| Meteorological history | |
|---|---|
| Duration | 13 January 1362 |
| Overall effects | |
| Fatalities | 25,000 |
| Areas affected | British Isles, Netherlands, Northern Germany and Denmark |
Saint Marcellus's floodorGrote Mandrenke (Low Saxon: /ɣroːtə mandrɛŋkə/; Danish: Den Store Manddrukning, 'Great Drowning of Men')[1] 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, causing at least 25,000 deaths.[1] The storm tide is also called the "Second St. Marcellus flood" because it peaked on 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 from 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. These included Rungholt, said to have been located on the island of StrandinNorth Frisia, Ravenser OddinEast Yorkshire, and the harbour of DunwichinSuffolk.[2]
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,[3] and was characteristic of the unsettled and changeable weather in northern Europe at the beginning of the Little Ice Age.
 | This article related to a specific weather event is a stub. You can help Wikipedia by expanding it. |
 | This article about a flood is a stub. You can help Wikipedia by expanding it. |
