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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Keele River is a tributary of the Mackenzie River, about 410 kilometres (250 mi) long, in the western part of the Canadian Northwest Territories. Flowing in a generally northeast direction, it drains a sparsely populated, rugged area of the Mackenzie Mountains. Originating in a small lake near the border of the Northwest Territories and the Yukon, the Keele flows northwest to join the Tsichu and Intga Rivers, then cuts through the Backbone Ranges. The river turns…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Keele River is a tributary of the Mackenzie River, about 410 kilometres (250 mi) long, in the western part of the Canadian Northwest Territories. Flowing in a generally northeast direction, it drains a sparsely populated, rugged area of the Mackenzie Mountains. Originating in a small lake near the border of the Northwest Territories and the Yukon, the Keele flows northwest to join the Tsichu and Intga Rivers, then cuts through the Backbone Ranges. The river turns to the north as the Natla River comes in from the south. In this north-flowing section, the Ekwi River joins from the left before the Twitya River enters, also from the left, sending the Keele flowing eastwards around the Tigonankweine Range. The Toochingkla River flows in from the right, before the Keele cuts between the Canyon and Redstone Ranges. It then leaves the mountains and receives Middle Creek from the right, merging into the Mackenzie some 13 kilometres (8.1 mi) downstream from the Redstone River and 50 kilometres (31 mi) south-southeast of Tulita.