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On Flatwillow Creek: The Story of Montana's N Bar Ranch. Exceptional Books Ltd. ISBN 978-0-944-482209 . This article about a property in Montana on the National Register of Historic Places is a stub .
Flatwillow lay along local roads south of the town of Winnett, the county seat of Petroleum County. [2] at an elevation of 3,225 feet (983 m). [1] Flatwillow's post office first opened on March 27, 1883 and closed on April 15, 1907, only to be reopened on August 1, 1908. The post office was again closed on April 30, 1946. [3]
Flat Willow Colony is a Hutterite community [4] and census-designated place (CDP) in Musselshell County, Montana, United States.It is in the northern part of the county, 5 miles (8 km) east of U.S. Route 87 and 25 miles (40 km) north-northeast of Roundup, the Musselshell county seat.
There are at least nine named lakes and reservoirs in Petroleum County, Montana. Lakes. Little Bear Lake, , el. 3,100 feet (940 m) [1] Wild Horse ...
The Pike Creek Hills, are a small range of hills 8.3 miles (13.4 km) west of the community of Flatwillow in Petroleum and Fergus counties in Montana. [1] [2] The highest elevation is an unnamed peak at 4,032 feet (1,229 m) with the stream valleys of Pike Creek to the north and Flatwillow Creek to the south at around 3,500 ft (1,100 m). [1]
Flat Top Mountain is located 9 miles (14 km) east-northeast of Noxon, Montana, in the Cabinet Mountains Wilderness, on land managed by Kaniksu National Forest and Kootenai National Forest. [ 1 ] [ 2 ] It is set west of the Continental Divide in the Cabinet Mountains which are a subrange of the Rocky Mountains . [ 1 ]
Hell Creek Recreation Area is a public recreation area managed by the Little Shell Tribe of Chippewa Indians of Montana occupying 337 acres (136 ha) on the south side of Fort Peck Lake twenty miles (32 km) due north of the community of Jordan, Montana. [4]
Geologically the Little Snowy Mountains are a continuation of the Big Snowy Anticlinorium structure to the west and is entirely underlain by sedimentary rock.The area adjacent to the Big Snowy Mountains is underlain by Mississippian limestone and mudstone and the main part of the range is underlain by the Pennsylvanian Alaska Bench Formation limestone with Jurassic Piper Formation (mudstone ...