Mount Tangkoko

(Redirected from Mount Tongkoko)

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, there is a flat lava dome Batu Angus. Historical records only show eruptions in the nineteenth century.[2]

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
Widthkm × 1.5 km (1.86 mi × 0.93 mi)[3]
Geography
Mount Tangkoko is located in Sulawesi
Mount Tangkoko
Mount Tangkoko
Location in Sulawesi
Country Indonesia
RegionSulawesi
ProvinceNorth Sulawesi
RegencyMinahasa
Geology
Mountain typestratovolcano with lava dome[3]
Type of rock[3]
Last eruption1880; 144 years ago (1880)[2]
Mount Tangkoko summit blanketed in cloud, its flanks covered in dense vegetation

The Tangkoko Batuangus Nature Reserve, in the northern part of Sulawesi island, is named after the volcano and is a refuge for 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. ^ a b c "Tangkoko-Duasudara". Global Volcanism Program. Smithsonian Institution. Retrieved 29 April 2023.
  3. ^ a b c "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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