The Pryor Mountains are a
mountain range in
Carbon and
Big Horn counties of
Montana, and
Big Horn County, Wyoming. They are located on the
Crow Indian Reservation and the
Custer National Forest
Custer National Forest is located primarily in the south central part of the U.S. state of Montana but also has separate sections in northwestern South Dakota. With a total area of , the forest comprises over 10 separate sections. While in the ...
, and portions of them are on private land.
They lie south of
Billings, Montana, and north of
Lovell, Wyoming.
[
The mountains are named for ]Sergeant
Sergeant (abbreviated to Sgt. and capitalized when used as a named person's title) is a rank in many uniformed organizations, principally military and policing forces. The alternative spelling, ''serjeant'', is used in The Rifles and other uni ...
Nathaniel Hale Pryor, a member of the Lewis and Clark Expedition who vainly pursued horses stolen from the expedition in the area. The Crow Nation, a Native American tribe which lived nearby, called the mountains Baahpuuo Isawaxaawuua ("Hitting Rock Mountains") because of the abundance of flint there (which was chipped into arrowheads).
According to Crow Nation folklore, Little People (a race of high dwarf-like people with spiritual powers) lived in these mountains.
Geology
The Pryor Mountains are a region of Montana and Wyoming.[Cruise and Griffiths, p. 185.] The Pryor Mountains consists of Paleozoic, Mesozoic and Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configura ...
sedimentary rocks[Geologic Map] the most prominent unit is limestone (known as the Madison Group limestone) laid down about 300 million years ago.[McRae and Jewell, p. 317.][Gordon and Krumm, p. 2.] The limestone and older sediments rest on Archean metamorphic rock consisting of gneiss and schists.[ The gneiss is exposed along the northeast escarpment of East Pryor Mountain.][ During the Laramide orogeny in the Late Cretaceous and ]Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million yea ...
Period (about 70 to 60 million years ago), the limestone was faulted and uplifted. The thick limestone blocks were tilted and uplifted as large blocks with the northeastern corner of the blocks forming the Bighorn and the Pryor Mountains.
Caves, carved by groundwater, can be found in the limestone throughout the Pryors.[Aarstad, et al., p. 214.] Among the better known are Big Ice Cave on the eastern edge of Pryor Mountain, and Mystery Cave (which contains some of the best speleothems of all the caves in the Pryors). Among the more notable are False Cougar Cave on East Pryor Mountain (which was used by Native Americans at times in the past), Shield Trap Cave (which features a vertical shaft about deep), Little Ice Cave, and Bell Trap Cave (which is similar to Shield Trap). Other popular features of the Pryors include Froggs Fault, a huge fissure in the earth, and a buffalo jump near Dry Head Lookout.[Pospisil, Allan. "Where the Wild Mustangs Play." ''New York Times.'' May 2, 1971.] Just below Dry Head Lookout is a small pocket in the cliff face surrounded by a low man-made fence of rock. This is a place used by several Native American tribes for vision quests, and as of 1971 was perhaps the last undisturbed such place in the United States.
The tallest peak in the Pryor Mountains is East Pryor Mountain (elevation ).
The Bighorn River flows north from Wyoming and through the plateau between the Bighorn and Pryor mountains. The river flows between the two mountain ranges, and has cut the Bighorn Canyon
Bighorn Canyon National Recreation Area is a national recreation area established by an act of Congress on October 15, 1966, following the construction of the Yellowtail Dam by the Bureau of Reclamation. It straddles the border between Wyoming ...
deep into the limestone.
Crooked Creek, one of the few perennial streams in the area, divides the Pryors in two and is one of the few places where Yellowstone cutthroat trout may be found.[French, Brett. "Wild Horse Range Pressured By Overgrazing." ''Billings Gazette.'' July 12, 2009.](_blank)
Accessed 2011-06-07. The Pryors contain the most diverse bat habitat in Montana as well, with 10 species found there.
Wild horse refuge
The Pryor Mountains are also home to the Pryor Mountains Wild Horse Range
The Pryor Mountains Wild Horse Range is a refuge for a historically significant herd of free-roaming mustangs, the Pryor Mountain mustang, feral horses colloquially called "wild horses", located in the Pryor Mountains of Montana and Wyoming in t ...
, a protected area that is home to a herd of free-roaming feral horses.["Wild Horses." Billings Field Office. Bureau of Land Management. United States Department of the Interior. May 2, 2011.](_blank)
Accessed 2011-05-18. This herd was the subject of the 1995 documentary film ''Cloud: Wild Stallion of the Rockies'' and its sequel, the 2003 documentary film ''Cloud's Legacy: The Wild Stallion Returns''.
See also
* List of mountain ranges in Montana
References
Bibliography
*Aarstad, Rich; Arguimbau, Ellen; Baumler, Ellen; Prosild, Charlene L.; and Shovers, Brian. ''Montana Place Names From Alzada to Zortman.'' Helena, Mont.: Montana Historical Society Press, 2009.
*Clawson, Roger and Shandera, Katherine A. ''Billings: The City and the People.'' Billings, Mont.: Billings Gazette, 1993.
*Committee on Ungulate Management in Yellowstone National Park, National Research Council. ''Ecological Dynamics on Yellowstone's Northern Range.'' Washington, D.C.: National Academy Press, 2002.
*Cruise, David and Griffiths, Alison. ''Wild Horse Annie and the Last of the Mustangs: The Life of Velma Johnston.'' New York:Scribner, 2010.
*Frey, Rodney. ''The World of the Crow Indians: As Driftwood Lodges.'' Norman, Okla.: University of Oklahoma Press, 1993.
*Gordon, Paul and Krumm, Bob. ''Bighorn Canyon National Recreation Area.'' Tucson, Ariz.: Southwest Parks and Monuments Association, 1999.
*Hill, Cherry. ''Cherry Hill's Horsekeeping Almanac: The Essential Month-by-Month Guide for Everyone Who Keeps or Cares for Horses.'' North Adams, Mass.: Storey Publishing, 2007.
*Hodges, Montana and Feldman, Robert. ''Rockhounding Montana.'' Guiford, Conn.: Globe Pequot Press, 2006.
*Holt, John. ''Kicking Up Trouble: Upland Bird Hunting in the West.'' Bozeman, Mont.: Wilderness Adventures Press, 1994.
*Holt, Johnny and Diers, Ginny. ''Coyote Nowhere: In Search of America's Last Frontier.'' Guilford, Conn.: Lyons Press, 2004.
Lopez, David A., ''Geologic Map of the Bridger 30' x 60' Quadrangle, Montana,''
Montana Bureau of Mines and Geology, Geologic Map Series No. 58, 2000 with the U.S. Geological Survey
*Massingham, Rhonda. ''Among Wild Horses: A Portrait of the Pryor Mountain Mustangs.'' North Adams, Mass.: Storey Publishing, 2006.
*McRae, W.C. and Jewell, Judy. ''Montana.'' Berkeley, Calif.: Avalon Travel, 2009.
*Montgomery, M.R. ''Many Rivers to Cross: Of Good Running Water, Native Trout, and the Remains of Wilderness.'' New York: Simon and Schuster, 1996.
*Rowles, Genevieve. ''Adventure Guide to Montana.'' Edison, N.J.: Hunter Publishing, 2000.
*Saindon, Robert A. ''Explorations Into the World of Lewis and Clark.'' Great Falls, Mont.: Lewis and Clark Trail Heritage Foundation, 2003.
*Voight, Barry and Voight, Mary Anne. ''Rock Mechanics, the American Northwest.'' University Park, Pa.: Pennsylvania State University, 1974.
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Ranges of the Rocky Mountains
Mountain ranges of Montana
Mountain ranges of Wyoming
Landforms of Carbon County, Montana
Landforms of Big Horn County, Montana