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   » » Wiki: Altiplano
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The Altiplano (Spanish for "high plain"), Collao (Quechua and : Qullaw, meaning "place of the ") or Andean Plateau, in west-central South America, is the most extensive high on Earth outside . The plateau is located at the latitude of the widest part of the north–south-trending . The bulk of the Altiplano lies in , but its northern parts lie in , its southwestern fringes lie in , and it extends into .

Many towns and several cities are on the plateau, including and Oruro in Bolivia and and in Peru. The northeastern part of the Altiplano is more humid than the southwestern part, which has several salares (salt flats), due to its aridity. At the Bolivia–Peru border lies , the largest lake in South America. Farther south, in Bolivia, Lake Poopó existed until recently, but by December 2015, it had completely dried up, and was declared defunct. Whether that lake, which had been the second-largest in Bolivia, can be restored is unclear.

The Altiplano was the site of several pre-Columbian cultures, including the Chiripa, , and the . Spain conquered the region in the 16th century.

Today, major economic activities in the Altiplano include mining, and vicuña herding, and services (in its cities). The area also attracts some international tourism.


Geography
The Altiplano is an area of inland drainage () lying in the central , occupying parts of northern Chile, western Bolivia, southern Peru, and northwest Argentina. Its elevation averages about 3,750 meters (12,300 feet), slightly less than that of the . Unlike conditions in , the Altiplano is dominated by massive active of the Central Volcanic Zone to the west, such as (6288 m), (5,816 m), Parinacota (6348 m), Guallatiri (6071 m), (5,728 m), (6,008 m), and (5,916 m), and the Cordillera Real in the northeast with (6,368 m), Huayna Potosí (6,088 m), Janq'u Uma (6,427 m) and (6,438 m). The , one of the driest areas on the planet, lies to the southwest of the Altiplano; to the east lies the humid Amazon rainforest.

The Altiplano is noted for hypoxic air caused by very . The communities located in the Altiplano include , , , and .


Geology
Several mechanisms have been put forth for the formation of the Altiplano plateau; hypotheses try to explain why the topography in the Andes incorporates this large area of low relief at high altitude (high plateau) within the :
  1. Existence of weaknesses in the Earth's crust prior to tectonic shortening: Such weaknesses would cause the partition of tectonic deformation and uplift into the eastern and western cordillera, leaving the necessary space for the formation of the altiplano basin.
  2. processes rooted in the might have contributed to uplift of the plateau.
  3. Climate has controlled the spatial distribution of erosion and sediment deposition, controlling the lubrication along the subducting , hence influencing the transmission of tectonic forces into South America.
  4. Climate also determined the formation of internal drainage (endorheism) and sediment trapping within the Andes, potentially blocking tectonic deformation in the central area between the two cordilleras, and expelling deformation towards the flanks of the orogen.Garcia-Castellanos, D., 2007. The role of climate during high plateau formation. Insights from numerical experiments. Earth Planet. Sci. Lett. 257, 372-390,
  5. Convective removal of the dense lower beneath the Altiplano caused that region to isostatically "float" higher.

At various times during the epoch, both the southern and northern Altiplano areas were covered by vast . Remnants are , straddling the Peru–Bolivia border, and Poopó, a that extends south of Oruro, Bolivia. Salar de Uyuni, locally known as Salar de Tunupa, and are two large, dry, salt flats formed after the Altiplano paleolakes dried out.


Climate
The term Altiplano is sometimes used to identify the altitude zone and the type of climate that prevails within it is colder than that of the tierra fría, but not as cold as that of the . Scientists classify the latter as commencing at an elevation around 4,500 meters (or about 15,000 feet). Alternate names used in place of altiplano in this context include puna and páramos.

In general, the climate is cool and humid to semiarid and even , with mean annual temperatures that vary from near the western mountain range to near Lake Titicaca; total annual rainfall ranges between less than to the southwest to more than near and over Lake Titicaca. The diurnal cycle of temperature is very wide, with maximum temperatures on the order of and the minimum on the order of .

The coldest temperatures occur in the southwestern portion of the Altiplano during winter - June and July. The seasonal cycle of rainfall is marked, with the rainy season concentrated between December and March. The rest of the year tends to be very dry, cool, windy, and sunny. Snowfall may happen between April and September, especially to the north, but it is not very common, occurring between one and five times a year.


See also


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