Cordillera Paine

The Cordillera Paine is a mountain group in Torres del Paine National Park in Chilean Patagonia. It is located 280 km (170 mi) north of Punta Arenas, and about 1,960 km (1218mi) south of the Chilean capital Santiago. It belongs to the Commune of Torres del Paine in Última Esperanza Province of Magallanes and Antártica Chilena Region. No accurate surveys have been published, and published elevations have been claimed to be seriously inflated, so most of the elevations given on this page are approximate.[1] Paine means "blue" in the native Tehuelche (Aonikenk) language and is pronounced PIE-nay.[2]

This article is about the mountain range. For the national park in Chile, see Torres del Paine National Park. For the Chilean commune, see Torres del Paine, Chile.
Cordillera Paine
Torres del Paine, Chile
Highest point
PeakCerro Paine Grande
Elevation2,884 m (9,462 ft)
Coordinates50°59′56″S 73°05′43″W 
Geography
NASA image with annotations
CountryChile
RegionMagallanes y Antártica Chilena
Range coordinates51°S 73°W
Parent rangePatagonian Andes
Geology
Age of rock12 Myr
Type of rockGranite

Peaks

The highest summit of the range is Cerro Paine Grande. For a long time its elevation was claimed to be 3,050 m or 3,251 m, but in August 2011 it was ascended for the third time, measured using GPS and found to be 2,884 m.[3]

The three Towers of Paine (Spanish: Torres del Paine) form the centrepiece of Parque Nacional Torres del Paine. The South Tower of Paine (about 2,500 m in elevation,[1] is now thought to be the highest of the three, although this has not been definitely established. It was first climbed by Armando Aste. The Central Tower (about 2,460 m or 8,100 feet[1] in elevation) was first climbed in 1963 by Chris Bonington and Don Whillans. In 2017, three Belgian climbers, Nico Favresse, Siebe Vanhee and Sean Villanueva O'Driscoll, made the first free ascent up the rock face (about 1,200 m or 4000 feet). The North Tower (about 2,260 m in elevation) was first climbed by Guido Monzino.

Other summits include the Cuerno Principal, about 2,100 m in elevation,[1] and Cerro Paine Chico, which is usually quoted at about 2,650 m.[1]

Geology
Torres del Paine mafic sill complex built up by successive magma injections

The range is made up of a yellowish granite underlain by grey gabbro-diorite laccolith and the sedimentary rocks it intrudes, deeply eroded by glaciers. The steep, light colored faces are eroded from the tougher, vertically jointed granitic rocks, while the foothills and dark cap rocks are the sedimentary country rock, in this case flysch deposited in the Cretaceous and later folded.[4]

The radiometric age for the quartz diorite at Cerro Paine is 12 ± 2 million years by the rubidium-strontium method and 13 ± 1 million years by the potassium-argon method.[5] More precise ages of 12.59 ± 0.02 and 12.50 ± 0.02 million years for the earliest and latest identified phases of the intrusion, respectively, were achieved using Uranium–lead dating methods on single zircon crystals.[6] Basal gabbro and diorite were dated by a similar technique to 12.472 ± 0.009 to 12.431 ± 0.006 million years.[7] Thus, magma was intruded and crystallized over 162 ± 11 thousand years. High resolution dating and excellent 3-D exposure of the laccolith and its vertical feeding system allow detailed reconstruction of the Torres del Paine fossil magma chamber history.[8]

Hiking
Lago Pehoé

The Torres del Paine National Park—an area of 2,400 km²—was declared a Biosphere Reserve by the UNESCO in 1978 and receives about 250,000 visitors annually.[9] Trails and some campsites are maintained by Chile's National Forest Corporation, and mountain huts provide shelter and basic services.

The Paine "horns," with the typical extreme weather of the region
gollark: Gree™ings.
gollark: ++remind 17:21:50 uncontingent
gollark: ++remind 7h contingency 291V (spontaneous ubq nonexistence)
gollark: Oh dear.
gollark: We could even use the highly reliable osmarksVPS™, with its low* 80ms latency to Europe.

See also

References
  1. Biggar, John, 2015. The Andes: A Guide for Climbers (4th edition, ISBN 978-0-9536087-4-4). Several elevations given by this authority are much lower than those given by other authorities, and the higher elevations are not supported by official Chilean IGM maps.
  2. Abraham, Rudolf (2011). Torres del Paine: Trekking in Chile's Premier National Park. Milnthorpe: Cicerone Press. p. 17. ISBN 978-1-84965-356-5. Retrieved 4 August 2015.
  3. "Dispatch #7 - Expedición Paine Grande RELOADED". andesgear.expenews.com.
  4. Altenberger, Uwe; Oberhänsli, Roland; Putlitz, Benita; Wemmer, Klaus (1 July 2003). "Tectonic controls and Cenozoic magmatism at the Torres del Paine, southern Andes (Chile, 51°10'S)". Revista geológica de Chile. 30 (1): 65–81. doi:10.4067/S0716-02082003000100005.
  5. Martin Halpern "Regional Geochronology of Chile South of 50 degrees Latitude", Bulletin Geological Society of America, v. 84, p. 2410, 1973.
  6. Juergen Michel, Lukas Baumgartner, Benita Putlitz, Urs Schaltegger and Maria Ovtcharova, Incremental growth of the Patagonian Torres del Paine Laccolith over 90 k.y., Geology, 36(6):459-462, 2008.
  7. Leuthold, Julien; Müntener, Othmar; Baumgartner, Lukas; Putlitz, Benita; Ovtcharova, Maria; Schaltegger, Urs (2012). "Time resolved construction of a bimodal laccolith (Torres del Paine, Patagonia)". Earth and Planetary Science Letters. 325–326: 85–92. doi:10.1016/j.epsl.2012.01.032.
  8. Leuthold, Julien; Müntener, Othmar; Baumgartner, Lukas; Putlitz, Benita (2014). "Petrological constraints on the recycling of mafic crystal mushes and intrusion of braided sills in the Torres del Paine Mafic Complex (Patagonia)" (PDF). Journal of Petrology. 55 (5): 917–949. doi:10.1093/petrology/egu011.
  9. http://www.conaf.cl/wp-content/files_mf/1486060377Tot_a%C3%B1o_2016.pdf
  • Biggar, John, 2015. The Andes: A Guide for Climbers (4th edition, ISBN 978-0-9536087-4-4).
  • Kearney, Alan, 1993. Mountaineering in Patagonia. Seattle USA: Cloudcap.
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