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The non-endorheic altiplano extends southward into Argentina and Chile. The Altiplano (Spanish for "high plain"), Collao (Quechua and Aymara: Qullaw, meaning "place of the Qulla") or Andean Plateau, in west-central South America, is the most extensive high plateau on Earth outside Tibet.
A male Andean cock-of-the-rock, a species found in humid Andean forests and the national bird of Peru Herds of alpacas near Ausangate mountain Main article: Fauna of the Andes The Andes are rich in fauna: With almost 1,000 species, of which roughly 2/3 are endemic to the region, the Andes are the most important region in the world for ...
The Andes mountain range as seen from a plane, between Santiago de Chile and Mendoza, Argentina, in summer. The Andes (/ ˈ æ n d iː z / AN-deez), Andes Mountains or Andean Mountain Range (Spanish: Cordillera de los Andes; Quechua: Anti) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America.
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The Altiplano plateau or Meseta del Collasuyu to differentiate it from other Andean high plateaux is a wide and long-lived intermontane sedimentary basin with no outlet; it is endorheic. The Altiplano is an infill of sedimentary material from both Cordillera Occidental and Cordillera Oriental. The origin of the Altiplano and its great height ...
The Altiplano has large numbers of lakes and rivers that do not run into any ocean because they are enclosed by the Andean mountains. The most important river is the Desaguadero River, with a length of 436 km (271 mi), the longest river of the Altiplano; it begins in Lake Titicaca and then runs in a southeast direction to Poopó Lake.
Many areas are farmed. It extends from north-central Peru, adjacent to the páramos, and reaches southeast to along the eastern altiplano of Bolivia. [5] NT1002 Central Andean puna (Bolivia, Peru, Chile, Argentina) [6] – Covering most of southern Peru, the region is dominated by shrublands and thickets of tola shrubs. [5]
The Altiplano Basin (Spanish: Cuenca del Altiplano) is a sedimentary basin within the Andes in Bolivia and Peru. The basin is located on the Altiplano plateau between the Cordillera Occidental and the Cordillera Oriental. Over-all the basin has evolved through time in a context of horizontal shortening of Earth's crust. [1]