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Monte Penanggungan

Penanggungan

Estratovolcán · Indonesia · 1631 m

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.
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. · Foto: Photo by Lee Siebert, 1995 (Smithsonian Institution). · Wikimedia Commons
Tipo
Estratovolcán
País
Indonesia
Región
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Altitud
1631 m
Coordenadas
-7.616, 112.620
Última erupción
Desconocido
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

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.

Resumen de Wikipedia

El monte Penanggungan es un pequeño estratovolcán, ubicado al norte del complejo volcánico de Arjuno-Welirang en la provincia de Java Oriental de la isla de Java, en Indonesia. Tiene una cumbre de 1653 metros.

Wikipedia · CC BY-SA · Leer artículo completo →

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
200~200 · 1 erupciones · VEI máx. ?200200201201201

Línea de tiempo detallada

  1. 200VEI ?Estimación geológica
    200 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.