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Cerro Capurata
Mountain in Bolivia From Wikipedia, the free encyclopedia
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Cerro Capurata, also known as Elena Capurata or Quimsachatas[3] is a stratovolcano in the Andes of Bolivia and Chile.[4] To the south of Capurata lies Cerro Casparata and straight west Guallatiri, which shares a near-identical elevation with Capurata.[5]
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Geography and geomorphology
It is on the border of the Parinacota Province of Chile (Putre commune) and of the Bolivian province of Sajama (commune Turco).[1] Compared to Acotango and Humurata, Capurata's rocks are relatively well preserved. Some hydrothermal alteration, partly associated with fumarolic activity, is present however.[6] The total volume of the edifice is 19 cubic kilometres (4.6 cu mi)[7] and has been eroded by glaciers. The volcano is formed by lava domes, lava flows and pyroclastic flows.[8] Sulfur deposits formed by solfataras are also found on Capurata.[9] The west side of the mountain is covered with snow and ice.[10] Two crater depressions on the summit have an appearance that suggests a Holocene age.[8]
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Incan Ruins and First Ascent

A 10 by 5 metres (33 ft × 16 ft) ruin towards the northern site of the summit. The structure was probably built by the Inkas and it was photographed by Pedro Hauck during his last ascent in 2014.[11] The first recorded climb is by Pedro Rosende and Ignacio Morlans (Chile) in 10/07/1967.[12][13]
Elevation
It has an official height of 5990 metres,[14][a][b] but handheld GPS devices have indicated that it is actually 6,013 metres (19,728 ft)[19] or 6,014 metres (19,731 ft) high.[11]
See also
Notes
- The height of the nearest key col is 5,409 metres (17,746 ft),[1] leading to a topographic prominence of 602 metres (1,975 ft) with a topographical dominance of 12.08%. Its parent peak is Acotango and the Topographic isolation is 3.7 kilometres (2.3 mi).[1]
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References
External links
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