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Geological Formation

Cerro Torre

Inselbergs and Crystalline Monoliths

Cerro Torre is a slender granite spire rising to about 3,128 meters in the Southern Patagonian Ice Field on the border of Argentina and Chile, part of the same granite batholith, intruded and cooled deep underground over the last several million years, that also produced the nearby Fitz Roy massif. Its extremely steep, narrow form is the product of intense glacial erosion: surrounding softer rock and less resistant portions of the granite mass were stripped away by the ice field's glaciers, while the hardest, most resistant granite core was carved into an almost vertical needle, further sharpened by the region's severe wind, ice and precipitation. Frequently capped by a mushroom-like formation of rime ice built up by Patagonia's ferocious winds, Cerro Torre is regarded as one of the most technically demanding and visually striking granite spires on Earth.

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Classification
Protected Status
UNESCO World Heritage Site 1
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Glaciation, Processes

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Source Wikidata: Cerro Torre

Also in Geography Atlas: where this subject is found.

Source Wikidata: Cerro Torre
Sources
1. Los Glaciares National Park (Wikipedia)
  • Description of the northern half
    The northern half consists of part of Viedma Lake, the Viedma Glacier and a few minor glaciers, and a number of mountains very popular among fans of climbing and trekking, including Mount Fitz Roy and Cerro Torre.
  • Lead section, World Heritage
    In 1981, it was declared a World Heritage Site by UNESCO.
View the Source
Wikidata: Cerro Torre
Wikidata Q1056102, class allow-list match (w-wdresolver-0926)View the Source
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