Coropuna, also called Nevado Coropuna for its perpetual snow cover, rises in the Andes of southeast-central Peru, its highest of several summits reaching about 6,377 meters, making it the country's third-highest volcanic complex. It is a dormant compound volcano spread across roughly 240 square kilometers, carrying the most extensive ice cap anywhere in Earth's tropical zone, with outlet glaciers descending from its summits toward lower ground. Below about 5,000 meters, diverse ecosystems including forests, wetlands and grasslands support agricultural and pastoral communities on its lower slopes. This entity documents Coropuna specifically as a geological formation, Peru's third-highest volcanic complex and the site of the most extensive ice cap in the tropics.
Facts
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Source Coropuna (Wikipedia)
Caused By
Wikidata P31 formation-type mapped to formative process Volcanism via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Coropuna (Wikipedia)
In Discipline
Wikidata P31 formation-type mapped to discipline Volcanology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Coropuna
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Source Wikidata: Coropuna
Sources
1. Coropuna (Wikipedia)
Lead paragraph
Coropuna is a dormant volcano located in the Andes mountains of southeast-central Peru.
Associated With: Miocene, Lead, age Miocene
These are composed chiefly of ignimbrites and lava flows on a basement formed by Middle Miocene ignimbrites and lava flows.
Associated With: Quaternary, Lead, age Quaternary
The Coropuna complex has been active for at least five million years, with the bulk of the current cone having been formed during the Quaternary.
Caused By: Volcanism, Lead, process Volcanism
These are composed chiefly of ignimbrites and lava flows on a basement formed by Middle Miocene ignimbrites and lava flows.
View the SourceWikidata: Coropuna
Wikidata Q946035, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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