The Idaho Batholith underlies most of Boise National Forest, forming the forest's Boise, Salmon River, and West mountain ranges; the forest reaches a maximum elevation of 9,730 feet (2,970m) on Steel Mountain. Common land cover includes sagebrush steppe and spruce-fir forests; there are 9,600 miles (15,400km) of streams and rivers and 15,400 acres (62km2) of lakes and reservoirs. Boise National Forest contains 75 percent of the known populations of Sacajawea's bitterroot, a flowering plant endemic to Idaho.
The Shoshone people occupied the forest before European settlers arrived in the early 19th century. Many of the early settlers were trappers and prospectors before gold was discovered in 1862. After the 1860s Boise Basin gold rush ended, mining of tungsten, silver, antimony, and gold continued in the forest until the mid-twentieth century. Recreation facilities include over 70 campgrounds, whitewater and flatwater boating, cabin rentals, and 1,300 miles (2,100km) of trails for hiking, biking, horseback riding, and motorized off-road vehicle use. The Forest Service has an objective to maintain timber, range, water, recreation, and wildlife for multiple use and sustained yield of its resources.
History
A hydraulic jet being used to mine placers in the Boise Basin in 1929The CCC constructed many structures throughout the forest from 1933 until 1942, including this guard station in 1933.
Archaeological evidence indicates that human habitation in Idaho began towards the end of the last ice age: bone fragments about 10,000 years old have been found in Wilson Butte Cave, an inflationary cave on the Snake River Plain believed to have been occupied by indigenous people until as recently as the 17th century.[6] A change of climate around 7000 years ago dried up much of the Great Basin, forcing the Shoshone people northward into the mountainous areas of central Idaho.[7] Most of what is now Boise National Forest was sparsely inhabited by Native Americans, and several archaeological sites, including campsites, rock shelters, burial grounds, and pictographs have been found along rivers in the area.[8] Trappers and fur traders of European descent first arrived in the area in the early 1800s, starting with John Jacob Astor's Pacific Fur Company in October 1811. Donald Mackenzie and Francois Payette trapped in the area of Boise National Forest in 1819.[9] By 1840, the fur trade was coming to an end, but the westward migration on the Oregon Trail, which passed south of the forest, was beginning.[10] The first settlers moved into the mountains in the 1860s after gold was discovered in Idaho, which forced many of the Shoshone out and led to conflicts throughout the state, including the Bannock War in southern Idaho.[8]
Prospectors George Grimes and Moses Splawn were the first to discover gold in the forest at the eponymous Grimes Creek on August 2, 1862. Subsequent gold discoveries at Rocky Bar in 1863 and Atlanta in 1864 increased the rush of people to Idaho, and in 1863 Idaho City, with a population of 6,267, surpassed Portland, Oregon as the largest city in the Pacific Northwest. The Idaho gold rush was largely over by 1870, and the population of the Boise Basin fell from 16,000 to 3,500.[11] In 1898 the forest's first gold dredge was built in Placerville and followed by several others. By 1951, when the last dredges shut down, at least 2.3 million ounces (65.2 million grams) of gold had been produced from the Boise Basin area.[12]Silver was mined along the Crooked River from 1882 until 1921, but a silver mine at Silver Mountain proved unsuccessful.[13] Following a shortage of mercury during World War II, mines in the Stibnite area became the country's largest producer of tungsten and second largest source of mercury.[14] The most important known placer deposit of niobium and tantalum in the United States is located in Bear Valley.[14] From 1953 until 1959, dredges there produced $12.5 million ($131million today[15]) in niobium, tantalum, and uranium. Other minerals mined in the forest include antimony and molybdenum.[14]
U.S. Forest Service
Lucky Peak Nursery grows trees for restoration projects throughout the Intermountain region.
Boise National Forest was created on July 1, 1908, from part of Sawtooth National Forest, and originally covered 1,147,360 acres (4,643.2km2).[3] By the Forest Reserve Act of 1891, the U.S. Congress granted the U.S. President the authority to establish forest reserves out of Public Domain Lands that were subject to disposal (homesteads, sales, etc.) administered by the United States General Land Office, which had been placed under the authority of the U.S. Department of the Interior in 1849.[16] With the passage of the Transfer Act of 1905, forest reserves were transferred to the U.S. Department of Agriculture in the newly created U.S. Forest Service.[17] Present-day Boise National Forest was first protected as part of two forest reserves by proclamations issued by President Theodore Roosevelt: Sawtooth Forest Reserve (created on May 29, 1905, and expanded on November 6, 1906) and Payette Forest Reserve (created on June 3, 1905).[3] After forest reserves were renamed national forests in 1908, Boise National Forest was split from Sawtooth National Forest into an independent national forest. Emile Grandjean was the forest's first supervisor, serving from 1908 to 1922.[18] On April 1, 1944, the entirety of what was then Payette National Forest was transferred to Boise National Forest, and simultaneously Weiser and Idaho national forests were combined to reestablish the present-day Payette National Forest, which is to the north of Boise National Forest. In 1933 the Boise Basin Experimental Forest was created on 8,740 acres (35.4km2) of the forest near Idaho City to study the management of ponderosa pine.[19] The Lucky Peak Nursery was established in 1959 to produce trees for planting on burned or logged lands on the national forests of the Intermountain region.[20][21]
After the creation of the Civilian Conservation Corps (CCC) in 1933, nine camps and eight subcamps were set up in Boise National Forest, but the number of camps was reduced from 1934 until the program was closed in 1942. Work conducted by the CCC included fire suppression, fish habitat improvement, and construction of guard houses, fire lookouts, campgrounds, roads, and trails, among other facilities.[22]
Management
Map of Boise (orange) and surrounding national forests (green)
Boise National Forest is managed by the U.S. Forest Service, an agency within the Department of Agriculture, as five units called ranger districts. The ranger districts are Cascade (400,000 acres or 1,600 square kilometers), Emmett (350,000 acres or 1,400 square kilometers), Idaho City (400,000 acres), Lowman (400,000 acres), and Mountain Home (650,000 acres or 2,600 square kilometers); each has an office in their respective cities and is managed by a district ranger, while forest headquarters are located in the city of Boise.[23]Congress proclaimed 2,648,273 acres (10,717.18km2) of Idaho part of Boise National Forest, but the forest manages only 2,203,703 acres (8,918.07km2).[2][24] The proclaimed boundary is set and can only be changed by Congress whereas the administered boundary can be shifted among adjacent national forests without congressional approval. For management (and from the visitor's perspective) the forest's boundaries are its administered area.[24]
Land areas of Boise National Forest administered by or proclaimed part of another national forest
Trinity Mountain is the second highest point in the forest.Warm Lake is the largest natural lake in Boise National Forest.
Elevations in the forest range from 2,800 feet (850m) in the North Fork Payette River Canyon to 9,730 feet (2,970m) at the top of Steel Mountain, a gain of 6,930 feet (2,110m).[28] The forest contains several subranges of the Rocky Mountains, including the Boise, Salmon River, and West mountain ranges. Much of the forest is underlain by the Idaho Batholith, and the forest is dominated by granitic rock, but intrusions of basalt can be found to the west and other volcanic rocks to the south.[29]
North of the South Fork Payette River and east of the North Fork Payette River, the forest is part of the Salmon River Mountains, which extend north and east outside the forest's boundaries. The South Fork Salmon River Range and the North Fork Range are subranges of the Salmon River Mountains within Boise National Forest.[30][31][32][33] The Boise Mountains cover much of the southern portion of the forest and contain the forest's highest point, Steel Mountain, but the range's highest point, Two Point Mountain, lies outside of the forest's boundary.[34][35][36] The Trinity Mountains are a subrange in southeastern part of the Boise Mountains that reach their peak at 9,451 feet (2,881m) on Trinity Mountain.[37][38] The westernmost portion of the forest south and west of Lake Cascade are part of the West Mountains, which reach their highest point at 8,320 feet (2,540m) on Snowbank Mountain.[39][40][41][42] The Danskin Mountains are a smaller range on the forest's southern border that run northwest to southeast.[37][43]
Waterways
The Arrowrock Dam, pictured in 1938, was the tallest dam in the world from 1915 until 1924.
There are an estimated 9,600 miles (15,400km) of perennial and intermittent streams and 15,400 acres (62km2) of lakes and reservoirs in the forest. The Forest Service provides access to and recreation opportunities at the seven reservoirs it borders, although it does not own or manage them. There are numerous natural lakes in the forest, most of which are tarns created by alpine glaciers during the Pleistocene. The largest, Warm Lake, is 26 miles (42km) east of Cascade in Valley County; many of the smaller lakes are in the Trinity and West mountains.[45][46][47] Annual water yield on the forest is estimated at 4.1million acre-feet (5.1billioncubic meters).[29] The southern portion of the forest is drained by the Boise River, the central and western portions by the Payette River, northeastern portion by the Salmon River, and far western portions of the Emmett Ranger District by the Weiser River.[37] All four rivers are tributaries of the Snake River, which itself is a tributary of the Columbia River in the Pacific basin.[48]
Daily high temperatures range from 9 to 29°F (−13 to −2°C) in winter to 80 to 90°F (27 to 32°C) in summer, while lower elevations can experience conditions over 100°F (38°C). Idaho's mountain ranges can block Arctic air in the winter, but when cold air masses do enter the area, they sometimes stagnate in the Snake and Salmon river valleys, causing very cold temperatures to persist. Summer and fall are generally dry, while intense short-duration thunderstorms can occur in late spring and early summer as atmospheric moisture interacts with warm temperatures and steep topography via orographic lifting. During winter, warm, moist air from the Pacific Ocean often brings rain at lower elevations in addition to snowfall throughout the forest. The influence of these Pacific maritime air masses increases as latitude increases in the forest. Average annual snowfall ranges from 55 inches (140cm) in drier areas and at lower elevations to 70 inches (180cm) in wetter locations and higher elevations. The growing season within the forest ranges from over 150 days in lower elevations to less than 30 days in alpine areas.[29]
Boise National Forest is within the Idaho Batholith ecoregion, which is a level IIIecoregion in the larger level I Northwestern Forested Mountains.[52] In addition to species listed or proposed for listing as threatened or endangered under the Endangered Species Act, the Forest Service maintains an independent listing of sensitive species for which it is directed to "develop and implement management practices to ensure that species do not become threatened or endangered because of Forest Service actions."[53] As of February 2013 there were 27 species in Boise National Forest listed as sensitive species: 6 mammals, 1 amphibian, 1 fish, 13 birds, and 6 plants.[54]
Flora
The riparian zone along rivers can be quite narrow, quickly transitioning to drier Douglas fir and ponderosa pine forests.
An estimated 76 percent of Boise National Forest is forest, which according to the Forest Service is considered land capable of supporting trees on at least 50 percent of its area. The forests are primarily coniferousevergreens, dominated by Douglas fir and ponderosa and lodgepole pines at lower elevations and Engelmann spruce, subalpine fir, and whitebark pine at higher elevations. Grand fir and western larch (a coniferous deciduous tree) grow in the northern part of the forest where there are moister conditions. Quaking aspen, a broadleaf deciduous tree, grows both in stands among conifers and in monotypic stands throughout the forest at elevations above 5,000 feet (1,500m). Non-forested areas occupy 23 percent of the forest, primarily on south-facing slopes, lower elevations in the forest's southern latitudes, or high-elevation areas and are dominated by grasses, forbs, or shrubs.[55]
Sacajawea's bitterroot is a plant species endemic to central Idaho, including parts of Boise National Forest, being found nowhere else in the world. Only about two dozen populations of the plant are known to exist, and three-quarters of these are in Boise National Forest. It is usually found at elevations ranging from 5,000 feet (1,500m) to 9,500 feet (2,900m) above sea level and produces white flowers shortly after snowmelt.[56][57]
Boise National Forest is directed by the U.S. Forest Service to "control the establishment, spread, or invasion of non-indigenous plant species in otherwise healthy native vegetative ecosystems."[58] The forest's plan addresses the need to control invasive plants, and management efforts include chemical, mechanical, and biological control methods. Invasive plants that are of particular concern in Boise National Forest include spotted knapweed, yellow star-thistle, rush skeletonweed, and leafy spurge, among others.[59][60]
In cool, moist areas ranging from 4,800 feet (1,500m) to 6,800 feet (2,100m), Douglas fir is predominant. Lodgepole pine and quaking aspen may be found alongside Douglas fir in cooler areas, both moist and dry, but particularly where frost pockets form. Understories in this forest type are dominated by mountain maple, mountain ash, and blue huckleberry in moister areas and white spirea, common snowberry, elk sedge, and pinegrass in drier areas.[62] Between 3,400 feet (1,000m) and 6,500 feet (2,000m) in the moist northern parts of the forest, grand fir is predominant and western larch is one of the first trees to become established during ecological succession following disturbances, whereas understories consist of mountain maple, mountain ash, blue huckleberry, and mallow ninebark.[63] Subalpine fir dominates from 4,800 feet (1,500m) to 7,500 feet (2,300m) along with mountain maple, serviceberry, Scouler's willow, Sitka alder, menziesia, Utah honeysuckle, and mountain ash.[64]
Sacajawea's bitterroot is a small plant that grows to be 1.2 to 2.75 inches (30 to 70mm) tall.
Lodgepole pine dominates in cold, dry areas from 5,200 feet (1,600m) to 9,200 feet (2,800m). The understory in lodgepole pine forests can be sparse but includes grasses, forbs, huckleberries, and grouse whortleberry, although fires in these forests are typically lethal to trees and understories alike.[64] At the highest elevations, forests consist of subalpine fir alongside whitebark pine and Engelmann spruce. Grasses and forbs tolerant to freezing throughout the growing season occupy the understory.[64]
Timber wolves are top predators that were reintroduced amidst controversy to central Idaho in the mid-1990s to restore ecosystem stability. The wolves have since expanded their range and established packs in most of Boise National Forest. Wolves and mountain lions are the forest's top large mammal predators and have no predators of their own except humans.[69][70]:12 Most of the forest's native mammal species are present in the forest, with the exception of grizzly bears, which have become locally extinct, and plans for their reintroduction to central Idaho have been proposed since the 1990s but have not progressed.[71][72]
Of the 28 fish species present in the forest, 11 are not native and have been introduced by humans.[55]Rainbow trout, chinook salmon, westslope cutthroat trout, bull trout, and mountain whitefish are all native to some of the forest's waterways, while brook trout are a common invasive species that compete with the forest's salmonids.[68] The forest's management indicator species is bull trout because they are sensitive to habitat changes and depend on specific habitat conditions.[73]Sockeye salmon are native to the Salmon River watershed in the northern part of the forest, but dam construction on the Columbia and Snake rivers has hampered the migration of this anadromous fish and caused its population to collapse. Warm Lake supports the forest's only native population of Kokanee salmon, the resident (non-migratory) form of sockeye salmon. However, due to introductions by humans, Anderson Ranch, Arrowrock, Lucky Peak, and Deadwood reservoirs now support populations of Kokanee salmon.[74][75][76] To provide additional recreational fishing opportunities, the Idaho Department of Fish and Game stocks several of the forest's waterways with rainbow trout, while reservoirs are also stocked with Kokanee or chinook salmon and Lake Cascade is stocked with coho salmon and steelhead, the anadromous form of rainbow trout.[77][78]
Over 270 bird species have been observed in central Idaho, including 36 accidental species – those that are not normally found in the region but have been observed on at least one occasion. Golden eagles and greater sage-grouse can be found over sagebrush steppe, whereas bald eagles can be seen along rivers. The Forest Service has listed northern goshawks, flammulated owls, and white-headed woodpeckers as a sensitive species in the forest.[54][79][80]
The Elk Complex Fire burned 146,832 acres (594.21km) in 2013.
Boise National Forest's 2010 forest plan recognizes that fire and other disturbances play important roles in maintaining the character and function of ecosystems. However, previous management strategies (as recently as the 1990 forest plan) treated fire as an undesirable process, and the Organic Act of 1897 explicitly stated that forests were to be protected from destruction by fire.[55] In historic conditions fires naturally occurred on the landscape; the suppression of fires allowed dead trees to accumulate in excess of historic levels and land cover types to change, such as a shift to higher shrub and tree densities.[82] An estimated 14 percent of the land in Boise National Forest has been affected by fires since the early 1990s, and about 10 percent of the land capable of timber production was burned so severely that land cover shifted from forest to grass and shrubland (as of 2010).[83]
A Sikorsky S-64 Skycrane fighting the Ridge Fire, which burned 5,315 acres (21.51km) in 2013
Between 2004 and 2013 an average of 74,325 acres (300.78km2) were burned by fires per year with a maximum of 346,500 acres (1,402km2) in 2007 and a minimum of 152 acres (0.62km2) in 2008.[85] For example, in 2012 there were 26 fires started by people and 109 started by lightning, which together burned a total of 152,000 acres (620km2). The Trinity Ridge Fire alone burned 146,800 acres (594km2) over two months, although it was not confined to Boise National Forest lands.[86]
The revised 2010 forest plan recognized the need to develop plans to manage wildfires at the wildland–urban interface, use prescribed fire as a tool to manage ecosystem health, and meet air quality requirements set by the Clean Air Act.[87] The forest operates a fire management plan under federal fire policy that gives fire personnel direction for responding to unintended ignitions. Occasionally, area closures and restrictions on use, such as prohibition of campfires, are implemented to aid in wildfire prevention. Following severe fires, area closures may be put in place to protect the public from risks such as falling trees and landslides.[85][88] Proactive fire management strategies include prescribed burns and mechanical reduction of fuel levels. For instance, in 2014 Boise National Forest planned to conduct 7,919 acres (32.05km2) of prescribed burns and 155 acres (0.63km2) of mechanical treatment.[89] The forest seasonally maintains staff at seven fire lookout towers, while six others remain unstaffed.[90]
Recreation
A campsite in Yellow Pine Campground, one of over 70 campgrounds in the forestA trail passes through grasses and penstemon on a drier hillside capable of supporting few trees.
There are over 70 campgrounds in Boise National Forest and groups of more developed recreation facilities at the Trinity Mountains, Warm Lake, and Deadwood and Sage Hen reservoirs.[37] As in most national forests, the majority of the land in Boise National Forest is open to dispersed camping (outside of developed campgrounds).[91] One of the forest's fire lookouts, Deadwood Lookout, is now available as a cabin for the public to rent, among other sites.[92][93] Bicycles are allowed on forest roads and on more than 1,300 miles (2,100km) of multiple-use trails, whereas over 1,200 miles (1,900km) of trails are open to motorized recreation.[94] The Danskin Mountains Off-Highway Vehicle Trail System contains 150 miles (240km) of motorcycle and ATV trails on 60,000 acres (24,000ha) of land that is generally open from April through November. The forest's Trinity Mountain Recreation Area includes the highest drivable (4-wheel drive recommended) road in Idaho, which ascends to the Trinity Mountain Lookout at an elevation of over 9,400 feet (2,900m).[95] In 2013 revenues from recreation and special use fees amounted to $454,635, while expenses totaled US$352,550; the difference is allocated to the following season's startup costs.[96]
Waterways
Rivers in Boise National Forest offer the opportunity for rafting and kayaking through rapids up to class four, with the most difficult sections on the South Fork and main stems of the Payette River. Numerous developed boat launch sites provide access to rivers for whitewater enthusiasts, and Dagger Falls is the primary launching site for visitors to the Middle Fork of the Salmon River and Frank Church River of No Return Wilderness. Motorized boating is permitted on Anderson Ranch Reservoir, Deadwood Reservoir, and Warm Lake.[95]
Winter activities
During winter, visitors to the forest can participate in activities including snowmobiling, snowshoeing, and downhill and cross-country skiing. The Bogus Basin ski area is located within the forest north of Boise and has 7 chairlifts and 53 runs on 2,600 acres (11km2) of skiable terrain.[97] There are 137 miles (220km) of groomed snowmobile trails in the Garden Valley system in the Emmett Ranger District[23] and several Mongolian-style yurts available for rental in winter.[95]
Scenic roads
Boise National Forest is home to three of Idaho's scenic byways, all of which are paved highways accessible to roadworthy vehicles. The Payette River Scenic Byway is an 80-mile (130km) route between Eagle and McCall on Idaho State Highway 55. The route follows the Payette River between McCall and Horseshoe Bend, but the majority of the highway does not pass through Boise National Forest; only a small portion north of Horseshoe Bend is in the Emmett Ranger District. Over half of the 35-mile (56km) Wildlife Canyon Scenic Byway, which travels between highway 55 and Lowman, passes through the forest, parallels the South Fork of the Payette River, and is signed as the Banks-Lowman Road. The Ponderosa Pine Scenic Byway is a 130-mile (210km) road between Stanley and Boise following Idaho State Highway 21. This route passes over Arrowrock Reservoir and through Idaho City and Lowman, where it connects with the Wildlife Canyon Byway. North and east of Lowman the byway partially follows the South Fork of the Payette River before ascending to the 7,037-foot (2,145m)Banner Creek Summit at the forest's boundary with Salmon-Challis National Forest.[95][98][99][100]
The Snake River is a major river in the interior Pacific Northwest region of the United States. About 1,080 miles (1,740 km) long, it is the largest tributary of the Columbia River, which is the largest North American river that empties into the Pacific Ocean. Beginning in Yellowstone National Park, western Wyoming, it flows across the arid Snake River Plain of southern Idaho, the rugged Hells Canyon on the borders of Idaho, Oregon and Washington, and finally the rolling Palouse Hills of southeast Washington. It joins the Columbia River just downstream from the Tri-Cities, Washington, in the southern Columbia Basin.
The Gospel Hump Wilderness is a federally-protected wilderness area that covers 205,796 acres (83,283 ha) of the state of Idaho. Managed by the U.S. Forest Service in the U.S. Department of Agriculture, it received wilderness designation on February 24, 1978 through the passage of the Endangered American Wilderness Act and is part of Nez Perce National Forest. As part of the National Wilderness Preservation System, the Gospel Hump Wilderness is an area where human development and use are restricted and people are to remain only visitors.
The Frank Church—River of No Return Wilderness Area is a protected wilderness area in Idaho. It was created in 1980 by the United States Congress and renamed in 1984 as the Frank Church-River of No Return Wilderness Area in honor of U.S. Senator Frank Church.
Salmon–Challis National Forest is located in east central sections of the U.S. state of Idaho. At 4,235,940 acres it is one of the largest national forests in the lower 48 states and also has most of the land area of the Frank Church–River of No Return Wilderness, which is the largest wilderness area south of Alaska.
The Payette River is an 82.7-mile-long (133.1 km) river in southwestern Idaho and a major tributary of the Snake River.
Bitterroot National Forest comprises 1.587 million acres (6,423 km2) in west-central Montana and eastern Idaho of the United States. It is located primarily in Ravalli County, Montana, but also has acreage in Idaho County, Idaho (29.24%), and Missoula County, Montana (0.49%).
The Sawtooth Wilderness is a federally-protected wilderness area that covers 217,088 acres (87,852 ha) of the state of Idaho. Managed by the U.S. Forest Service in the U.S. Department of Agriculture, it was designated the Sawtooth Primitive Area in 1937 to preserve the scenic beauty of the Sawtooth Mountains. On August 22, 1972 Public Law 92-400 designated the Primitive Area as the Sawtooth Wilderness and part of the newly created Sawtooth National Recreation Area. As part of the National Wilderness Preservation System, the Sawtooth Wilderness is an area where human development and use are restricted and people are to remain only visitors. According to the United States Environmental Protection Agency, the Sawtooth Wilderness has some of the clearest air in the lower 48 states.
The Payette National Forest is a U.S. National Forest located in central western Idaho, in parts of Valley, Idaho, Adams, and Washington counties. The land area consists of approximately 2.3 million acres (9,300 km2) of federally managed lands. It is bordered by Hells Canyon National Recreation Area and the Hells Canyon to the west, Salmon-Challis National Forest to the east, Boise National Forest to the south, and the Nez Perce National Forest to the north. The Payette National Forest is a part of the Intermountain Region. It is under the jurisdiction of a forest supervisor in McCall and is divided into five ranger districts: McCall, Krassel, New Meadows, Council, and Weiser.
Sawtooth National Forest is a National Forest that covers 2,110,408 acres in the U.S. states of Idaho and Utah. Managed by the U.S. Forest Service in the U.S. Department of Agriculture, it was originally named the Sawtooth Forest Reserve in a proclamation issued by President Theodore Roosevelt on May 29, 1905. On August 22, 1972, a portion of the forest was designated as the Sawtooth National Recreation Area (SNRA), which includes the Sawtooth, Cecil D. Andrus–White Clouds, and Hemingway–Boulders wilderness areas. The forest is managed as four units: the SNRA and the Fairfield, Ketchum, and Minidoka Ranger Districts.
The Sawtooth Range is a mountain range of the Rocky Mountains in central Idaho, United States, reaching a maximum elevation of 10,751 feet (3,277 m) at the summit of Thompson Peak. It encompasses an area of 678 square miles (1,756 km2) spanning parts of Custer, Boise, Blaine, and Elmore counties, and is bordered to the east by the Sawtooth Valley. Much of the mountain range is within the Sawtooth Wilderness, part of the Sawtooth National Recreation Area and Sawtooth National Forest.
Deadwood Reservoir is a reservoir in the western United States, in Valley County, Idaho. Located in the mountains of the Boise National Forest about 25 miles (40 km) southeast of Cascade, the 3,000-acre (12 km2) body on the Deadwood River is created by Deadwood Dam. The river flows south from the dam and is a tributary of the South Fork of the Payette River. The reservoir and vicinity is commonly used for camping, water skiing, fishing, canoeing, and other outdoor recreation. The full pool surface elevation is just above a mile-high at 5,334 ft (1,626 m) above sea level.
The U.S. state of Idaho borders six other U.S. states and one Canadian province. The states of Washington and Oregon are to the west, Nevada and Utah are to the south, and Montana and Wyoming are to the east. Idaho also shares a short border with the Canadian province of British Columbia to the north.
Banner Creek Summit is a mountain pass in the western United States in central Idaho, at an elevation of 7,037 feet (2,145 m) above sea level. Traversed by State Highway 21, the Ponderosa Pine Scenic Byway, it is located on the border of Custer County and Boise County, also the border of the Challis and Boise National Forests, immediately northwest of the Sawtooth Range.
State Highway 21 (SH-21), also known as the Ponderosa Pine Scenic Byway, is a state highway in Idaho. It runs from Boise to Stanley, primarily as a two-lane road. With two-thirds of its length in Boise County, it passes by historic Idaho City and the village of Lowman to the western edge of the Sawtooth Mountains, then along their northern boundary to Stanley.
The Little Salmon River is a tributary of the Salmon River in Idaho in the western United States. The river is approximately 51 miles (82 km) in length and drains 576 square miles (1,490 km2) of land.
The North Fork Payette River is a river in the western United States in western Idaho. It flows about 113 miles (182 km) southwards from the Salmon River Mountains to near Banks, where it empties into the Payette River, a tributary of the Snake River. It drains a watershed of 912 square miles (2,360 km2), consisting of mountains and forests, and valleys filled with large lakes and wetlands.
The South Fork Salmon River is an 86-mile (138 km) tributary of the Salmon River in Idaho and Valley Counties in central Idaho. The river drains a rugged, lightly populated wilderness watershed in the Salmon River Mountains. It is the second-largest tributary of the Salmon River, after the Middle Fork.
The West Mountains are a mountain range in the U.S. state of Idaho, spanning part of Boise and Payette national forests. The highest point in the range is Snowbank Mountain at an elevation of 8,320 feet (2,540 m) above sea level. The range is bordered to the east by the Payette River and the North Fork Payette River, which separate the range from the Boise Mountains.
Snowbank Mountain is the highest point in the West Mountains, in Boise National Forest, Idaho with a summit elevation of 8,320 feet (2,540 m) above sea level. It is located 21.92 miles (35.28 km) from Nick Peak, its line parent, giving it a prominence of 3,080 feet (940 m). The east side of Snowbank Mountain is drained by the North Fork Payette River, while the west side is drained by Squaw Creek, which is also a tributary of the Payette River.
The Deadwood River is a 43.5-mile (70.0 km) tributary of the South Fork Payette River, flowing through Boise National Forest in Valley and Boise counties, Idaho in the United States. It joins the South Fork Payette River about 3 miles (4.8 km) west of Lowman. The source of the Deadwood River is below the Deadwood summit on forest road 579 in the Salmon River Mountains. The Deadwood Dam was completed in 1931 and impounded the river to form Deadwood Reservoir.
↑ "Steel Mountain". Geographic Names Information System. U.S. Geological Survey. Archived from the original on June 30, 2020. Retrieved August 11, 2014.
↑ "Two Point Mountain". Geographic Names Information System. U.S. Geological Survey. Retrieved August 11, 2014.
1 2 3 4 5 U.S. Forest Service (2012). Boise National Forest (Map). 1:126,720. U.S. Forest Service.
↑ "Trinity Mountains". Geographic Names Information System. U.S. Geological Survey. Retrieved December 26, 2014.
↑ "West Mountains". Geographic Names Information System. U.S. Geological Survey. Retrieved August 11, 2014.
↑ Doerner, James P.; Carrara, Paul E. (1999). "Deglaciation and postglacial vegetation history of the West Mountains, West-central Idaho, U.S.A.". Arctic, Antarctic, and Alpine Research. 131 (3): 303–311. doi:10.2307/1552261. JSTOR1552261.
↑ Eldridge, George Homans (1895). A Geological Reconnaissance Across Idaho. U.S. Geological Survey. p.223.
↑ 2010 Boise National Forest Amended Forest Plan p. A-21
↑ 2010 Boise National Forest Amended Forest Plan p. A-22
↑ 2010 Boise National Forest Amended Forest Plan p. A-23
1 2 3 2010 Boise National Forest Amended Forest Plan p. A-24
↑ 2010 Boise National Forest Amended Forest Plan p. A-26
↑ 2010 Boise National Forest Amended Forest Plan p. A-28
↑ 2010 Boise National Forest Amended Forest Plan p. II-24
1 2 3 Alden, Peter; Grassy, John; Cassie, Brian; Kahl, Jonathan D. W.; Leventer, Amy; Mathews, Daniel; Zomlefer, Wendy B. (1998). National Audubon Society Field Guide to the Rocky Mountain States (1sted.). New York: Alfred A. Knopf. ISBN0-679-44681-8.
↑ Ring, Ray (May 27, 2002). "Wolf at the Door". High Country News. Archived from the original on November 20, 2012. Retrieved July 15, 2013.
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