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The Wind River Range (or "Winds" for short) is a mountain range of the Rocky Mountains in western Wyoming in the United States. The range runs roughly NW–SE for approximately 100 mi (160 km). The Continental Divide follows the crest of the range and includes Gannett Peak, which at 13,802 ft (4,207 m), is the highest peak in Wyoming; and also Fremont Peak at 13,750 ft (4,191 m), the third highest peak in Wyoming. There are more than 40 other named peaks in excess of 12,999 ft (3,962 m). With the exception of the Grand Teton in the Teton Range, the next 19 highest peaks in Wyoming after Gannett are also in the Winds.[3]

Wind River Range
Wind River Range highcountry
Highest point
PeakGannett Peak[1]
Elevation13,804 ft (4,207 m)
Coordinates43°11′04″N 109°39′12″W
Length100 mi (160 km) NW/SE
Width30 mi (48 km) SW/NE
Area2,800 sq mi (7,300 km2)
The Wind River Range highlighted in pink
CountryUnited States
Parent rangeRocky Mountains
A Shoshone encampment in the Wind River Mountains of Wyoming, photographed by W. H. Jackson, 1870
A Shoshone encampment in the Wind River Mountains of Wyoming, photographed by W. H. Jackson, 1870
Green River Lakes and Squaretop Mountain[2]
Green River Lakes and Squaretop Mountain[2]
Titcomb Lakes
Titcomb Lakes
Looking across the Bonneville Basin to Mount Bonneville and Raid Peak.
Looking across the Bonneville Basin to Mount Bonneville and Raid Peak.

Two large national forests including three wilderness areas encompass most of the mountain range. Shoshone National Forest is on the eastern side of the continental divide while Bridger-Teton National Forest is on the west. Both national forests and the entire mountain range are an integral part of the Greater Yellowstone Ecosystem. Portions of the east side of the range are inside the Wind River Indian Reservation.


Indigenous peoples of the Great Basin, such as the Shoshones and Absarokas (Crow) Native Americans, lived in the range beginning 7000 and 9000 years ago. Villages as high as 10,000 ft (3,000 m) in elevation, dating from 700 to 2000 BC, have recently been studied by archaeologists. These villages were established by the Sheepeater band of Shoshone during pine nut harvesting season. One, dubbed "High Rise", has 60 lodges over a space of 26 acres and was recently added to the National Register of Historic Places.[4]

One of the men from the Lewis and Clark expedition, John Colter, is thought to be the first European American person to view the range when he visited the area around 1807, though little is known about his travels through the area. In 1812, a party led by Wilson Price Hunt were the first to cross South Pass, at the southern end of the range, the pass which marked the continental divide and crest of the Rocky Mountains and became an important portion of the Oregon Trail.[1]

Climbing was pursued in the mid to late 1800s by men such as John C. Fremont, typically for the purpose of surveying the region. Early climbers to come purely for recreation began arriving in the 1920s. Gannett Peak, the range and Wyoming's tallest, was first climbed by Arthur Tate and Floyd Stahlnaker in 1922. Most of the early climbing in the region focused around the Titcomb Basin, slowly radiating outwards. Today, the Titcomb Basin remains one of the area's busiest recreation attractions along with the Cirque of the Towers to the south.[1]

Much of the Wind River Range received federal protection as National Forest primitive areas during 1931–32. The Wind River Range is now largely protected by three federal wilderness areas. These include the Bridger Wilderness on the western slope, designated in 1964, and the Fitzpatrick Wilderness and Popo Agie Wilderness on the eastern slope, designated in 1976 and 1984 respectively. Together these wilderness areas protect 728,020 acres (294,620 ha), making the Wind River Range one of the largest road-free areas in the continental United States. Part of the eastern slope of the Wind River Range is also under the protection of the Wind River Indian Reservation.


The Winds are composed primarily of a granitic batholith which is granite rock formed deep under the surface of the Earth, over one billion years ago. Over hundreds of millions of years, rocks that were once covering this batholith eroded away. As the land continued to rise during the Laramide orogeny, further erosion occurred until all that remained were the granitic rocks.[5] The ice ages beginning 500,000 years ago began carving the rocks into their present shapes. Within the Winds, numerous lakes were formed by the glaciers and numerous cirques, or circular valleys, were carved out of the rocks, the most well known being the Cirque of the Towers, in the southern section of the range. Shoshone National Forest claims that there are 16 named and 140 unnamed glaciers just on the east side of the range for a total of 156, with another 27 reported by Bridger-Teton National Forest for the western slopes of the range. Several of these are the largest glaciers in the U.S. Rocky Mountains. Gannett Glacier which flows down the north slope of Gannett Peak, is the largest single glacier in the Rocky Mountains of the U.S., and is located in the Fitzpatrick Wilderness in Shoshone National Forest.


Several major rivers have headwaters on either side of the range. The Green and Big Sandy rivers drain southward from the west side of the range, while the Wind River drains eastward through the Shoshone Basin. The Green is the largest fork of the Colorado River while the Wind River, after changing its name to the Bighorn River, is the largest fork of the Yellowstone River. The range includes several canyons on either side, including Silas Canyon and Sinks Canyon both on the eastern side. The canyons are carved by rivers such as the Middle Fork of the Popo Agie which feeds the Wind River.

The Bridger Wilderness contains over 1,300 lakes. These lakes range in size from less than 3 acres (1 ha) to over 200 acres (81 ha), with an average size of about 10 acres (4 ha). Historically, the lakes and streams of the Bridger Wilderness were devoid of fish, as were most alpine lakes throughout the Rocky Mountains. The first known transplant of fish into the area took place in 1907 when Colorado River cutthroat trout were introduced into North Fork Lake. Considerable fish stocking by individuals, the U.S. Forest Service, and the Wyoming Game & Fish Department, occurred between 1924 and 1935.[6]


Lake d'Amalia, late 19th century
Lake d'Amalia, late 19th century
Wind River Range – looking southwest from near the top of Fremont Peak – during a backpacking trip.
Wind River Range – looking southwest from near the top of Fremont Peak – during a backpacking trip.

The Winds are known to have a small grizzly bear population, primarily in the northernmost areas. Other mammals include the black bear, elk, moose, mule deer, pronghorn, bighorn sheep, mountain lion and wolverine. Bald eagles, falcons and hawks are just a few of the 300 species of birds known to inhabit the region. The streams and lakes are home to Yellowstone cutthroat, rainbow, brook, brown, lake, and golden trout—about 2.5 million of which were stocked by a local explorer named Finis Mitchell and his wife during the Great Depression. The forests are dominated by lodgepole pine, whitebark pine, subalpine fir, and Engelmann spruce.

The range sits alongside many of the animal migration routes in the United States and contains several important passes, notably South Pass, 7,549 ft (2,301 m), at the south end of the range, which was one of the more important passes on the Oregon Trail as it passed through the Rockies. Aside from South Pass, which is at the southernmost tip of the range, no roads cross the mountains until Union Pass, 9,209 ft (2,807 m) at the northern terminus of the range. There are many passes between tall peaks across the continental divide, which runs through the entire range.


The Winds are a popular recreation destination and the vast wilderness areas attract hikers, climbers and skiers. The Winds have many back country areas that see heavy use despite the relative remoteness of many of the trail-heads and the long approaches from those trail-heads to reach routes. Two of the more popular backpacking destinations are the Titcomb Basin (commonly accessed via the Elkhart Park Trailhead)[7] and the Cirque of the Towers (commonly accessed via the Big Sandy Trailhead).[8] The exposed granite in the higher elevations of the range is particularly attractive to climbers and areas such as Cirque of the Towers in the southern portion of the range are facing overuse issues as a result.[1] According to the White Pine Ski Resort website, the Winds are home to one ski area, White Pine, the only lift-accessible skiing and snowboarding in the range. Located near Pinedale, it is the oldest ski area in Wyoming.[9]


The Wind River Range has a number of trailheads for backpackers to explore, including:

A longtime popular destination for outdoor enthusiasts, the Wind River Range has also played host to a number of wilderness and outdoor education programs. The number of trailheads and terrain variety have made it an ideal stage for learning and exploration.[10]


Encountering bears is a concern in the Wind River Range.[11] There are other concerns as well, including bugs, wildfires, adverse snow conditions and nighttime cold temperatures.[12]

Importantly, there have been notable incidents, including accidental deaths, due to falls from steep cliffs (a misstep could be fatal in this class 4/5 terrain) and due to falling rocks, over the years, including 1993,[13] 2007 (involving an experienced NOLS leader),[14] 2015[15] and 2018.[16] Other incidents include a seriously injured backpacker being airlifted near SquareTop Mountain[2] in 2005,[17] and a fatal hiker incident (from an apparent accidental fall) in 2006 that involved state search and rescue.[18] The U.S. Forest Service does not offer updated aggregated records on the official number of fatalities in the Wind River Range.

See also


  1. Kelsey, Joe (1980). Climbing and Hiking in the Wind River Mountains. The Sierra Club. ISBN 0-87156-267-7.
  2. Funk, Jason (2009). "Squaretop Mountain Rock Climbing". Mountain Project. Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  3. "Wyoming 13,000-foot Peaks". Peakbagger. Retrieved April 6, 2007.
  4. Watson, Traci (October 20, 2013). "Wyoming site reveals more prehistoric mountain villages". USA Today. Retrieved October 20, 2013.
  5. Steidtmann, James R.; Middleton, Larry T.; Shuster, Mark W. (1989). "Post-Laramide (Oligocene) uplift in the Wind River Range, Wyoming". Geology. The Geological Society of America. 17 (1): 38–41. doi:10.1130/0091-7613(1989)017<0038:plouit>;2.
  6. A Guide to Bridger Wilderness Fishing Lakes. 1979, U.S. Department of Agriculture.
  7. "Titcomb Basin – Wind River Range, WY (40 mile route)". November 19, 2019.
  8. "Cirque of the Towers Loop – Wind River Range, WY (45 mile loop)". August 7, 2019.
  9. "White Pine Ski Resort". Retrieved November 9, 2012.
  10. Staff (2016). "Wind River Mountain Range: Higher, Longer, Deeper – Woming's Largest Range". Retrieved March 16, 2019.
  11. Staff (April 24, 2017). "Bear Safety in Wyoming's Wind River Country". Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  12. Ballou, Dawn (July 27, 2005). "Wind River Range condition update - Fires, trails, bears, Continental Divide". PineDaleOnline News. Archived from the original on April 21, 2021. Retrieved May 31, 2022.
  13. Staff (1993). "Falling Rock, Loose Rock, Failure to Test Holds, Wyoming, Wind River Range, Seneca Lake". American Alpine Club. Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  14. MacDonald, Dougald (August 14, 2007). "Trundled Rock Kills NOLS Leader". Climbing. Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  15. Staff (December 9, 2015). "Officials rule Wind River Range climbing deaths accidental". Casper Star-Tribune. Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  16. Dayton, Kelsey (August 24, 2018). "Deadly underestimation". WyoFile News. Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  17. Staff (July 22, 2005). "Injured man rescued from Square Top Mtn - Tip-Top Search & Rescue helps 2 injured on the mountain". PineDaleOnline News. Archived from the original on July 26, 2021. Retrieved May 31, 2022.
  18. Staff (September 1, 2006). "Incident Reports - September, 2006 - Wind River Search". Archived from the original on January 27, 2020. Retrieved May 31, 2022.

На других языках

[de] Wind River Range

Die Wind River Range [.mw-parser-output .IPA a{text-decoration:none}wɪnd ˈɹɪvə˞ ɹeɪndʒ] (dt. „Wind-Fluss-Bergkette“), kurz Winds, ist ein Gebirgszug der Rocky Mountains. Die Bergkette verläuft im Westen des US-Bundesstaates Wyoming von Nordwest in südöstliche Richtung und bildet auf einer Länge von rund 190 km einen Teil der kontinentalen Wasserscheide Nordamerikas. Innerhalb der Bergkette befinden sich mit dem Gannett Peak der höchste Berg in Wyoming, sowie, mit Ausnahme des Grand Teton in der Teton Range, die zwanzig höchsten Berge des Bundesstaates.
- [en] Wind River Range

[es] Cordillera Wind River

La cordillera Wind River (en inglés, Wind River Range, que significa «cordillera del río Viento») (o familiarmente, los «Winds», vientos), es una cordillera de los Estados Unidos localizada en el oeste del estado de Wyoming, una de las estribaciones orientales de las Montañas Rocosas. La cordillera discurre en dirección aproximada NW—SE, durante unos 160 km.

[fr] Chaîne de Wind River

La chaîne de Wind River est une chaîne de montagnes des Rocheuses située dans l’Ouest du Wyoming aux États-Unis. Elle s’étend sur environ 160 km dans une direction NO-SE. Le Continental Divide suit les crêtes de la chaîne montagneuse dont le point culminant se nomme pic Gannett (4 207 m) et qui constitue le point culminant du Wyoming. Il existe plus de trente sommets dont l’altitude avoisine ou dépasse les 4 000 mètres[1]. Les montagnes appartiennent en partie au domaine propre à deux forêts nationales américaines comportant trois réserves sauvages. Il s’agit de la forêt nationale de Shoshone et de la forêt nationale de Bridger-Teton. Ces forêts font elles-mêmes partie intégrante du Greater Yellowstone Ecosystem. Une partie des montagnes appartient aussi à la réserve indienne de Wind River.

[ru] Уинд-Ривер (хребет)

Уи́нд-Ри́вер[2] (англ. Wind River Range) — горный хребет на западе штата Вайоминг (США), в системе Скалистых гор.

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