1912 Tacloban | |
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| Total costs | N/A |
| Deaths | 15000 |
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 1997 Soufriere Hills | |
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| Total costs | N/A |
| Deaths | 19 |
The Soufrière Hills are an active, complex stratovolcano with many lava domes forming its summit on the Caribbean island of Montserrat. After a long period of dormancy, the Soufrière Hills volcano became active in 1995 and has continued to erupt ever since. Its eruptions have rendered more than half of Montserrat uninhabitable, destroying the capital city, Plymouth, and causing widespread evacuations: about two-thirds of the population have left the island. Chances Peak in the Soufrière Hills was the highest summit on Montserrat until the mid-1990s, but it has since been eclipsed by various rising and falling volcanic domes during the recent volcanic activity.The volcano is andesitic in nature, and the current pattern of activity includes periods of lava dome growth, punctuated by brief episodes of dome collapse which result in pyroclastic flows, ash venting, and explosive eruption. The volcano is monitored by the Montserrat Volcano Observatory. Volcanic gas emissions from this volcano are measured by a Multi-Component Gas Analyzer System, which detects pre-eruptive degassing of rising magmas, improving prediction of volcanic activity.The Centre Hills in the central part of the island and the Silver Hills in the north are older volcanic massifs related to the subduction zone. There are three main parts of the island: the central zone, subduction and exclusion.
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