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Mount Tondano

Mount Tondano in the province of North Sulawesi, Sulawesi, Indonesia, has a 20 × 30 km wide caldera which was formed in the Late Miocene or Early Pliocene[2] by a massive eruption. Post caldera activity includes pyroclastic cones, obsidian flows and geothermal areas in the caldera area. Lake Tondano lies in the east side of the caldera.[1]

Mount Tondano
Highest point
Elevation1,202 m (3,944 ft)[1]
Coordinates1°14′N 124°50′E / 1.23°N 124.83°E / 1.23; 124.83[1]
Geography
Mount Tondano
Sulawesi, Indonesia
Geology
Mountain typeCaldera
Last eruptionUnknown

The 5 km long and 3.5 km wide ellipsoidal Pangolombian caldera lies entirely within the Tondano Caldera, and formed from a large eruption of an older Somma volcano.[2]

In more recent times, the somma volcanoes of Soputan, Sempu, Lokon-Empung and Mahawu have been constructed along the rim of the Tondano caldera, with Soputan being the youngest and most frequently active of the group.[1] The Tondano caldera has been investigated as a potential source for geothermal energy to support the growing population in the vicinity of the caldera.[2] Energy demand has been growing in Indonesia, and the Tondano caldera system could potentially provide clean energy for thousands of residents in northern Sulawesi.[2]

See also

References

  1. ^ a b c d "Tondano Caldera". Global Volcanism Program. Smithsonian Institution. Retrieved 2006-12-31.
  2. ^ a b c d "Lahendong Geothermal Field, Indonesia: Geothermal Model based on wells LHD-23 and LHD-28" (PDF). December 2010.

mount, tondano, province, north, sulawesi, sulawesi, indonesia, wide, caldera, which, formed, late, miocene, early, pliocene, massive, eruption, post, caldera, activity, includes, pyroclastic, cones, obsidian, flows, geothermal, areas, caldera, area, lake, ton. Mount Tondano in the province of North Sulawesi Sulawesi Indonesia has a 20 30 km wide caldera which was formed in the Late Miocene or Early Pliocene 2 by a massive eruption Post caldera activity includes pyroclastic cones obsidian flows and geothermal areas in the caldera area Lake Tondano lies in the east side of the caldera 1 Mount TondanoHighest pointElevation1 202 m 3 944 ft 1 Coordinates1 14 N 124 50 E 1 23 N 124 83 E 1 23 124 83 1 GeographyMount TondanoSulawesi IndonesiaGeologyMountain typeCalderaLast eruptionUnknownThe 5 km long and 3 5 km wide ellipsoidal Pangolombian caldera lies entirely within the Tondano Caldera and formed from a large eruption of an older Somma volcano 2 In more recent times the somma volcanoes of Soputan Sempu Lokon Empung and Mahawu have been constructed along the rim of the Tondano caldera with Soputan being the youngest and most frequently active of the group 1 The Tondano caldera has been investigated as a potential source for geothermal energy to support the growing population in the vicinity of the caldera 2 Energy demand has been growing in Indonesia and the Tondano caldera system could potentially provide clean energy for thousands of residents in northern Sulawesi 2 See also Edit Indonesia portalList of volcanoes in IndonesiaReferences Edit a b c d Tondano Caldera Global Volcanism Program Smithsonian Institution Retrieved 2006 12 31 a b c d Lahendong Geothermal Field Indonesia Geothermal Model based on wells LHD 23 and LHD 28 PDF December 2010 This North Sulawesi location article is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Mount Tondano amp oldid 1153121745, wikipedia, wiki, book, books, library,

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