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1833 West Bengal Tropical Cyclone vs. 1968 Dasht-e...
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1833 West Bengal Tropical Cyclone vs 1968 Dasht-e Bayaz and Ferdows earthquake

1833 West Bengal Tropical Cyclone
1968 Dasht-e Bayaz and Ferdows earthquake
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1833 West Bengal Tropical Cyclone

Total costsN/A
Deaths 50000

Informations

The years before 1890 featured the pre-1890 North Indian Ocean cyclone seasons. Each season was an event in the annual cycle of tropical cyclone formation. The North Indian tropical cyclone season has no bounds, but they tend to form between April and December, peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. Below are the most significant cyclones in the time period. Because much of the North Indian coastline is near sea level and prone to flooding, these cyclones can easily kill many with storm surge and flooding. These cyclones are among the deadliest on earth in terms of numbers killed.

Source: Wikipedia
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1968 Dasht-e Bayaz and Ferdows earthquake

Total costsN/A
Deaths 15000

Informations

The Dasht-e Bayaz and Ferdows earthquakes occurred in Dashte Bayaz, Kakhk and Ferdows, Iran in late August and early September 1968. The mainshock measured 7.4 on the moment magnitude scale and had a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Damage was heavy in the affected areas with thousands of lives lost in the first event and many hundreds more in the second strong event.

Source: Wikipedia

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