Sessional papers of the Dominion of Canada 1911 . No. 9.—Red Pine Chiitc where Kipawa River enters the head of Kipawa Lake. McLaughlin is near this jdcturesque fall wliicli will bp obliterated at full reservoir 19a—2J 20 DEIAllTMEXr OF PLllLIV \i;Ks 1 GEORGE v., A. 1911 RESULTS EXPECTED. The Kipawa basin will accumulate during ordinary years enough water to cover2,000 square miles 1 foot in depth. That is, Kipawa lake proper, 110 square miles area,would have to rise about 20 feet to hold the whole run off. Its surface now fliietuatesfrom zero to ten feet, so 10 feet more ove
Sessional papers of the Dominion of Canada 1911 . No. 9.—Red Pine Chiitc where Kipawa River enters the head of Kipawa Lake. McLaughlin is near this jdcturesque fall wliicli will bp obliterated at full reservoir 19a—2J 20 DEIAllTMEXr OF PLllLIV \i;Ks 1 GEORGE v., A. 1911 RESULTS EXPECTED. The Kipawa basin will accumulate during ordinary years enough water to cover2,000 square miles 1 foot in depth. That is, Kipawa lake proper, 110 square miles area,would have to rise about 20 feet to hold the whole run off. Its surface now fliietuatesfrom zero to ten feet, so 10 feet more over the lake would impound all the availablewater. Off the 2,200 square miles of Kipawa basin, the drainage for 190!.l will be asfollows (estimated from daily discharge chart of Quinze rapids):— Accumulation and emptying Kipawa reservoir. Constant flow desired, 3,800 cubic feet per second. Month. Averageinflow. Excessover desired3,800. Deficit under desired. 3,800. Usingstorage. April c. f. s. 1,600 10,000 4,800 3,000 2, SOU 2,800 2,400 1,100 1,100 900 0. f. s. 6,2008,2001,000 c. f. ,200 sq. ml. ft. sq. ml. May June July 620820lOO ^ August September October . ... .... 8001,0001,0
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Keywords: ., bookauthorcanadapa, bookcentury1800, bookdecade1860, bookyear1868
