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1570 All Saints Flood vs. 1815 Mount Tambora -...
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1570 All Saints Flood vs 1815 Mount Tambora

1570 All Saints Flood
1815 Mount Tambora
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1570 All Saints Flood

Total costsN/A
Deaths 20000

Informations

The All Saints' Flood (Dutch: Allerheiligenvloed) of 1570 was a disaster which happened on November 1, on the Dutch and German coast. Affected cities include Egmond, Bergen op Zoom and Saeftinghe. On 1 November 1570, the Domeinraad council in Bergen op Zoom had warned the dijkgraafs of the south and north quarters of a 'very excessive high flood' 'considering those big storms of wind starting yesterday'. A storm surge pushed the water to unprecedented heights, even higher than those at the flood disaster of 1953. It broke innumerable dikes on the Dutch coasts, as a result of which there were enormous floods and immense damage. The total number of dead is thought to have been in the tens of thousands, but exact data is not available. Tens of thousands of people became homeless. Livestock was lost in huge numbers. Winter stocks of food and fodder were destroyed. The Allerheiligenvloed marks the origin of the Verdronken Land van Saeftinghe (verdronken meaning 'drowned'). In Zeeland the small islands Wulpen, Koezand, Cadzand and Stuivezand were permanently lost. It was confirmed that the floods drowned 20,000 people.

Source: Wikipedia
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1815 Mount Tambora

Total costsN/A
Deaths 250100

Informations

The 1815 eruption of Mount Tambora was the most powerful volcanic eruption in recorded human history, with a Volcanic Explosivity Index (VEI) of 7. The eruption ejected 160–213 cubic kilometres (38–51 cu mi) of material into the atmosphere. It is the most recently known VEI-7 event and the most recent confirmed VEI-7 eruption.Mount Tambora is on the island of Sumbawa in present-day Indonesia, then part of the Dutch East Indies. Although its eruption reached a violent climax on 10 April 1815, increased steaming and small phreatic eruptions occurred during the next six months to three years. The ash from the eruption column dispersed around the world and lowered global temperatures in an event sometimes known as the Year Without a Summer in 1816. This brief period of significant climate change triggered extreme weather and harvest failures in many areas around the world. Several climate forcings coincided and interacted in a systematic manner that has not been observed after any other large volcanic eruption since the early Stone Age.

Source: Wikipedia

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