1783 Laki and Grimsvoetn | |
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| Total costs | N/A |
| Deaths | 33000 |
Laki (Icelandic pronunciation: [ˈlaːcɪ]) or Lakagígar ([ˈlaːkaˌciːɣar̥], Craters of Laki) is a volcanic fissure in the western part of Vatnajökull National Park, Iceland, not far from the volcanic fissure of Eldgjá and the small village of Kirkjubæjarklaustur. The fissure is properly referred to as Lakagígar, while Laki is a mountain that the fissure bisects. Lakagígar is part of a volcanic system centered on the volcano Grímsvötn and including the volcano Thordarhyrna. It lies between the glaciers of Mýrdalsjökull and Vatnajökull, in an area of fissures that run in a southwest to northeast direction. The system erupted violently over an eight-month period between June 1783 and February 1784 from the Laki fissure and the adjoining volcano Grímsvötn, pouring out an estimated 42 billion tons or 14 km3 (3.4 cu mi) of basalt lava and clouds of poisonous hydrofluoric acid and sulfur dioxide compounds that contaminated the soil, leading to the death of over 50% of Iceland's livestock population, and the destruction of the vast majority of all crops. This led to a famine which then killed approximately 69% of the island's human population. The lava flows also destroyed 21 villages. The Laki eruption and its aftermath caused a drop in global temperatures, as 120 million tons of sulfur dioxide was spewed into the Northern Hemisphere. This caused crop failures in Europe and may have caused droughts in North Africa and India.
Source: Wikipedia 1935 Yangtze Flood | |
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| Total costs | N/A |
| Deaths | 145000 |
The 1935 Yangtze flood struck China during a decade of flooding, famine and social turmoil. It is considered to be the fifth deadliest flood in recorded history, with a death toll of 145,000 and displacement of millions. As a result of the flood, millions of survivors were faced with hardship due to displacement, injury, loss of property as well as food shortages and famine.Four years earlier in 1931, after three years of drought, both the Yangtze and Yellow Rivers experienced significant flooding. Known as the 1931 China Floods, they were considered to be the worst non-pandemic disaster of the century because of the millions of deaths they led to indirectly. With the 1935 floods following on so soon from the 1931 floods, flood relief infrastructure, which included drainage reservoirs and floodwater channels, was soon overwhelmed.The Yangtze River flooding primarily affected the provinces of Hubei, Hunan, Jiangxi, Anhui, Jiangsu and Zhejiang, all of which are located in the middle to lower reaches of the river.
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