Cerro Toro
Cerro Toro is a Cretaceous landform of the Magallanes Foreland in the Patagonian region of southeastern Chile. The Cerro Toro is an element of the southern Andes and a product of the Andean orogeny, caused by the subduction of the Nazca Plate beneath the South American Plate. The formation of the Cerro Toro began in the Jurassic. The Cueva del Milodón Natural Monument is situated on the southern flank of Cerro Benítez, a lower hill associated with the formation of Cerro Toro.
Elevation: 2027 m
Country: Chile
Explore topics:
- Cerro Toro hiking routes
- Cerro Toro best routes
- Cerro Toro camping
- Cerro Toro parking
- Cerro Toro car park
- Cerro Toro difficulty
- Cerro Toro family friendly
- Cerro Toro dog friendly
- Cerro Toro sunrise hike
- Cerro Toro sunset hike