Langila
Complex volcano · Papua New Guinea · 1330m

- Type
- Complex volcano
- Country
- Papua New Guinea
- Region
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Elevation
- 1330m
- Coordinates
- -5.525, 148.420
- Last eruption
- 2026
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-Basalt
Geological summary
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.
From Wikipedia
Langila 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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Eruption history
Detailed timeline
- 2015VEI 2Observed2015-10-22 – 2026-03-16Crater 2
- 2013VEI ?Observed2013-10-23 – 2013-12-01
- 2012VEI 1Observed2012-12-01 – 2012-12-05Summit craters
- 2012VEI 0Observed2012-07-21 – 2012-07-21
- 2011VEI 0Observed2011-07-28 – 2011-07-28
- 2009VEI 2Observed2009-09-16 – 2010-02-16Crater 2
- 2006VEI 2Observed2006-08-09 – 2008-07-06
- 2005VEI 2Observed2005-04-19 – 2006-03-31
- 2004VEI 2Observed2004-01-20 – 2004-01-27
- 2004VEI 2Observed2004-11-24 – 2004-12-25
- 2002VEI 2Observed2002-05-25 – 2003-04-09Crater 2
- 1973VEI 3Observed1973-02-24 – 2000-10-16Crater 3, Crater 2
- 1971VEI 2Observed1971-01-26 – 1972-07-05Crater 2
- 1970VEI 2Observed1970-05-20 – 1970-09-22Crater 2
- 1969VEI 2Observed1969-09-29 – 1969-09-29Crater 2 or 3
- 1967VEI 2Observed1967-01-19 – 1968-06-16Crater 2, Crater 3
- 1964VEI 2Observed1964-12-04 – 1966-09-23Crater 2, Crater 3
- 1962VEI 2Observed1962-03-16 – 1963-08-11Crater 2, Crater 3
- 1960VEI 2Observed1960-12-19 – 1961-09-25Crater 3, Crater 2
- 1958VEI 2Observed1958-04-21 – 1958-06-04Crater 2
- 1956VEI 2Observed1956-03-25 – 1956-03-31Crater 2
- 1955VEI 2Observed1955-02-15 – 1955-02-17Crater 2
- 1955VEI 2Observed1955-06-01 – 1955-06-16Crater 2
- 1954VEI 3Observed1954-05-18 – 1954-11-13Crater 2
- 1942 (±5 yrs)VEI 1Geological estimate1942 – OngoingCrater 2
- 1907VEI 2Observed1907 – OngoingNE Crater (crater 2)
- 1900VEI 2Observed1900 – OngoingNorth Crater (crater 1)
- 1890VEI 0Observed1890 – Ongoing
- 1884VEI 2Observed1884 – Ongoing
- 1878VEI 2Observed1878 – OngoingCrater 2
External links
⚠ For reference only. Not for emergency response.