Milk River (Alberta–Montana)
The Milk River in Writing-on-Stone Provincial Park
|Name origin: Named by the Lewis and Clark Expedition for its milky color|
|Countries||United States, Canada|
|Source||Confluence of South and Middle Forks|
|- location||Glacier County, Montana|
|- elevation||4,403 ft (1,342 m)|
|- location||Valley County, Montana|
|- elevation||2,024 ft (617 m)|
|- coordinates||Coordinates: |
|Length||729 mi (1,173 km)|
|Basin||23,800 sq mi (61,642 km2) |
|Discharge||for Nashua, Montana, 22.7 mi (36.5 km) from the mouth|
|- average||618 cu ft/s (17 m3/s) |
|- max||45,300 cu ft/s (1,283 m3/s)|
|- min||0 cu ft/s (0 m3/s)|
The Milk River is a tributary of the Missouri River, 729 mi (1,173 km) long, in the United States state of Montana and the Canadian province of Alberta. Rising in the Rocky Mountains, the river drains a sparsely populated, semi-arid watershed of 23,800 sq mi (62,000 km2), ending just east of Fort Peck, Montana.
It is formed in Glacier County in northwestern Montana, 21 miles (34 km) north of Browning, Montana, by the confluence of its South and Middle forks. The 30-mile (48 km) long South Fork and 20-mile (32 km) long Middle Fork both rise in the Rocky Mountains just east of Glacier National Park, in the Blackfeet Indian Reservation. Much of the water in the North Fork is diverted from the St. Mary River through a canal and inverted siphon.
The main stream flows east-northeast into southern Alberta, where it is joined by the North Fork of the Milk River, from there It flows past the town of Milk River and Writing-on-Stone Provincial Park, then turns southeast into Montana, running east along the north side of the Sweetgrass Hills, turning south, passing through the Fresno Dam, then east past Havre and along the north side of the Fort Belknap Indian Reservation. Near Malta, it turns north, then southeast, flowing past Glasgow and joining the Missouri in Valley County, Montana, 5 miles (8 km) downstream from Fort Peck Dam.
- "the water of this river possesses a peculiar whiteness, being about the colour of a cup of tea with the admixture of a tablespoonfull of milk. from the colour of its water we called it Milk river."
This appearance results from clays and silts suspended in its waters. These fine-grained sediments result from the erosion of soft clay-rich rocks along the Milk River basin in southern Alberta, such as the Foremost, Oldman and Dinosaur Park formations.
At the time of Lewis's exploration, the Milk River drainage was legally part of the United States as a component of the Louisiana Purchase. However, in 1818 U.S. negotiators swapped a portion of the Milk River watershed that lay north of 49° north latitude, receiving in exchange a parcel of Red River of the North drainage that had previously been part of British North America.
In 1908, the waters of the Milk River were the subject of a United States Supreme Court case clarifying the water rights of American Indian reservations. The case is known as Winters v. United States.
- Montana Stream Access Law
- List of longest rivers of Canada
- List of longest rivers of the United States (by main stem)
- List of rivers of Montana
- List of rivers of Alberta
- "Milk River". Geographic Names Information System. United States Geological Survey. 1980-04-04. Retrieved 2011-10-28.
- "Overview of the Milk River Watershed". Milk River Watershed Council Canada. Archived from the original on July 29, 2013.
- "USGS Gage #06174500 on the Milk River at Nashua, MT" (PDF). National Water Information System. U.S. Geological Survey. 2010. Retrieved 2011-10-28.
- "Milk River Project". U.S. Bureau of Reclamation. 2011-05-11. Retrieved 2011-10-28.
- Prior, G. J., Hathaway, B., Glombick, P.M., Pana, D.I., Banks, C.J., Hay, D.C., Schneider, C.L., Grobe, M., Elgr, R., and Weiss, J.A. (2013). "Bedrock Geology of Alberta. Alberta Geological Survey, Map 600". Retrieved 2013-08-13.
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