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Fotos al azar
Latest news
Satellite image of Tangkubanparahu volcano on  7 Sep 2019
Saturday, Sep 07, 2019
Volcanic Ash Advisory Center Wellington (VAAC) issued the following report: ... [Leer más]
Explosion in progress this morning. Credit: PVMBG
Friday, Aug 02, 2019
Following increasing seismicity, gas emissions and deformation, and an isolated phreatic eruption last week, activity has again increased after a slight drop-off, with a number of further explosions over the last day. The alert level was raised to 2 (Waspdada) on a scale of 1-4; an exclusion zone of 1500m is in place. [Leer más]
 

Tangkubanparahu volcano

Stratovolcano 2084 m (6,837 ft.)
West Java, Indonesia, -6.77°S / 107.6°E
Current status: normal or dormant (1 out of 5)
Tangkubanparahu webcams / datos en tiempo real | Reports
Tangkubanparahu volcano books
Last update: 7 Sep 2019 (Volcanic Ash Advisory)
Typical eruption style: Explosive. Frequent phreatic explosions during the past centuries.
Erupciones del volcán Tangkubanparahu: 1826, 1829, 1842, 1846, 1896, 1910, 1926, 1929, 1952, 1957, 1961, 1965, 1967, 1969, 1983, 1985(?), 2013 (21 Feb-6 Mar, 5 Oct), 2019 No hay terremotos recientes
Fecha / HoraRevista / ProfundidadDistanciaUbicación
Tangkubanparahu (also known as Tangkuban Perahu) is a broad shield-like stratovolcano overlooking Indonesia's former capital city of Bandung. Its scenic beauty and the closeness to Bandung makes it a very popular tourist destination.

Background:

Tangkuban Parahu was constructed within the 6 x 8 km Pleistocene Sunda caldera. The volcano's low profile is the subject of legends referring to the mountain of the "upturned boat."
The age the caldera-forming eruption exceeds the >40,000 year range of radiocarbon dating (Newhall and Dzurisin, 1988). The rim of Sunda caldera forms a prominent ridge on the western side; elsewhere the caldera rim is largely buried by deposits of Tangkubanparahu volcano. The dominantly small phreatic historical eruptions recorded since the 19th century have originated from several nested craters within an elliptical 1 x 1.5 km summit depression.
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Sources:
- GVP, Smithsonian Institution
- Newhall C G, Dzurisin D, 1988. Historical unrest at large calderas of the world. U S Geol Surv Bull, 1855: 1108 p, 2 vol


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