ペナンガンガン山

Penanggungan

成層火山 · Indonesia · 1631m

Gunung Penanggungan, seen here from Tengger caldera to its east, was constructed immediately north of the Arjuno-Welirang massif with its flanks forming the ridge at the left. Lava flows from flank vents give the volcano an irregular profile. Lava flows have descended all flanks of the volcano and pyroclastic flow deposits form an apron around it. · 写真: Photo by Lee Siebert, 1995 (Smithsonian Institution). · Wikimedia Commons

タイプ: 成層火山
国: Indonesia
地域: Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
標高: 1631m
座標: -7.616, 112.620
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

Gunung Penanggungan, one of Java's most revered mountains, is a small stratovolcano immediately north of the Arjuno-Welirang massif. Numerous ruins of sanctuaries, monuments, and sacred bathing places dating from 977-1511 CE are found on the northern and western flanks. Lava flows from flank vents descend to all sides and pyroclastic-flow deposits form an apron around it. It was mapped as similar in age to Arjuno-Welirang and Semeru volcanoes by van Bemmelen (1937). Considered to be extinct for at least 1000 years, its last eruption may have occurred about 200 CE.

Wikipedia の要約

英語版の要約

Mount Penanggungan is a small stratovolcano, immediately north of the Arjuno-Welirang volcanic complex in East Java province, Java island, Indonesia. Mount Penanggungan is about 40 kilometers (24.8 mi) south of Surabaya, and can be seen from there on a clear day. Several Hindu-Buddhist sanctuaries, sacred places and monuments are on the western slope of the mountain dating from AD 977–1511. Lava flows and pyroclastic deposits are around the volcano.

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噴火履歴

概要 (VEI時系列)

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詳細タイムライン

200年VEI ?地質学的推定
200 ~ 進行中

外部リンク

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