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1700 Tseax Cone vs. 1954 Yangtze River Flood -...
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1700 Tseax Cone vs 1954 Yangtze River Flood

1700 Tseax Cone
1954 Yangtze River 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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1954 Yangtze River Flood

Total costsN/A
Deaths 30000

Informations

From June to September 1954, the Yangtze River Floods were a series of catastrophic floodings that occurred mostly in Hubei Province. Due to unusually high volume of precipitation as well as an extraordinarily long rainy season in the middle stretch of the Yangtze River late in the spring of 1954, the river started to rise above its usual level in around late June. Despite efforts to open three important flood gates to alleviate the rising water by diverting it, the flood level continued to rise until it hit the historic high of 44.67 m (146.6 ft) in Jingzhou, Hubei and 29.73 m (97.5 ft) in Wuhan. The number of dead from this flood was estimated at around 33,000, including those who died of plague in the aftermath of the disaster.

Source: Wikipedia

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