Soviet famine 1932-1933 | |
|---|---|
| Total costs | N/A |
| Deaths | 8000000 |
The Soviet famine of 1932–1933 was a famine in the major grain-producing areas of the Soviet Union, including Ukraine, Northern Caucasus, Volga Region, Kazakhstan, the South Urals, and West Siberia. About 5.7 to 8.7 million people are estimated to have lost their lives. Joseph Stalin and other party members had ordered that kulaks were 'to be liquidated as a class', and became a target for the state. The richer, land-owning peasants were labeled kulaks and were portrayed by the Bolsheviks as class enemies, which culminated in a Soviet campaign of political repressions, including arrests, deportations, and executions of large numbers of the better-off peasants and their families in 1929–1932.Major contributing factors to the famine include the forced collectivization in the Soviet Union of agriculture as a part of the first five-year plan, forced grain procurement, combined with rapid industrialisation, a decreasing agricultural workforce, and several severe droughts. Some scholars have classified the famine in Ukraine and Kazakhstan as genocides which were committed by Stalin's government, targeting ethnic Ukrainians and Kazakhs, while others dispute the relevance of any ethnic motivation, as is frequently implied by that term, instead, they focus on the class dynamics which existed between the land-owning peasants (kulaks) with strong political interest in private property, and the ruling Soviet Communist party's fundamental tenets which were diametrically opposed to those interests. Gareth Jones was the first Western journalist to report the devastation.
Source: Wikipedia 1600 Huaynaputina | |
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| Total costs | N/A |
| Deaths | 1500 |
Huaynaputina ( WY-nə-puu-TEE-nə; Spanish: [wajnapuˈtina]) is a volcano in a volcanic high plateau in southern Peru. Lying in the Central Volcanic Zone of the Andes, it was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. Huaynaputina is a large volcanic crater, lacking an identifiable mountain profile, with an outer stratovolcano and three younger volcanic vents within an amphitheatre-shaped structure that is either a former caldera or a remnant of glacial erosion. The volcano has erupted dacitic magma. In the Holocene, Huaynaputina has erupted several times, including on 19 February 1600 – the largest eruption ever recorded in South America – which continued with a series of events into March. Witnessed by people in the city of Arequipa, it killed at least 1,000–1,500 people in the region, wiped out vegetation, buried the surrounding area with 2 metres (7 ft) of volcanic rock and damaged infrastructure and economic resources. The eruption had a significant impact on Earth's climate, causing a volcanic winter: temperatures in the Northern Hemisphere decreased; cold waves hit parts of Europe, Asia and the Americas; and the climate disruption may have played a role in the onset of the Little Ice Age. Floods, famines, and social upheavals resulted. This eruption has been computed to measure 6 on the Volcanic Explosivity Index (VEI). The volcano has not erupted since 1600. There are fumaroles in the amphitheatre-shaped structure, and hot springs occur in the region, some of which have been associated with Huaynaputina. The volcano lies in a remote region where there is little human activity, but about 30,000 people live in the immediately surrounding area, and another one million in the Arequipa metropolitan area. If an eruption similar to the 1600 event were to occur, it would quite likely lead to a high death toll and cause substantial socioeconomic disruption. The Peruvian Geophysical Institute announced in 2017 that Huaynaputina would be monitored by the Southern Volcanological Observatory, and seismic observation began in 2019.
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