Cerro Cañapa Explained

Cerro Cañapa
Elevation M:5882
Elevation Ref:[1]
Prominence M:1595
Prominence Ref:[2]
Listing:Ultra
Location:Potosí Department, Bolivia
Map:Bolivia
Coordinates:-21.45°N -72°W

Cerro Cañapa is an elongated mountain in Bolivia, with a height of 5882 m, close to the border with Chile. Note that the international border in this area is a straight line that runs from Cerro Araral to Ollagüe, leaving Cerro Cañapa completely in Bolivian territory.

The mountain forms an enormous backdrop to the colorful lakes Cañapa and Hedionda.

The mountain is constructed from andesite and dacite. Volcanism of Canapa was influenced by local northwest-striking normal fault zones which also affected the Luxsar and Toconce volcanoes.[3] The range is partially underpinned by modern ignimbrites. Canapa has deposits left by solfataras.[4] The volcanic range is 50- long and may have originated from deep-seated basement lineaments.[5] Volcanism is Pliocene-Pleistocene in age.[6]

See also

Notes and References

  1. Topographic map Cerro Araral, Chile; Bolivia SF-19-7, Joint Operations Graphic 1:250,000, U.S. National Imagery and Mapping Agency
  2. http://peaklist.org/WWlists/ultras/bolivia.html "Bolivia Ultra-Prominences"
  3. Tibaldi. A.. Corazzato. C.. Rovida. A.. Miocene–Quaternary structural evolution of the Uyuni–Atacama region, Andes of Chile and Bolivia. Tectonophysics. June 2009. 471. 1–2. 114–135. 10.1016/j.tecto.2008.09.011.
  4. Book: Avila-Salinas. Waldo. Andean Magmatism and Its Tectonic Setting . Petrologic and tectonic evolution of the Cenozoic volcanism in the Bolivian western Andes. Geological Society of America Special Papers . 265. 1991. 245–258. 0072-1077. 10.1130/SPE265-p245. 0-8137-2265-9 .
  5. Jacques. JohnM.. A tectonostratigraphic synthesis of the Sub-Andean basins: implications for the geotectonic segmentation of the Andean Belt. Journal of the Geological Society. 160. 5. 2003. 687–701. 0016-7649. 10.1144/0016-764902-088. 131412884 .
  6. 355825. Cañapa.