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Geological Formation

Copper Canyon

Gorges and Canyons

Copper Canyon, or Barranca del Cobre, is a network of canyons in the Sierra Tarahumara of Chihuahua, Mexico, cut into a thick sequence of volcanic rock, mostly rhyolitic tuff, erupted roughly 30 million years ago and later uplifted as part of the Sierra Madre Occidental. The canyon system, whose combined extent and depth exceed those of the Grand Canyon in the United States, was carved by six rivers draining the plateau, whose downcutting kept pace with regional tectonic uplift over millions of years, producing steep-walled gorges that in places plunge more than 1,800 meters from rim to river. The canyon takes its name from copper and other mineral deposits found within its walls, and it remains home to the Raramuri, or Tarahumara, people, whose traditional settlements are built into the canyon terrain.

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Classification
Protected Status
National Park or Reserve 1
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Sources
1. Copper Canyon (Wikipedia)
  • Conservation section
    Mexico established the Parque Nacional Barranca del Cobre (Copper Canyon National Park) to showcase this remote area.
  • In Group: Canyons, Lead paragraph
    Copper Canyon (Spanish: Barrancas del Cobre) is a system of six distinct canyons in the Sierra Madre Occidental in the southwestern part of the state of Chihuahua in northwestern Mexico that is 65,000 square kilometres (25,000 sq mi) in size.
View the Source
Wikidata: Copper Canyon
Wikidata Q674485, class allow-list match (w-wdresolver-0926)View the Source
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