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The Lac Wiyâshâkimî (the official name, in French language, French, formerly Lac à l'Eau Claire, a calque of the lake's name, Wiyâšâkamî, in Northern East Cree, changed form of ''wâšâkamî'' or ''wâšekamî'' in more southerly Cree dialects), also called the Clearwater Lakes in English and Allait Qasigialingat by the Inuit, are a pair of annular lakes on the Canadian Shield in Quebec, Canada, near Hudson Bay.
The lakes are actually a single body of water with a sprinkling of islands forming a "dotted line" between the eastern and western parts. Its name in Cree is due to the clear water it holds. There are actually 25 lakes with names that mean "Clearwater Lake" in the province (26 if the ''Petit lac à l'Eau Claire'' — the Small Clearwater Lake — is included). Collectively, this body of water is the largest, northernmost and the second-largest natural lake in Quebec after Lake Mistassini.
In 1896, the explorer and geologist Albert Peter Low, a member of the Geological Survey of Canada, provided a probable explanation for the lakes' descriptive Cree name by highlighting the extraordinary clarity and depth of their icy waters.
New 40Ar/39Ar dating of the Clearwater Lake impact structures (Québec, Canada) – Not the binary asteroid impact it seems?
Geochim. Cosmochim. Acta (in press). Both Clearwater impact structures also carry different geophysical (natural remanent magnetization) signatures and different geochemical fingerprints of the impacting meteorite in the impactite, impact melt of each crater.Palme, H., Janssens, M.-J., Takahashi, H., Anders, E. and Hertogen, J. 1978. Meteoritic material at five large impact craters. Geochim. Cosmochim. Acta 42, 313–323.
Online version
)
Aerial Exploration of the Clearwater West StructureAerial Exploration of the Clearwater East Structure
{{Impact cratering on Earth Impact craters of Quebec Lakes of Nord-du-Québec Ordovician impact craters Permian impact craters Impact crater lakes
The Lac Wiyâshâkimî (the official name, in French language, French, formerly Lac à l'Eau Claire, a calque of the lake's name, Wiyâšâkamî, in Northern East Cree, changed form of ''wâšâkamî'' or ''wâšekamî'' in more southerly Cree dialects), also called the Clearwater Lakes in English and Allait Qasigialingat by the Inuit, are a pair of annular lakes on the Canadian Shield in Quebec, Canada, near Hudson Bay.
The lakes are actually a single body of water with a sprinkling of islands forming a "dotted line" between the eastern and western parts. Its name in Cree is due to the clear water it holds. There are actually 25 lakes with names that mean "Clearwater Lake" in the province (26 if the ''Petit lac à l'Eau Claire'' — the Small Clearwater Lake — is included). Collectively, this body of water is the largest, northernmost and the second-largest natural lake in Quebec after Lake Mistassini.
In 1896, the explorer and geologist Albert Peter Low, a member of the Geological Survey of Canada, provided a probable explanation for the lakes' descriptive Cree name by highlighting the extraordinary clarity and depth of their icy waters.
Impact craters
The Clearwater Lakes occupy the near-circular depressions of two eroded impact craters (astroblemes).Robertson, P.B. & Grieve, R.A.F. 1975 Impact structures in Canada: Their recognition and characteristics. Journal of the Royal Astronomical Society of Canada, v. 69, pp. 1-21. The eastern and western craters are and in diameter, respectively. Both craters were previously believed to have the same age, 290 ± 20 million years (Permian period), promoting the long-held idea that they formed simultaneously. According to this doublet impact crater theory initially proposed by Michael R. Dence and colleagues in 1965, the impactors may have been gravitationally bound as a binary asteroid, a suggestion also made by Thomas Wm. Hamilton in a 1978 letter to ''Sky & Telescope'' magazine in support of the then-controversial theory that asteroids may possess moons (such as, for example, asteroid 243 Ida with its satellite Dactyl). Clearwater East and Clearwater West are both complex craters with distinct central peaks. These peaks are caused by the gravitational collapse of crater walls and subsequent rebound of the compressed crater floor. Lake water and sediments cover the central peak of Clearwater East, but bathymetric surveys of the lake floor and core drilling confirm the presence of a peak in its center.Ordovician
However, repeated Argon–argon dating, 40Ar/39Ar dating of impactite, impact melt rocks from both impact craters suggests that Clearwater East has an age of approximately 460–470 million years, corresponding to the Ordovician, Middle Ordovician time period.Permian
Clearwater West was formed 286.2 ± 2.6 million years ago, in the Cisuralian, Early Permian.Bottomley, R.J., York, D., and Grieve, R.A.F. 1990. 40Argon-39Argon dating of impact craters. Proc. 20th Lunar Planet. Sci. Conf., LPI, Houston, pp. 421–431.Schmieder, M., Schwarz, W. H., Trieloff, M., Tohver, E., Buchner, E., Hopp, J. & Osinski, G. R. 2014New 40Ar/39Ar dating of the Clearwater Lake impact structures (Québec, Canada) – Not the binary asteroid impact it seems?
Geochim. Cosmochim. Acta (in press). Both Clearwater impact structures also carry different geophysical (natural remanent magnetization) signatures and different geochemical fingerprints of the impacting meteorite in the impactite, impact melt of each crater.Palme, H., Janssens, M.-J., Takahashi, H., Anders, E. and Hertogen, J. 1978. Meteoritic material at five large impact craters. Geochim. Cosmochim. Acta 42, 313–323.
Micro climate
Because of its size, Lac à l'Eau Claire can affect the micro climate, local climate, as attested to by the distribution of plant species. Although the lake's shorelines are populated mainly by Boreal ecosystem, boreal species, the flora of the central islands in the western basin of the lake is characteristically arctic, making the islands an arctic enclave.National park
A vast area surrounding the lakes, Richmond Gulf (''Lac Guillaume-Delisle''), and Iberville Lake (''Lac D'Iberville'') are part of the Tursujuq National Park, Quebec's largest national park, opened in 2012.Ministère du Développement durable, de l'Environnement et des Parcs, ''Provisional Master Plan Parc national des Lacs-Guillaume-Delisle-et-à-l'Eau-Claire'', Quebec, 2008,Online version
)
See also
* Nastapoka arc, an embayment of Hudson Bay 140 km to the west, discredited as an impact craterNotes
References
External links
Aerial Exploration of the Clearwater West Structure
{{Impact cratering on Earth Impact craters of Quebec Lakes of Nord-du-Québec Ordovician impact craters Permian impact craters Impact crater lakes