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Latest news
Monday, Jan 12, 2015
The volcano was placed on higher alert level (2 on a scale 1-4) on 31 Dec, as signs of volcanic unrest have recently been increasing (deformation, seismic activity). ... [more]
Tuesday, Oct 15, 2013
No more eruptions have occurred since the series of 11 phreatic explosions between Saturday and Tuesday last week (5-8 Oct), but VSI continues to detect volcanic tremor. ... [more]

Tangkubanparahu volcano

Stratovolcano 2084 m (6,837 ft.)
West Java, Indonesia, -6.77°S / 107.6°E
Current status: restless (2 out of 5)
Tangkubanparahu webcams / live data
Tangkubanparahu volcano books
Last update: 12 Jan 2015
Typical eruption style: Explosive. Frequent phreatic explosions during the past centuries.
Tangkubanparahu volcano eruptions: 1826, 1829, 1842, 1846, 1896, 1910, 1926, 1929, 1952, 1957, 1961, 1965, 1967, 1969, 1983, 1985(?)
TimeMag. / DepthDistanceLocation
Tue, 18 Jul
Tue, 18 Jul 05:58 UTCM 4.1 / 24.5 km17 km- 8km SE of Banjaran, Indonesia
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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