Cerro Toro is a Cretaceous landform of the Magallanes Foreland in the Patagonian region of southeastern Chile.[1][2] 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.[3]
| Cerro Toro | |
|---|---|
  Cerro Toro Location of Cerro Toro in Chile | |
| Highest point | |
| Elevation | 320 m (1,050 ft) |
| Coordinates | 52°14′27″S 74°37′57″W / 52.24083°S 74.63250°W / -52.24083; -74.63250 |
| Geography | |
| Country |  Chile |
| State | Magallanes y la Antártica Chilena |
| Parent range | Andes |
| Geology | |
| Orogeny | Andean |
 | This Magallanes and Antártica Chilena Region location article is a stub. You can help Wikipedia by expanding it. |
 | This article about a regional geological feature is a stub. You can help Wikipedia by expanding it. |
