Cotacotani Lake

Last updated
Cotacotani
Quta Qutani
Near Lago Chungara, Chile (20929175651).jpg
Relief Map of Chile.jpg
Red pog.svg
Cotacotani
Quta Qutani
Rio-lauca.svg
Location Arica-Parinacota Region
Coordinates 18°11′S69°13′W / 18.183°S 69.217°W / -18.183; -69.217
Primary inflows Benedicto Morales River, El Encuentro Creek
Primary outflows Desaguadero River
Catchment area 119 km2 (46 sq mi) [1]
Basin  countriesChile
Surface area6 km2 (2.3 sq mi) [1]
Max. depth10 m (33 ft)
Surface elevation4,495 m (14,747 ft) [1]
References [1]

Laguna de Cotacotani (Hispanicized expression) or Quta Qutani (Aymara quta lake, [2] the reduplication signifies there is a group or complex of something, -ni is a suffix to indicate ownership, "the one with a group of lakes") is a lake [3] located in the Andean Altiplano of the Parinacota Province, Arica-Parinacota Region, Chile. It lies 4 km northwest of Chungará Lake, which is one of the highest lakes in the world and is surrounded by several volcanoes, such as the Payachata volcanic group (Parinacota and Pomerape), Sajama volcano and Wallatiri.

Cotacotani is separated from the lake Chungará by a strip of volcanic rock and receives groundwater inflow from that lake, however its major sources are Benedicto Morales River and El Encuentro Creek. Cotacotani Lake's main feature is the considerable number of islands and islets that it holds, which are really lava hummocks generated by a past volcanic event. With a surface of 6 km2, the Cotacotani holds a volume of water between 30 and 40 million of m³, which empty through Lauca River into Coipasa Lake, in Bolivia.

Although much of its present hummocky topography is related to a large volcanic debris avalanche occurred in the zone, this lacustrine area was not originated by such event. Recent investigations suggests that Cotacotani originated as a series of kettle hole ponds. [4]

Cotacotani lies close to the Route CH-11 which connects Arica and La Paz via Tambo Quemado International Pass. The lake is located about 54 km east of Putre and 9 km west of the border with Bolivia, within Lauca National Park.

Cotacotani Lake lies in the Tarapaca Region of Chile and within the Lauca National Park. The region has been volcanically active since the Miocene, the volcanoes Guane Guane, Parinacota and Ajoya rise northwest, northeast and south of the lake. Of these Parinacota has been recently active and deposits from a huge landslide are found on its southwestern foot; Cotacotani Lake has formed on these deposits [5] which are about 18,000 years before present old. [6]

The lake is technically a compound structure consisting of many disconnected water bodies with an average surface height of 4,526 metres (14,849 ft) between rocky blocks of andesite and rhyolite that were formed by the Parinacota huge landslide. The largest water body has a surface area that fluctuates between 5.2–4.1 square kilometres (2.0–1.6 sq mi) and a maximum depth of 20 metres (66 ft); some of the water bodies merge during lake level highstands. [5] The volume of the lake is about 30,000,000 cubic metres (1.1×109 cu ft). [7]

The Benedicto Morales River is the principal tributary and is fed by springs on the foot of Parinacota, [5] another tributary is called El Encuentro [7] in addition to groundwater inflow from Lake Chungara. [8] The Cotacotani Lakes also have an outlet in a wetland that in turn gives rise to the Lauca River. [5] There have been projects in the past to pump water from Lake Chungara into the Cotacotani Lakes which are active since 1983 [7] but were then halted by a ruling of the Supreme Court of Chile in 1985. [9]

Precipitation at Lake Chungara close to Cotacotani is about 331 millimetres per year (13.0 in/year) owing to the effects of the Southeast Pacific High and the rain shadow of the Andes and occurs mainly during December–March in the so-called "Bolivian Winter" when Atlantic moisture arrives. [5] The average temperature is about 1 °C (34 °F) but varies greatly by hour and season. [6]

Vegetation consists of wetlands, tussock, shrubs and Polylepis trees. [6] Orestias fish [10] and Biomphalaria snails live in the waters of Cotacotani Lake. [11]

See also

Related Research Articles

<span class="mw-page-title-main">Parinacota (volcano)</span> Volcano on the border of Chile and Bolivia

Parinacota, Parina Quta or Parinaquta is a dormant stratovolcano on the border of Bolivia and Chile. Together with Pomerape it forms the Nevados de Payachata volcanic chain. Part of the Central Volcanic Zone of the Andes, its summit reaches an elevation of 6,380 metres (20,930 ft) above sea level. The symmetrical cone is capped by a summit crater with widths of 1 kilometre (0.62 mi) or 1,000 metres (3,300 ft). Farther down on the southern slopes lie three parasitic centres known as the Ajata cones. These cones have generated lava flows. The volcano overlies a platform formed by lava domes and andesitic lava flows.

<span class="mw-page-title-main">Payachata</span>

Payachata or Paya Chata is a north–south trending complex of potentially active volcanos on the border of Bolivia and Chile, directly north of Chungará Lake. The complex contains two peaks, Pomerape to the north and Parinacota to the south. On the Bolivian side the volcanoes are located in the Oruro Department, Sajama Province, Curahuara de Carangas Municipality, and on the Chilean side they lie in the Arica y Parinacota Region, Parinacota Province.

<span class="mw-page-title-main">Arica y Parinacota Region</span> Region of Chile

The Arica y Parinacota Region is one of Chile's 16 first order administrative divisions. It comprises two provinces, Arica and Parinacota. It borders Peru's Department of Tacna to the north, Bolivia's La Paz and Oruro departments to the east and Chile's Tarapacá Region to the south. Arica y Parinacota is the 5th smallest, the 3rd least populous and the 6th least densely populated of the regions of Chile. Arica is the region's capital and largest city.

<span class="mw-page-title-main">Lauca National Park</span> Wildlife park in northern Chile

Lauca National Park is located in Chile's far north, in the Andean range. It encompasses an area of 1,379 km2 of altiplano and mountains, the latter consisting mainly of enormous volcanoes. Las Vicuñas National Reserve is its neighbour to the south. Both protected areas, along with Salar de Surire Natural Monument, form Lauca Biosphere Reserve. The park borders Sajama National Park in Bolivia.

<span class="mw-page-title-main">Tacora</span> Stratovolcano in Parinacota Province, Chile

Tacora is a stratovolcano located in the Andes of the Arica y Parinacota Region of Chile. Near the border with Peru, it is one of the northernmost volcanoes of Chile. It is part of the Central Volcanic Zone in Chile, one of the four volcanic belts of the Andes. The Central Volcanic Zone has several of the highest volcanoes in the world. Tacora itself is a stratovolcano with a caldera and a crater. The youngest radiometric age is 50,000 years ago and it is heavily eroded by glacial activity.

<span class="mw-page-title-main">Lauca River</span> River in Bolivia and Chile

The Lauca River is a binational river. It originates in the Chilean Altiplano of the Arica and Parinacota Region, crosses the Andes and empties into Coipasa Lake in Bolivia.

Parinacota, Parina Quta or Parinaquta may refer to:

<span class="mw-page-title-main">Arintica</span> Mountain in Chile

Arintica is a stratovolcano located in Arica y Parinacota Region of Chile, near the border with Bolivia. It lies north of the Salar de Surire.

<span class="mw-page-title-main">Taapaca</span> Volcano in Chile

Taapaca is a Holocene volcanic complex in northern Chile's Arica y Parinacota Region. Located in the Chilean Andes, it is part of the Central Volcanic Zone of the Andean Volcanic Belt, one of four distinct volcanic chains in South America. The town of Putre lies at the southwestern foot of the volcano.

<span class="mw-page-title-main">Central Andean dry puna</span>

The Central Andean dry puna (NT1001) is an ecoregion in the montane grasslands and shrublands biome, located in the Andean Altiplano in South America. It is a part of the Puna grassland.

<span class="mw-page-title-main">Jayu Quta (Ladislao Cabrera)</span> Crater in Bolivia

Jayu Quta is a maar partially filled with water, in the Bolivian Altiplano, north of the Salar de Uyuni and east of the Salar de Coipasa. It is situated in the Oruro Department, Ladislao Cabrera Province, Salinas de Garci Mendoza Municipality, Villa Esperanza Canton. It was originally misidentified as a meteorite impact crater.

<span class="mw-page-title-main">Canal Lauca</span>

The Canal Lauca is an artificial channel to divert the waters of the Lauca River westward through a canal and tunnel into the Azapa Valley for purposes of irrigation in the valley and hydroelectric-power generation. Its construction began 1948 and water diversion began 14 years later from a dam located about 16 miles southwest of Lago Cotacotani Lake.

<span class="mw-page-title-main">Kunturiri (Bolivia and Chile)</span>

Kunturiri is a volcano in the Andes on the border of Bolivia and Chile which rises up to 5,762 metres (18,904 ft). On the Chilean side it is located in the Arica and Parinacota Region and on the Bolivian side in the Oruro Department, Sajama Province, Curahuara de Carangas Municipality, Sajama Canton as well as in the La Paz Department, Pacajes Province, Calacoto Municipality, Ulloma Canton.

The Caldera Lauca is a caldera in the Arica y Parinacota Region of Chile. It is located in the Cordillera Occidental, in the valley of the Lauca River. The elliptic caldera has an east-west extension of 23 kilometres (14 mi) and 50 kilometres (31 mi) in north-south direction, buried beneath the late Miocene Vilañuñumani-Tejene volcanic complex in the north and ending at Chucal in the south. The 21 mya Oxaya Ignimbrite originates in the caldera. The eastern border of the caldera is buried beneath younger ignimbrites and deposits but is located east of the Guallatiri volcano. An Oligocene fault marks the western edge of the caldera.

Lauca is a 5,140 metres (16,860 ft) high andesitic stratovolcano in the Central Volcanic Zone of the Andes on the Altiplano in northern Chile. Administratively it is located in Putre, Arica y Parinacota Region. The volcano was active during the Late Miocene from 10.5 million years ago onwards. A major ignimbrite collapsed the volcano in the Late Pliocene.

<span class="mw-page-title-main">Isluga River</span> River

Isluga River is a river in Chile and Bolivia, and is also known as Sitani or Arabilla. It starts at the confluence of the rivers Chaguane and Huinchuta and flows for 54 kilometres (34 mi) before reaching the Laguna Mucalliri of the Salar de Coipasa. It receives water from the volcanoes Isluga, Cabaray and Quimsachata as well as the Sierra Uscana.

<span class="mw-page-title-main">Nevado Sajama</span>

Nevado Sajama is an extinct stratovolcano and the highest peak in Bolivia. The mountain is located in Sajama Province, in Oruro Department. It is situated in Sajama National Park and is a composite volcano consisting of a stratovolcano on top of several lava domes. It is not clear when it erupted last but it may have been during the Pleistocene or Holocene.

<span class="mw-page-title-main">Chungará Lake</span> Lake situated in the Lauca National Park, Chile

Chungará is a lake situated in the extreme north of Chile at an elevation of 4,517 metres (14,820 ft), in the Altiplano of Arica y Parinacota Region in the Lauca National Park. It has a surface area of about 21.5–22.5 square kilometres (8.3–8.7 sq mi) and has a maximum depth of about 26–40 metres (85–131 ft). It receives inflow through the Río Chungara with some minor additional inflows, and loses most of its water to evaporation; seepage into the Laguna Quta Qutani plays a minor role.

<span class="mw-page-title-main">Chapiquiña Power Plant</span> Hydroelectric power station in Chile

Chapiquiña power plant is a hydroelectric power plant in northern Chile. It takes water from the Canal Lauca and produces electrical power through a Pelton turbine.

<span class="mw-page-title-main">Guallatiri</span> Mountain in Parinacota Province Chile

Guallatiri is a 6,071-metre (19,918 ft) high volcano in Chile. It is located southwest of the Nevados de Quimsachata volcanic group; some sources Guallatiri is considered a part of the Nevados de Quimsachata. Guallatiri is a stratovolcano with numerous fumaroles around the summit. The summit may be either a lava dome or a pyroclastic cone, while the lower flanks of the volcano are covered by lava flows and lava domes. The volcano's eruptions have produced mostly dacite along with andesite and rhyolite.

References

  1. 1 2 3 4 (in Spanish) IRD en Chile: Lagunas Cotacotani Archived 2006-11-27 at the Wayback Machine
  2. Radio San Gabriel, "Instituto Radiofonico de Promoción Aymara" (IRPA) 1993, Republicado por Instituto de las Lenguas y Literaturas Andinas-Amazónicas (ILLLA-A) 2011, Transcripción del Vocabulario de la Lengua Aymara, P. Ludovico Bertonio 1612 (Spanish-Aymara-Aymara-Spanish dictionary)
  3. It is considered as one or several lakes, depending on sources.
  4. "Geological constraints on the emplacement mechanism of the Parinacota debris avalanche, northern Chile" (PDF). Retrieved 2007-08-07.
  5. 1 2 3 4 5 Herrera, Christian; Pueyo, Juan José; Sáez, Alberto; Valero-Garcés, Blas L. (2006). "Relación de aguas superficiales y subterráneas en el área del lago Chungará y lagunas de Cotacotani, norte de Chile: un estudio isotópico". Revista Geológica de Chile. 33 (2): 299–325. doi: 10.4067/S0716-02082006000200005 . ISSN   0716-0208.
  6. 1 2 3 Schwalb, Antje; Burns, Stephen J; Kelts, Kerry (April 1999). "Holocene environments from stable isotope stratigraphy of ostracods and authigenic carbonate in Chilean Altiplano Lakes". Palaeogeography, Palaeoclimatology, Palaeoecology. 148 (1–3): 153–168. doi:10.1016/S0031-0182(98)00181-3. ISSN   0031-0182.
  7. 1 2 3 MLADINIC, PEDRO A.; HREPIC, NICOLAS V.; QUINTANA, EMÍLIO H. (1987). "Caracterización física y química de las águas de los lagos Chungará y Cotacotani" (PDF). Arch. Biol. Med. Exp. (in Spanish). 20: 89–94.
  8. Bao, R.; Hernández, A.; Sáez, A.; Giralt, S.; Prego, R.; Pueyo, J.J.; Moreno, A.; Valero-Garcés, B.L. (December 2015). "Climatic and lacustrine morphometric controls of diatom paleoproductivity in a tropical Andean lake". Quaternary Science Reviews. 129: 96–110. doi:10.1016/j.quascirev.2015.09.019. hdl: 2445/69292 . ISSN   0277-3791.
  9. Urrutia Silva, Osvaldo (2013). "Jurisprudencia nacional, nuevos Tribunales Ambientales y derecho internacional del medio ambiente". Revista de Derecho (Valparaíso) (40): 475–507. doi: 10.4067/S0718-68512013000100015 . ISSN   0718-6851.
  10. Vila, I.; Morales, P.; Scott, S.; Poulin, E.; Véliz, D.; Harrod, C.; Méndez, M. A. (8 February 2013). "Phylogenetic and phylogeographic analysis of the genusOrestias(Teleostei: Cyprinodontidae) in the southern Chilean Altiplano: the relevance of ancient and recent divergence processes in speciation" (PDF). Journal of Fish Biology. 82 (3): 927–943. doi:10.1111/jfb.12031. ISSN   0022-1112. PMID   23464552.
  11. COLLADO, GONZALO A.; MENDEZ, MARCO A. (25 July 2012). "Phylogenetic relationships and taxonomy of Altiplano populations of Biomphalaria (Gastropoda: Planorbidae): inference from a multilocus approach". Zoological Journal of the Linnean Society. 165 (4): 797. doi: 10.1111/j.1096-3642.2012.00829.x . ISSN   0024-4082.