Course
The river originates south of the Great Bear Lake. It flows south-east through a series of rapids north of the Horn Plateau, then has a meandered flow. Fawn Lake is a complex wetland formed along the middle course of the Horn River, and is followed downstream by the Second Lake. The river turns south-west, where the Mink Lake is formed along its course. The Laferte River also flows into the Mink Lake. Horn River then flows south, and it receives the waters of the Bluefish River before it empties into the Mackenzie River, 100 kilometres (62 mi) downstream from the Great Slave Lake), immediately upstream from Mills Lake, at an elevation of 150 metres (490 ft).
The arch made by the river defines the Horn Plateau, a flat elevated area that rises up to 820 metres (2,690 ft)) to the north and east, while the south is defined by the Mackenzie River east of Fort Simpson.
Africa is a continent comprising 63 political territories, representing the largest of the great southward projections from the main mass of Earth's surface. Within its regular outline, it comprises an area of 30,368,609 km2 (11,725,385 sq mi), excluding adjacent islands. Its highest mountain is Mount Kilimanjaro; its largest lake is Lake Victoria.
The Continental Divide of the Americas is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and Arctic Ocean, including those that drain into the Gulf of Mexico, the Caribbean Sea, and Hudson Bay.
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The Horn River Formation is a stratigraphic unit of Devonian age in the Western Canadian Sedimentary Basin.
The Fort Simpson Formation is a stratigraphical unit of Devonian age in the Western Canadian Sedimentary Basin.
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The Nahanni Formation is a stratigraphical unit of Givetian age in the Western Canadian Sedimentary Basin.
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