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Mount Tongkoko

Tangkoko-Duasudara

Stratovulcano · 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
Stratovulcano
Paese
Indonesia
Regione
Western Pacific Volcanic Regions / Sangihe Volcanic Arc
Altitudine
1334 m
Coordinate
1.518, 125.185
Ultima eruzione
1880
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

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.

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1680~1700 · 3 eruzioni · VEI max. 51800~1820 · 1 eruzioni · VEI max. 21820~1840 · 1 eruzioni · VEI max. 01840~1860 · 1 eruzioni · VEI max. 21860~1880 · 1 eruzioni · VEI max. 116801720178018201860

Cronologia dettagliata

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

Link esterni

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