Cerro Toro is a

Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of ...

landform of the Magallanes Foreland in the

Patagonia Patagonia () refers to a geographical region that encompasses the southern end of South America, governed by Argentina and Chile. The region comprises the southern section of the Andes Mountains with lakes, fjords, temperate rainforests, and g ...

n region of southeastern

Chile Chile, officially the Republic of Chile, is a country in the western part of South America. It is the southernmost country in the world, and the closest to Antarctica, occupying a long and narrow strip of land between the Andes to the east a ...

. The Cerro Toro is an element of the southern

Andes The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S ...

and a product of the

Andean orogeny The Andean orogeny ( es, Orogenia andina) is an ongoing process of orogeny that began in the Early Jurassic and is responsible for the rise of the Andes mountains. The orogeny is driven by a reactivation of a long-lived subduction system alon ...

, caused by the subduction of the Nazca Plate beneath the South American Plate. The formation of the Cerro Toro began in the

Jurassic The Jurassic ( ) is a geologic period and stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of ...

. 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.Hogan, 2008

References

Bibliography

C. Michael Hogan (2008) ''Cueva del Milodon'', The Megalithic Portal, ed. A. Burnham
* Stephen M. Hubbard, Brian W. Romans and Stephan A. Graham (2008) ''Deep-water foreland basin deposits of the Cerro Toro Formation, Magallanes basin, Chile: architectural elements of a sinuous basin axial channel belt'', Sedimentology, Mar. 2008 * V.A. Ramos and J. Duncan Keppie (1999) ''Laurentia-Gondwana Connections Before Pangea'', Geological Society of America

See also

References

Bibliography

Further reading