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Puyehue Lake (Spanish pronunciation: [puˈjewe]), (Mapudungun: puye, "small fish" and hue, "place") is an Andean piedmont lake on the border of Los Lagos Region with Los Ríos Region of Chile.

Puyehue Lake
View of the lake with Puyehue volcano in the background
Puyehue Lake
Coordinates40°41′01″S 72°27′46″W
Primary inflowsGol-Gol River
Primary outflowsPilmaiquén River
Catchment area1,267 km2 (489 sq mi)
Basin countriesChile
Max. length23 km (14 mi)
Max. width11.5 km (7.1 mi)
Surface area157 km2 (61 sq mi)[1]
Max. depth123 m (404 ft)[2]
Water volume12.6 km3 (10,200,000 acre⋅ft)[2]
Surface elevation212 m (696 ft)[1]
IslandsFresia Island, Cuicui Islands
SettlementsEntre Lagos
ReferencesCuenca del río Bueno[1]

Puyehue is a lake of glacial origin. Several times during the Pleistocene glaciations, the lake depression was occupied by a large glacial lobe of the Patagonian Ice Sheet, which formed a series of moraines along its western shore. The lake has an east-west elongated shape with Fresia Island in the middle and two minor peninsulas pointing toward the island, one from the north and one from the south. The lake has a remarkably smooth shoreline, with only one inlet of significance: Futacullín Bay on the south.[1] Entre Lagos at the western end is the only town on the lake.

As with most other lakes of southern Chile, Puyehue Lake acts as a sediment trap for material from the Andes. Sediment cores taken from Puyehue Lake in 2001 and 2002 have been interpreted as supporting the existence of the Little Ice Age in the Southern Hemisphere.[3] A longer sediment core from the same site was used to reconstruct the evolution of the lake and its drainage basin during the last 18,000 years.[4][5][6]

At the time the glacier occupying the Puyhue basin had retreated during deglaciation as to calv at a proglacial Puyehue Lake the glacier at Rupanco basin (40°49' S) was at its maximum extent. For a time meltwater from the Rupanco glacier flowed north into Puyehue Lake.[7]

The 2011 Puyehue Volcano eruption polluted the Golgol River, a source of the lake, killing fish. Pyroclastic material reached Puyehue Lake through river transport, which resulted in the deposition of a layer of volcanic ash at the bottom of the lake.[8][9]

Topography of the region. The Puyehue-Cordón Caulle massif is located between Ranco and Puyehue Lake
Topography of the region. The Puyehue-Cordón Caulle massif is located between Ranco and Puyehue Lake

In the 16th century the lake was known to the Spanish as Llobén, from the Huilliche word of llofën meaning "abundant and continuous rain."[10]


References


  1. Cuenca del río Bueno Archived 2015-09-24 at the Wayback Machine
  2. Campos, H., Steffen, W., Agüero, G., Parra, O., Zúñiga, L., 1989. Estudios limnologicos en el Lago Puyehue (Chile): morfometria, factores fisicos y quimicos, plancton y productividad primaria. Medio Ambiente 10, 36–53.
  3. Bertrand, Sébastien (2005). "Temporal evolution of sediment supply in Lago Puyehue (Southern Chile) during the last 600 yr and its climatic significance". Quaternary Research. 64 (2): 163–175. Bibcode:2005QuRes..64..163B. doi:10.1016/j.yqres.2005.06.005.
  4. De Batist, Marc; Fagel, Nathalie; Loutre, Marie-France; Chapron, Emmanuel (2007). "A 17,900-year multi-proxy lacustrine record of Lago Puyehue (Chilean Lake District): introduction". Journal of Paleolimnology. 39 (2): 151–161. doi:10.1007/s10933-007-9113-2.
  5. Bertrand, Sébastien; Sterken, Mieke; Vargas-Ramirez, Lourdes; De Batist, Marc; Vyverman, Wim; Lepoint, Gilles; Fagel, Nathalie (2010). "Bulk organic geochemistry of sediments from Puyehue Lake and its watershed (Chile, 40°S): Implications for paleoenvironmental reconstructions". Palaeogeography, Palaeoclimatology, Palaeoecology. 294 (1–2): 56–71. Bibcode:2010PPP...294...56B. doi:10.1016/j.palaeo.2009.03.012. hdl:1912/2742.
  6. Moernaut, Jasper; De Batist, Marc; Charlet, Francois; Heirman, Katrien; Chapron, Emmanuel; Pino, Mario; Brümmer, Robert; Urrutia, Roberto (2007). "Giant earthquakes in South-Central Chile revealed by Holocene mass-wasting events in Lake Puyehue". Sedimentary Geology. 195 (3–4): 239–256. Bibcode:2007SedG..195..239M. doi:10.1016/j.sedgeo.2006.08.005.
  7. Heirman, Katrien; De Batist, Marc; Charlet, Francois; Moernaut, Jasper; Chapron, Emmanuel; Brümmer, Robert; Pino, Mario; Urrutia, Roberto (2011). "Detailed seismic stratigraphy of Lago Puyehue: implications for the mode and timing of glacier retreat in the Chilean Lake District". Journal of Quaternary Science. 26 (7): 665–674. Bibcode:2011JQS....26..665H. doi:10.1002/jqs.1491.
  8. Lago Puyehue tiene 10 centímetros de piedra pómez en el fondo tras erupción, Austral de Osorno, 2 de diciembre de 2014.
  9. Bertrand, Sébastien; Daga, Romina; Bedert, Robin; Fontijn, Karen (2014). "Deposition of the 2011-2012 Cordón Caulle tephra (Chile, 40°S) in lake sediments: Implications for tephrochronology and volcanology". Journal of Geophysical Research: Earth Surface. 119 (12): 2555–2573. Bibcode:2014JGRF..119.2555B. doi:10.1002/2014JF003321.
  10. Bernales Lillo, Mario (1984). "Aspectos diacrónicos en la toponimia de Valdivia". Anales de la Universidad de Chile (in Spanish). 5 (5): 79–94.



На других языках


[de] Lago Puyehue

Der Lago Puyehue ist ein großer See im Süden Chiles.
- [en] Puyehue Lake

[es] Lago Puyehue

El lago Puyehue se ubica en el límite de la Provincia de Ranco, con la Provincia de Osorno, en la Región de Los Lagos.

[fr] Lac Puyehue

Le lac Puyehue, terme mapudungun signifiant en français « Lieu des Puyes »[1], est un lac du Sud du Chili, situé à la limite de la province de Valdivia et de la province d'Osorno, dans la région des Lacs.

[ru] Пуеуэ (озеро)

Пуеуэ[1] (исп. Puyehue ) — озеро на юге Чили. Открыто в 1553 году Франсиско де Вильягра. Расположено в 870 км к югу от чилийской столицы Сантьяго на чилийской стороне Анд. Площадь озера в настоящее время — 164 км²[2]. Находится на высоте 212 м над уровнем моря. Наибольшая глубина 123 м[2]. Ледникового происхождения. На озере находятся острова Куикуи и остров Фресия. У восточной оконечности озера находится одноимённый посёлок[3]. Крупнейший населённый пункт — Энтре-Лагос с населением около 4 тысяч человек расположен на юго-западном берегу. По южному берегу проходит международная автомобильная дорога, соединяющая чилийскую провинцию Осорно и аргентинскую Неукен.



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