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.
Source: Wikipedia 1960 Agadir earthquake | |
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| Total costs | N/A |
| Deaths | 12000 |
The 1960 Agadir earthquake occurred 29 February at 23:40 Western European Time near the city of Agadir, located in western Morocco on the shore of the Atlantic Ocean. Despite the earthquake's moderate Mw scale magnitude of 5.8, its relatively shallow depth (15.0 km) resulted in strong surface shaking, with a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Between 12,000 and 15,000 people (about a third of the city's population of the time) were killed and another 12,000 injured with at least 35,000 people left homeless, making it the most destructive and deadliest earthquake in Moroccan history. Particularly hard hit were Founti, the Kasbah, Yachech (iḥšaš) and the Talbordjt area. The earthquake's shallow focus, close proximity to the port city of Agadir, and unsatisfactory construction methods were all reasons declared by earthquake engineers and seismologists as to why it was so destructive.
Source: Wikipedia
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