Galunggung
Estratovolcán · Indonesia · 2168 m

- Tipo
- Estratovolcán
- País
- Indonesia
- Región
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- Altitud
- 2168 m
- Coordenadas
- -7.250, 108.058
- Última erupción
- 1984
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
The forested slopes of Galunggung in western Java SE of Bandung are cut by a 2-km-wide collapse scarp open towards the ESE. The "Ten Thousand Hills of Tasikmalaya" dotting the plain below the volcano are debris-avalanche hummocks from the collapse about 4,200 years ago. An eruption in 1822 produced pyroclastic flows and lahars that killed over 4,000 people. A series of major explosive eruptions starting in April 1982 destroyed a number of villages, killed as many as 30 people, and forced over 60,000 to evacuate. Pyroclastic flows and heavy widespread ash caused significant damage. A large passenger jet that encountered the ash plume on 24 June lost power to all four engines but managed to land safely in Jakarta. The 1982 activity destroyed a 1918 dome and formed the Warirang crater, almost as wide as the valley, about 2 km down from the summit.
Resumen de Wikipedia
Resumen en inglésMount Galunggung is an active stratovolcano in West Java, Indonesia, around 80 km (50 mi) southeast of the West Java provincial capital, Bandung. Mount Galunggung is part of the Sunda Arc extending through Sumatra, Java and the Lesser Sunda Islands, which has resulted from the subduction of the Australian Plate beneath the Eurasian Plate.
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Historial de erupciones
Línea de tiempo detallada
- 1984VEI 1Observado1984-01-09 – 1984-01-31
- 1982VEI 4Observado1982-04-05 – 1983-01-08New crater at Gunung Jadi location
- 1918VEI 1Observado1918-07-17 – 1918-07-30Gunung Jadi
- 1894VEI 3Observado1894-10-17 – 1894-12
- 1822VEI 5Observado1822-10-08 – 1822-12-01
- 850 (±50 años)VEI ?Estimación geológica850 – En curso
- 2250 a. C. (±150 años)VEI 5Estimación geológicaBCE 2250 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.