Sessional papers of the Dominion of Canada 1911 . is really a widereach of the main river. The Winawiash river flows into Expanse from the cast and is little known, theWanowie drains in from the south. The Smooth river drains the Little Roger and AVhitefish lakes from the iiorth intoQuinze, about ten miles south from Expanse. OUTLETS. The oidy outlet of these reservoirs is through the Quinze rapids (really a part ofthe Ottawa), which in fifteen miles descends 275 feet into Paulson bay at the northend of Lake Timiskaming. This stream has recently (May 12, 1909) been let forpower purposes, and a
Sessional papers of the Dominion of Canada 1911 . is really a widereach of the main river. The Winawiash river flows into Expanse from the cast and is little known, theWanowie drains in from the south. The Smooth river drains the Little Roger and AVhitefish lakes from the iiorth intoQuinze, about ten miles south from Expanse. OUTLETS. The oidy outlet of these reservoirs is through the Quinze rapids (really a part ofthe Ottawa), which in fifteen miles descends 275 feet into Paulson bay at the northend of Lake Timiskaming. This stream has recently (May 12, 1909) been let forpower purposes, and a careful survey has been made by interested parties, who havekindly favoured us with a copy. SHORE LINE. Thb margin of both Lakes Quinze and Expanse arc, so far as has been seen, rock—and well forested with pine, spruce, birch and poplar, and could easily hold a riseof 10 feet above high water. 1009, which seems to have been the highest recorded. Themarginal belt of timber that will be water-killed should be cleared before raising No. 11.—Devil Chute of the Quinzt* Kapids, tlnuiigii which the ( Ht;i\va Ri\ti th scends fruiii E\i)fiii^eand ^uinze hikes to Timiskaniing Lake, opposite Haileylmiy.
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Keywords: ., bookauthorcanadapa, bookcentury1800, bookdecade1860, bookyear1868
