Langila
Vulcano complesso · Papua New Guinea · 1330 m

- Tipo
- Vulcano complesso
- Paese
- Papua New Guinea
- Regione
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Altitudine
- 1330 m
- Coordinate
- -5.525, 148.420
- Ultima eruzione
- 2026
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
Langila, one of the most active volcanoes of New Britain, consists of a group of four small overlapping composite basaltic-andesitic cones on the lower E flank of the extinct Talawe volcano in the Cape Gloucester area of NW New Britain. A rectangular, 2.5-km-long crater is breached widely to the SE; Langila was constructed NE of the breached crater of Talawe. An extensive lava field reaches the coast on the N and NE sides of Langila. Frequent mild-to-moderate explosive eruptions, sometimes accompanied by lava flows, have been recorded since the 19th century from three active craters at the summit. The youngest and smallest crater (no. 3 crater) was formed in 1960 and has a diameter of 150 m.
Sintesi da Wikipedia
Riassunto in ingleseLangila is one of the most active volcanoes of New Britain, Papua New Guinea. It consists of four overlapping volcanic cones on the eastern flank of an older extinct volcano, Talawe. Talawe is the largest volcano in Cape Gloucester. There have been dozens of recorded eruptions since the 19th century from three separate volcanic craters at the summit of Langila. The most recent eruptive cycle of Langila began in August 2006 and continued into early 2007. Volcanic activity at Langila consists of Strombo-Vulcanian and Vulcanian eruptions and lava flows. Langila is one of the most active volcanoes in the Bismark archipelago. The smallest crater is crater number 3.
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Storia delle eruzioni
Cronologia dettagliata
- 2015VEI 2Osservata2015-10-22 – 2026-03-16Crater 2
- 2013VEI ?Osservata2013-10-23 – 2013-12-01
- 2012VEI 1Osservata2012-12-01 – 2012-12-05Summit craters
- 2012VEI 0Osservata2012-07-21 – 2012-07-21
- 2011VEI 0Osservata2011-07-28 – 2011-07-28
- 2009VEI 2Osservata2009-09-16 – 2010-02-16Crater 2
- 2006VEI 2Osservata2006-08-09 – 2008-07-06
- 2005VEI 2Osservata2005-04-19 – 2006-03-31
- 2004VEI 2Osservata2004-01-20 – 2004-01-27
- 2004VEI 2Osservata2004-11-24 – 2004-12-25
- 2002VEI 2Osservata2002-05-25 – 2003-04-09Crater 2
- 1973VEI 3Osservata1973-02-24 – 2000-10-16Crater 3, Crater 2
- 1971VEI 2Osservata1971-01-26 – 1972-07-05Crater 2
- 1970VEI 2Osservata1970-05-20 – 1970-09-22Crater 2
- 1969VEI 2Osservata1969-09-29 – 1969-09-29Crater 2 or 3
- 1967VEI 2Osservata1967-01-19 – 1968-06-16Crater 2, Crater 3
- 1964VEI 2Osservata1964-12-04 – 1966-09-23Crater 2, Crater 3
- 1962VEI 2Osservata1962-03-16 – 1963-08-11Crater 2, Crater 3
- 1960VEI 2Osservata1960-12-19 – 1961-09-25Crater 3, Crater 2
- 1958VEI 2Osservata1958-04-21 – 1958-06-04Crater 2
- 1956VEI 2Osservata1956-03-25 – 1956-03-31Crater 2
- 1955VEI 2Osservata1955-02-15 – 1955-02-17Crater 2
- 1955VEI 2Osservata1955-06-01 – 1955-06-16Crater 2
- 1954VEI 3Osservata1954-05-18 – 1954-11-13Crater 2
- 1942 (±5 anni)VEI 1Stima geologica1942 – In corsoCrater 2
- 1907VEI 2Osservata1907 – In corsoNE Crater (crater 2)
- 1900VEI 2Osservata1900 – In corsoNorth Crater (crater 1)
- 1890VEI 0Osservata1890 – In corso
- 1884VEI 2Osservata1884 – In corso
- 1878VEI 2Osservata1878 – In corsoCrater 2
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