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Indonesia · Estratovolcán

Monte Patuha

Patuha

Tipo
Estratovolcán
Altitud
2422 m
Última erupción
Desconocido
An aerial view from the NNW shows the two summit craters of Gunung Patuha volcano in the foreground. Steep-walled Taman Saat crater (left) is located NW of lake-filled Kawah Putih (right). The dashed circle at the middle left indicates an unvegetated area called the “Tugeslibde crater.”
An aerial view from the NNW shows the two summit craters of Gunung Patuha volcano in the foreground. Steep-walled Taman Saat crater (left) is located NW of lake-filled Kawah Putih (right). The dashed circle at the middle left indicates an unvegetated area called the “Tugeslibde crater.” · Foto: Photo published in Taverne, 1926 "Vulkaanstudien op Java," (courtesy of Volcanological Survey of Indonesia).
Tipo
Estratovolcán
País
Indonesia
Región
Sunda y Banda / Sunda Volcanic Arc
Altitud
2422 m
Coordenadas
-7.162, 107.400
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica
Resumen geológico

The forested andesitic Gunung Patuha rises SW of the plain of Bandung in western Java. Patuha is the northern peak of a roughly 5-km-long N-S volcanic massif, and has a 300 m crater at the summit. A few hundred meters down the SE flank is a 400 x 500 m crater almost completely filled with a shallow greenish lake, Kawah Putih. Sulfur deposits are present around the shoreline and near active fumaroles on the crater walls. A large debris-avalanche deposit extends down the NE flank. The volcano was formed during the late Pleistocene, but no Holocene eruptions are known.

Resumen de Wikipedia

Resumen en inglés

Mount Patuha is a twin stratovolcano about 50 km to the southwest of Bandung in West Java, Indonesia. It is located in the Bandung District of West Java. It is one of numerous volcanoes in this area; others in the region include Mount Malabar, Mount Wayang, and Mount Papandayan.

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