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Geological Formation

Aconcagua

Structural and Tectonic Formations

Aconcagua rises in the Principal Cordillera of the Andes in Mendoza Province, Argentina, reaching a summit elevation of about 6,967 meters, the highest mountain in the Americas, the highest peak outside Asia, and the highest point in both the Western and Southern Hemispheres. It is a non-volcanic peak raised by Andean tectonic uplift, the second-most topographically prominent peak in the world after Everest, and one of the Seven Summits, the highest peaks on each continent. This entity documents Aconcagua specifically as a geological formation, a distinct facet from its treatment as a place and landform on the Geography Atlas; this entry covers the mountain's tectonic origin and its standing as the highest peak of the Americas and of the Southern and Western Hemispheres.

Facts
Classification
Protected Status
Locally or Regionally Protected 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Aconcagua

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Aconcagua
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Aconcagua
Sources
1. Aconcagua (Wikipedia)
Lead section (protected-status)
Quote, Lead section (protected-status)
It is bounded by the Vacas Valley to the north and east and the Horcones Inferior Valley to the west and south, and is protected within Aconcagua Provincial Park.
View the Source
Wikidata: Aconcagua
Wikidata Q39739, class allow-list match (w-wdresolver-0926)View the Source
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