1881 Thumb fire | |
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| Total costs | N/A |
| Deaths | 282 |
The Thumb Fire took place on September 5, 1881, in the Thumb area of Michigan in the United States. The fire, which burned over a million acres (4,000 km²) in less than a day, was the consequence of drought, hurricane-force winds, heat, the after-effects of the Port Huron Fire of 1871, and the ecological damage wrought by the era's logging techniques. The blaze, also called the Great Thumb Fire, the Great Forest Fire of 1881 and the Huron Fire, killed 282 people in Sanilac, Lapeer, Tuscola and Huron counties. The damage estimate was $2,347,000 in 1881, equivalent to $62,940,066 when adjusted for inflation. The fire sent enough soot and ash up into the atmosphere that sunlight was partially obscured at many locations on the East Coast of the United States. In New England cities, the sky appeared yellow and projected a strange luminosity onto buildings and vegetation. Twilight appeared at 12 noon. September 6, 1881, became known as Yellow Tuesday or Yellow Day because of the ominous nature of this atmospheric event.
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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