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Geological Formation

Alpamayo

Structural and Tectonic Formations

Alpamayo, also known by its older name Shuyturaju, stands in the Cordillera Blanca of the Peruvian Andes, immediately beside the slightly taller peak Quitaraju, with Alpamayo Creek rising on its northwestern flank. It is a non-volcanic, ice-clad granite peak, part of the same tectonically uplifted range that includes Huascarán, and is widely regarded as one of the most strikingly symmetrical, pyramid-shaped mountains in the Cordillera Blanca, a reputation that has made it one of the most photographed peaks in the Peruvian Andes. This entity documents Alpamayo specifically as a geological formation, a strikingly symmetrical glaciated peak of the Cordillera Blanca.

Facts
Classification
Protected Status
National Park or Reserve 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: Alpamayo

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: Alpamayo
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Alpamayo
Sources
1. Alpamayo (Wikipedia)
Category: Huascarán National Park
Quote, Category: Huascarán National Park
Wikipedia category: Huascarán National Park
View the Source
Wikidata: Alpamayo
Wikidata Q829688, class allow-list match (w-wdresolver-0926)View the Source
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