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パトゥハ山

Patuha

成層火山 · Indonesia · 2422m

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.” · 写真: Photo published in Taverne, 1926 "Vulkaanstudien op Java," (courtesy of Volcanological Survey of Indonesia).
タイプ
成層火山
Indonesia
地域
スンダ・バンダ / Sunda Volcanic Arc
標高
2422m
座標
-7.162, 107.400
最終噴火
不明
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Andesite / Basaltic Andesite
地質学的概要

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.

噴火履歴

詳細タイムライン

噴火記録はありません。

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。