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Manicouagan Reservoir

Coordinates: 51°23′N 68°42′W / 51.383°N 68.700°W / 51.383; -68.700
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Manicouagan Reservoir
LocationQuebec
Coordinates51°23′N 68°42′W / 51.383°N 68.700°W / 51.383; -68.700
Typenatural lake, annular lake, reservoir, impact crater lake
Primary outflowsManicouagan River
Basin countriesCanada
Surface area1,942 km2 (750 sq mi)
Surface elevation342 m (1,122 ft) to 359 m (1,178 ft) (Dates: 1980 to 2005)
IslandsRené-Levasseur Island

Manicouagan Reservoir (also Lake Manicouagan) is an annular lake in central Quebec, Canada. The lake covers an area of 1,942 km², and its eastern shore is accessible via Route 389. The island in the centre of the lake is known as René-Levasseur Island, and its highest point is Mount Babel. The lake and island are clearly seen from space and are sometimes called the "eye of Quebec." In 2007, the Manicouagan lake was astronaut Marc Garneau's nomination for the CBC's Seven Wonders of Canada competition. It bears a strikeing resemblance to Strong Sad's head, a gray, depressing character from Homestarrunner.com, a flash-cartoon made by The Brothers Chaps.

Manicouagan impact crater

The crater in winter, as seen from the space shuttle (north is to the lower right)

Manicouagan Reservoir lies within the remnant of an ancient eroded impact crater (astrobleme). The crater was formed following the impact of a Template:Km to mi diameter asteroid which excavated a crater originally about Template:Km to mi wide although erosion and deposition of sediments have since reduced the visible diameter to about Template:Km to mi. It is the fifth-largest confirmed impact crater known on earth.[1] Mount Babel is interpreted as the central peak of the crater, formed by post-impact uplift.

Recent research has shown that impact melt within the crater has an age of 214±1 million years. As this is 12±2 million years before the end of the Triassic, the impact that produced the crater cannot have been the cause of the Triassic-Jurassic extinction event.[2]

Hydroelectric project

File:Manic5 dam.png
Daniel-Johnson Dam, the primary dam on the Manicouagan Reservoir, supports the Manic-5 hydro-power station

The lake was enlarged by flooding the earlier Lake Mouchalagan[3] and Manicouagan by construction of the massive Manicouagan or Manic series of hydroelectric projects undertaken by Hydro-Québec, the provincial electrical utility, during the 1960s, including the stations Manic-2, Manic-3, and Manic-5. The complex of dams is also called the Manic-Outardes project because the rivers involved are the Manicouagan and the Outardes.

The Manicouagan lake acts as a giant hydraulic battery for Hydro-Québec. In the peak period of the winter cold, the lake surface is usually lower, since the turbines are run all the time at peak load to meet the massive electrical heating needs of the province. The surface of the lake also experiences low levels in the extreme periods of heat in New England during the summer, since in that period Hydro-Québec sells electrical energy to the joint New England grid and individual utilities in the United States.

See also

References

  1. ^ Earth Impact Database
  2. ^ Hodych, J.P. (1992). "Did the Manicouagan impact trigger end-of-Triassic mass extinction?". Geology. 20: pp.51.54. doi:10.1130/0091-7613(1992)020<0051:DTMITE>2.3.CO;2. {{cite journal}}: |pages= has extra text (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  3. ^ http://ottawa-rasc.ca/wiki/index.php?title=Odale-Articles-Manicouagan