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Lake Musters and Lake Colhué Huapí

Lake Musters and Lake Colhué Huapí (45°25′S 69°11′W / 45.417°S 69.183°W / -45.417; -69.183, at altitudes of around 260 metres (850 ft)) form the terminal stage of the Senguerr River endorheic basin, located in the patagonic central region of Argentina in the south of Chubut province. Closest populated area is Sarmiento, an 8,000 inhabitant former Welsh immigrant colony. The lakes gave their names to the Mustersan and Colhuehuapian South American land mammal ages.

Hybrid map and satellite view of lakes Musters and Colhué Huapí

Description edit

Inflow edit

The basin lakes are fed mainly by the eastward running Senguerr river which begins its journey in the glacial lakes La Plata and Fontana in the Andes. The inflow ranges from 35 to 54m³/sec and varies seasonally and yearly greatly.

Outflow edit

Both lakes have naturally a high evaporation process in the dry Patagonian environment by means of strong winds action and solar radiation. In shallow Colhué Huapi evaporation is much increased. In past decades, when excessive inflows did take place, water discharged to the birth branches of Chico River and eventually reached Chubut River. This occasional process last happened in 1939, since then Chico River is mostly a dry one.

Lake Musters
 
 
Lake Musters
LocationSarmiento Department, Chubut Province
Coordinates45°22′S 69°11′W / 45.367°S 69.183°W / -45.367; -69.183 (Lake Musters)
Primary inflowsSenguerr river
Primary outflowsSenguerr river
Catchment area9,700 km2 (3,700 sq mi)
Basin countriesArgentina
Surface area450 km2 (170 sq mi)
Average depth20 m (66 ft)
Max. depth38.5 m (126 ft)
Water volume8,280 hm3 (6,710,000 acre⋅ft)
Shore length1150 km (93 mi)
1 Shore length is not a well-defined measure.

Lake Musters edit

This lake, once called Otrón by the ancient tehuelches[citation needed], received its current name in 1876 from naturalist and geographer Francisco Pascasio Moreno who aimed to honour the Patagonian adventurer George Chaworth Musters.

Musters occupies a Cretaceous conformed depression in the central Patagonic mesa in the Golfo San Jorge Basin. It receives the highly branched inflow of Senguerr river by its southern coast after a 350 kilometres (220 mi) voyage from the Andes. Several of those branches reach lake Colhué Huapí by a sinuous course called Falso Senguerr; the only permanent one feeding such lake.

The lake is of tectonic origin, with average depths of 20 metres (66 ft), which gives a deep blue water hue. It is considered mesotrophic, based on its nutrient and algae mass (<5.2 g/m3 or 0.0088 lb/cu yd). Musters presents an abundant aquatic fauna comprising Patagonian perch (Percichthys trucha) and patagonian silversides (Odontesthes microlepidotus). Also, as is the case with most Patagonian lakes, foreign salmonidae have been implanted, like Salvelinus fontinalis, rainbow trout, and in lesser amounts, Salmo fario. These species have added environmental pressure over two native species nowadays endangered in the lake (Diplomystres viedmensis mesembrinus and Galaxias platei).[1]

Lake Colhué Huapí
 
 
Lake Colhué Huapí
LocationChubut Province
Coordinates45°29′38″S 68°45′26″W / 45.49389°S 68.75722°W / -45.49389; -68.75722 (Lake Colhué Huapi)
Typeendorheic
Primary inflowsSenguerr river
Primary outflowsevaporation
Catchment area10,900 km2 (4,200 sq mi)
Basin countriesArgentina
Max. length50 km (31 mi)[2]
Surface area810 km2 (310 sq mi)
Average depth2 m (6 ft 7 in)
Max. depth5.5 m (18 ft)
Water volume1,620 hm3 (1,310,000 acre⋅ft)
References[2]

Lake Colhué Huapí edit

The name of this large water mirror comes from the Mapuche language Mapudungun. Colhué means "reddish or red place" and Huapí means "island".[3] It is a reference to one of the many clay conformed islands of such lake.[citation needed] The lake was named in official Argentine cartography by explorer Francisco Moreno who reached the lake in 1876.[3] Subsequent analysis have shown that Moreno appear to have mistaken it for the larger General Carrera Lake whom indigenous Tehuelches called Coluguape.[3]

Colhué Huapi fills a shallow depression formed by strong eolean action over an area of fine clays. It is fed by the Falso Senguerr river, a sinuous branch of main Senguerr River. The lake coast is dominated by extensive wetlands mainly at its feeding zone. In contrast to its neighbour Musters (separated by a 12 kilometres (7.5 mi) wide and 695 metres (2,280 ft) high isthmus) Colhué has an average depth of 2 metres (6.6 ft) and high water turbidity due to suspended sediments deposited by constant wind.

It is considered an argilotrophic brackish water lake because of its high levels of inorganic sediments in suspension. As with lake Musters, and despite the high water opacity, Patagonian perch and silversides have large populations. Of high interest is the native big mouth perch (Percichthys colhuehuapensis) currently[when?] endangered by pressure of human-introduced foreign salmonidae.

Environmental concerns edit

Several water offtakes have been progressively placed at lake Musters for drinking water supply, as well as many diversions of the Senguerr river to feed oil extraction facilities in the nearby region. This complicated the already resented water balance of the whole system to the extent of near-collapse at Colhué Huapí, whose peripheral surface continuously retracts and dries.[4] The hydrological equilibrium of the whole basin has been negative in the past seventy years.[when?] Currently[when?] these lakes' situation could be defined as compromised.

References edit

  1. ^ Bibliografía de los Peces Continentales Patagónicos, Ricardo A. Ferriz, Aquatec, 1998 2010-11-05 at the Wayback Machine
  2. ^ a b RIVAS, A., 1978, Batimetría del lago Colhué Huapí. Informe Técnico del Centro Nacional Patagónico, Contribución N° 18, 1-8 p.
  3. ^ a b c Melo, Walter D.; Scordo, Facundo; Perillo, Gerardo M. E.; Píccolo, M. Cintia (2017). "Identificación del lago "Coluguape" en la cartografía histórica (1775-1898): Su vinculación con el lago Buenos aires-General Carrera y el sistema lacustre Musters-Colhue Huapi" [Identification of the "Coluguape" lake in historical cartography (1775-1898): Its connection to the Buenos Aires-General Carrera lake and Musters- Colhue Huapi lake system]. Magallania (in Spanish). 45 (1): 15-33. doi:10.4067/S0718-22442017000100015.
  4. ^ Kokot, R. R. (December 2004). "Erosión en la costa patagónica por cambio climático". Revista de la Asociación Geológica Argentina. 59 (4): 715–726.

External links edit

  • Lakes Muster, Colhué Huapí and Senguerr River - tourism information

lake, musters, lake, colhué, huapí, altitudes, around, metres, form, terminal, stage, senguerr, river, endorheic, basin, located, patagonic, central, region, argentina, south, chubut, province, closest, populated, area, sarmiento, inhabitant, former, welsh, im. Lake Musters and Lake Colhue Huapi 45 25 S 69 11 W 45 417 S 69 183 W 45 417 69 183 at altitudes of around 260 metres 850 ft form the terminal stage of the Senguerr River endorheic basin located in the patagonic central region of Argentina in the south of Chubut province Closest populated area is Sarmiento an 8 000 inhabitant former Welsh immigrant colony The lakes gave their names to the Mustersan and Colhuehuapian South American land mammal ages Hybrid map and satellite view of lakes Musters and Colhue Huapi Contents 1 Description 1 1 Inflow 1 2 Outflow 2 Lake Musters 3 Lake Colhue Huapi 4 Environmental concerns 5 References 6 External linksDescription editInflow edit The basin lakes are fed mainly by the eastward running Senguerr river which begins its journey in the glacial lakes La Plata and Fontana in the Andes The inflow ranges from 35 to 54m sec and varies seasonally and yearly greatly Outflow edit Both lakes have naturally a high evaporation process in the dry Patagonian environment by means of strong winds action and solar radiation In shallow Colhue Huapi evaporation is much increased In past decades when excessive inflows did take place water discharged to the birth branches of Chico River and eventually reached Chubut River This occasional process last happened in 1939 since then Chico River is mostly a dry one Lake Musters nbsp nbsp Lake MustersLocationSarmiento Department Chubut ProvinceCoordinates45 22 S 69 11 W 45 367 S 69 183 W 45 367 69 183 Lake Musters Primary inflowsSenguerr riverPrimary outflowsSenguerr riverCatchment area9 700 km2 3 700 sq mi Basin countriesArgentinaSurface area450 km2 170 sq mi Average depth20 m 66 ft Max depth38 5 m 126 ft Water volume8 280 hm3 6 710 000 acre ft Shore length1150 km 93 mi 1 Shore length is not a well defined measure Lake Musters editThis lake once called Otron by the ancient tehuelches citation needed received its current name in 1876 from naturalist and geographer Francisco Pascasio Moreno who aimed to honour the Patagonian adventurer George Chaworth Musters Musters occupies a Cretaceous conformed depression in the central Patagonic mesa in the Golfo San Jorge Basin It receives the highly branched inflow of Senguerr river by its southern coast after a 350 kilometres 220 mi voyage from the Andes Several of those branches reach lake Colhue Huapi by a sinuous course called Falso Senguerr the only permanent one feeding such lake The lake is of tectonic origin with average depths of 20 metres 66 ft which gives a deep blue water hue It is considered mesotrophic based on its nutrient and algae mass lt 5 2 g m3 or 0 0088 lb cu yd Musters presents an abundant aquatic fauna comprising Patagonian perch Percichthys trucha and patagonian silversides Odontesthes microlepidotus Also as is the case with most Patagonian lakes foreign salmonidae have been implanted like Salvelinus fontinalis rainbow trout and in lesser amounts Salmo fario These species have added environmental pressure over two native species nowadays endangered in the lake Diplomystres viedmensis mesembrinus and Galaxias platei 1 nbsp Lake Musters nbsp Paragliding at Lake Musters Lake Colhue Huapi nbsp nbsp Lake Colhue HuapiLocationChubut ProvinceCoordinates45 29 38 S 68 45 26 W 45 49389 S 68 75722 W 45 49389 68 75722 Lake Colhue Huapi TypeendorheicPrimary inflowsSenguerr riverPrimary outflowsevaporationCatchment area10 900 km2 4 200 sq mi Basin countriesArgentinaMax length50 km 31 mi 2 Surface area810 km2 310 sq mi Average depth2 m 6 ft 7 in Max depth5 5 m 18 ft Water volume1 620 hm3 1 310 000 acre ft References 2 Lake Colhue Huapi editThe name of this large water mirror comes from the Mapuche language Mapudungun Colhue means reddish or red place and Huapi means island 3 It is a reference to one of the many clay conformed islands of such lake citation needed The lake was named in official Argentine cartography by explorer Francisco Moreno who reached the lake in 1876 3 Subsequent analysis have shown that Moreno appear to have mistaken it for the larger General Carrera Lake whom indigenous Tehuelches called Coluguape 3 Colhue Huapi fills a shallow depression formed by strong eolean action over an area of fine clays It is fed by the Falso Senguerr river a sinuous branch of main Senguerr River The lake coast is dominated by extensive wetlands mainly at its feeding zone In contrast to its neighbour Musters separated by a 12 kilometres 7 5 mi wide and 695 metres 2 280 ft high isthmus Colhue has an average depth of 2 metres 6 6 ft and high water turbidity due to suspended sediments deposited by constant wind It is considered an argilotrophic brackish water lake because of its high levels of inorganic sediments in suspension As with lake Musters and despite the high water opacity Patagonian perch and silversides have large populations Of high interest is the native big mouth perch Percichthys colhuehuapensis currently when endangered by pressure of human introduced foreign salmonidae nbsp Lake Colhue Huapi nbsp Fauna present at the Lake Colhue Huapi Environmental concerns editSeveral water offtakes have been progressively placed at lake Musters for drinking water supply as well as many diversions of the Senguerr river to feed oil extraction facilities in the nearby region This complicated the already resented water balance of the whole system to the extent of near collapse at Colhue Huapi whose peripheral surface continuously retracts and dries 4 The hydrological equilibrium of the whole basin has been negative in the past seventy years when Currently when these lakes situation could be defined as compromised References edit Bibliografia de los Peces Continentales Patagonicos Ricardo A Ferriz Aquatec 1998 Archived 2010 11 05 at the Wayback Machine a b RIVAS A 1978 Batimetria del lago Colhue Huapi Informe Tecnico del Centro Nacional Patagonico Contribucion N 18 1 8 p a b c Melo Walter D Scordo Facundo Perillo Gerardo M E Piccolo M Cintia 2017 Identificacion del lago Coluguape en la cartografia historica 1775 1898 Su vinculacion con el lago Buenos aires General Carrera y el sistema lacustre Musters Colhue Huapi Identification of the Coluguape lake in historical cartography 1775 1898 Its connection to the Buenos Aires General Carrera lake and Musters Colhue Huapi lake system Magallania in Spanish 45 1 15 33 doi 10 4067 S0718 22442017000100015 Kokot R R December 2004 Erosion en la costa patagonica por cambio climatico Revista de la Asociacion Geologica Argentina 59 4 715 726 External links editPhotos of Lake Musters Lakes Muster Colhue Huapi and Senguerr River tourism information Retrieved from https en wikipedia org w index php title Lake Musters and Lake Colhue Huapi amp oldid 1180647797, wikipedia, wiki, book, books, library,

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