Barrancas del Cobre and the canyon country around Creel
Published on 09/22/2026 at 14:28 | Editorial responsibility: Rafael MĂĽller, Editor-in-Chief AD HOC NEWS
Barrancas del Cobre is a vast canyon region in Mexico’s Sierra Madre Occidental, centred around the mountain town of Creel in Chihuahua. Its defining feature is a linked landscape of deep ravines, forested uplands, cliffs and river valleys, rather than a single viewpoint or isolated gorge.
Barrancas del Cobre: a landscape of connected ravines
The name Barrancas del Cobre refers to a group of canyons in the Sierra Tarahumara. The landscape includes Urique, Batopilas, Sinforosa, Candameña and other major ravines, each with its own combination of rock walls, woodland and cultivated terraces. The canyons cut through a high plateau covered by pine and fir forests, creating a pronounced contrast between the uplands and the warmer valleys below.
Urique Canyon is the deepest and most widely recognised section of the system. Its walls descend from the plateau towards the RĂo Urique, while the surrounding terrain contains narrow valleys, steep slopes and scattered settlements. The relief is visible from viewpoints around Creel and from routes leading deeper into the Sierra Tarahumara.
Creel between forest, rock and canyon country
Creel lies at roughly 2,350 m (7,710 ft) above sea level on the highland edge of the canyon region. The town is surrounded by conifer forests, granite formations, meadows and small lakes. Nearby landmarks include the Valle de los Monjes, the Valle de las Ranas and Lago de Arareko.
The rock formations around Creel are part of the same highland scenery that frames Barrancas del Cobre. Tall granite pillars rise from wooded valleys, while volcanic and sedimentary rocks appear across the wider mountain landscape. At Divisadero, the plateau meets the canyon rim, with broad views over ravines and distant ridges.
The Rarámuri presence in the Sierra Tarahumara
Barrancas del Cobre is also the homeland of the Rarámuri, a people whose communities are spread through the Sierra Tarahumara. The name Tarahumara remains widely used in Spanish, while Rarámuri is the name used by the people themselves. Their language, traditions and settlements form an essential part of the region’s identity.
Rarámuri communities live in both the highlands and the canyon valleys. Agriculture, craftwork and local trade are connected with the difficult terrain, where settlements may be separated by steep ravines and long mountain routes. Visitors encounter this cultural landscape through towns, markets, museums, trails and community-run activities.
Visiting Barrancas del Cobre: what travellers from Western Europe should know
- Creel is the principal highland base for the canyon region. The Chihuahua al PacĂfico railway, known as El Chepe, connects Creel with the wider rail route through the Sierra Madre.
- The terrain combines high-altitude forest with steep canyon slopes. Viewpoints and trails may include uneven ground, exposed rock and substantial gradients.
- The official language is Spanish and the currency is the Mexican peso.
- Entry requirements depend on your nationality; UK travellers can check the FCDO travel advice at gov.uk/foreign-travel-advice, Irish travellers the Department of Foreign Affairs at ireland.ie.
Searching for Barrancas del Cobre on social platforms
These links open searches for Barrancas del Cobre on each platform.Frequently asked questions about Barrancas del Cobre
Where is Barrancas del Cobre?
Barrancas del Cobre is in Chihuahua, north-western Mexico, within the Sierra Madre Occidental. Creel is the main highland town associated with the region.
What can visitors expect in the canyon region?
The landscape combines forested plateaux, deep ravines, rock formations, viewpoints, railway travel and Rarámuri communities. Conditions vary sharply between the highlands and the canyon valleys.
What makes Barrancas del Cobre distinctive?
Its identity comes from the scale and variety of the connected canyon system. Pine-covered uplands, granite formations and deep river valleys form one continuous mountain landscape.
