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Latest news
Спутниковое изображение вулкана Tangkubanparahu  7 Sep 2019
Saturday, Sep 07, 2019
Консультативный центр по вулканическому пеплу (VAAC) в Wellington выпустил следующий отчет: ... [подробнее]
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. [подробнее]
 

Tangkubanparahu вулкан

Стратовулкан 2084 m (6,837 ft.)
Западная Ява, Индонезия, -6.77°S / 107.6°E
Текущее состояние: беспокойный (2 из 5)
Tangkubanparahu Веб-камеры / данные в реальном времени | Reports
Tangkubanparahu volcano books
Last update: 7 Sep 2019 (Volcanic Ash Advisory)
Типичный извержения стиль: Explosive. Frequent phreatic explosions during the past centuries.
Tangkubanparahu Вулкан-извержения: 1826, 1829, 1842, 1846, 1896, 1910, 1926, 1929, 1952, 1957, 1961, 1965, 1967, 1969, 1983, 1985(?), 2013 (21 Feb-6 Mar, 5 Oct), 2019 Нет недавних землетрясений
ВремяМагнитный / ГлубинаРасстояниеМестоположение
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.

Справочная информация:

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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