Javascript must be enabled to use all features of this site and to avoid misfunctions
1951 Mount Lamington vs. 1362 Grote Mandraenke -...
HOME
Select category:
Disasters
Select category
NEW

Advertising

Cancel

Search in
Close

1951 Mount Lamington vs 1362 Grote Mandraenke

1951 Mount Lamington
1362 Grote Mandraenke
Change

1951 Mount Lamington

Total costsN/A
Deaths 2942

Informations

Mount Lamington is an andesitic stratovolcano in the Oro Province of Papua New Guinea. The forested peak of the volcano had not been recognised as such until its devastating eruption in 1951 that caused about 3,000 deaths.The volcano rises to 1680 meters above the coastal plain north of the Owen Stanley Range. A summit complex of lava domes and crater remnants rises above a low-angle base of volcaniclastic deposits that are dissected by radial valleys. A prominent broad 'avalanche valley' extends northward from the breached crater.The mountain was named after Charles Cochrane-Baillie, 2nd Baron Lamington who was Governor of Queensland.

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