51:
501:
131:
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334:. In 2017, three Belgian climbers, Nico Favresse, Siebe Vanhee and Sean Villanueva O'Driscoll, made the first free ascent up the rock face, which is about 1,200 m (3,900 ft). The North Tower (about 2,260 m (7,410 ft) in elevation) was first climbed in 1958 by
306:
The highest summit of the range is Cerro Paine Grande. For a long time its elevation was claimed to be 3,050 or 3,251 m (10,007 or 10,666 ft), but in August 2011 it was ascended for the third time, measured using GPS and found to be 2,884 m (9,462 ft).
369:
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
322:. The South Tower of Paine (about 2,500 m (8,200 ft) in elevation, is now thought to be the highest of the three, although this has not been definitely established. It was first climbed in 1963 by
711:
Leuthold, Julien; MĂĽntener, Othmar; Baumgartner, Lukas; Putlitz, Benita; Ovtcharova, Maria; Schaltegger, Urs (2012). "Time resolved construction of a bimodal laccolith (Torres del Paine, Patagonia)".
701:
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.
341:
Other summits include the Cuerno
Principal, about 2,100 m (6,900 ft) in elevation, and Cerro Paine Chico, which is usually quoted at about 2,650 m (8,690 ft).
286:. 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.
559:). 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.
283:
744:"Petrological constraints on the recycling of mafic crystal mushes and intrusion of braided sills in the Torres del Paine Mafic Complex (Patagonia)"
155:
91:
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Martin
Halpern "Regional Geochronology of Chile South of 50 degrees Latitude", Bulletin Geological Society of America, v. 84, p. 2410, 1973.
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0.02 million years for the earliest and latest identified phases of the intrusion, respectively, were achieved using
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in 1978 and receives about 250,000 visitors annually. Trails and some campsites are maintained by Chile's
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methods on single zircon crystals. Basal gabbro and diorite were dated by a similar technique to 12.472
884:
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662:"Tectonic controls and Cenozoic magmatism at the Torres del Paine, southern Andes (Chile, 51°10'S)"
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326:. The Central Tower (about 2,460 m (8,070 ft) in elevation) was first climbed in 1963 by
267:
221:
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The Torres del Paine
National Park—an area of 2,400 km (930 sq mi)—was declared a
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and its vertical feeding system allow detailed reconstruction of the Torres del Paine fossil
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Altenberger, Uwe; Oberhänsli, Roland; Putlitz, Benita; Wemmer, Klaus (1 July 2003).
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Photograph of the cordillera from Estero Ăšltima
Esperanza, 50 km to the south
742:
Leuthold, Julien; MĂĽntener, Othmar; Baumgartner, Lukas; Putlitz, Benita (2014).
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This article is about the mountain range. For the national park in Chile, see
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11 thousand years. High resolution dating and excellent 3-D exposure of the
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http://www.conaf.cl/wp-content/files_mf/1486060377Tot_a%C3%B1o_2016.pdf
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0.006 million years. Thus, magma was intruded and crystallized over 162
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The Paine "horns", with the typical extreme weather of the region
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The radiometric age for the quartz diorite at Cerro Paine is 12
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Torres del Paine: Trekking in Chile's
Premier National Park
825:
489:, and mountain huts provide shelter and basic services.
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x666AFSFASDDFFA Patagonia Webcam and maps from Paine
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A view of the Torres from
Mirador base de las Torres
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595:"Dispatch #7 – Expedición Paine Grande RELOADED"
357:complex built up by successive magma injections
266:is located 280 km (170 mi) north of
8:
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27:Mountain group in Torres del Paine, Chile
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284:Magallanes and Antártica Chilena Region
294:(Aonikenk) language and is pronounced
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361:The range is made up of a yellowish
713:Earth and Planetary Science Letters
25:
840:Torres del Paine Circuit Planning
365:underlain by grey gabbro-diorite
320:Parque Nacional Torres del Paine
129:
49:
797:The Andes: A Guide for Climbers
679:10.4067/S0716-02082003000100005
549:The Andes: A Guide for Climbers
34:. For the Chilean commune, see
880:Torres del Paine National Park
870:Landforms of Magallanes Region
835:Torres del Paine on summitpost
572:. Milnthorpe: Cicerone Press.
253:Torres del Paine National Park
156:Magallanes y Antártica Chilena
32:Torres del Paine National Park
1:
409:. More precise ages of 12.59
79:2,884 m (9,462 ft)
812:Mountaineering in Patagonia
520:Los Glaciares National Park
487:National Forest Corporation
310:The three Towers of Paine (
290:means "blue" in the native
276:Commune of Torres del Paine
135:NASA image with annotations
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729:10.1016/j.epsl.2012.01.032
666:Revista GeolĂłgica de Chile
584:. Retrieved 4 August 2015.
318:) form the centrepiece of
29:
865:Ăšltima Esperanza Province
814:. Seattle USA: Cloudcap.
395:rubidium-strontium method
280:Ăšltima Esperanza Province
127:
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860:Mountain ranges of Chile
763:10.1093/petrology/egu011
613:"1962 – Torri del Paine"
568:Abraham, Rudolf (2011).
721:2012E&PSL.325...85L
405:1 million years by the
393:2 million years by the
353:Torres del Paine mafic
251:is a mountain group in
55:Torres del Paine, Chile
36:Torres del Paine, Chile
599:andesgear.expenews.com
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407:potassium-argon method
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810:Kearney, Alan, 1993.
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107:50.99889°S 73.09528°W
795:Biggar, John, 2015.
751:Journal of Petrology
547:Biggar, John, 2015.
274:. It belongs to the
112:-50.99889; -73.09528
772:20.500.11850/103136
427:Uranium–lead dating
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715:. 325–326: 85–92.
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382:and later folded.
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69:Cerro Paine Grande
61:Highest point
875:Miocene magmatism
805:978-0-9536087-4-4
582:978-1-84965-356-5
557:978-0-9536087-4-4
479:Biosphere Reserve
378:deposited in the
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163:Range coordinates
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672:(1): 65–81.
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644:. Retrieved
641:erratic-rock
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620:. Retrieved
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372:country rock
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332:Don Whillans
324:Armando Aste
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268:Punta Arenas
248:
246:
235:Type of rock
203:Parent range
885:Cordilleras
222:Age of rock
208:Patagonian
188: /
110: /
85:Coordinates
854:Categories
646:2020-11-08
622:2020-11-08
526:References
473:Lago Pehoé
380:Cretaceous
264:cordillera
98:73°05′43″W
95:50°59′56″S
461:history.
455:laccolith
367:laccolith
292:Tehuelche
260:Patagonia
185:51°S 73°W
123:Geography
75:Elevation
515:Fitz Roy
509:See also
272:Santiago
190:-51; -73
717:Bibcode
481:by the
363:granite
345:Geology
312:Spanish
296:PIE-nay
257:Chilean
240:Granite
216:Geology
142:Country
803:
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483:UNESCO
465:Hiking
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397:and 13
391:
387:
376:flysch
262:. The
152:Region
747:(PDF)
574:p. 17
302:Peaks
288:Paine
210:Andes
146:Chile
801:ISBN
578:ISBN
553:ISBN
355:sill
330:and
247:The
176:73°W
173:51°S
66:Peak
767:hdl
759:doi
725:doi
674:doi
282:of
278:in
255:in
228:Myr
226:12
856::
807:).
765:.
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38:.
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.