yesterday'. A storm surge pushed the water to unprecedented heights, even higher than those at the flood disaster of 1953. It broke innumerable dikes on the Dutch coasts, as a result of which there were enormous floods and immense damage. The total number of dead is thought to have been in the tens of thousands, but exact data is not available. Tens of thousands of people became homeless. Livestock was lost in huge numbers. Winter stocks of food and fodder were destroyed. The Allerheiligenvloed marks the origin of the Verdronken Land van Saeftinghe (verdronken meaning 'drowned'). In Zeeland the small islands Wulpen, Koezand, Cadzand and Stuivezand were permanently lost. It was confirmed that the floods drowned 20,000 people.
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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