Sessional papers of the Dominion of Canada 1911 . , 4.!. —Miti-rmg statiimuii tlie Ietawawii Xo. liapidn, of tlie J<u M,.Mie Kiver. OS _ «- w= ^ E ^ o <a: o \ o O < ~ iij Q o S o o to 1 CD 2< ^ f o / z ./ I ~5 2 < ? < ; <~ -) Q. o< o 8 in c 5 - aN003S a3d X33J DiaOD Nl 39aVH0Sia OTTAWA RIVER STORAGE 77 SESSIONAL PAPER No. 19a liyland creek flows in from the north about 50 miles above the mouth and tenmiles below the river alters its course abruptly to northeast. At High Falls, 30 milesfrom Chats lake, the river descends over the schist o
Sessional papers of the Dominion of Canada 1911 . , 4.!. —Miti-rmg statiimuii tlie Ietawawii Xo. liapidn, of tlie J<u M,.Mie Kiver. OS _ «- w= ^ E ^ o <a: o \ o O < ~ iij Q o S o o to 1 CD 2< ^ f o / z ./ I ~5 2 < ? < ; <~ -) Q. o< o 8 in c 5 - aN003S a3d X33J DiaOD Nl 39aVH0Sia OTTAWA RIVER STORAGE 77 SESSIONAL PAPER No. 19a liyland creek flows in from the north about 50 miles above the mouth and tenmiles below the river alters its course abruptly to northeast. At High Falls, 30 milesfrom Chats lake, the river descends over the schist outcrop into Calabogie lake (507feet above sea) and from here down its coursi? is best understood from an inspection ofthe profile, page T8.
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Keywords: ., bookauthorcanadapa, bookcentury1800, bookdecade1860, bookyear1868
