1912 Tacloban | |
|---|---|
| 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 1815 Mount Tambora | |
|---|---|
| Total costs | N/A |
| Deaths | 250100 |
The 1815 eruption of Mount Tambora was the most powerful volcanic eruption in recorded human history, with a Volcanic Explosivity Index (VEI) of 7. The eruption ejected 160–213 cubic kilometres (38–51 cu mi) of material into the atmosphere. It is the most recently known VEI-7 event and the most recent confirmed VEI-7 eruption.Mount Tambora is on the island of Sumbawa in present-day Indonesia, then part of the Dutch East Indies. Although its eruption reached a violent climax on 10 April 1815, increased steaming and small phreatic eruptions occurred during the next six months to three years. The ash from the eruption column dispersed around the world and lowered global temperatures in an event sometimes known as the Year Without a Summer in 1816. This brief period of significant climate change triggered extreme weather and harvest failures in many areas around the world. Several climate forcings coincided and interacted in a systematic manner that has not been observed after any other large volcanic eruption since the early Stone Age.
Source: Wikipedia
Welcome to 