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Mount Tangkoko

(Redirected from Mount Tongkoko)

Mount Tangkoko
Mount Tangkoko as viewed from the sea
Highest point
Elevation1,113 m (3,652 ft)[1]
Coordinates1°31′05″N 125°11′06″E / 01.518°N 125.185°E / 01.518; 125.185[2]
Dimensions
Width3 km × 1.5 km (1.86 mi × 0.93 mi)[3]
Geography
Mount Tangkoko is located in Sulawesi
Mount Tangkoko
Mount Tangkoko
Location within Sulawesi
Country
Indonesia
Sulawesi
North Sulawesi
Minahasa
Geology
stratovolcano with lava dome[3]
Rock types[3]
Last eruption1880; 146 years ago (1880)[2]
Mount Tangkoko summit blanketed in cloud, its flanks covered in dense vegetation

Mount Tangkoko[4] is a stratovolcano in the north of Sulawesi island in Indonesia. Its summit has an elongated deep crater.On the east flank is a flat lava dome, Batu Angus. Historical records only show eruptions in the 17th and 19th centuries, including a possible VEI5 eruption in 1680.[2]

The Tangkoko Batuangus Nature Reserve, in the northern part of Sulawesi island, is named after the volcano and home to such species as the Celebes crested macaque and spectral tarsier.

See also

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References

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Citations

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  1. "Tangkoko-Duasudara - synonyms & subfeatures". Global Volcanism Program. Smithsonian Institution. Retrieved 29 April 2023.
  2. 1 2 3 "Tangkoko-Duasudara". Global Volcanism Program. Smithsonian Institution. Retrieved 29 April 2023.
  3. 1 2 3 "Tangkoko-Duasudara - general information". Global Volcanism Program. Smithsonian Institution. Retrieved 29 April 2023.
  4. "Aset Sejarah Alam Dunia dan Rumah Satwa Sulawesi" [World natural history assets and Sulawesi animal house]. Nasional.Kompas.com (in Indonesian). Kompas. 30 April 2008. Retrieved 29 April 2023.

Bibliography

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  • Morrice, M G; Jezek, P A; Gill, J B; Whitford, D J; Monoarfa, M (1983). "An introduction to the Sangihe arc: volcanism accompanying arc-arc collision in the Molucca Sea, Indonesia". J. Volcanol. Geotherm. Res. 19: 135–165.
  • Tatsumi, Y; Murasaki, M; Arsadi, E M; Nohda, S (1991). "Geochemistry of Quaternary lavas from NE Sulawesi: transfer of subduction components into the mantle wedge". Contr Mineral Petr. 107: 137–149.
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