The Lac Wiyâshâkimî, also called the Clearwater Lakes in English, is a calque of Wiyâšâkamî in Northern East Cree 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. The name is due to the clear water it holds. There are actually 25 lakes with that name in the province. These are the largest and 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. The eastern and western craters are and in diameter, respectively. Both craters were previously believed to have the same age, 290 ± 20 million years, 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. However, repeated 40Ar/39Ar dating of impact melt rocks from both impact craters suggests that Clearwater East has an age of approximately 460–470 million years, corresponding to the Ordoviciantime period, whereas Clearwater West was formed 286.2 ± 2.6 million years ago, in the Early Permian. Both Clearwater impact structures also carry different geophysical signatures and different geochemical fingerprints of the impacting meteorite in the impact melt of each crater. 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.
Micro climate
Because of its size, Lac à l'Eau Claire can affect the local climate, as attested to by the distribution of plant species. Although the lake's shorelines are populated mainly by boreal species, the flora of the central islands in the western basin of the lake is characteristically arctic, making the islands an arctic enclave.
