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1912 Bangladesh Cyclone vs. 1931 Fuyun earthquake -...
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1912 Bangladesh Cyclone vs 1931 Fuyun earthquake

1912 Bangladesh Cyclone
1931 Fuyun earthquake
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1912 Bangladesh Cyclone

Total costsN/A
Deaths 40000

Informations

The following is a list of tropical cyclones by year. Since the year 957, there have been at least 12,791 recorded tropical or subtropical cyclones in the Atlantic, Pacific, and Indian Oceans, which are known as basins. Collectively, tropical cyclones caused more than US$1.2 trillion in damage, unadjusted for inflation, and have killed more than 2.6 million people. Most of these deaths were caused by a few deadly cyclones, including the 1881 Haiphong typhoon, the 1931 Shanghai typhoon, the 1970 Bhola cyclone, Typhoon Nina in 1975, the 1991 Bangladesh cyclone, and Cyclone Nargis in 2008. In the North Atlantic Ocean, there have been 2,462 tropical cyclones, including at least 1,150 hurricanes, which have maximum sustained winds of at least 64 knots (74 mph, 119 km/h). The storms collectively killed more than 180,000 people. In the eastern Pacific Ocean, there have been 1,313 tropical cyclones, including 552 hurricanes; the storms collectively killed 8,467 people. In the western Pacific Ocean, there have been 4,648 tropical cyclones, including at least 1,485 typhoons; the storms collectively killed more than 1.4 million people. In the North Indian Ocean, there have been at least 1,551 tropical cyclones, including 262 that attained the equivalent of hurricane status; the storms collectively killed over 1 million people. There have been at least 2,768 tropical cyclones in the Southern Hemisphere. Storms with an asterisk (*) originated in another basin.

Source: Wikipedia
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1931 Fuyun earthquake

Total costsN/A
Deaths 10000

Informations

The 1931 Fuyun earthquake (富蕴地震) occurred on August 10 at 21:18 UTC. The epicenter was near Fuyun County of northern Xinjiang, China. It was a Mw 8.0 earthquake and had a surface rupture of 171 km with a maximal horizontal displacement of 14 m along the Koktokay-Ertai fault zone (可可托海-二台断裂带). The Koktokay-Ertai fault has a slip rate of 4±2 mm per year. The rupture of this earthquake was caused by right-lateral strike-slip movement with normal component. The rupture is well preserved and becomes one of the main features of the Koktokay National Geopark (可可托海国家地质公园) located in Koktokay.

Source: Wikipedia

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