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1700 Tseax Cone vs. 1164 St. Juliana Flood -...
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1700 Tseax Cone vs 1164 St. Juliana Flood

1700 Tseax Cone
1164 St. Juliana Flood
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1700 Tseax Cone

Total costsN/A
Deaths 2000

Informations

The Tseax Cone ( SEE-aks), also called the Tseax River Cone or the Aiyansh Volcano, is a young and active cinder cone and adjacent lava flows associated with the Nass Ranges and the Northern Cordilleran Volcanic Province. It is located east of Crater Creek at outlet of Melita Lake, southeast of Gitlakdamix and 60 kilometres (37 mi) north of Terrace, British Columbia, Canada. The volcano is in a valley above and east of the Tseax River, about 20 kilometres (12 mi) south of the river's junction with the larger Nass River. The Tseax Cone is one of the most accessible volcanic centres in British Columbia.

Source: Wikipedia
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1164 St. Juliana Flood

Total costsN/A
Deaths 10000

Informations

Storm tides of the North Sea are coastal floods associated with extratropical cyclones crossing over the North Sea, the severity of which are affected by the shallowness of the sea and the orientation of the shoreline relative to the storm's path, as well as the timing of tides. The water level can rise to more than 5 metres (17 ft) above the normal tide as a result of storm tides. Northern Germany and Denmark are particularly susceptible to storm tides. The coastline of the German Bight forms an L-shape facing northwest. Also vulnerable are the United Kingdom and the Netherlands, where the sea shallows and is funnelled toward the English Channel. Storm tides are a regular occurrence in the North Sea basin; several form each year. Although most do not cause significant damage, the impact of some has been devastating. During one, the February flood of 1825, the Danish coastline changed, as the North Jutlandic Island became separated from the Jutland Peninsula.

Source: Wikipedia

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