Indian great famine 1876-1878 | |
|---|---|
| Total costs | N/A |
| Deaths | 5500000 |
The Great Famine of 1876–1878 was a famine in India under Crown rule. It began in 1876 after an intense drought resulting in crop failure in the Deccan Plateau. It affected south and Southwestern India—the British-administered presidencies of Madras and Bombay, and the princely states of Mysore and Hyderabad—for a period of two years. In 1877 famine came to affect regions northward, including parts of the Central Provinces and the North-Western Provinces, and a small area in the Punjab. The famine ultimately affected an area of 670,000 square kilometres (257,000 sq mi) and caused distress to a population totalling 58,500,000. The excess mortality in the famine has been estimated in a range whose low end is 5.6 million human fatalities, high end 9.6 million fatalities, and a careful modern demographic estimate 8.2 million fatalities. The famine is also known as the Southern India famine of 1876–1878 and the Madras famine of 1877.
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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