Langila
Gunung api kompleks · Papua New Guinea · 1330 m

- Tipe
- Gunung api kompleks
- Negara
- Papua New Guinea
- Wilayah
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Ketinggian
- 1330 m
- Koordinat
- -5.525, 148.420
- Letusan terakhir
- 2026
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisLangila 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.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 2015VEI 2Teramati2015-10-22 – 2026-03-16Crater 2
- 2013VEI ?Teramati2013-10-23 – 2013-12-01
- 2012VEI 1Teramati2012-12-01 – 2012-12-05Summit craters
- 2012VEI 0Teramati2012-07-21 – 2012-07-21
- 2011VEI 0Teramati2011-07-28 – 2011-07-28
- 2009VEI 2Teramati2009-09-16 – 2010-02-16Crater 2
- 2006VEI 2Teramati2006-08-09 – 2008-07-06
- 2005VEI 2Teramati2005-04-19 – 2006-03-31
- 2004VEI 2Teramati2004-01-20 – 2004-01-27
- 2004VEI 2Teramati2004-11-24 – 2004-12-25
- 2002VEI 2Teramati2002-05-25 – 2003-04-09Crater 2
- 1973VEI 3Teramati1973-02-24 – 2000-10-16Crater 3, Crater 2
- 1971VEI 2Teramati1971-01-26 – 1972-07-05Crater 2
- 1970VEI 2Teramati1970-05-20 – 1970-09-22Crater 2
- 1969VEI 2Teramati1969-09-29 – 1969-09-29Crater 2 or 3
- 1967VEI 2Teramati1967-01-19 – 1968-06-16Crater 2, Crater 3
- 1964VEI 2Teramati1964-12-04 – 1966-09-23Crater 2, Crater 3
- 1962VEI 2Teramati1962-03-16 – 1963-08-11Crater 2, Crater 3
- 1960VEI 2Teramati1960-12-19 – 1961-09-25Crater 3, Crater 2
- 1958VEI 2Teramati1958-04-21 – 1958-06-04Crater 2
- 1956VEI 2Teramati1956-03-25 – 1956-03-31Crater 2
- 1955VEI 2Teramati1955-02-15 – 1955-02-17Crater 2
- 1955VEI 2Teramati1955-06-01 – 1955-06-16Crater 2
- 1954VEI 3Teramati1954-05-18 – 1954-11-13Crater 2
- 1942 (±5 tahun)VEI 1Perkiraan geologi1942 – BerlangsungCrater 2
- 1907VEI 2Teramati1907 – BerlangsungNE Crater (crater 2)
- 1900VEI 2Teramati1900 – BerlangsungNorth Crater (crater 1)
- 1890VEI 0Teramati1890 – Berlangsung
- 1884VEI 2Teramati1884 – Berlangsung
- 1878VEI 2Teramati1878 – BerlangsungCrater 2
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.