1949 Khait landslide vs. 1219 St.'s Marcellus Flood...

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1949 Khait landslide vs 1219 St.'s Marcellus Flood

1949 Khait landslide

1219 St.'s Marcellus Flood

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1949 Khait landslide
Total costs	N/A
Deaths	28000

Informations

The Khait or Hoit landslide occurred on July 10, 1949 in the Hoit district in the Gharm Oblast in the Tajikistan, then part of the Soviet Union. 'Khait' is a transliteration from Russian: Хаит; local modern spelling: Hoit (Tajik: Ҳоит). The landslide was triggered by the 1949 Khait earthquake and buried 33 villages and has by some estimates killed 28,000 people. News of the landslide was not publicly revealed by the government and details of the disaster were not revealed until after the fall of the Soviet Union. A marble statue of a woman with her head and hands lowered and an expression of grief was later erected at the site.

Source: Wikipedia

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1219 St.'s Marcellus Flood
Total costs	N/A
Deaths	36000

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

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1949 Khait landslide vs 1219 St.'s Marcellus Flood