Javascript must be enabled to use all features of this site and to avoid misfunctions
1901 Eastern United States heat wave vs. 1362 Grote...
HOME
Select category:
Disasters
Select category
NEW

Advertising

Cancel

Search in
Close

1901 Eastern United States heat wave vs 1362 Grote Mandraenke

1901 Eastern United States heat wave
1362 Grote Mandraenke
Change

1901 Eastern United States heat wave

Total costsN/A
Deaths 9500

Informations

The 1901 eastern United States heat wave was the most severe and deadly heat wave in the United States prior to the 1930s Dust Bowl. Although the heat wave did not set many still-standing daily temperature records, it was exceptionally prolonged – covering without interruption the second half of June and all of July – and centered upon more highly populated areas than later American heat waves. The heat wave accompanied a major drought in the Ohio Valley and Upper Midwest, with Illinois recording what remains its driest calendar year since records have been kept, and Missouri receiving only 0.21 inches (5.3 mm) above its driest calendar year of 1953.

Source: Wikipedia
Change

1362 Grote Mandraenke

Total costsN/A
Deaths 40000

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

More intresting stuff