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Principal Cordillera ( es, Cordillera Principal) is the Andean mountain range that makes up the boundary between Central Chile and neighbouring areas of Argentina. It is also a
continental divide A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, n ...
between the Atlantic and the Pacific watersheds. It extends in a north–south direction in the Argentine provinces of
La Rioja La Rioja () is an autonomous community and province in Spain, in the north of the Iberian Peninsula. Its capital is Logroño. Other cities and towns in the province include Calahorra, Arnedo, Alfaro, Haro, Santo Domingo de la Calzada, and ...
, San Juan and Mendoza and the Chilean regions of
Valparaíso Valparaíso (; ) is a major city, seaport, naval base, and educational centre in the commune of Valparaíso, Chile. "Greater Valparaíso" is the second largest metropolitan area in the country. Valparaíso is located about northwest of Santiago ...
,
Santiago Santiago (, ; ), also known as Santiago de Chile, is the capital and largest city of Chile as well as one of the largest cities in the Americas. It is the center of Chile's most densely populated region, the Santiago Metropolitan Region, wh ...
, O'Higgins and
Maule Maule may refer to: Places * Maule Region, one of the 15 Regions that make up the Chilean territory * Maule River, river in Central Chile, which gives name to the Maule Region * Maule, Chile, commune and town of Talca province in the Maule Region ...
. To the east of the Principal Cordillera lies the Frontal Cordillera which is fully in Argentina.
Aconcagua Aconcagua () is a mountain in the Principal Cordillera of the Andes mountain range, in Mendoza Province, Argentina. It is the highest mountain in the Americas, the highest outside Asia, and the highest in the Southern Hemisphere with a summ ...
, the tallest mountain outside Asia, lies in the Principal Cordillera.


Geological history

What is today the Principal Cordillera was once a depression that accumulated sediments.Charrier ''et al''. 2006, pp. 93–94. Lava flows from ancient volcanoes also found their way to the depression. Today these sequences of
sedimentary Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles ...
and volcanic rock can be observed high in the Andes, implying their basin was closed and uplifted by tectonic inversion. The said rocks are grouped in the Abanico and Farellones Formation. Tectonic inversion took place 21 to 16 million years (Ma) ago, yet the associated pulse of uplift continued until about 8 Ma ago. The Miocene
continental divide A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, n ...
was about 20 km to the west of the modern water divide that makes up the
Argentina–Chile border The Argentina–Chile border is the longest international border of South America and the third longest in the world after the Canada–United States border and the Kazakhstan–Russia border. With a length of , it separates Argentina from Chile ...
. Subsequent
river incision River incision is the narrow erosion caused by a river or stream that is far from its base level. River incision is common after tectonic uplift of the landscape. Incision by multiple rivers result in a dissected landscape, for example a dissected ...
shifted the divide to the east leaving old flattish surfaces hanging. Compression and uplift in this part of the Andes has continued into the present. The Principal Cordillera had risen to heights that allowed for the development of
valley glacier A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over ...
s about 1 Ma ago.


References

;Bibliography * Argentina–Chile border Geography of La Rioja Province, Argentina Geography of San Juan Province, Argentina Mountain ranges of Argentina Mountain ranges of Chile Geography of Maule Region Geography of Mendoza Province Geography of O'Higgins Region Geography of Santiago Metropolitan Region Geography of Santiago, Chile Geography of Valparaíso Region {{Mendoza-geo-stub