1257 Mount Samalas | |
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| Total costs | N/A |
| Deaths | 20000 |
In 1257, a catastrophic eruption occurred at the Samalas volcano on the Indonesian island of Lombok. The event had a probable Volcanic Explosivity Index of 7, making it one of the largest volcanic eruptions during the current Holocene epoch. It created eruption columns reaching tens of kilometres into the atmosphere and pyroclastic flows that buried much of Lombok and crossed the sea to reach the neighbouring island of Sumbawa. The flows destroyed human habitations, including the city of Pamatan, which was the capital of a kingdom on Lombok. Ash from the eruption fell as far as 340 kilometres (210 mi) away in Java; the volcano deposited more than 10 cubic kilometres (2.4 cu mi) of rocks and ash. The eruption was witnessed by people who recorded it on the Babad Lombok, a document written on palm leaves. It left behind a large caldera that contains Lake Segara Anak. Later volcanic activity created more volcanic centres in the caldera, including the Barujari cone, which remains active. The aerosols injected into the atmosphere reduced the solar radiation reaching the Earth's surface, causing a volcanic winter and cooling the atmosphere for several years. This led to famines and crop failures in Europe and elsewhere, although the exact scale of the temperature anomalies and their consequences is still debated. The eruption may have helped trigger the Little Ice Age, a centuries-long cold period during the last thousand years. Before the site of the eruption was known, an examination of ice cores around the world had found a large spike in sulfate deposition around 1257, providing strong evidence of a large volcanic eruption having occurred somewhere in the world. In 2013, scientists linked the historical records about Mount Samalas to these spikes.
Source: Wikipedia 1789-1793 Doji bara famine | |
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| Total costs | N/A |
| Deaths | 11000000 |
The Doji bara famine (also Skull famine) of 1791–1792 in the Indian subcontinent was brought on by a major El Niño event lasting from 1789–1795 and producing prolonged droughts. Recorded by William Roxburgh, a surgeon with the British East India Company, in a series of pioneering meteorological observations, the El Niño event caused the failure of the South Asian monsoon for four consecutive years starting in 1789.The resulting famine, which was severe, caused widespread mortality in Hyderabad, Southern Maratha Kingdom, Deccan, Gujarat, and Marwar (then all ruled by Indian rulers). In regions like the Madras Presidency (governed by the East India Company), where the famine was less severe, and where records were kept, half the population perished in some districts, such as in the Northern Circars. In other areas, such as Bijapur, although no records were kept, both the famine and the year 1791 came to be known in folklore as the Doji bara (also Doĝi Bar) or the 'skull famine,' on account, it was said, of the 'bones of the victims which lay unburied whitening the roads and the fields.' As in the Chalisa famine of a decade earlier, many areas were depopulated from death or migration. According to one study, a total of 11 million people may have died during the years 1789–1792 as a result of starvation or accompanying epidemics of disease.
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