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1912 Tacloban vs. 1783 Laki and Grimsvoetn -...
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1912 Tacloban vs 1783 Laki and Grimsvoetn

1912 Tacloban
1783 Laki and Grimsvoetn
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1912 Tacloban

Total costsN/A
Deaths 15000

Informations

Tacloban ( tak-LOH-ban; Tagalog pronunciation: [tɐkˈloban]), officially the City of Tacloban (Waray: Syudad han Tacloban; Tagalog: Lungsod ng Tacloban), is a 1st class highly urbanized city in the Eastern Visayas region of the Philippines. The city is autonomous from the province of Leyte, although it serves as its provincial capital. According to the 2020 census, Tacloban has a population of 251,881, making it the most populous city in the Eastern Visayas.  The city is located 360 miles (580 km) southeast from Manila. Tacloban City was briefly the capital of the Philippines under the Commonwealth Government, from 20 October 1944 to 27 February 1945. In an extensive survey conducted by the Asian Institute of Management Policy Center and released in July 2010, Tacloban City ranks as the fifth most competitive city in the Philippines, and second in the emerging cities category. On 8 November 2013, the city was largely destroyed by Typhoon Haiyan, having previously suffered similar destruction and loss of life in 1897 and 1912. On 17 January 2015, Pope Francis visited Tacloban during his Papal Visit to the Philippines and held a mass at Barangay San Jose, and later he led mass of 30,000 people in front of the airport.

Source: Wikipedia
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1783 Laki and Grimsvoetn

Total costsN/A
Deaths 33000

Informations

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

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