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Mount Tongkoko

Tangkoko-Duasudara

Estratovolcán · Indonesia · 1334 m

The 1149-m-high elongated Tongkoko volcano, seen in this composite photo from the south, rises above Bitung city and is the NE-most volcano on the island of Sulawesi.  The summit of the volcano, which is elongated in a NW-SE direction, contains a large crater with a central cone.  Historical eruptions have occurred since 1680 from both the summit and an east flank vent, Batu Angus.  Tongkoko volcano and its neighbor Dua Saudara are the most prominent features of Gunung Dua Saudara National Park, a noted wildlife preserve.
The 1149-m-high elongated Tongkoko volcano, seen in this composite photo from the south, rises above Bitung city and is the NE-most volcano on the island of Sulawesi. The summit of the volcano, which is elongated in a NW-SE direction, contains a large crater with a central cone. Historical eruptions have occurred since 1680 from both the summit and an east flank vent, Batu Angus. Tongkoko volcano and its neighbor Dua Saudara are the most prominent features of Gunung Dua Saudara National Park, a noted wildlife preserve. · Foto: Photo by A.R. Sumailani, 1973 (Volcanological Survey of Indonesia). · Wikimedia Commons
Tipo
Estratovolcán
País
Indonesia
Región
Western Pacific Volcanic Regions / Sangihe Volcanic Arc
Altitud
1334 m
Coordenadas
1.518, 125.185
Última erupción
1880
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The eastern peninsula at the far NE end of Sulawesi near the city of Bitung is occupied by a volcanic complex consisting of two major edifices within a nature reserve. To the north is Tangkoko (also known as Tongkoko), with a large caldera (~3 x 1.5 km) elongated towards the SE from the highest rim point; the rim at the opposite end is more than 400 m lower. Eruptions occurred from the summit crater in the 17th century and in 1801, when the caldera also reportedly contained a cone surrounded by a lake. About 1.5 km down the outer E flank is the Batuangus (or Batu Angus) lava dome, formed in 1801, along with an adjacent vent (Baru Batuangus) that has been the source of all subsequent eruptions. The higher Duasudara (also Dua Suadara) edifice is ~4.5 km SW of the Tangkoko summit. A NE-facing scarp appears to have a hummocky debris flow that reaches the base of Tangkoko.

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1680~1700 · 3 erupciones · VEI máx. 51800~1820 · 1 erupciones · VEI máx. 21820~1840 · 1 erupciones · VEI máx. 01840~1860 · 1 erupciones · VEI máx. 21860~1880 · 1 erupciones · VEI máx. 116801720178018201860

Línea de tiempo detallada

  1. 1880VEI 1Observado
    1880 – En curso
    Batu Angus
  2. 1843VEI 2Observado
    1843 – 1846
    Batu Angus
  3. 1821VEI 0Observado
    1821 – En curso
    Batu Angus Baru
  4. 1801VEI 2Observado
    1801 – En curso
    Summit and east flank (Batu Angus)
  5. 1694VEI 3Observado
    1694 – En curso
  6. 1683VEI 3Observado
    1683 – En curso
  7. 1680VEI 5Observado
    1680 – En curso

Enlaces externos

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