Shoshone National Forest: Difference between revisions
→Human history: adjust |
→Geography and geology: rm duplicate links |
||
(239 intermediate revisions by 16 users not shown) | |||
Line 1: | Line 1: | ||
{{Use mdy dates|date=November 2013}} |
|||
{{featured article}} |
{{featured article}} |
||
{{Infobox protected area |
{{Infobox protected area |
||
| name = Shoshone National Forest |
| name = Shoshone National Forest |
||
| iucn_category = VI |
| iucn_category = VI |
||
| photo = |
| photo = Francs Peak.jpg |
||
| photo_caption = [[ |
| photo_caption = [[Francs Peak]] is the tallest peak in the Absaroka Range |
||
| map = USA relief |
| map = USA relief |
||
| map_caption = |
| map_caption = |
||
Line 12: | Line 13: | ||
| long_d = 109 | long_m = 36 | long_s = 49 | long_EW = W |
| long_d = 109 | long_m = 36 | long_s = 49 | long_EW = W |
||
| region = US |
| region = US |
||
| coords_ref = <ref name=gnis>{{cite gnis|id=1603974|name=Wapiti Ranger Station|accessdate= |
| coords_ref = <ref name=gnis>{{cite gnis|id=1603974|name=Wapiti Ranger Station|accessdate=August 31, 2013}}</ref> |
||
| area = {{convert| |
| area = {{convert|2466909|acre|ha}}<ref name=acreage>{{cite web|title=Land Areas of the National Forest System|url=http://www.fs.fed.us/land/staff/lar/LAR2011/LAR2011_Book_A5.pdf|publisher=U.S. Department of Agriculture|accessdate=August 31, 2013|format=pdf|date=September 30, 2011}}</ref> |
||
| established = March 3, 1891 |
| established = March 3, 1891 |
||
| visitation_num = 646,000<ref>{{cite web|title=National Visitor Use Monitoring|url=http://apps.fs.usda.gov/nrm/nvum/results/A02014.aspx/Round2|publisher=U.S. |
| visitation_num = 646,000<ref name=visits>{{cite web|title=National Visitor Use Monitoring|url=http://apps.fs.usda.gov/nrm/nvum/results/A02014.aspx/Round2|publisher=U.S. Department of Agriculture|accessdate=August 31, 2013}}</ref> |
||
| visitation_year = 2009 |
| visitation_year = 2009 |
||
| governing_body = [[United States Forest Service|U.S. Forest Service]] |
| governing_body = [[United States Forest Service|U.S. Forest Service]] |
||
| url = http://www.fs.usda.gov/shoshone/ |
| url = http://www.fs.usda.gov/shoshone/ |
||
}} |
}} |
||
'''Shoshone National Forest''' ({{IPAc-en |
'''Shoshone National Forest''' ({{IPAc-en|ʃ|oʊ|ˈ|ʃ|oʊ|n|iː}} {{Respell|shoh|SHOH|nee}})<ref>{{cite web|title=Shoshone|url=http://www.answers.com/topic/shoshone|publisher=Answers|accessdate=March 23, 2013}}</ref> is the first [[Federal government of the United States|federally]] protected [[United States National Forest|National Forest]] in the United States and covers nearly {{convert|2500000|acre}} in the [[U.S. state|state]] of [[Wyoming]].<ref name=shoshone>{{cite web|title=Welcome to Shoshone National Forest|url=http://www.fs.usda.gov/shoshone|publisher=U.S. Department of Agriculture|accessdate=August 31, 2013}}</ref> Originally a part of the [[Yellowstone Timberland Reserve]], the forest is managed by the [[United States Forest Service]] and was created by an act of [[United States Congress|Congress]] and signed into law by [[President of the United States|U.S. President]] [[Benjamin Harrison]] in 1891. Shoshone National Forest is one of the first nationally protected land areas anywhere. [[Native Americans in the United States|Native American]]s have lived in the region for at least 10,000 years, and when the region was first explored by white adventurers, forestlands were occupied by several different tribes. Never heavily settled or exploited, the forest has retained most of its wildness. Shoshone National Forest is a part of the [[Greater Yellowstone Ecosystem]], a nearly unbroken expanse of federally protected lands encompassing an estimated {{convert|20000000|acre}}. |
||
The [[Absaroka Mountains|Absaroka]] and [[Beartooth Mountains]] are partly in the northern section of the forest. The [[Wind River Range]] is in the southern portion and contains [[Gannett Peak]], the tallest mountain in Wyoming.<ref name=shoshone/> [[Yellowstone National Park]] forms part of the boundary to the west; south of Yellowstone, the [[Continental Divide of the Americas|Continental Divide]] separates the forest from its neighbor [[Bridger-Teton National Forest]] to the west. The eastern boundary includes privately owned property, lands managed by the U.S. [[Bureau of Land Management]] and the [[Wind River Indian Reservation]], which belongs to the [[Shoshone]] and [[Arapahoe]] Indians. [[Custer National Forest]] along the [[Montana]] border is on the northern frontier. The [[Oregon Trail]], the 19th century [[covered wagon]] route, passes just south of the forest, where broad and gentle [[South Pass (Wyoming)|South Pass]] allowed the migrants to bypass the rugged mountains to the north. |
|||
[[File:Shoshone wy map.jpg|thumb|400px|Shoshone National Forest, locator map]] |
|||
Shoshone National Forest has virtually all the original animal and plant species that were there when white explorers such as [[John Colter]] and [[Jim Bridger]] first visited the region. The forest is home to the [[Grizzly bear]], [[cougar]], [[moose]], tens of thousands of [[elk]] as well as the largest herd of [[bighorn sheep]] in the U.S. The streams in the forest are considered to have some of the best game species fishing opportunities in the U.S. and one of the few places where one can catch [[Yellowstone cutthroat trout]]. More than 1,300 miles of hiking trails, 32 campgrounds and adjacent forests and parklands provide numerous recreational opportunities. There are four [[wilderness]] areas within the forest, protecting more than half of the [[land management|managed land]] area from development. From [[sagebrush]] plains through dense [[spruce]] and [[fir]] forest to craggy mountain peaks, Shoshone National Forest has a rich [[biodiversity]] rarely matched in any protected area. |
|||
== Human history == |
== Human history == |
||
[[File:Shoshoni tipis.jpg|thumb| |
[[File:Shoshoni tipis.jpg|thumb|Shoshone encampment in the Wind River Mountains of Wyoming, photographed by W. H. Jackson, 1870]] |
||
Shoshone National Forest is named after the [[Shoshone|Shoshone Indians]], who, along with other [[Native Americans in the United States|Native American]] groups such as the [[Lakota people|Lakota]], [[Crow Tribe|Crow]] and [[Northern Cheyenne]], were the major tribes encountered by the first |
Shoshone National Forest is named after the [[Shoshone|Shoshone Indians]], who, along with other [[Native Americans in the United States|Native American]] groups such as the [[Lakota people|Lakota]], [[Crow Tribe|Crow]] and [[Northern Cheyenne]], were the major tribes encountered by the first white explorers into the region. [[Archaeology|Archeological]] evidence suggests that the presence of Indian tribes in the area extends back at least 10,000 years.<ref name=history>{{cite web|title=History and Culture|url=http://www.fs.usda.gov/main/shoshone/learning/history-culture|publisher=U.S. Forest Service|accessdate=August 31, 2013}}</ref> The forest provided an abundance of game meat, wood products, and shelter during the winter months from the more exposed [[Great Plains|high plains]] to the east. Portions of the more mountainous regions were frequented by the Shoshone and Sioux for spiritual healing and [[vision quest]]s. By early 1840s, [[Washakie]] had become the leader of the easternmost branch of the Shoshone Indians.<ref name=hebard>{{cite book|last=Hebard|first=Grace R.|title=Washakie, Chief of the Shoshones|year=1995|publisher=Bison Books|isbn=978-0803272781|page=56|url=http://books.google.com/?id=H72qQ3R5mq0C&printsec=frontcover&dq=Washakie,+Chief+of+the+Shoshones#v=onepage&q=chieftainship&f=false|accessdate=August 31, 2013}}</ref> At the [[Fort Bridger Treaty Council of 1868]] Washakie negotiated with the U.S. Government for {{convert|44000000|acre}}) to be preserved as tribal lands. Subsequent amendments to the treaty reduced the actual acreage to approximately {{convert|2000000|acre}} and is known today as the [[Wind River Indian Reservation]].<ref name=capace>{{cite book|last=Capace|first=Nancy|title=Encyclopedia of Wyoming|year=2007|publisher=Somerset Publishers, Inc|isbn=978-0403096138|page=88|url=http://books.google.com/?id=PRsh2LRuoQMC&printsec=frontcover&dq=Encyclopedia+of+Wyoming#v=onepage&q=treaty%20of%20fort%20bridger&f=false|accessdate=August 31, 2013}}</ref><ref name=johansen>{{cite book|last=Johansen|first=Bruce E.|title=Encyclopedia of American Indian History|publisher=ABC-CLIO|isbn=978-1851098187|page=1127|coauthors=Barry M. Pritzker|url=http://books.google.com/?id=sGKL6E9_J6IC&printsec=frontcover&dq=Encyclopedia+of+American+Indian+History#v=snippet&q=fort%20bridger%20treaty&f=false|accessdate=August 31, 2013|date=July 23, 2007}}</ref> |
||
In 1957, [[Mummy Cave]] was rediscovered by a local resident on the north side of the North Fork Shoshone River, adjacent to U.S. Routes [[U.S. Route 14|14]]/[[U.S. Route 16|16]]/[[U.S. Route 20|20]], {{convert|15|mi|abbr=on}} east of Yellowstone National Park.<ref name=mummy>{{cite web|title=Mummy Cave|url=http://wyoshpo.state.wy.us/NationalRegister/Site.aspx?ID=324|publisher=Wyoming State Historic Preservation Office|accessdate=September 29, 2013}}</ref> Subsequent archeological excavations in the 1960s produced evidence that the cave had been occupied for over 9,000 years.<ref name=husted>{{cite web|last=Husted|first=Wilfred M.|coauthors=Robert Edgar|title=The Archeology of Mummy Cave, Wyoming: An Introduction to Shoshonean Prehistory|url=http://www.nps.gov/history/mwac/publications/pdf/spec4.pdf|publisher=National Park Service|format=pdf|year=2002|accessdate=September 29, 2013}}</ref> The oldest deposits in the cave yielded [[prismatic blade|prismatic stone blades]] and other artifacts created by paleoindians and the surrounding soils were [[Radiocarbon dating|radiocarbon dated]] to 7,300 BC. The evidence indicates the cave was occupied from at least 7280 BC to 1580 AD.<ref name=mummy/> Besides projectile points, the cave also produced well preserved feathers, animal hides and other usually perishable materials. Additionally, the mummified remains of an individual buried inside a rock [[cairn]] were unearthed, which were dated to 800 AD.<ref name=husted/> Considered one of the finest paleoindian archeological assemblages in the Rocky Mountain region, the site was placed on the [[National Register of Historic Places]] list in 1981.<ref name=nris>{{NRISref|version=2010a}}</ref> |
|||
[[File:Wolf Mine Shaft.jpg|left|thumb|Wolf [[shaft mining|Mine shaft]] at abandoned [[gold mine]]]] |
|||
[[File:Wapiti Ranger Station.jpg|thumb|left|Wapiti Ranger Station]] |
|||
In the early 19th century, the forest was visited by [[mountain man|mountain men]] and explorers such as [[John Colter]] and [[Jim Bridger]]. Colter is the first white man known to have visited both the Yellowstone region and the forest, which he did between 1807 and 1808.<ref name=utley>{{cite book|last=Utley|first=Robert M.|title=After Lewis and Clark: Mountain Men and the Paths to the Pacific|year=2004|publisher=Bison Books|isbn=978-0803295643|pages=15–16|url=http://books.google.com/?id=2lCSVm2rP-IC&printsec=frontcover&dq=After+Lewis+and+Clark:+Mountain+Men+and+the+Paths+to+the+Pacific#v=onepage&q=John%20Colter&f=false|accessdate=August 31, 2013}}</ref> Having been an original member of the [[Lewis and Clark Expedition]], Colter requested permission from Meriwether Lewis to leave the expedition after it had finished crossing the [[Rocky Mountains]] during their return journey from the Pacific Ocean. Colter teamed up with two unaffiliated explorers the expedition had encountered, but soon thereafter decided to explore regions south of where his new partners wished to venture.<ref name=utley/> Traveling first into the northeastern region of what is today Yellowstone National Park, Colter then explored the [[Absaroka Mountains]], crossing over [[Togwotee Pass]] and entering the valley known today as [[Jackson Hole]].<ref name=daugherty1>{{cite web|last=Daugherty|first=John|title=The Fur Trappers|url=http://www.nps.gov/history/history/online_books/grte2/hrs3.htm|work=A Place Called Jackson Hole|publisher=Grand Teton Natural History Association|accessdate=August 31, 2013}}</ref> Colter survived a [[grizzly bear]] attack and a pursuit by a band of [[Blackfeet]] Indians who had taken his horse.<ref name=utley/> The explorer later provided William Clark, who had been his commander on the Lewis and Clark Expedition, with previously unknown information on the regions he had explored, which Clark published in 1814.<ref name=burns>{{cite web|last=Burns|first=Ken|title=Private John Colter|url=http://www.pbs.org/lewisandclark/inside/jcolt.html|work=Lewis and Clark: The Journey of the Corps of Discovery|publisher=PBS|accessdate=August 31, 2013}}</ref> |
|||
Travels by [[fur trade|fur trappers]] and adventurers, such as [[Manuel Lisa]] and Jim Bridger from 1807 to 1840, completed the exploration of the region. With the decline of the fur trade in the late 1840s and much of the prized [[beaver]] long since made scarce by over-trapping, few white explorers entered the forest over the next few decades.<ref name=daugherty1/> The first federally financed expedition which passed through portions of Shoshone National Forest was the [[Raynolds Expedition]] of 1860, led by [[United States Army Corps of Engineers#Corps of Topographical Engineers|topographical engineer]] Captain [[William F. Raynolds]].<ref name=baldwin>{{cite web|last=Baldwin|first=Kenneth H.|title=Terra Incognita: The Raynolds Expedition of 1860|work=Enchanted Enclosure|publisher=U.S. Army|date=November 15, 2004|url=http://www.cr.nps.gov/history/online_books/baldwin/chap2.htm|accessdate=August 31, 2013}}</ref> The expedition included geologist and naturalist [[Ferdinand Vandeveer Hayden]] and was guided by mountain man Jim Bridger. Though the Raynolds Expedition was focused on exploration of the Yellowstone region, several efforts to enter what later became Yellowstone National Park were impeded by heavy snows across the mountain passes such as [[Two Ocean Pass]]. The expedition finally crossed the northern Wind River Range at a pass they named [[Union Pass]] and entered Jackson Hole valley to the south of Yellowstone.<ref name=baldwin/> Hayden led another expedition through the region in 1871. Hayden was primarily interested in documenting the Yellowstone country west of the forest, but his expedition also established that the forest was a prime resource that merited protection. Travels in the forest in the 1880s by later U.S. President [[Theodore Roosevelt]], who was also a strong advocate of land [[conservation movement|conservation]], as well as by General [[Philip Sheridan]], provided the impetus that subsequently established the Yellowstone Timberland Reserve in 1891, creating the first national forest in the U.S.<ref name=shoshone/><ref>{{cite book|last=Steen|first=Harold K.|title=The beginning of the National Forest System|publisher=U.S. Forest Service|year=1991|url=http://books.google.com/?id=lw5hof80GXwC&pg=PA24&dq=yellowstone+timberland+reserve#v=onepage&q=yellowstone%20timberland%20reserve&f=false|accessdate=August 31, 2013}}</ref> |
|||
In the early 19th century, the forest was visited by [[mountain man|mountain men]] and explorers such as [[John Colter]] and [[Jim Bridger]]. Colter is the first white man known to have visited both the Yellowstone region and the forest, which he did between 1806 and 1808.<ref name="colter">{{cite book |author=Robert Marshall M. Utley |year=2004 |title=After Lewis and Clark: Mountain Men and the Paths to the Pacific |editor=|publisher=Bison Books, [[University of Nebraska Press]] |location=Lincoln, NE 2004 ISBN 0-8032-9564-2}}</ref> Having been an original member of the Lewis and Clark Expedition, Colter requested permission from Meriwether Lewis to leave the expedition after it had finished crossing the [[Rocky Mountains]] during their return journey from the [[Pacific Ocean]]. Colter teamed up with two unaffiliated explorers the expedition had encountered, but soon thereafter decided to explore regions south of where his new partners wished to venture. Traveling first into the northeastern region of what is today Yellowstone National Park, Colter then explored the [[Absaroka Mountains]], crossing over [[Togwotee Pass]] and entering the valley known today as [[Jackson Hole]]. Colter survived a [[grizzly bear]] attack and a pursuit by a band of [[Blackfeet]] Indians who had taken his horse. The explorer later provided William Clark, who had been his commander on the Lewis and Clark Expedition, with previously unknown information on the regions he had explored, which Clark published in 1814.<ref name="clark">{{cite web |publisher=PBS |author=Ken Burns |title=Private John Colter |work=Lewis and Clark, The Journey of the Corps of Discovery |url=http://www.pbs.org/lewisandclark/inside/jcolt.html |accessdate=2006-10-15}}</ref> |
|||
[[File:Wolf Mine Shaft.jpg|right|thumb|Wolf mine shaft at abandoned gold mine]] |
|||
In 1902, President Roosevelt first greatly expanded the reserve and then divided the reserve into four separate units, with Shoshone being the largest. Upon the creation of the [[United States Forest Service|U.S. Forest Service]] in 1905, the reserve was designated a [[United States National Forest|National Forest]], but the current wording and title were formulated forty years later in 1945. A remnant of the earliest years of the forest management is the [[Wapiti Ranger Station]] which is located west of [[Cody, Wyoming]]. The station was built in 1903 and is the oldest surviving ranger station in any national forest, and is now designated a [[National Historic Landmark]].<ref>{{cite web|title=Wapiti Ranger Station|work=National Historic Landmarks Program|publisher=National Park Service|url=http://tps.cr.nps.gov/nhl/detail.cfm?ResourceID=568&resourceType=Building|accessdate=August 31, 2013}}</ref> |
|||
Prior to the establishment of the Wind River Indian Reservation, the [[United States Cavalry|U.S. Cavalry]] constructed Fort Brown on the reservation lands, which was subsequently renamed [[Fort Washakie]].<ref name=mccoy>{{cite book|last=McCoy|first=Michael|title=Off the Beaten Path Wyoming: A Guide to Unique Places|year=2007|publisher=GPP Travel|isbn=978-0762744312|pages=152–153|url=http://books.google.com/?id=X60kQYBZEwgC&printsec=frontcover&dq=Off+the+Beaten+Path+Wyoming:+A+Guide+to+Unique+Places.#v=onepage&q=fort%20washakie&f=false|accessdate=August 31, 2013}}</ref> During the late 19th century, the fort was staffed by [[African American|African-American]] members of the U.S. Cavalry, better known as the [[Buffalo Soldiers]], including the second African-American graduated from the [[United States Military Academy]], [[John Hanks Alexander]].<ref>{{cite book|last=Reef|first=Catherine|title=African Americans in the Military|year=2010|publisher=Facts on File, Incorporated|isbn=9780816078394|page=6|url=http://books.google.com/?id=bq8dVn_W2XQC&pg=PT26&dq=john+hanks+alexander+fort+washakie#v=onepage&q=john%20hanks%20alexander%20fort%20washakie&f=false|accessdate=August 31, 2013}}</ref> Chief Washakie is buried at the fort, which is located immediately east of the forest boundary.<ref name=mccoy/> Rumor has it that [[Sacajawea]], the Shoshone Indian who provided invaluable assistance to [[Meriwether Lewis]] and [[William Clark (explorer)|William Clark]] during the Lewis and Clark Expedition, is also buried here, but it is now considered that this is unlikely and that her actual burial place was [[Fort Lisa (North Dakota)|Fort Lisa]] in North Dakota.<ref>{{cite web|title=Burial Sites|url=http://www.nps.gov/jeff/historyculture/burial-sites.htm|work=The Lewis and Clark Journey of Discovery|publisher=National Park Service|accessdate=August 31, 2013}}</ref> |
|||
Travels by [[fur trade|fur trappers]] and adventurers, such as [[Manuel Lisa]] and Jim Bridger from 1807 to 1840, completed the exploration of the region. With the decline of the fur trade in the late 1840s and much of the prized [[beaver]] long since made scarce by over-trapping, few white explorers entered the forest over the next few decades. Explorations under direction of [[Ferdinand Vandeveer Hayden|F.V. Hayden]] in 1871 were the first federally financed and supported. Hayden was primarily interested in documenting the Yellowstone country west of the forest, but his expedition also established that the forest was a prime resource that merited protection. Travels in the forest in the 1880s by later U.S. President [[Theodore Roosevelt]], who was also a strong advocate of land [[conservation movement|conservation]], as well as by General [[Philip Sheridan]], provided the impetus that subsequently established the Yellowstone Timberland Reserve in 1891, creating the first national forest in the U.S.<ref name="yellsto">{{cite book |last=Haines |first=Aubrey L. |title=The Yellowstone Story |publisher=University Press of Colorado |year=1977 |edition=Revised |volume=2 |page=94 |chapter=14 |isbn=0-87081-391-9}}</ref> |
|||
[[File:Wapiti Ranger Station.jpg|thumb|[[Wapiti Ranger Station]]]] |
|||
In 1902 President Roosevelt first greatly expanded the reserve and then divided the reserve into four separate units, with Shoshone being the largest. Upon the creation of the [[United States Forest Service|U.S. Forest Service]] in 1905, the reserve was designated a [[United States National Forest|National Forest]], but the current wording and title were formulated forty years later in 1945. A remnant of the earliest years of the forest management is the [[Wapiti Ranger Station]] which is located west of [[Cody, Wyoming]]. The station was built in 1903 and is the oldest surviving ranger station in any national forest, and is now designated a [[National Historic Landmark]].<ref>{{cite web |title=Wapiti Ranger Station |work=National Historic Landmarks Program |publisher=National Park Service |date=|url=http://tps.cr.nps.gov/nhl/detail.cfm?ResourceID=568&resourceType=Building |accessdate=2007-01-12}}</ref> |
|||
During the last decade of the 19th century, minerals such as |
During the last decade of the 19th century, minerals such as gold were mined with limited success. The last mine was abandoned in 1907, but [[placer mining|panning]] for gold is still allowed in many areas of the forest, and in most circumstances no permit is required.<ref name=kirwin>{{cite web|title=The History of Kirwin|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/learning/kids/?cid=stelprdb5182989|accessdate=August 31, 2013}}</ref><ref>{{cite web|title=Shoshone National Forest - FAQs|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/home/?cid=stelprdb5176591|accessdate=August 31, 2013}}</ref> After the end of the mining era, numerous camps were established by the [[Civilian Conservation Corps]] to help combat unemployment during the [[Great Depression]] of the 1930s. The camps housed groups of unemployed men who were paid by the federal government to build roads, hiking trails, and campgrounds for future travelers to the Yellowstone region.<ref name=otis>{{cite book|last=Otis|first=Alison T.|title=The Forest Service and the Civilian Conservation Corps, 1933-42|year=1986|publisher=U.S. Forest Service|isbn=9781236205001|pages=24–26|url=http://books.google.com/?id=f0qHwwF4V5wC&pg=PA23&dq=civilian+conservation+corps+construction+projects+in+wyoming#v=onepage&q=civilian%20conservation%20corps%20construction%20projects%20in%20wyoming&f=false|accessdate=August 31, 2013}}</ref> Visitation to national forests like Shoshone increased dramatically after [[World War II]] with the advent of better roads and accessibility to the region.<ref name=miller>{{cite book|last=Miller|first=Char|title=Atlas of US and Canadian Environmental History|year=2013|publisher=Routledge|isbn=9781136755248|page=138|url=http://books.google.com/?id=QD0LTYaBjKEC&pg=PA138&dq=road+improvements+after+WW+2+lead+to+more+vistors+to+national+forests#v=onepage&q=road%20improvements%20after%20WW%202%20lead%20to%20more%20vistors%20to%20national%20forests&f=false|accessdate=August 31, 2013}}</ref> |
||
== Forest management == |
== Forest management == |
||
[[File:Shoshone wy map.jpg|thumb|300px|Shoshone National Forest highlighted in light green]] |
|||
Shoshone National Forest is managed by the [[United States Forest Service|U.S. Forest Service]], an agency within the [[United States Department of Agriculture|U.S. Department of Agriculture]]. The forest is separated into five districts and has a staff of 145 employees. The annual operating budget is [[United States dollar|$]]15,000,000, with much of it from [[federal grant|grants]]. The headquarters and a visitor center are in [[Cody, Wyoming]] and a smaller information center is in [[Lander, Wyoming]]. There are local [[National Park Ranger|ranger]] district offices in [[Cody, Wyoming|Cody]], [[Dubois, Wyoming|Dubois]], and [[Lander, Wyoming|Lander]].<ref>[http://www.ufwda.org/pdfs/USDAForestServiceRangerDistricts.pdf USFS Ranger Districts by State]</ref> |
|||
Shoshone National Forest is managed by the U.S. Forest Service, an agency within the [[United States Department of Agriculture|U.S. Department of Agriculture]]. The forest is separated into five districts and from 2008 and 2012 had an average staff of 165 employees and an annual operating budget of [[United States dollar|$]]17,500,000.<ref name=taylor>{{cite web|last=Taylor|first=David T.|coauthors=Thomas Foulke and Roger H. Coupal|title=Shoshone National Forest Economic Profile|publisher=University of Wyoming Department of Agricultural & Applied Economics and the U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5379182.pdf|date=March 21, 2012|page=87|format=pdf|accessdate=September 2, 2013}}</ref> The headquarters and a visitor center are in Cody, Wyoming and a smaller information center is in [[Lander, Wyoming]]. There are local ranger district offices in Cody, [[Dubois, Wyoming|Dubois]] and Lander.<ref>{{cite web|title=USFS Ranger Districts by State|publisher=U.S. Forest Service|url=http://www.ufwda.org/pdfs/USDAForestServiceRangerDistricts.pdf|format=pdf|accessdate=August 31, 2013}}</ref> |
|||
Shoshone National Forest practices [[conservation biology|conservation]] of resources, which ensures a sustainable flow of some raw materials from the forest, such as lumber for construction purposes and [[wood pulp]] for paper products.<ref name=mission>{{cite web|title=Sustainable Operations|publisher=U.S. Forest Service|url=http://www.fs.fed.us/sustainableoperations/|accessdate=September 2, 2013}}</ref> The forest averages an annual harvest of 4.5 million board-feet of timber for the purposes of commercial log home construction and another 2.5 million board-feet of wood collection from dead and down trees that are used for firewood and poles.<ref name=taylor2>{{cite web|last=Taylor|first=David T.|coauthors=Thomas Foulke and Roger H. Coupal|title=Shoshone National Forest Economic Profile|publisher=University of Wyoming Department of Agricultural & Applied Economics and the U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5379182.pdf|date=March 21, 2012|page=73|format=pdf|accessdate=September 15, 2013}}</ref> Additionally, low-scale mineral extraction and [[oil exploration|oil]] and [[natural gas|gas]] exploration and recovery are also conducted, though in Shoshone National Forest this has become less common due to a consensus to protect the natural surroundings. Only {{convert|8570|acre|abbr=on}} of oil and gas leases were filed as of 2013.<ref>{{cite web|last=Bleizeffer|first=Dustin|title=Don’t count on a rush of drilling rigs in the Shoshone National Forest|publisher=WyoFile|url=http://wyofile.com/dustin/comments-suggest-wyoming-residents-support-conservation-on-shoshone-national-forest/|date=August 23, 2013|accessdate=September 2, 2013}}</ref> More common than logging and mining are the lease options that are offered to ranchers to allow them to graze cattle and sheep.<ref name=taylor3>{{cite web|last=Taylor|first=David T.|coauthors=Thomas Foulke and Roger H. Coupal|title=Shoshone National Forest Economic Profile|publisher=University of Wyoming Department of Agricultural & Applied Economics and the U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5379182.pdf|date=March 21, 2012|page=53|format=pdf|accessdate=September 15, 2013}}</ref> The U.S. Forest Service provides guidelines and enforces environmental regulations to ensure that resources are not [[overexploited]] and that necessary commodities are available for future generations, though conservation groups have voiced concerns over the management practices of the leasing program and especially cattle overgrazing problems.<ref name=ws>{{cite web|title=Beartooth Front, Wyoming|work=Too Wild to Drill|publisher=Wilderness Society|url=http://wilderness.org/sites/default/files/legacy/TWTD-WY-Beartooth.pdf|format=pdf| |
|||
accessdate=September 2, 2013}}</ref> Leases for sheep grazing have declined considerably since the 1940s while cattle grazing has remained relatively constant.<ref>{{cite web|title=Analysis of the Management Situation|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5356003.pdf|date=February 2012|pages=79–81|format=pdf|accessdate=September 15, 2013}}</ref> |
|||
accessdate=2007-01-12| archiveurl = http://web.archive.org/web/20070715111856/http://www.wilderness.org/WhereWeWork/Wyoming/TWTD-Beartooth.cfm| archivedate = July 15, 2007}}</ref> |
|||
The efforts of [[environmentalism|environmentalists]] combined with public demand led to the creation of [[wilderness]] designated zones beginning in 1964 within most U.S. Government land areas that fit the criteria of wilderness. The wilderness designation provides a much higher level of land protection and prohibits any alterations by man to the resource. In Shoshone National Forest, less than ten percent of the total area is utilized for land lease, [[forestry|logging]] or mineral extraction. The rest of the forest is either designated wilderness, reserved for habitat protection for plants and animals, or set aside for visitor recreation. However, the overgrazing of cattle in [[riparian]] areas and into zones not within lease agreements are continuous points of argument. Oil and gas exploration interest groups also lobby to explore regions that may adversely impact wildlife habitat.<ref name="oil">{{cite web |author=[[Wyoming Outdoor Council]] |title=Setbacks on the Shoshone National Forest |url=http://www.wyomingoutdoorcouncil.org/news/newsletter/docs/1999b/shoshone.php |accessdate=2006-10-15|archiveurl=http://web.archive.org/web/20061002230223/http://www.wyomingoutdoorcouncil.org/news/newsletter/docs/1999b/shoshone.php |archivedate=October 2, 2006 |deadurl=yes}}</ref> Plans to build roads into nonwilderness areas for easier extraction of timber have come under fire and are not in compliance with recent legislation that prohibits such construction.<ref name="timber">{{cite web |author=[[Wyoming Outdoor Council]] |title=Shoshone National Forest Pulls Timber Sale |url=http://www.wyomingoutdoorcouncil.org/news/newsletter/docs/2002c/dickcreek.php |accessdate=2006-10-15|archiveurl=http://web.archive.org/web/20061002232902/http://www.wyomingoutdoorcouncil.org/news/newsletter/docs/2002c/dickcreek.php |archivedate=October 2, 2006 |deadurl=yes}}</ref> Illegal [[off-roading|off-road]] motorized transport by [[all-terrain vehicle]]s and [[snowmobile]]s continues to be a problem, especially in wilderness areas. Lastly, protection of [[threatened species|threatened]] and [[endangered species]] such as the [[grizzly bear|grizzly]] and [[wolf]] is sometimes met with opposition from local ranching interests.<ref name="ens">{{cite web |author=|title=Bears Outlawed in Wyoming Counties Over Food Fight |publisher=Environmental News Service |url=http://www.ens-newswire.com/ens/apr2002/2002-04-03-02.asp |accessdate=2007-01-12}}</ref> |
|||
== Natural resources == |
== Natural resources == |
||
{{See also|Ecology of the Rocky Mountains}} |
{{See also|Ecology of the Rocky Mountains}} |
||
=== Flora === |
=== Flora === |
||
[[File:Aspen tree grove in Shoshone National Forest.jpg|thumb|A grove of Quaking |
[[File:Aspen tree grove in Shoshone National Forest.jpg|thumb|A grove of Quaking Aspen and Lodgepole Pine in the spring]] |
||
Shoshone National Forest |
Shoshone National Forest is an integral part of the [[Greater Yellowstone Ecosystem]], which has 1,700 documented species of plants.<ref name=Wuerthner>{{cite book|last=Wuerthner|first=George|title=Yellowstone: A Visitor's Companion|year=1992|publisher=Stackpole Books|isbn=978-0811730785|page=65|url=http://books.google.com/?id=VWt3GUrR-tcC&pg=PA64&dq=number+of+documented+plant+species+in+greater+yellowstone+ecosystem#v=onepage&q=number%20of%20documented%20plant%20species%20in%20greater%20yellowstone%20ecosystem&f=false|edition=1|accessdate=November 2, 2013|chapter=Flora}}</ref> Since the elevation of the land in the forest ranges from {{convert|4600|to|13804|ft|abbr=on}}, which is more than {{convert|9000|ft|abbr=on}}, the forest has a wide variety of ecosystems.<ref name=about>{{cite web|title=About the forest|url=http://www.fs.usda.gov/main/shoshone/about-forest|publisher=U.S. Department of Agriculture|accessdate=November 2, 2013}}</ref><ref name=enright>{{cite book|last=Enright|first=Kelly|title=America's Natural Places: Rocky Mountains and Great Plains|year=1992|publisher=Greenwood|isbn=978-0313353154|page=137|url=http://books.google.com/?id=AKME9xeG5hsC&pg=PA137&dq=shoshone+national+forest+ecosystems#v=onepage&q=shoshone%20national%20forest%20ecosystems&f=false|accessdate=November 2, 2013}}</ref> Lower elevations often have [[sagebrush]] and [[grassland|grass]]-dominated [[vegetation]] types, while forested areas are dominated by various combinations of tree and shrub species. These include [[lodgepole pine]], which along with [[Juniperus scopulorum|Rocky Mountain juniper]], and [[Aspen|quaking aspen]] are found at elevations up to {{convert|9000|ft|abbr=on}}.<ref name=enright/> At higher elevations [[subalpine fir]], [[Engelmann spruce]], [[whitebark pine]] and [[limber pine]], are common, each occurring up to [[tree line|timberline]].<ref name=enright/> The region above timberline makes up 25 percent of the total acreage of the forest and of that 13 percent is listed as just either barren, rock or ice.<ref name=vg>{{cite web|title=Shoshone National Forest Visitor Guide|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5330186.pdf|format=pdf|accessdate=January 4, 2014}}</ref> The types of plant species is highly dependent on the amount of water available, and trees are more commonly found on higher slopes due to the longer lasting snowfall which keeps the soil moister for a longer time into the summer months. Along lower elevation [[riparian]] corridors, [[Populus sect. Aegiros|cottonwoods]] and [[willow]]s are typically dominant. Numerous plant species are [[endemic (ecology)|endemic]] to the region including some that are rare. Among them, the [[Draba|whitlow grass]], [[Brassicaceae|fremont bladderpod]], shoshonea, and the [[Asteraceae|north fork Easter daisy]] provide vivid white and yellow flowers during the spring and summer.<ref name=plants>{{cite web|title=Rare Plants of Shoshone National Forest (USFS R-2)|work=Wyoming Rare Plant Field Guide, US Forest Service Rare Plant List|publisher=U.S. Geological Survey |url=http://www.npwrc.usgs.gov/resource/distr/others/wyplant/shoshone.htm|accessdate=September 30, 2013}}</ref> |
||
[[Exotic species]] of flora that are not native to the region include [[Cirsium arvense|Canada thistle]], [[Carduus nutans|Musk thistle]], [[Centaurea maculosa|Spotted knapweed]], [[Euphorbia esula|Leafy spurge]] and [[Linaria vulgaris|Yellow toadflax]].<ref name=houston>{{cite web|last=Houston|first=Kent E.|coauthors=Walter J. Hartung and Carol J. Hartung|title=A Field Guide for Forest Indicator Plants, Sensitive Plants, and Noxious Weeds of the Shoshone National Forest, Wyoming|publisher=U.S. Department of Agriculture|url=http://www.fs.fed.us/rm/pubs/rmrs_gtr084.pdf|format=pdf|pages=155–171|accessdate=November 2, 2013|date=October 2001}}</ref> These non-native plant species are considered noxious, impacting native plant communities and the species that thrive on them.<ref name=houston/> Native species such as the [[Mountain pine beetle]] are having an enormous negative impact on some tree species.<ref name=beetle>{{cite web|title=Bark Beetle Epidemic|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/landmanagement/?cid=STELPRDB5358725|accessdate=November 2, 2013}}</ref> A survey of the forest performed in 2010 indicated that over {{convert|1000000|acre}} of timberland had been impacted by insects such as the Mountain pine beetle, [[Dendroctonus rufipennis|spruce bark beetle]] and [[Dendroctonus pseudotsugae|Douglas fir beetle]], and that the insects had killed between 25 and 100 percent of the trees in the impacted areas.<ref name=impact>{{cite web|title=Shoshone National Forest – vegetation management projects in 2011|publisher=U.S. Forest Service|url=https://fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5260311.pdf|format=pdf|accessdate=November 2, 2013}}</ref> The forest service is addressing the situation by performing controlled burns, selling dead trees as firewood, timber harvesting and spraying the highest value areas.<ref name=beetle/> |
|||
[[Exotic species]], accidentally introduced by tourists, are usually found near roadways and campgrounds. The [[mountain pine beetle]] is a naturally occurring insect species that is known to infest forest groves, and is particularly common in areas with numerous lodgepole pines and fir trees.<ref name="beetle">{{cite web |author=U.S. Forest Service, U.S. Department of Agriculture |title=Forest Works to Counter Carter Mountain Threats |url=http://www.fs.fed.us/r2/shoshone/news/2003/11_04_carter_mountain_project.shtml |accessdate=2006-10-15}}</ref> During strong infestations, the beetle can wipe out huge areas of forest, increasing [[wildfire]] potential and reducing habitat and the sustainability of the forest. The Forest Service has an invasive species control effort that identifies and attempts to contain the further spread of non-native plants.<ref name="invasive">{{cite web |author=Shoshone National Forest Planning Staff |title=Draft, Forest Plan Comprehensive Evaluation Report |url=http://www.fs.fed.us/r2/shoshone/projects/planning/revision/revision_documents/2005_05_31_draft_fpcer_version1.pdf |accessdate=2006-10-15|format=PDF}}</ref> |
|||
=== Fauna === |
=== Fauna === |
||
[[File:Grizzly Bear sow and cub in Shoshone National Forest.jpg|thumb|right|Grizzly bear mother and cub]] |
|||
Since the migration of the [[endangered species|endangered]] grey wolf into Shoshone National Forest after the successful [[wolf reintroduction|Wolf Reintroduction]] Program in the Yellowstone region commenced in the late 1990s, virtually all of the known 50 [[mammal]] species that existed prior to white settlement still exist. |
|||
Since the migration of the [[endangered species|endangered]] [[gray wolf]] into Shoshone National Forest after the successful [[wolf reintroduction]] program in the Yellowstone region commenced in the mid-1990s, all of the known 70 [[mammal]] species that existed prior to white settlement still exist in the forest.<ref name=enright/> Altogether, at least 335 species of wildlife call Shoshone National Forest their home, including the largest population of [[Bighorn sheep]] and one of the few locations [[Grizzly bear]]s can still be found in the [[Contiguous United States|contiguous U. S.]].<ref name=vg/> |
|||
[[File:Grizzly Bear sow and cub in Shoshone National Forest.jpg|thumb|left|[[Grizzly bear|Grizzly]] sow and cub]] |
|||
At least 700 grizzly bears are believed to exist in the Greater Yellowstone Ecosystem, which includes Shoshone National Forest, with approximately 125 grizzlies in the forest.<ref name=enright/><ref name=grizzly>{{cite web|title=Grizzly Bear Conservation and Recovery|publisher=U.S. Department of Agriculture|url=http://www.fs.fed.us/biology/resources/pubs/issuepapers/Issueupdate_GrizRecovery_Sept2013.pdf|format=pdf|date=September 2013|accessdate=November 15, 2013}}</ref> The grizzly is listed as a [[threatened species]] by the [[U.S. Fish and Wildlife Service]], and the forest is one of their last strongholds. For what are considered to be "nuisance bears", non-lethal traps are set to capture them so that they can be relocated to remote areas, away from civilization.<ref name=moody>{{cite web|last=Moody|first=David|coauthors=Dennie Hammer, Mark Bruscino, Dan Bjornlie, Ron Grogan and Brian Debolt|title=Wyoming Grizzly Bear Management Plan|publisher=Wyoming Game and Fish Department|url=http://wgfd.wyo.gov/web2011/Departments/Wildlife/pdfs/WYGRIZBEAR_MANAGEMENTPLAN0000716.pdf|pages=25–31|format=pdf|date=July 2005|accessdate=December 15, 2013}}</ref> In the case of the grizzly, each captured bear is tranquilized and then [[ear tag]]ged with an identifying number. Each number is registered, and if the bear continues to return to areas where they pose a risk of imminent threat to human safety, they are exterminated.<ref name=moody/> The grizzly recovery efforts implemented by federal agencies have often resulted in major disagreements with local landowners and surrounding municipalities.<ref name=grizzly/> This situation occurs less frequently with the smaller and less aggressive [[American black bear|black bear]]. An active management program, in conjunction with other National Forests and National Parks within the Greater Yellowstone Ecosystem, works cooperatively to maximize human safety and to ensure habitat protection for both species of endemic bears. Visitors are mandated to store their food in their vehicles or in steel containers found in campgrounds, and [[bear-resistant food storage container|bear-proof]] trash receptacles are located in the front-country zones throughout the forest. In the [[backcountry]], food must be stored some distance from campsites, and other related precautions are enforced to help prevent bad encounters.<ref name=vg/> |
|||
[[File:Bighorn Sheep in Shoshone National Forest.jpg|thumb| |
[[File:Bighorn Sheep in Shoshone National Forest.jpg|thumb|left|Bighorn Sheep]] |
||
The [[cougar]] (mountain lion) and the gray wolf are large [[apex predator]]s that inhabit the forest. Since the 1990s wolf reintroduction program in Yellowstone National Park, wolves have migrated into the forest and established permanent packs.<ref name=wolf1>{{cite web|title=2012 Wyoming Gray Wolf Population Monitoring and Management Annual Report|url=http://www.fws.gov/mountain-prairie/species/mammals/wolf/annualrpt12/2012_WY_Annual_Report_FINAL_2013-04-04.pdf|publisher=Wyoming Game and Fish Department|accessdate=December 21, 2013|author=K.J. Mills and R.F. Trebelcock, eds.|page=1|format=pdf|year=2013}}</ref> Approximately a dozen wolf packs totaling 70 individual wolves were documented in the forest in 2012.<ref name=wolf2>{{cite web|title=2012 Wyoming Gray Wolf Population Monitoring and Management Annual Report|url=http://www.fws.gov/mountain-prairie/species/mammals/wolf/annualrpt12/2012_WY_Annual_Report_FINAL_2013-04-04.pdf|publisher=Wyoming Game and Fish Department|accessdate=December 21, 2013|author=K.J. Mills and R.F. Trebelcock, eds.|pages=8–9|format=pdf|year=2013}}</ref> The wolf was delisted as endangered once their population levels had reached management objectives and limited hunting of wolves was permitted in the forest starting in 2012.<ref>{{cite web|title=Wolves in Wyoming|url=http://wgfd.wyo.gov/web2011/wildlife-1000380.aspx|publisher=Wyoming Game and Fish Department|accessdate=December 21, 2013|year=2013}}</ref><ref>{{cite web|title=Gray Wolf Hunting Seasons|url=http://wgfd.wyo.gov/web2011/Departments/Hunting/pdfs/REGULATIONS_CH470002742.pdf|publisher=Wyoming Game and Fish Commission|accessdate=December 21, 2013|format=pdf|year=2012}}</ref> Cougars are generally noctural and rarely seen but hunting of this species is also allowed in highly regulated harvests.<ref>{{cite web|title=Mountain Lion Hunting Seasons|url=http://wgfd.wyo.gov/web2011/imgs/QRDocs/REGULATIONS_CH42_BROCHURE.pdf|publisher=Wyoming Game and Fish Commission|accessdate=December 21, 2013|format=pdf|year=2012}}</ref> Wolverines are rare and elusive so documentation is oftentimes only from their tracks.<ref>{{cite web|last=Murphy|first=Kerry|title=Wolverine Conservation in Yellowstone National Park|publisher=National Park Service|url=http://www.nrccooperative.org/pdfs/Wolverine_report_final_high_web_public[1].pdf|format=pdf|accessdate=December 21, 2013|date=March 2011}}</ref> The [[Canada lynx]] was native to the forest, but no known populations may still exist due to the rarity of its primary food source, the [[Snowshoe hare]]. Shoshone National Forest is considered critical habitat for lynx recovery since the species is listed as threatened under the [[Endangered Species Act]] and the forest is in their historical range.<ref>{{cite web|title=Proposed Revision of the Critical Habitat Designation for the Canada Lynx and Revised Definition of the Contiguous United States Distinct Population Segment of Canada Lynx|publisher=U.S. Fish and Wildlife Service|url=http://www.fws.gov/mountain-prairie/species/mammals/lynx/09112013LynxCHQandA.pdf|format=pdf|year=2013|accessdate=December 21, 2013}}</ref> Other generally carnivorous mammals include [[coyote]], [[bobcat]], [[weasel]], [[marten]], [[ferret]] and [[American badger|badger]].<ref name=species2>{{cite web|title=Shoshone National Forest Species of Interest Report|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5199969.pdf|publisher=U.S. Forest Service|accessdate=December 22, 2013|pages=65–68|format=pdf|date=April 2009}}</ref> |
|||
The [[mountain lion]] (also known as the puma or cougar) and the gray wolf are the major [[carnivore]]s that inhabit the forest. The [[nocturnal]] mountain lion is rarely seen and their numbers are not known, but evidence such as numerous paw prints suggests they are widespread. The wolf has migrated into the forest from Yellowstone National Park but is less common in the forest. The population of wolves is hoped to increase over time for this endangered species. Other omnivorous mammals in the forest include the [[wolverine]], [[coyote]], [[bobcat]], [[weasel]], [[marten]] and [[ferret]]. Additionally, the [[beaver]], [[marmot]], [[pika]], [[raccoon]] and [[badger]] are commonly found throughout the forest. |
|||
Omnivorous mammals such as the [[raccoon]] and [[Western spotted skunk|skunk]] and herbivore mammal species such as the [[North American porcupine|porcupine]] and [[American pika|pika]], are common to the forest.<ref name=species2/><ref name=orabona>{{cite web|last=Orabona|first=Andrea|title=Atlas of Birds, Mammals, Amphibians and Reptiles in Wyoming|url=http://wgfd.wyo.gov/web2011/Departments/Wildlife/pdfs/WILDLIFE_ANIMALATLAS0002711.pdf|publisher=Wyoming Game and Fish Department|accessdate=December 21, 2013|coauthors=Courtney Rudd, Martin Grenier, Zack Walker, Susan Patla, and Bob Oakleaf|format=pdf|date=June 2012}}</ref> The [[beaver]] is considered a species of special interest to Shoshone National Forest since its dam building activities improve habitat for numerous other species such as the [[moose]], breeding waterfowl, various amphibians and other species dependent on a riparian environment.<ref name=species1>{{cite web|title=Shoshone National Forest Species of Interest Report|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5199969.pdf|publisher=U.S. Forest Service|accessdate=December 22, 2013|pages=6–11|format=pdf|date=April 2009}}</ref> |
|||
Native herbivores such as the [[moose]] are found in small numbers near waterways, especially at lower elevations. [[Elk]] (also known as wapiti), [[mule deer]] and [[pronghorn]] (also called pronghorn antelope) are some of the most commonly seen mammals and there are some small populations of [[bison]]. [[Bighorn sheep]] and [[mountain goat]]s inhabit the rocky terrain and highest elevations. During the winter, the largest bighorn sheep herd in the [[Continental United States|lower 48 states]] congregate in the region around [[Dubois, Wyoming]]; however, their numbers since 1990 have been greatly diminished due to disease and coyote predation.<ref name="bighorn">{{cite web |author=National Bighorn Sheep Interpretive Center |title=Estimated Whiskey Mountain Bighorn Sheep Population |url=http://www.bighorn.org/bj.asp |accessdate=2006-10-15|archiveurl=http://web.archive.org/web/20060828195729/http://bighorn.org/bj.asp |archivedate=August 28, 2006}}</ref> |
|||
Native herbivores such as the moose are found in small numbers near waterways, especially at lower elevations. Moose populations in northwestern Wyoming and other areas of North America have been on the decline since the end of the 20th century, possibly due to a parasite.<ref>{{cite news|last=French|first=Brett|title=Montana, Wyoming trying to understand why moose populations are plummeting|publisher=Billings Gazette|url=http://billingsgazette.com/lifestyles/recreation/montana-wyoming-trying-to-understand-why-moose-populations-are-plummeting/article_cf1fcb02-9699-56d8-9b34-9b297fd4dc5f.html|date=September 17, 2012|accessdate=December 21, 2013}}</ref> There were an estimated 739 moose in the forest in 2006 which is almost 300 fewer than there were 20 years earlier.<ref name=species1/><ref name=population>{{cite web|title=Shoshone National Forest Comprehensive Evaluation Report|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5201453.pdf|format=pdf|date=December 2007|accessdate=December 21, 2013}}</ref> Other ungulate species are much more common and there are over 20,000 [[elk]] (also known as wapiti) and 40,000 [[mule deer]].<ref name=population/> Bighorn sheep and [[mountain goat]]s inhabit the rocky terrain and highest elevations. During the winter, one of the largest bighorn sheep herds in the [[Continental United States|lower 48 states]] congregate in the region around [[Dubois, Wyoming]]; however, their numbers since 1990 have been diminished due to disease transmitted from contact with domesticated sheep and goats.<ref>{{cite web|last=Mlodik|first=Cory|title=Risk Analysis of Disease Transmission between Domestic Sheep and Goats and Rocky Mountain Bighorn Sheep|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5383002.pdf|date=April 2012|accessdate=December 21, 2013}}</ref> An estimated 5,000 bighorn sheep are found throughout the forest and a small but stable population of 200 mountain goats reside in the northernmost portions of the forest.<ref name=population/> [[Bison]] and [[pronghorn]] antelope are two other ungulates that live on the forest and have sustainable populations.<ref name=species2/> |
|||
An estimated 300 species of birds are found in the forest at least part of the year. [[Bald Eagle|Bald]] and [[golden eagle]]s are more common now than they have been for decades and tend to inhabit areas near waterways. [[Peregrine falcon]], [[Merlin (bird)|merlin]], [[hawk]]s and the [[great horned owl]] are other birds of prey that have become more widespread. The gregarious [[black-billed magpie]] and [[Clark's nutcracker]] (in the [[Corvidae|crow family]]) frequent areas near campgrounds and lakes. The [[trumpeter swan]] is found in very limited numbers, primarily in or near lakes and streams. Other waterfowl such as the [[great blue heron]], [[white pelican]], [[Canada goose]] and numerous species of [[duck]]s are also seen. [[Common Pheasant|pheasant]], [[sage grouse]] and [[wild turkey]] are widely distributed across the open sage lands. |
|||
An estimated 300 species of birds are found in the forest at least part of the year. [[Bald Eagle]], [[Peregrine falcon]], [[Swainson’s hawk]] and the [[Prairie falcon]] are birds of prey that are relatively common.<ref name=species2/> Waterfowl such as [[Western grebe]], [[Northern pintail]], [[Great blue heron]] and [[Barrow’s goldeneye]] have stable populations and rare sightings of [[Trumpeter swan]]s are reported.<ref name=species2/> [[Common Pheasant|pheasant]], [[ruffed grouse]] and [[wild turkey]] are widely distributed across the open sage lands. [[Harlequin duck]] and [[Northern goshawk]] are generally rare but management plans were implemented to protect various habitats these two species frequent to try and increase their population numbers.<ref name=species1/> |
|||
[[File:Yellowstone Cutthroat Trout.jpg|thumb|left|[[Yellowstone cutthroat trout]]]] |
|||
There are eight species and subspecies of [[trout]] present in streams in the Forest, with the [[cutthroat trout]] being the only species native to Wyoming. The [[Yellowstone cutthroat trout]] is found only in the forest and adjacent parks and is one of four subspecies of cutthroat trout in the forest. Additional game fish species include [[arctic grayling]], [[Coregonus|mountain whitefish]] and the [[Sturgeon|shovelnose sturgeon]].<ref name="fishing">{{cite web |author=U.S. Forest Service, U.S. Department of Agriculture |title=Shoshone National Forest Fishing |url=http://www.fs.fed.us/r2/shoshone/recreation/fishing/snf_fish_site/fish_index.html |accessdate=2006-10-15}}</ref> |
|||
[[File:Yellowstone Cutthroat Trout.jpg|thumb|right|Yellowstone cutthroat trout]] |
|||
There are few [[reptile]]s in the forest; however, several snake species including the venomous [[Rattlesnake|prairie rattlesnake]] can be found at lower elevations along with other reptiles such as the [[Painted Turtle|western painted turtle]] and the [[Box Turtle|ornate box turtle]]. Amphibians such as the [[Frog|Columbia spotted frog]], [[tiger salamander]] and the [[Toad|boreal toad]] are relatively common. |
|||
Fish found in Shoshone National Forest include at least six species and subspecies of trout including [[Rainbow trout|Rainbow]], [[Brook trout|Brook]] and [[Brown trout]]. The [[Yellowstone cutthroat trout]] is widespread throughout the Greater Yellowstone Ecosystem, but in the forest is mostly limited to the [[Shoshone River]].<ref name=fishguide>{{cite web|title=Wyoming Fishing Guide|publisher=Wyoming Game and Fish Department|url=http://wgfd.wyo.gov/web2011/Departments/Fishing/pdfs/WGFD_FISHINGGUIDE0000393.pdf|format=pdf|year=2011|accessdate=December 29, 2013}}</ref><ref name=gresswell>{{cite web|last=Gresswell|first=Robert|title=Yellowstone Cutthroat Trout (Oncorhynchus clarkii bouvieri): A Technical Conservation Assessment|publisher=U.S. Geological Survey|url=http://www.fs.fed.us/r2/projects/scp/assessments/yellowstonecutthroattrout.pdf|format=pdf|date=June 30, 2009|accessdate=December 29, 2013}}</ref> The [[Coregonus|mountain whitefish]] is also found in the Shoshone River, while the [[Burbot]] is found in two streams in the southern regions of the forest.<ref name=fishguide/> |
|||
Insects such as [[mosquito]]s and [[fly|black flies]] can be pesky in the spring and summer and at the highest altitudes are known to be very bothersome. |
|||
There are more than a dozen species of [[reptile]]s in the forest including the venomous [[Rattlesnake|prairie rattlesnake]] which can be found at lower elevations.<ref name=orabona/> The [[Painted Turtle|western painted]] and the [[Box Turtle|ornate box turtle]] are turtle species known to exist and about eight species of lizards such as the [[Greater short-horned lizard]] have been documented.<ref name=orabona/> Amphibians such as the [[Frog|Columbia spotted frog]] and the [[Toad|boreal toad]] are considered species of concern because of their high susceptibility to disease, habitat loss and human introduced toxins.<ref name=species1/> Boreal toads are found at elevations of between {{convert|7380|and|11800|ft|abbr=on}} and the Columbia spotted frog can live at elevations as high as {{convert|9480|ft|abbr=on}} in the Greater Yellowstone Ecosystem.<ref name=species1/> |
|||
Exotic species of fauna such as the [[Zebra mussel|Zebra]] and [[Quagga mussel]]s and the [[New Zealand mud snail]] are invasive species that can greatly impact fish species. Though the mussel species are not known to be in Wyoming, several surrounding regions have reported them. The New Zealand mud snail has been found in the Shoshone River east of the forest. Forest managers have established a preventative program to try and keep these species from entering forest waterways.<ref>{{cite web|title=Aquatic Invasive Species|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/landmanagement/?cid=STELPRDB5358127|accessdate=December 29, 2013}}</ref> |
|||
=== Wilderness === |
=== Wilderness === |
||
[[File:Popo Agie Wilderness Wind River Range.jpg|thumb|[[Popo Agie Wilderness]]]] |
[[File:Popo Agie Wilderness Wind River Range.jpg|thumb|[[Popo Agie Wilderness]]]] |
||
The forest contains four areas of pristine [[wilderness]] that have remained largely untouched by human activities such as mining, logging, and road and building construction. The four regions |
The forest contains four areas of pristine [[wilderness]]es that have remained largely untouched by human activities such as mining, logging, and road and building construction. The four regions include the [[North Absaroka Wilderness|North Absaroka]], [[Washakie Wilderness|Washakie]], [[Fitzpatrick Wilderness|Fitzpatrick]] and [[Popo Agie Wilderness]]es.<ref name=about/> Additionally, a small portion of the [[Absaroka-Beartooth Wilderness]] extends into the extreme northwestern part of the forest, along the Montana border. In Shoshone National Forest, {{convert|1400000|acre|abbr=on}}, constituting 56 percent of the forest is designated wilderness.<ref name=wilderness>{{cite web|title=Wilderness|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/specialplaces/?cid=stelprdb5183021|accessdate=September 7, 2013}}</ref><ref name=vg/> The wilderness designation provides a much higher level of land protection and prohibits any alterations by man to the resource.<ref name=nwps>{{cite web|last=Landres|first=Peter|coauthors=Shannon Meyer|title=National Wilderness Preservation System Database: Key Attributes and Trends, 1964 Through 1999|publisher=U.S. Department of Agriculture|url=http://www.fs.fed.us/rm/pubs/rmrs_gtr018.pdf|page=1|format=pdf|date=July 2000|accessdate=September 7, 2013}}</ref> |
||
The [[Wilderness Act|Wilderness Act of 1964]] enhanced the protection status of remote and/or undeveloped land already contained within federally administered protected areas. Passage of the act ensured that no human improvements would take place aside from those already existing. The protected status in wilderness designated zones prohibits road and building construction, |
The [[Wilderness Act|Wilderness Act of 1964]] enhanced the protection status of remote and/or undeveloped land already contained within federally administered protected areas. Passage of the act ensured that no human improvements would take place aside from those already existing. The protected status in wilderness designated zones prohibits road and building construction, oil and mineral exploration or [[mining|extraction]], and logging, and also prohibits the use of motorized equipment, including even bicycles. The only manner in which people can enter wilderness areas is either on foot or [[equestrianism|horseback]]. [[Hunting]] and [[fishing]] are permitted in the wilderness, just as they are throughout the forest, provided those engaging in such activities have the proper licenses and permits.<ref name=wilderness2>{{cite web|title=The National Wilderness Preservation System|publisher=Wilderness.net|work=The Wilderness Act of 1964|url=http://www.wilderness.net/index.cfm?fuse=NWPS&sec=legisAct|accessdate=September 7, 2013}}</ref> |
||
=== Fire ecology === |
=== Fire ecology === |
||
{{see also|Fire ecology|Wildfire#Ecology}} |
{{see also|Fire ecology|Wildfire#Ecology}} |
||
Shoshone National Forest has an active Fire Management Program which recognizes that [[forest fire]]s are a natural part of the ecosystem; however, this was not always the case. Historic fire fighting efforts, which emphasized quickly extinguishing all fires, created huge sources of fuel in the form of dead and dying trees. After the catastrophic fires in the Yellowstone region in 1988, an effort to identify areas of similar fire potential was implemented. Working cooperatively with the [[National Interagency Fire Center]], a multiagency effort of federal, state and local resources, and local land owners on the Wildland-Urban Interface, a system of fire restrictions, fuels management, and a [[controlled burn]] plan was developed to reduce the chances of a huge catastrophic fire.<ref name="fire">{{cite web |author=U.S. Forest Service, U.S. Department of Agriculture |title=Wildland Fire Management |url=http://www.fs.fed.us/r2/shoshone/fire/wildland_fire/index.shtml |accessdate=2006-10-15}}</ref> |
|||
[[Thunderstorm|Lightning storms]] cause 70% of the wildfires in the forest. These are usually produced by thunderstorms that have a lot of energy but little associated moisture, a common occurrence during midsummer. The remainder of the wildfires are attributed to neglected [[campfire]]s and other human carelessness. |
|||
[[File:Forest fire in Shoshone National Forest 2001.jpg|thumb|Dinwoody spot fire in 2001]] |
[[File:Forest fire in Shoshone National Forest 2001.jpg|thumb|Dinwoody spot fire in 2001]] |
||
Fire Management officials in Shoshone National Forest recognize that [[forest fire]]s are a natural part of the ecosystem; however, this was not always the case. 20th century fire fighting efforts, especially in the first half of that century, emphasized quickly extinguishing all fires, as fire was seen as completely detrimental to a forest.<ref name=aplet>{{cite journal|last=Aplet|first=Gregory H.|title=Evolution of Wilderness Fire Policy|journal=International Journal of Wilderness|volume=12|issue=1|pages=9–13|date=April 2006|url=http://www.wilderness.net/library/documents/IJWApr06_Aplet.pdf|format=pdf|accessdate=December 30, 2013}}</ref> In 1935, fire management officials established the ''10 am rule'' for all fires on federal lands, which recommended aggressive attack on fires and to have them controlled by 10 am, the day after they are first detected.<ref name=10am>{{cite web|title=Evolution of Federal Wildland Fire Management Policy|work=Review and Update of the 1995 Federal Wildland Fire Management Policy January 2001|publisher=National Park Service, U.S. Forest Service|date=January 2001|url=http://www.nwcg.gov/branches/ppm/fpc/archives/fire_policy/docs/chp1.pdf|format=pdf|accessdate=December 30, 2013}}</ref><ref name=omi1>{{cite book|last=Omi|first=Phillip N.|title=Forest Fires: A Reference Handbook|chapter=Institutionalization of Fire Exclusion|publisher=ABC-CLIO|date=May 23, 2005|page=67|url=http://books.google.com/books?id=0Ts_oE23Wu8C&lpg=PA67&dq=Institutionalization%20of%20Fire%20Exclusion&pg=PA67#v=onepage&q=Institutionalization%20of%20Fire%20Exclusion&f=true|isbn=978-1851094387}}</ref> This was intended to prevent fires from remaining active into the afternoon when the rising temperatures and more turbulent air caused fires to expand and become more erratic.<ref name=omi2>{{cite book|last=Omi|first=Phillip N.|title=Forest Fires: A Reference Handbook|chapter=Institutionalization of Fire Exclusion|publisher=ABC-CLIO|date=May 23, 2005|page=131|url=http://books.google.com/books?id=0Ts_oE23Wu8C&lpg=PA67&dq=Institutionalization%20of%20Fire%20Exclusion&pg=PA131#v=onepage&q=erratic&f=false|isbn=978-1851094387}}</ref> However, this policy led to an increase in fuels because fires were oftentimes extinguished before they had a chance to burn out dead and dying old growth. It was in a stand of old growth fir trees in Shoshone National Forest that the [[Blackwater fire of 1937]] killed 15 fighters during a firestorm {{convert|35|mi|abbr=on}} west of Cody, Wyoming. The fire was one of the deadliest in terms of forest firefighter deaths in U.S. history.<ref name=deaths>{{cite web|title=Deadliest Incidents Resulting in the Deaths of 8 or More Firefighters|publisher=National Fire Protection Association|url=http://www.nfpa.org/research/reports-and-statistics/the-fire-service/fatalities-and-injuries/deadliest-incidents-resulting-in-the-deaths-of-8-or-more-firefighters|accessdate=December 30, 2013|date=February 2012}}</ref> |
|||
Between the years 1970 and 2012, Shoshone National Forest averaged 25 fires annually, of which half were due to natural ignition from lightning, which accounted for 90 percent of the total acreage burned. The remaining acreage that burned was due to campfires that got out of control or from other causes.<ref name=fmp1>{{cite web|title=Shoshone National Forest Fire Management Plan - 2012|publisher=U.S. Forest Service|url=http://gacc.nifc.gov/rmcc/dispatch_centers/r2cdc/predictive/fuels_fire_danger/SHF%20FMP/shf%20fmp%202012%20final%204-16-12.pdf|format=pdf|pages=46–49|year=2012|accessdate=January 4, 2014}}</ref> In Shoshone National Forest, the highest fire incidence is generally in the months of August and September.<ref name=fmp1/> An average of {{convert|2334|acre|abbr=on}} burns annually, with the worst year in the past century being 1988, when {{convert|194430|acre|abbr=on}} burned from fires that had spread from the conflagration that engulfed Yellowstone National Park and the surrounding region.<ref name=fmp1/> After the [[Yellowstone fires of 1988|Yellowstone region fires of 1988]], an effort to identify areas of similar fire potential was implemented.<ref name=aplet/> Fire managers at Shoshone National Forest work with a number of outside agencies to incorporate fire restrictions, fuels management, and a [[controlled burn]] plans to reduce the chances of a catastrophic fire.<ref name=fire>{{cite web|title=Fire and fuels management|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/landmanagement/resourcemanagement/?cid=stelprdb5192920|accessdate=December 30, 2013}}</ref> The dead and dying trees which have been killed by various species of bark beetle may have a great impact on future forest fires.<ref name=impact/> Fire managers have stated the worst time for increased fire activity is 1-2 years after the trees are killed and then again after the trees have fallen many years later.<ref>{{cite web|title=About the epidemic|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/main/barkbeetle/aboutepidemic|accessdate=December 30, 2013}}</ref> |
|||
In the case of unnatural wildfires, the forest has a policy of complete suppression except in cases of prescribed burns, which are a part of the Fire Management Plan. An average of 25 fires occur every year, and larger fires of over {{convert|1000|acre|km2}} occur about every three years. In 2003 more than 50 fires were recorded, of which five affected an area greater than {{convert|1000|acre}}.<ref name="fire"/> |
|||
The forest maintains a full-time fire staff of a dozen individuals through the summer. Their jobs include maintaining a high level of preparedness, keeping a vigilant lookout for fire activity, responding to reports of fires, maintaining equipment, monitoring weather and relative atmospheric dryness, and preparing daily fire activity reports, which are used to post fire information for visitors and staff. The forest has five wildland fire engines, pumps, hand tools and many miles of fire hose at its disposal. A helicopter can be summoned quickly, along with a regional base for a team of [[smokejumper]]s and [[aerial firefighting|air tankers]] used to provide air support in the manner of [[flame retardant|retardant]] and water drops.<ref name="fire"/> In the case of larger fires, the National Interagency Fire Command can mobilize available resources within days or even hours. |
|||
== Geography and geology == |
== Geography and geology == |
||
[[File:Gannett Peak.jpg|thumb|[[Gannett Peak]] is the highest mountain in Wyoming and the forest]] |
[[File:Gannett Peak.jpg|thumb|[[Gannett Peak]] is the highest mountain in Wyoming and the forest.]] |
||
Shoshone National Forest borders [[Yellowstone National Park]] and [[Bridger-Teton National Forest]] to the west. The [[Continental Divide of the Americas|Continental Divide]] demarks the boundary between Shoshone and Bridger-Teton National Forests. Along the [[Montana]] border, Shoshone National Forest borders [[Custer National Forest]] to the north.<ref name=fmp1/> Private property, property belonging to the state of Wyoming and lands administered by the [[Bureau of Land Management]] form the eastern boundaries. Lastly, the Wind River Indian Reservation also borders on the east, and bisects a smaller southern section which includes the Popo Agie Wilderness and the Washakie Ranger District.<ref>{{cite web|title=Washakie Ranger District|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/about-forest/?cid=stelprdb5191040|accessdate=January 17, 2014}}</ref> |
|||
The altitude in the forest ranges from {{convert|4600|ft}} near Cody, Wyoming, to {{convert|13804|ft}} at the top of [[Gannett Peak]], an elevation gain of over {{convert|9200|ft}}. Of the three major [[mountain range]]s found in the forest, they are [[geology|geologically]] distinct from each other. All of the mountains are a part of the [[Rocky Mountains|Rockies]] and are at the transitional point between the central Rockies and the northern Rockies. The [[Absaroka Mountains]] were named after the [[Crow tribe|Crow]] Indian tribe, although they only inhabited the far northernmost part to the mountain range. The majority of the Absaroka Mountains are contained within the forest, with the highest peak being [[Francs Peak]] at {{convert|13153|ft|m}}. Stretching north to south through the northern and eastern sections of the forest, they span over {{convert|100|mi|km}} from the [[Montana]] border to south of [[Dubois, Wyoming]]. |
|||
The altitude in the forest ranges from {{convert|4600|ft}} near Cody, Wyoming, to {{convert|13804|ft|abbr=on}} at the top of [[Gannett Peak]], an elevation gain of over {{convert|9200|ft|abbr=on}}.<ref name=fmp1/> Of the three major [[mountain range]]s found in the forest, they are [[geology|geologically]] distinct from each other. All of the mountains are a part of the Rocky Mountains. In the northern and central portions of the forest lie the [[Absaroka Mountains]] which were named after the [[Crow tribe|Crow]] Indian tribe.<ref name=absaroka>{{cite web|title=Absaroka Beartooth Wilderness|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/specialplaces/?cid=stelprdb5190252|accessdate=January 18, 2014}}</ref> The majority of the Absaroka Mountains are contained within the forest, with the highest peak being [[Francs Peak]] at {{convert|13158|ft|abbr=on}}.<ref name=francs>{{cite peakbagger|pid=5311|name=Francs Peak, Wyoming|accessdate=January 4, 2014}}</ref><ref name=antweiler>{{cite journal|last=Antweiler|first=John C.|coauthors=Carl L. Bieniewski|title=Northern part of the Washakie Wilderness and Nearby Roadless Areas, Wyoming|journal=U.S. Geological Survey Professional Paper|volume=2|issue=1300|pages=1272–1275|publisher=U.S. Geological Survey|date=984|url=http://books.google.com/?id=HcfOaXOMRbcC&pg=PA1173&dq=francs+peak+tallest+in+absaroka#v=onepage&q=francs%20peak%20tallest%20in%20absaroka&f=false|accessdate=January 18, 2014}}</ref> The peaks of the Absaroka are [[basaltic]] in origin, having been the result of volcanic activity estimated to have occurred 50 million years ago during the [[Eocene]] [[epoch (geology)|epoch]].<ref name=antweiler/> The rocks are composed of mostly [[andesite]] and [[breccia]]s deposited for millions of years during volcanic events and are atop more ancient [[sedimentary rock]]s that are considered to have economically viable mineral wealth.<ref name=antweiler/> Gold was mined from the slopes of Francs Peak between the years 1890 and 1915, and the small [[ghost town]] of Kirwin remains as a legacy of that period.<ref name=kirwin/> Major tributaries of the [[Bighorn River]], such as the Shoshone and [[Greybull River]]s, originate in the Absaroka Mountains. Important [[mountain pass|passes]] through the Absarokas include [[Sylvan Pass (Wyoming)|Sylvan Pass]], which leads to the eastern entrance of Yellowstone National Park; and [[Togwotee Pass]], which provides access to Jackson Hole and [[Grand Teton National Park]].<ref>{{cite book|last=Larson|first=T.A.|title=Wyoming: A Guide to Its History, Highways, and People|publisher=University of Nebraska Press|isbn=978-0803268548|page=429|url=http://books.google.com/?id=sObNp2jHduEC&pg=PA429&dq=Sylvan+Pass+absaroka+mountains#v=onepage&q=Sylvan%20Pass%20absaroka%20mountains&f=false|accessdate=January 18, 2014|date=March 1, 1981}}</ref><ref>{{cite book|last=Adkison|first=Ron|title=Hiking Wyoming's Wind River Range|publisher=Falcon Guides|isbn=978-1560444022|page=1|url=http://books.google.com/?id=iSzkDm5UAssC&pg=PA1&dq=togwotee+pass+absaroka+mountains#v=onepage&q=togwotee%20pass%20absaroka%20mountains&f=false|accessdate=January 18, 2014|date=June 1, 1996}}</ref> |
|||
Important [[mountain pass|passes]] through the Absarokas include [[Sylvan Pass (Wyoming)|Sylvan Pass]], which leads to the eastern entrance of Yellowstone National Park; and [[Togwotee Pass]], which provides access to Jackson Hole and [[Grand Teton National Park]]. The peaks of the Absaroka are [[basaltic]] in origin, having been the result of volcanic activity estimated to have occurred 50 million years ago during the [[Eocene]] [[epoch (geology)|epoch]].<ref name="absarokas">{{cite web |author=U.S. Geological Survey, U.S. Department of the Interior |title=Absaroka Mountains |work=America's Volcanic Past |url=http://vulcan.wr.usgs.gov/LivingWith/VolcanicPast/Places/volcanic_past_montana.html |accessdate=2006-10-15}}</ref> The rocks themselves are relatively dark and consist of [[rhyolite]], [[andesite]] and [[breccia]]s. Because of the erosional influences of [[glacier]]s and water and the relative softness of the rocks, the Absarokas are quite craggy in appearance. [[Gold]] was mined from the slopes of [[Francs Peak]] until 1907, and the small [[ghost town]] of Kirwin is still visited. Few lakes exist in the Absarokas, but the headwaters of both the [[Bighorn River|Bighorn]] and [[Yellowstone River]]s are found there. |
|||
[[File:Beartooth Lake in Shoshoe National Forest.jpg|thumb|Beartooth Lake |
[[File:Beartooth Lake in Shoshoe National Forest.jpg|thumb|left|Beartooth Lake]] |
||
In the far north of Shoshone National Forest a small portion of the Beartooth Mountains are located north of the [[Clarks Fork of the Yellowstone River]]. The Beartooths are composed of [[Precambrian]] [[granite|granitic]] rocks that are amongst the oldest found on Earth.<ref>{{cite book|title=Earth's Oldest Rocks|publisher=Elsevier Science|editors=Martin J. Van Kranendonk, R. Hugh Smithies, and Vickie Bennett|isbn=978-0080552477|pages=780–781|url=http://books.google.com/?id=lIRpMW6gLm4C&pg=PA780&dq=age+of+rocks+in+the+beartooth+mountains#v=onepage&q=beartooth%20mountains&f=false|accessdate=January 18, 2014|date=October 26, 2007}}</ref> Although often considered a part of the Absaroka Mountains, the Beartooths are distinct in appearance and geologic history.<ref name=absaroka/> Uplifted approximately 70 million years ago during the [[Laramide orogeny]], the Beartooths consist of vast windswept plateaus and rugged peaks with sheer cliff faces. The [[Beartooth Highway]] ([[U.S. Highway 212 (Wyoming)|U.S. Highway 212]]) crosses {{convert|10974|ft|m|adj=on|sigfig=3}} Beartooth Pass, and from there descends to the northeast entrance to Yellowstone National Park. |
|||
[[File:Cirque of the Towers.jpg |
[[File:Cirque of the Towers.jpg|thumb|right|Cirque of the Towers]] |
||
The Wind River Range is in the southern portion of the forest and is composed primarily of granitic rock |
The Wind River Range is in the southern portion of the forest and is composed primarily of Precambrian granitic rock.<ref name=winds>{{cite web|title=Wind River Range|publisher=Wyoming State Geological Survey|url=http://www.wsgs.uwyo.edu/research/stratigraphy/WindRiverRange/Default.aspx|year=2013|accessdate=January 21, 2014}}</ref> Gannett Peak, the tallest mountain in Wyoming, is in the northern part of the range. Altogether eight peaks exceed {{convert|13500|ft|abbr=on}} and 119 rise at least {{convert|12000|ft|abbr=on}} above sea level.<ref>{{cite book|last=Kelsey|first=Joe|title=Climbing and Hiking in the Wind River Mountains|publisher=Falcon Guides|url=http://books.google.com/?id=FYEVAAAAQBAJ&pg=PA432&dq=wind+river+range+peaks+over+12000+feet|isbn=978-0762780785|date=July 16, 2013|page=432|accessdate=January 21, 2014}}</ref> [[Fremont Peak (Wyoming)|Fremont Peak]], the second highest peak in the range, was originally believed to be the tallest mountain in the Rocky Mountains due to its prominence when viewed from the [[Oregon Trail]] by early pioneers.<ref name=cooper>{{cite book|last=Cooper|first=Ed|title=Soul of the Rockies: Portraits of America's Largest Mountain Range|publisher=Falcon Guides|url=http://books.google.com/?id=yRggz0glL3gC&lpg=PT98&dq=fremont%20peak%20tallest%20in%20rockies&pg=PT98#v=onepage&q=fremont%20peak%20tallest%20in%20rockies&f=false|isbn=978-0762749416|date=November 25, 2008|pages=76–82|accessdate=January 21, 2014}}</ref> The Wind River Range is popular with mountain climbers because of its solid rock and variety of routes.<ref name=windriver>{{cite web|title=Wind River Ranger District|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/about-forest/districts/?cid=stelprdb5191039|accessdate=January 21, 2014}}</ref> The [[Cirque of the Towers]] in the [[Popo Agie Wilderness]] is one of the more popular climbing and hiking destinations, and an estimated 200 different climbing routes are located within the peaks that surround the [[cirque (landform)|cirque]].<ref name=cooper/> |
||
There are over 500 |
There are over 500 lakes in the forest, and {{convert|1000|mi|abbr=on}} of streams and rivers.<ref name=dow>{{cite book|last=Dow|first=Fred|coauthor=Suzanne Dow|title=U.S. National Forest Campground Guide Rocky Mountain Region|publisher=Authorhouse|url=http://books.google.com/?id=3OnLh3hF4ZIC&pg=PA507&lpg=PA507&dq=one+thousand+miles+of+streams+in+shoshone+national+forest|isbn=978-0759630239|page=507|year=2001|accessdate=January 21, 2014}}</ref> The Clarks Fork of the Yellowstone River is federally-designated as a [[National Wild and Scenic Rivers System|Wild and Scenic River]] for {{convert|22|mi|abbr=on}} through the forest, with cliffs towering up to {{convert|2000|ft|abbr=on}} as the river winds through a gorge. The forest is on the eastern slopes of the Continental Divide, and the rivers flow into the [[Atlantic Ocean|Atlantic Ocean basin]]. |
||
=== Glaciology === |
=== Glaciology === |
||
According to the U.S. Forest Service, Shoshone National Forest has the greatest number of |
According to the U.S. Forest Service, Shoshone National Forest has the greatest number of glaciers of any National Forest in the Rocky Mountains. The forest recreation guide lists 16 named and 140 unnamed glaciers within the forest, all in the Wind River Range. Forty-four of these glaciers are in the Fitzpatrick Wilderness, centered around the highest mountain peaks.<ref>{{cite web|title=Fitzpatrick Wilderness|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/specialplaces/?cid=stelprdb5190243|accessdate=January 11, 2014}}</ref><ref name=vg/> However, the state water board for Wyoming lists only 63 glaciers for the entire Wind River Range, which includes glaciers in adjacent Bridger-Teton National Forest.<ref name=state>{{cite web|last=Hutson|first=Harold J|title=Wyoming State Water Plan|url=http://waterplan.state.wy.us/plan/bighorn/techmemos/glaciers.html|accessdate=January 11, 2014}}</ref> Researchers claim that for most of the period that glaciers have been known to exist in the forest, that they have been in a state of general retreat, with glacial mass losses of as much as 25 percent between the years 1985 and 2009.<ref name=rice>{{cite web|last=Rice|first=Janine|coauthors=Andrew Tredennick, and Linda A. Joyce|title=Climate Change on the Shoshone National Forest, Wyoming: A Synthesis of Past Climate, Climate Projections, and Ecosystem Implications|date=January 2012|publisher=U.S. Forest Service|url=http://www.fs.fed.us/rm/pubs/rmrs_gtr264.pdf|format=pdf|pages=24–25|accessdate=January 11, 2014}}</ref> |
||
Reversing the growth that occurred during the [[Little Ice Age]] (1350–1850), there has been a [[Retreat of glaciers since 1850|reduction of mountain glacial ice]] |
Reversing the growth of mid-latitude glaciers that occurred during the [[Little Ice Age]] (1350–1850), there has been a [[Retreat of glaciers since 1850|world-wide reduction of mountain glacial ice]] since, with some regions losing as much as 50 percent of their peak ice cover. This can be correlated by examining [[photography|photographic]] evidence of glaciers taken over time even with an absence of other means of documentation.<ref name=hall>{{cite journal|last=Hall|first=Myrna|coauthors=Daniel Fagre|title=Modeled Climate-Induced glacier change in Glacier National Park, 1850–2100|volume=53|issue=2|publisher=Bioscience|date=February 2003|url=http://www.nrmsc.usgs.gov/files/norock/products/GCC/Bioscience_Hall_03.pdf|format=pdf|accessdate=January 12, 2014}}</ref> The behavior of the glaciers of Shoshone National Forest is consistent with this pattern. In one study of [[Dinwoody Glacier|Dinwoody]] and [[Gannett Glacier]]s, during the period from 1958-1983, the thickness of these glaciers was reduced {{convert|77|and|61|ft|abbr=on}}, respectively.<ref name=retreat>{{cite web|last=Pochop|first=Larry|coauthors=Richard Marston, Greg Kerr, David Veryzer, Marjorie Varuska and Robert Jacobel|title=Glacial Icemelt in the Wind River Range, Wyoming|work=Water Resources Data System Library|url=http://library.wrds.uwyo.edu/wrp/90-16/90-16.html|date=July 1990|accessdate=January 12, 2014}}</ref> |
||
[[File:Gannet Peak with Gannett Glacier.jpg|thumb|left|Gannett Glacier on the slopes of Gannett Peak]] |
|||
Gannett Glacier, on the northeast slope of Gannett Peak, is the largest single glacier in the U.S. Rocky Mountains. It has reportedly lost over 50 percent of its volume since 1920 with 25 percent of that occurring between the years 1980-1999.<ref name=urbigkit>{{cite news |first=Cat |last=Urbigkit |title=Glaciers shrinking |date=September 1, 2005 |publisher=Sublette Examiner |url=http://www.sublette.com/examiner/v5n23/v5n23s3.htm|accessdate=January 14, 2014}}</ref> [[Upper Fremont Glacier]] has been studied more than any other glacier in the Wind River Range. Scientist have obtained [[ice core]]s from the Upper Fremont Glacier and found that there have been measurable changes in the atmosphere over the past several hundred years.<ref>{{cite web|title=Glacial Ice Cores Reveal a Record of Natural and Anthropogenic Atmosphere Mercury Deposition for the Last 270 Years|url=http://toxics.usgs.gov/pubs/FS-051-02/|publisher=U.S. Geological Survey|date=June 2002|accessdate=January 14, 2014}}</ref> The Upper Fremont Glacier and the [[Quelccaya Ice Cap]] in the [[Andes]] of South America both show nearly identical atmospheric records, which indicate a global linkage of atmospheric conditions over time.<ref>{{cite web|title=Fremont Glacier, Wyoming USA|publisher=National Oceanic and Atmospheric Administration|url=http://www.ncdc.noaa.gov/paleo/icecore/trop/fremont/fremont.html|accessdate=January 15, 2014}}</ref> |
|||
[[File:Gannet Peak with Gannett Glacier.jpg|thumb|left|[[Gannett Glacier]]]] |
|||
The behavior of the glaciers of Shoshone National Forest is consistent with this pattern. The area covered by glaciers shrank by 50% in the century after they were first photographed in the late 1890s. Research between 1950 and 1999 demonstrated that the glaciers shrank by over a third in that period. Research also indicates that the glacial retreat was proportionately greater in the 1990s than in any other decade of the last 100 years.<ref name="retreat">{{cite web |author=Larry Pochop, Richard Marston, Greg Kerr, David Veryzer, Marjorie Varuska and Robert Jacobel |title=Glacial Icemelt in the Wind River Range, Wyoming |work=Water Resources Data System Library |url=http://library.wrds.uwyo.edu/wrp/90-16/90-16.html |accessdate=2006-10-15}}</ref> [[Gannett Glacier]], on the northeast slope of Gannett Peak, is the largest single glacier in the U.S. Rocky Mountains. It has reportedly lost over 50% of its volume since 1920 with 25% of that loss since 1980.<ref name="retreating">{{cite news |first=Cat |last=Urbigkit |title=Glaciers shrinking |date=September 1, 2005 |publisher=Sublette Examiner |url=http://www.sublette.com/examiner/v5n23/v5n23s3.htm}}</ref> [[Upper Fremont Glacier]] has been studied more than any other in the Wind River Range. Scientist have obtained [[ice core]]s from the Fremont Glacier and found that there have been measurable changes in the atmosphere over the past 500 years.<ref>{{cite web |last=Reddy |first=Michael |url=http://wwwbrr.cr.usgs.gov/projects/SW_corrosion/idahoice/fremont.html |title=Upper Fremont Glacier |work=Aqueous Crystal Growth and Dissolution Kinetics of Earth Surface Materials |publisher=U.S. Geological Survey |accessdate=2007-01-14|archiveurl=http://web.archive.org/web/20070212054127/http://wwwbrr.cr.usgs.gov/projects/SW_corrosion/idahoice/fremont.html |archivedate=February 12, 2007 |deadurl=yes}}</ref><ref>{{cite web |last=Reddy |first=M.M. |coauthors=D.L. Naftz, P.F. Schuster |url=http://wwwbrr.cr.usgs.gov/projects/SW_corrosion/icecore/ |title=Ice-Core Evidence of Rapid Climate Shift during the Termination of the Little Ice Age |publisher=U.S. Geological Survey |accessdate=2007-01-14|archiveurl=http://web.archive.org/web/20051220063700/http://wwwbrr.cr.usgs.gov/projects/SW_corrosion/icecore/ |archivedate=December 20, 2005}}</ref> |
|||
The small glaciers in the forest are less able to resist melting than the great ice sheets of [[Greenland]] and [[Antarctica]]. Once a glacier begins retreating, it may fall into disequilibrium and be unable to find [[glacier mass balance|mass balance]] ([[accumulation zone|accumulation]] versus [[ablation|melting]] rate) at any size. Without a favorable climate change, it will continue to retreat until it disappears.<ref |
The small glaciers in the forest are less able to resist melting than the great ice sheets of [[Greenland]] and [[Antarctica]]. Once a glacier begins retreating, it may fall into disequilibrium and be unable to find [[glacier mass balance|mass balance]] ([[accumulation zone|accumulation]] versus [[ablation|melting]] rate) at any size. Without a favorable climate change, it will continue to retreat until it disappears.<ref>{{cite web |last=Pelto|first=Mauri|title=The Disequilbrium of North Cascade, Washington Glaciers 1984–2004 |url=http://www.nichols.edu/departments/glacier/diseqilibrium.html |accessdate=January 15, 2014}}</ref> Loss of glacial ice already reduces the summer glacial runoff that supplies water to streams and lakes and provides a cold-water source vital to certain fish and plant species. This, in turn, may have a significant impact on the forest ecosystem over time.<ref name=state/> |
||
== Climate == |
== Climate == |
||
Wyoming is an arid state, averaging {{convert|12.68|in|cm}} of precipitation annually.<ref>{{cite web|title=Precipitation|work=The National Atlas of the United States of America|publisher=U.S. Department of the Interior|url=http://www.nationalatlas.gov/printable/images/pdf/precip/pageprecip_wy3.pdf|format=pdf|accessdate=January 4, 2014}}</ref> However, Shoshone National Forest is located in and near some of the largest mountain ranges in the state, and consequently receives anywhere between {{convert|15|and|70|in|abbr=on}} annually.<ref name=fmp1/> Higher elevations in the forest not only get more precipitation than lower elevations, but also have lower overall temperatures, with summertime highs around {{convert|60|°F|°C}} and lows near {{convert|35|°F|°C|abbr=on}} while lower elevations may be {{convert|20|°F|°C|abbr=on}} or more warmer on average.<ref name=fmp1/> Humidity levels throughout the forest are low, especially at higher altitudes. In the middle of the forest at the Wapiti Ranger Station, which is {{convert|30|mi|abbr=on}} west of the forest headquarters in Cody, Wyoming, January high and low temperatures are {{convert|35.8|and|13.2|°F|°C|abbr=on}}, while the July highs and lows are {{convert|81.4|and|49.1|°F|°C|abbr=on}}. The annual precipitation at Wapiti is {{convert|10.37|in|abbr=on}}.<ref name=nws>{{cite web|title=Monthly Station Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1971 - 2000|work=Wyoming|publisher=National Oceanic and Atmospheric Administration (NOAA)|url=http://cdo.ncdc.noaa.gov/climatenormals/clim81/WYnorm.pdf|format=pdf|date=February 2002|accessdate=January 4, 2014}}</ref> |
|||
Most of the precipitation falls in the winter and early spring, while summer is punctuated with widely scattered thunderstorms.<ref name=fmp1/> The autumn is usually cool and dry. Due to the altitude and dryness of the atmosphere, vigorous radiative cooling occurs throughout the year, and exceptional daily temperature variances are not uncommon.<ref>{{cite web|title=Temperature|publisher=Wyoming State Climate Office|url=http://www.wrds.uwyo.edu/sco/climateatlas/temperature.html|accessdate=January 4, 2014}}</ref> Consequently, the nights range from very cool in the summer to [[polar climate|extremely cold]] in the winter; therefore, visitors should always remember to bring along at least a jacket, even during the summer.<ref>{{cite web|title=Weather Climate|publisher=Wyoming Office of Tourism|url=http://www.wyomingtourism.org/overview/Weather-Climate/43666|accessdate=January 4, 2014}}</ref> Records indicate that the highest temperature ever recorded in the forest was {{convert|100|°F|°C|abbr=on}} in 1978, while the coldest was {{convert|-49|°F|°C|abbr=on}} in 1972.<ref>{{cite web|title=Monthly Averages for Wind River Ranger District - Shoshone NF|publisher=The Weather Channel|url=http://www.weather.com/weather/wxclimatology/monthly/graph/021405:13|accessdate=January 4, 2014}}</ref> |
|||
== Recreation == |
== Recreation == |
||
Shoshone National Forest receives an average of over half a million visitors a year.<ref name=visits/> Two visitor centers provide orientation, books, maps, and interpretive displays. One visitor center is at the Wapiti Wayside on the [[Buffalo Bill Cody Scenic Byway]], west of Cody, Wyoming and adjacent to the historic Wapiti Ranger Station while the other visitor center is to the south in Lander, Wyoming.<ref name=vg/> There are 30 vehicle access [[campground]]s in the forest, with up to 54 individual sites per campground. Approximately half of these campgrounds provide running water and restroom facilities and also provide for handicapped accessibility.<ref name=vg/><ref name=camp>{{cite web|title=Camping and Cabins|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/detail/shoshone/passes-permits/?cid=stelprdb5189083|accessdate=January 5, 2014}}</ref> Referred to as "front country" campgrounds, they also permit [[recreational vehicle]] access in most cases. All of the campgrounds are on a first come, first served basis although four campgrounds have sites that can be reserved in advance by contacting the National Reservation Service.<ref name=vg/><ref name=camp/> Due to the presence of grizzly bears, a few of the campgrounds require what is referred to as "hard-sided" camping only, and tent camping is not permitted.<ref name=vg/> |
|||
Shoshone National Forest receives an average of over half a million visitors a year.<ref name="visitation">{{cite web |
|||
[[File:Horseback riding Shoshone National Forest.jpg|thumb|right|Horseback riding in Greybull Ranger District]] |
|||
| author=U.S. Forest Service, U.S. Department of Agriculture| title=Planning Revision|url=http://www.fs.fed.us/r2/shoshone/projects/planning/revision/comments_requested/2005_12_draft_vision_niche.pdf| accessdate=2006-10-15|format=PDF}}</ref> Two visitor centers provide orientation, books, maps, and interpretive displays and are staffed by either forest service interpreters or volunteers. The Wapiti Wayside is on the [[Buffalo Bill Cody Scenic Byway]], west of [[Cody, Wyoming]] adjacent to the historic Wapiti Ranger Station; another visitor center is to the south in [[Lander, Wyoming]]. There are 30 vehicle access [[campground]]s in the forest, with up to 27 individual sites each. Approximately half of these campgrounds provide running water and restroom facilities and also provide for handicapped accessibility. Referred to as "front country" campgrounds, they also permit [[recreational vehicle]] access in most cases. All of the campgrounds are on a first come, first served basis except for the Rex Hale campground, which is on the National Recreation Reservation Service; a phone and web-based system that permits campsite reservation months ahead of time. Due to the presence of grizzly bears, some of the campgrounds require what is referred to as "hard-sided" camping only, and tent camping is not permitted. |
|||
For some visitors the greater solitude of the backcountry requires using [[Trail|hiking trails]] to [[backpacking (wilderness)|backpacking]] or horseback riding into more remote destinations. There are dozens of trails which total over {{convert|1600|mi|abbr=on}} located throughout the forest.<ref name=vg/> Many of the trailheads can be accessed at campgrounds, with shorter day hikes available as well.<ref name=dayhike>{{cite web|title=Day Hiking|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/activity/shoshone/recreation/hiking/?recid=35807&actid=50|accessdate=January 5, 2014}}</ref> The [[Continental Divide Trail]] has a {{convert|20|mi|adj=on}} section which passes through the forest and crosses the Continental Divide at Sheridan Pass.<ref name=cdt>{{cite web|title=Wyoming Access Points|publisher=Continental Divide Trail Coalition|url=http://www.continentaldividetrail.org/about-the-trail/wyoming-cdt/wyoming-access-points/|accessdate=January 5, 2014}}</ref> There is also the [[Nez Perce National Historic Trail]] and the Beartooth Loop National Recreation Trail, both of which are in the northern regions of the forest.<ref name=nezperce>{{cite web|title=Nez Perce National Historic Trail (NPNHT) FACTS|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5251775.pdf|format=pdf|accessdate=January 5, 2014}}</ref><ref>{{cite web|title=Beartooth loop|publisher=The National Recreation Trails Program|url=http://www.americantrails.org/NRTDatabase/trailDetail.php?recordID=2313|accessdate=January 5, 2014}}</ref> Some remote areas can also be accessed by horseback. Trailheads usually provide enough room for horse and pack animal trailers plus personal vehicles.<ref name=vg/> Along forest access roads, [[all-terrain vehicle]]s (ATV) are allowed, but since wilderness areas do not permit access by way of motorized transport, those who wish to visit such areas usually do so either by hiking in or on horseback.<ref>{{cite web|title=Motor Vehicle Use Map|publisher=U.S. Forest Service|url=http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5351442.pdf|format=pdf|date=2012|accessdate=January 8, 2014}}</ref><ref>{{cite web|title=Washakie Wilderness Fact Sheet|publisher=Wilderness.net|url=http://www.wilderness.net/printFactSheet.cfm?WID=632|accessdate=January 8, 2014}}</ref> |
|||
[[File:Pingora Peak and Lonesome Lake.jpg|thumb|left|[[Pingora Peak]] rises above Lonesome Lake in the Popo Agie Wilderness. Pingora is one of many peaks located in the [[Cirque of the Towers]].]] |
|||
[[File:Horseback riding Shoshone National Forest.jpg|thumb|left|Horseback riding in Greybull Ranger District]] |
|||
Hunting and fishing are popular recreational activities permitted throughout the forest. Many of the streams and rivers are considered to be "Blue Ribbon Trout Streams".<ref name=retallic>{{cite book|last=Retallic|first=Ken|title=Flyfisher's Guide to Wyoming: Including Grand Teton and Yellowstone National Parks|publisher=Wilderness Adventures Press|isbn=978-1932098105 |
|||
For some visitors the greater solitude of the "backcountry" requires accessing [[hiking|hiking trails]] and then [[backpacking (wilderness)|backpacking]] or [[equestrianism|horseback riding]] into more remote destinations. There are dozens of trails which total over {{convert|1500|mi}} spread throughout the forest. The [[Continental Divide Trail]] weaves its way through the forest, though it follows alternatively named trails for some of the distance.<ref name="trail">{{cite web |author=Continental Divide trail Alliance |title=Continental Divide National Scenic trail |url=http://www.cdtrail.org/site/static/wymap.html |accessdate=2007-01-14}}</ref> There is also the [[Nez Perce National Historic Trail]] and the Beartooth Loop National Recreation Trail, both of which are in the northern regions of the forest. Some remote areas can be accessed by horseback. Trailheads usually provide enough room for horse and pack animal trailers plus personal vehicles. Along forest access roads, [[all-terrain vehicle]]s are allowed, however there are plans to limit their use in most of the forest. |
|||
|pages=141–172|date=February 1, 2012|accessdate=January 8, 2014}}</ref> Though many streams and lakes have excellent opportunities to catch various species of trout, the north and south forks of the Shoshone River, the Greybull River and the Clark's Fork of the Yellowstone, the only federally designated [[Wild and Scenic River]] in Wyoming, are a few of the better locations to reign in a trophy level Rainbow or Yellowstone cutthroat trout.<ref name=retallic/> {{convert|1000|mi}} of streams and a hundred lakes that can be legally fished from provide plenty of elbow room during even the most crowded of fishing seasons. Hunting and fishing licenses are sponsored by the state of Wyoming and are available through the Wyoming Game and Fish Department.<ref>{{cite web|title=Wyoming Game and Fish Department Regulations|publisher=Wyoming Game and Fish Department|url=http://wgfd.wyo.gov/web2011/hunting-1000179.aspx|accessdate=January 8, 2014}}</ref> |
|||
[[Hunting]] and [[fishing]] are popular recreational activities permitted throughout the forest, provided that proper permits are obtained and the applicable rules and regulations are followed. Hunting regulations are altered each year to ensure certain species are protected from overhunting and to maximize personal safety. Many of the streams and rivers are considered to be "Blue Ribbon Trout Streams". {{convert|1700|mi}} of streams and 500 lakes that can be legally fished from, provide plenty of elbow room during even the most crowded of fishing seasons. Hunting and fishing licenses are sponsored by the state of Wyoming and are available through the Wyoming Game and Fish Department.<ref name="hunting">{{cite web |url=http://gf.state.wy.us/ |title=Wyoming Game and Fish Department |accessdate=2011-08-27}}</ref> |
|||
The southern section of the forest in the Wind River Range is the primary destination for [[mountaineering|mountain climbers]]. Nine of the highest 10 peaks in Wyoming are here, and the mountains are primarily of granitic rock with countless cliffs and sheer rock walls. The Cirque of the Towers is particularly popular as it has numerous peaks within a relatively short distance of each other. |
The southern section of the forest in the Wind River Range is the primary destination for [[mountaineering|mountain climbers]]. Nine of the highest 10 peaks in Wyoming are here, and the mountains are primarily of granitic rock with countless cliffs and sheer rock walls.<ref>{{cite peakbagger|lid=21344|title=Wyoming 13,000-foot Peaks|accessdate=January 11, 2014}}</ref> The Cirque of the Towers is particularly popular as it has numerous peaks within a relatively short distance of each other. Two particular climbs on the peaks in the cirque are considered amongst the finest climbing adventures available in the U.S.<ref>{{Fifty Classic Climbs|pages=171–183}}</ref> The Absaroka Range also attracts climbers but not of a technical nature since the rocks are not considered solid enough for good anchoring points.<ref>{{cite web|title=Francs Peak|publisher=Summitpost|url=http://www.summitpost.org/francs-peak/153323|accessdate=January 11, 2014}}</ref> For the tallest peaks in the Wind River Range, the entire summiting effort will take even experienced climbers many days due to the inaccessibility of the region and complexity of the climbing effort.<ref>{{cite book|last=Hunger|first=Bill|title=Wyoming: 110 of the State's Best Hiking Adventures|publisher=Falcon Guides|url=http://books.google.com/?id=Kznlx1YNZzwC&pg=PA151&dq=gannett+peak+wyoming+difficult#v=onepage&q=gannett%20peak%20wyoming%20difficult&f=false|date=June 3, 2008|page=151|isbn=978-0762734207|accessdate=January 11, 2014}}</ref> |
||
Winter activities include [[cross-country skiing]] and [[snowmobiling]], with {{convert|48|mi|abbr=on}} of groomed trails for cross-country skiing and over {{convert|300|mi|abbr=on}} for use by snowmobilers.<ref name=snow>{{cite web|title=Shoshone National Forest|publisher=Wyoming Office of Tourism|url=http://www.wyomingtourism.org/thingstodo/detail/Shoshone-National-Forest/4220|accessdate=January 11, 2014}}</ref> The region around Togwotee Pass allows snowmobilers easy access from paved roads and has snow depths of between {{convert|6|to|10|ft|abbr=on}} annually at elevations of {{convert|8000|to|10000|ft|abbr=on}}, which equates to a long season for winter activities.<ref>{{cite web|title=Continental Divide|publisher=Wyoming State Trails Program|url=http://wyotrails.state.wy.us/pdf/continentaldivide.pdf|format=pdf|date=2013|accessdate=January 11, 2014}}</ref> |
|||
Winter activities include [[cross-country skiing]] and [[snowmobiling]]. The Continental Divide Snowmobile Trail is a popular maintained snowmobile route that can be accessed from Togwotee Pass. With up to {{convert|40|ft}} of snow annually in the higher elevations, the snowmobile season extends usually from the beginning of December to the middle of April. [[Lander, Wyoming|Lander]], [[Cody, Wyoming|Cody]] and the area near Togwotee Pass are the hubs of snowmobile activity in the forest. Numerous outfitters rent snowmobiles on a daily basis and can provide guided trips for those less experienced, and a number of motels also remain open during the winter to provide food and lodging. Snowmobile activity has increased in the forest with increased restrictions on their use within Yellowstone National Park. |
|||
=== Scenic roads === |
=== Scenic roads === |
||
[[File:Sunlight bridge.jpg|thumb|Sunlight Bridge on the [[Chief Joseph Scenic Byway]]]] |
[[File:Sunlight bridge.jpg|thumb|Sunlight Bridge on the [[Chief Joseph Scenic Byway]]]] |
||
Shoshone National Forest forms the eastern boundary of Yellowstone National Park and the northeastern and eastern entrances to the park are both accessed by way of designated scenic roadways. A federally designated [[National Scenic Byways]] [[All-American Road]], the Beartooth Highway (U.S. Highway 212), weaves through the forest and serves as the northeastern entranceway to Yellowstone National Park.<ref>{{cite web|title=A Wild Road – The Beartooth Highway|publisher=Friends of the Beartooth|url=http://beartoothhighway.com/wild-beartooth/|accessdate=January 4, 2014}}</ref><ref name=beartooth>{{cite web|title=Beartooth Highway|publisher=Federal Higway Administration|url=http://www.fhwa.dot.gov/byways/byways/2281|accessdate=January 4, 2014}}</ref> [[Chief Joseph Scenic Byway]] ([[Wyoming Highway 296]]) connects Cody, Wyoming with the Beartooth Highway and follows the old trail in which [[Chief Joseph]] and the [[Nez Perce tribe]] attempted to flee the U.S. Cavalry in 1877.<ref>{{cite web|title=Chief Joseph Scenic Byway|publisher=Wyoming Office of Tourism|url=http://www.wyomingtourism.org/thingstodo/detail/Chief-Joseph-Scenic-Byway/2721|accessdate=January 4, 2014}}</ref> South of there, Buffalo Bill Cody Scenic Byway (US 14/16/20) heads west from Cody, Wyoming, passes through the forest and crosses Sylvan Pass as it enters Yellowstone.<ref>{{cite web|title=Buffalo Bill Cody Scenic Byway|publisher=Wyoming Office of Tourism|url=http://www.wyomingtourism.org/thingstodo/detail/Buffalo-Bill-Cody-Scenic-Byway/2577|accessdate=January 4, 2014}}</ref> Lastly, the [[Wyoming Centennial Scenic Byway]] (US 26/287) heads northwest from Dubois, Wyoming, over Togwotee Pass and enters Jackson Hole and Grand Teton National Park.<ref name=windriver/> Though the Beartooth Highway is the only one of these four roads that is a National Scenic Byway, all four of them have been designated Wyoming State Scenic Byways by the state of Wyoming.<ref>{{cite web|title=Scenic Byways and Backways|publisher=Wyoming Office of Tourism|url=http://www.wyomingtourism.org/thingstodo/overview/Scenic-Byways-and-Backways/1774|accessdate=Jauuary 4, 2014}}</ref> |
|||
[[Wyoming State Scenic Byway]]s.<ref name="byways">{{cite web |author=Federal Highway Administration, U.S. Department of Transportation |title=Explore Wyoming |work=America's Byways |url=http://www.byways.org/browse/states/WY/ |accessdate=2008-05-17}}</ref> |
|||
== References == |
== References == |
||
=== Cited references === |
|||
{{Reflist|colwidth=30em}} |
|||
=== General references === |
|||
{{refbegin}} |
|||
* {{cite web |
|||
| author=National Interagency Fire Center |
|||
| title=Links to wildland fire information |
|||
| work= |
|||
| url=http://www.nifc.gov/ |
|||
| accessdate=February 16, 2006}} |
|||
* {{cite web |
|||
| author=National Fire Plan |
|||
| title=What is the National Fire Plan |
|||
| url=http://www.fs.fed.us/r1/pgr/afterfire/nfp.html |
|||
| accessdate=August 27, 2011}} |
|||
* {{cite web |
|||
| author=Wyoming Game and Fish |
|||
| title=Official State List of Birds, Mammals, Amphibians, and Reptiles in Wyoming |
|||
| work=Wyoming Game & Fish Species List |
|||
| url=http://gf.state.wy.us/wildlife/nongame/SpeciesList/index.asp |
|||
| accessdate=February 16, 2006}} |
|||
{{refend}} |
|||
== Additional reading == |
|||
{{Commons}} |
{{Commons}} |
||
{{ |
{{Reflist}} |
||
* {{cite book |author=William J. Fritz |title=Roadside Geology of the Yellowstone Country |publisher=Mountain Press Publishing Company, Missoula |year=1985 |editor=|isbn=0-87842-170-X}} |
|||
* {{cite book |author=John O. Whitaker, National Audubon Society Staff |title=National Audubon Society Field Guide to North American Mammals |publisher=Knopf Publishing Group, New York, NY |year=1996 |editor=|isbn=0-679-44631-1}} |
|||
* {{cite book |author=Elbert L. Little |title=National Audubon Society Field Guide to North American Trees: Western Edition |publisher=Knopf Publishing Group, New York, NY |year=1980 |editor=|isbn=0-394-50761-4}} |
|||
* {{cite book |author=Robert Marshall M. Utley |title=After Lewis and Clark: Mountain Men and the Paths to the Pacific |publisher=Bison Books, Univ. of Nebraska Press, Lincoln, NE |year=2004 |editor=|isbn=0-8032-9564-2}} |
|||
* {{cite book |author=Rebecca Woods |title=Walking the Winds: A Hiking and Fishing Guide to Wyoming's Wind River Range |publisher=White Willow Publishing, Jackson WY |year=1994 |editor=|isbn=0-9642423-0-3}} |
|||
{{refend}} |
|||
[[Category:1891 establishments]] |
[[Category:1891 establishments in Wyoming]] |
||
[[Category:Greater Yellowstone Ecosystem]] |
[[Category:Greater Yellowstone Ecosystem]] |
||
[[Category:Landmarks in Wyoming]] |
[[Category:Landmarks in Wyoming]] |
||
Line 188: | Line 159: | ||
{{Link FA|fr}} |
{{Link FA|fr}} |
||
{{Link FA|pt}} |
{{Link FA|pt}} |
||
[[es:Bosque nacional Shoshone]] |
Revision as of 14:27, 4 March 2014
Shoshone National Forest | |
---|---|
IUCN category VI (protected area with sustainable use of natural resources) | |
Lua error in Module:Location_map at line 526: Unable to find the specified location map definition: "Module:Location map/data/USA relief" does not exist. | |
Location | Park, Fremont, Hot Springs, Sublette, and Teton counties, Wyoming, USA |
Nearest city | Cody, WY |
Area | 2,466,909 acres (998,323 ha)[1] |
Established | March 3, 1891 |
Visitors | 646,000[2] (in 2009) |
Governing body | U.S. Forest Service |
www |
Shoshone National Forest (/ʃoʊˈʃoʊniː/ shoh-SHOH-nee)[4] is the first federally protected National Forest in the United States and covers nearly 2,500,000 acres (1,000,000 ha) in the state of Wyoming.[5] Originally a part of the Yellowstone Timberland Reserve, the forest is managed by the United States Forest Service and was created by an act of Congress and signed into law by U.S. President Benjamin Harrison in 1891. Shoshone National Forest is one of the first nationally protected land areas anywhere. Native Americans have lived in the region for at least 10,000 years, and when the region was first explored by white adventurers, forestlands were occupied by several different tribes. Never heavily settled or exploited, the forest has retained most of its wildness. Shoshone National Forest is a part of the Greater Yellowstone Ecosystem, a nearly unbroken expanse of federally protected lands encompassing an estimated 20,000,000 acres (8,100,000 ha).
The Absaroka and Beartooth Mountains are partly in the northern section of the forest. The Wind River Range is in the southern portion and contains Gannett Peak, the tallest mountain in Wyoming.[5] Yellowstone National Park forms part of the boundary to the west; south of Yellowstone, the Continental Divide separates the forest from its neighbor Bridger-Teton National Forest to the west. The eastern boundary includes privately owned property, lands managed by the U.S. Bureau of Land Management and the Wind River Indian Reservation, which belongs to the Shoshone and Arapahoe Indians. Custer National Forest along the Montana border is on the northern frontier. The Oregon Trail, the 19th century covered wagon route, passes just south of the forest, where broad and gentle South Pass allowed the migrants to bypass the rugged mountains to the north.
Shoshone National Forest has virtually all the original animal and plant species that were there when white explorers such as John Colter and Jim Bridger first visited the region. The forest is home to the Grizzly bear, cougar, moose, tens of thousands of elk as well as the largest herd of bighorn sheep in the U.S. The streams in the forest are considered to have some of the best game species fishing opportunities in the U.S. and one of the few places where one can catch Yellowstone cutthroat trout. More than 1,300 miles of hiking trails, 32 campgrounds and adjacent forests and parklands provide numerous recreational opportunities. There are four wilderness areas within the forest, protecting more than half of the managed land area from development. From sagebrush plains through dense spruce and fir forest to craggy mountain peaks, Shoshone National Forest has a rich biodiversity rarely matched in any protected area.
Human history
Shoshone National Forest is named after the Shoshone Indians, who, along with other Native American groups such as the Lakota, Crow and Northern Cheyenne, were the major tribes encountered by the first white explorers into the region. Archeological evidence suggests that the presence of Indian tribes in the area extends back at least 10,000 years.[6] The forest provided an abundance of game meat, wood products, and shelter during the winter months from the more exposed high plains to the east. Portions of the more mountainous regions were frequented by the Shoshone and Sioux for spiritual healing and vision quests. By early 1840s, Washakie had become the leader of the easternmost branch of the Shoshone Indians.[7] At the Fort Bridger Treaty Council of 1868 Washakie negotiated with the U.S. Government for 44,000,000 acres (18,000,000 ha)) to be preserved as tribal lands. Subsequent amendments to the treaty reduced the actual acreage to approximately 2,000,000 acres (810,000 ha) and is known today as the Wind River Indian Reservation.[8][9]
In 1957, Mummy Cave was rediscovered by a local resident on the north side of the North Fork Shoshone River, adjacent to U.S. Routes 14/16/20, 15 mi (24 km) east of Yellowstone National Park.[10] Subsequent archeological excavations in the 1960s produced evidence that the cave had been occupied for over 9,000 years.[11] The oldest deposits in the cave yielded prismatic stone blades and other artifacts created by paleoindians and the surrounding soils were radiocarbon dated to 7,300 BC. The evidence indicates the cave was occupied from at least 7280 BC to 1580 AD.[10] Besides projectile points, the cave also produced well preserved feathers, animal hides and other usually perishable materials. Additionally, the mummified remains of an individual buried inside a rock cairn were unearthed, which were dated to 800 AD.[11] Considered one of the finest paleoindian archeological assemblages in the Rocky Mountain region, the site was placed on the National Register of Historic Places list in 1981.[12]
In the early 19th century, the forest was visited by mountain men and explorers such as John Colter and Jim Bridger. Colter is the first white man known to have visited both the Yellowstone region and the forest, which he did between 1807 and 1808.[13] Having been an original member of the Lewis and Clark Expedition, Colter requested permission from Meriwether Lewis to leave the expedition after it had finished crossing the Rocky Mountains during their return journey from the Pacific Ocean. Colter teamed up with two unaffiliated explorers the expedition had encountered, but soon thereafter decided to explore regions south of where his new partners wished to venture.[13] Traveling first into the northeastern region of what is today Yellowstone National Park, Colter then explored the Absaroka Mountains, crossing over Togwotee Pass and entering the valley known today as Jackson Hole.[14] Colter survived a grizzly bear attack and a pursuit by a band of Blackfeet Indians who had taken his horse.[13] The explorer later provided William Clark, who had been his commander on the Lewis and Clark Expedition, with previously unknown information on the regions he had explored, which Clark published in 1814.[15]
Travels by fur trappers and adventurers, such as Manuel Lisa and Jim Bridger from 1807 to 1840, completed the exploration of the region. With the decline of the fur trade in the late 1840s and much of the prized beaver long since made scarce by over-trapping, few white explorers entered the forest over the next few decades.[14] The first federally financed expedition which passed through portions of Shoshone National Forest was the Raynolds Expedition of 1860, led by topographical engineer Captain William F. Raynolds.[16] The expedition included geologist and naturalist Ferdinand Vandeveer Hayden and was guided by mountain man Jim Bridger. Though the Raynolds Expedition was focused on exploration of the Yellowstone region, several efforts to enter what later became Yellowstone National Park were impeded by heavy snows across the mountain passes such as Two Ocean Pass. The expedition finally crossed the northern Wind River Range at a pass they named Union Pass and entered Jackson Hole valley to the south of Yellowstone.[16] Hayden led another expedition through the region in 1871. Hayden was primarily interested in documenting the Yellowstone country west of the forest, but his expedition also established that the forest was a prime resource that merited protection. Travels in the forest in the 1880s by later U.S. President Theodore Roosevelt, who was also a strong advocate of land conservation, as well as by General Philip Sheridan, provided the impetus that subsequently established the Yellowstone Timberland Reserve in 1891, creating the first national forest in the U.S.[5][17]
In 1902, President Roosevelt first greatly expanded the reserve and then divided the reserve into four separate units, with Shoshone being the largest. Upon the creation of the U.S. Forest Service in 1905, the reserve was designated a National Forest, but the current wording and title were formulated forty years later in 1945. A remnant of the earliest years of the forest management is the Wapiti Ranger Station which is located west of Cody, Wyoming. The station was built in 1903 and is the oldest surviving ranger station in any national forest, and is now designated a National Historic Landmark.[18]
Prior to the establishment of the Wind River Indian Reservation, the U.S. Cavalry constructed Fort Brown on the reservation lands, which was subsequently renamed Fort Washakie.[19] During the late 19th century, the fort was staffed by African-American members of the U.S. Cavalry, better known as the Buffalo Soldiers, including the second African-American graduated from the United States Military Academy, John Hanks Alexander.[20] Chief Washakie is buried at the fort, which is located immediately east of the forest boundary.[19] Rumor has it that Sacajawea, the Shoshone Indian who provided invaluable assistance to Meriwether Lewis and William Clark during the Lewis and Clark Expedition, is also buried here, but it is now considered that this is unlikely and that her actual burial place was Fort Lisa in North Dakota.[21]
During the last decade of the 19th century, minerals such as gold were mined with limited success. The last mine was abandoned in 1907, but panning for gold is still allowed in many areas of the forest, and in most circumstances no permit is required.[22][23] After the end of the mining era, numerous camps were established by the Civilian Conservation Corps to help combat unemployment during the Great Depression of the 1930s. The camps housed groups of unemployed men who were paid by the federal government to build roads, hiking trails, and campgrounds for future travelers to the Yellowstone region.[24] Visitation to national forests like Shoshone increased dramatically after World War II with the advent of better roads and accessibility to the region.[25]
Forest management
Shoshone National Forest is managed by the U.S. Forest Service, an agency within the U.S. Department of Agriculture. The forest is separated into five districts and from 2008 and 2012 had an average staff of 165 employees and an annual operating budget of $17,500,000.[26] The headquarters and a visitor center are in Cody, Wyoming and a smaller information center is in Lander, Wyoming. There are local ranger district offices in Cody, Dubois and Lander.[27]
Shoshone National Forest practices conservation of resources, which ensures a sustainable flow of some raw materials from the forest, such as lumber for construction purposes and wood pulp for paper products.[28] The forest averages an annual harvest of 4.5 million board-feet of timber for the purposes of commercial log home construction and another 2.5 million board-feet of wood collection from dead and down trees that are used for firewood and poles.[29] Additionally, low-scale mineral extraction and oil and gas exploration and recovery are also conducted, though in Shoshone National Forest this has become less common due to a consensus to protect the natural surroundings. Only 8,570 acres (3,470 ha) of oil and gas leases were filed as of 2013.[30] More common than logging and mining are the lease options that are offered to ranchers to allow them to graze cattle and sheep.[31] The U.S. Forest Service provides guidelines and enforces environmental regulations to ensure that resources are not overexploited and that necessary commodities are available for future generations, though conservation groups have voiced concerns over the management practices of the leasing program and especially cattle overgrazing problems.[32] Leases for sheep grazing have declined considerably since the 1940s while cattle grazing has remained relatively constant.[33]
Natural resources
Flora
Shoshone National Forest is an integral part of the Greater Yellowstone Ecosystem, which has 1,700 documented species of plants.[34] Since the elevation of the land in the forest ranges from 4,600 to 13,804 ft (1,402 to 4,207 m), which is more than 9,000 ft (2,700 m), the forest has a wide variety of ecosystems.[35][36] Lower elevations often have sagebrush and grass-dominated vegetation types, while forested areas are dominated by various combinations of tree and shrub species. These include lodgepole pine, which along with Rocky Mountain juniper, and quaking aspen are found at elevations up to 9,000 ft (2,700 m).[36] At higher elevations subalpine fir, Engelmann spruce, whitebark pine and limber pine, are common, each occurring up to timberline.[36] The region above timberline makes up 25 percent of the total acreage of the forest and of that 13 percent is listed as just either barren, rock or ice.[37] The types of plant species is highly dependent on the amount of water available, and trees are more commonly found on higher slopes due to the longer lasting snowfall which keeps the soil moister for a longer time into the summer months. Along lower elevation riparian corridors, cottonwoods and willows are typically dominant. Numerous plant species are endemic to the region including some that are rare. Among them, the whitlow grass, fremont bladderpod, shoshonea, and the north fork Easter daisy provide vivid white and yellow flowers during the spring and summer.[38]
Exotic species of flora that are not native to the region include Canada thistle, Musk thistle, Spotted knapweed, Leafy spurge and Yellow toadflax.[39] These non-native plant species are considered noxious, impacting native plant communities and the species that thrive on them.[39] Native species such as the Mountain pine beetle are having an enormous negative impact on some tree species.[40] A survey of the forest performed in 2010 indicated that over 1,000,000 acres (400,000 ha) of timberland had been impacted by insects such as the Mountain pine beetle, spruce bark beetle and Douglas fir beetle, and that the insects had killed between 25 and 100 percent of the trees in the impacted areas.[41] The forest service is addressing the situation by performing controlled burns, selling dead trees as firewood, timber harvesting and spraying the highest value areas.[40]
Fauna
Since the migration of the endangered gray wolf into Shoshone National Forest after the successful wolf reintroduction program in the Yellowstone region commenced in the mid-1990s, all of the known 70 mammal species that existed prior to white settlement still exist in the forest.[36] Altogether, at least 335 species of wildlife call Shoshone National Forest their home, including the largest population of Bighorn sheep and one of the few locations Grizzly bears can still be found in the contiguous U. S..[37]
At least 700 grizzly bears are believed to exist in the Greater Yellowstone Ecosystem, which includes Shoshone National Forest, with approximately 125 grizzlies in the forest.[36][42] The grizzly is listed as a threatened species by the U.S. Fish and Wildlife Service, and the forest is one of their last strongholds. For what are considered to be "nuisance bears", non-lethal traps are set to capture them so that they can be relocated to remote areas, away from civilization.[43] In the case of the grizzly, each captured bear is tranquilized and then ear tagged with an identifying number. Each number is registered, and if the bear continues to return to areas where they pose a risk of imminent threat to human safety, they are exterminated.[43] The grizzly recovery efforts implemented by federal agencies have often resulted in major disagreements with local landowners and surrounding municipalities.[42] This situation occurs less frequently with the smaller and less aggressive black bear. An active management program, in conjunction with other National Forests and National Parks within the Greater Yellowstone Ecosystem, works cooperatively to maximize human safety and to ensure habitat protection for both species of endemic bears. Visitors are mandated to store their food in their vehicles or in steel containers found in campgrounds, and bear-proof trash receptacles are located in the front-country zones throughout the forest. In the backcountry, food must be stored some distance from campsites, and other related precautions are enforced to help prevent bad encounters.[37]
The cougar (mountain lion) and the gray wolf are large apex predators that inhabit the forest. Since the 1990s wolf reintroduction program in Yellowstone National Park, wolves have migrated into the forest and established permanent packs.[44] Approximately a dozen wolf packs totaling 70 individual wolves were documented in the forest in 2012.[45] The wolf was delisted as endangered once their population levels had reached management objectives and limited hunting of wolves was permitted in the forest starting in 2012.[46][47] Cougars are generally noctural and rarely seen but hunting of this species is also allowed in highly regulated harvests.[48] Wolverines are rare and elusive so documentation is oftentimes only from their tracks.[49] The Canada lynx was native to the forest, but no known populations may still exist due to the rarity of its primary food source, the Snowshoe hare. Shoshone National Forest is considered critical habitat for lynx recovery since the species is listed as threatened under the Endangered Species Act and the forest is in their historical range.[50] Other generally carnivorous mammals include coyote, bobcat, weasel, marten, ferret and badger.[51]
Omnivorous mammals such as the raccoon and skunk and herbivore mammal species such as the porcupine and pika, are common to the forest.[51][52] The beaver is considered a species of special interest to Shoshone National Forest since its dam building activities improve habitat for numerous other species such as the moose, breeding waterfowl, various amphibians and other species dependent on a riparian environment.[53]
Native herbivores such as the moose are found in small numbers near waterways, especially at lower elevations. Moose populations in northwestern Wyoming and other areas of North America have been on the decline since the end of the 20th century, possibly due to a parasite.[54] There were an estimated 739 moose in the forest in 2006 which is almost 300 fewer than there were 20 years earlier.[53][55] Other ungulate species are much more common and there are over 20,000 elk (also known as wapiti) and 40,000 mule deer.[55] Bighorn sheep and mountain goats inhabit the rocky terrain and highest elevations. During the winter, one of the largest bighorn sheep herds in the lower 48 states congregate in the region around Dubois, Wyoming; however, their numbers since 1990 have been diminished due to disease transmitted from contact with domesticated sheep and goats.[56] An estimated 5,000 bighorn sheep are found throughout the forest and a small but stable population of 200 mountain goats reside in the northernmost portions of the forest.[55] Bison and pronghorn antelope are two other ungulates that live on the forest and have sustainable populations.[51]
An estimated 300 species of birds are found in the forest at least part of the year. Bald Eagle, Peregrine falcon, Swainson’s hawk and the Prairie falcon are birds of prey that are relatively common.[51] Waterfowl such as Western grebe, Northern pintail, Great blue heron and Barrow’s goldeneye have stable populations and rare sightings of Trumpeter swans are reported.[51] pheasant, ruffed grouse and wild turkey are widely distributed across the open sage lands. Harlequin duck and Northern goshawk are generally rare but management plans were implemented to protect various habitats these two species frequent to try and increase their population numbers.[53]
Fish found in Shoshone National Forest include at least six species and subspecies of trout including Rainbow, Brook and Brown trout. The Yellowstone cutthroat trout is widespread throughout the Greater Yellowstone Ecosystem, but in the forest is mostly limited to the Shoshone River.[57][58] The mountain whitefish is also found in the Shoshone River, while the Burbot is found in two streams in the southern regions of the forest.[57]
There are more than a dozen species of reptiles in the forest including the venomous prairie rattlesnake which can be found at lower elevations.[52] The western painted and the ornate box turtle are turtle species known to exist and about eight species of lizards such as the Greater short-horned lizard have been documented.[52] Amphibians such as the Columbia spotted frog and the boreal toad are considered species of concern because of their high susceptibility to disease, habitat loss and human introduced toxins.[53] Boreal toads are found at elevations of between 7,380 and 11,800 ft (2,250 and 3,600 m) and the Columbia spotted frog can live at elevations as high as 9,480 ft (2,890 m) in the Greater Yellowstone Ecosystem.[53]
Exotic species of fauna such as the Zebra and Quagga mussels and the New Zealand mud snail are invasive species that can greatly impact fish species. Though the mussel species are not known to be in Wyoming, several surrounding regions have reported them. The New Zealand mud snail has been found in the Shoshone River east of the forest. Forest managers have established a preventative program to try and keep these species from entering forest waterways.[59]
Wilderness
The forest contains four areas of pristine wildernesses that have remained largely untouched by human activities such as mining, logging, and road and building construction. The four regions include the North Absaroka, Washakie, Fitzpatrick and Popo Agie Wildernesses.[35] Additionally, a small portion of the Absaroka-Beartooth Wilderness extends into the extreme northwestern part of the forest, along the Montana border. In Shoshone National Forest, 1,400,000 acres (570,000 ha), constituting 56 percent of the forest is designated wilderness.[60][37] The wilderness designation provides a much higher level of land protection and prohibits any alterations by man to the resource.[61]
The Wilderness Act of 1964 enhanced the protection status of remote and/or undeveloped land already contained within federally administered protected areas. Passage of the act ensured that no human improvements would take place aside from those already existing. The protected status in wilderness designated zones prohibits road and building construction, oil and mineral exploration or extraction, and logging, and also prohibits the use of motorized equipment, including even bicycles. The only manner in which people can enter wilderness areas is either on foot or horseback. Hunting and fishing are permitted in the wilderness, just as they are throughout the forest, provided those engaging in such activities have the proper licenses and permits.[62]
Fire ecology
Fire Management officials in Shoshone National Forest recognize that forest fires are a natural part of the ecosystem; however, this was not always the case. 20th century fire fighting efforts, especially in the first half of that century, emphasized quickly extinguishing all fires, as fire was seen as completely detrimental to a forest.[63] In 1935, fire management officials established the 10 am rule for all fires on federal lands, which recommended aggressive attack on fires and to have them controlled by 10 am, the day after they are first detected.[64][65] This was intended to prevent fires from remaining active into the afternoon when the rising temperatures and more turbulent air caused fires to expand and become more erratic.[66] However, this policy led to an increase in fuels because fires were oftentimes extinguished before they had a chance to burn out dead and dying old growth. It was in a stand of old growth fir trees in Shoshone National Forest that the Blackwater fire of 1937 killed 15 fighters during a firestorm 35 mi (56 km) west of Cody, Wyoming. The fire was one of the deadliest in terms of forest firefighter deaths in U.S. history.[67]
Between the years 1970 and 2012, Shoshone National Forest averaged 25 fires annually, of which half were due to natural ignition from lightning, which accounted for 90 percent of the total acreage burned. The remaining acreage that burned was due to campfires that got out of control or from other causes.[68] In Shoshone National Forest, the highest fire incidence is generally in the months of August and September.[68] An average of 2,334 acres (945 ha) burns annually, with the worst year in the past century being 1988, when 194,430 acres (78,680 ha) burned from fires that had spread from the conflagration that engulfed Yellowstone National Park and the surrounding region.[68] After the Yellowstone region fires of 1988, an effort to identify areas of similar fire potential was implemented.[63] Fire managers at Shoshone National Forest work with a number of outside agencies to incorporate fire restrictions, fuels management, and a controlled burn plans to reduce the chances of a catastrophic fire.[69] The dead and dying trees which have been killed by various species of bark beetle may have a great impact on future forest fires.[41] Fire managers have stated the worst time for increased fire activity is 1-2 years after the trees are killed and then again after the trees have fallen many years later.[70]
Geography and geology
Shoshone National Forest borders Yellowstone National Park and Bridger-Teton National Forest to the west. The Continental Divide demarks the boundary between Shoshone and Bridger-Teton National Forests. Along the Montana border, Shoshone National Forest borders Custer National Forest to the north.[68] Private property, property belonging to the state of Wyoming and lands administered by the Bureau of Land Management form the eastern boundaries. Lastly, the Wind River Indian Reservation also borders on the east, and bisects a smaller southern section which includes the Popo Agie Wilderness and the Washakie Ranger District.[71]
The altitude in the forest ranges from 4,600 feet (1,400 m) near Cody, Wyoming, to 13,804 ft (4,207 m) at the top of Gannett Peak, an elevation gain of over 9,200 ft (2,800 m).[68] Of the three major mountain ranges found in the forest, they are geologically distinct from each other. All of the mountains are a part of the Rocky Mountains. In the northern and central portions of the forest lie the Absaroka Mountains which were named after the Crow Indian tribe.[72] The majority of the Absaroka Mountains are contained within the forest, with the highest peak being Francs Peak at 13,158 ft (4,011 m).[73][74] The peaks of the Absaroka are basaltic in origin, having been the result of volcanic activity estimated to have occurred 50 million years ago during the Eocene epoch.[74] The rocks are composed of mostly andesite and breccias deposited for millions of years during volcanic events and are atop more ancient sedimentary rocks that are considered to have economically viable mineral wealth.[74] Gold was mined from the slopes of Francs Peak between the years 1890 and 1915, and the small ghost town of Kirwin remains as a legacy of that period.[22] Major tributaries of the Bighorn River, such as the Shoshone and Greybull Rivers, originate in the Absaroka Mountains. Important passes through the Absarokas include Sylvan Pass, which leads to the eastern entrance of Yellowstone National Park; and Togwotee Pass, which provides access to Jackson Hole and Grand Teton National Park.[75][76]
In the far north of Shoshone National Forest a small portion of the Beartooth Mountains are located north of the Clarks Fork of the Yellowstone River. The Beartooths are composed of Precambrian granitic rocks that are amongst the oldest found on Earth.[77] Although often considered a part of the Absaroka Mountains, the Beartooths are distinct in appearance and geologic history.[72] Uplifted approximately 70 million years ago during the Laramide orogeny, the Beartooths consist of vast windswept plateaus and rugged peaks with sheer cliff faces. The Beartooth Highway (U.S. Highway 212) crosses 10,974-foot (3,340 m) Beartooth Pass, and from there descends to the northeast entrance to Yellowstone National Park.
The Wind River Range is in the southern portion of the forest and is composed primarily of Precambrian granitic rock.[78] Gannett Peak, the tallest mountain in Wyoming, is in the northern part of the range. Altogether eight peaks exceed 13,500 ft (4,100 m) and 119 rise at least 12,000 ft (3,700 m) above sea level.[79] Fremont Peak, the second highest peak in the range, was originally believed to be the tallest mountain in the Rocky Mountains due to its prominence when viewed from the Oregon Trail by early pioneers.[80] The Wind River Range is popular with mountain climbers because of its solid rock and variety of routes.[81] The Cirque of the Towers in the Popo Agie Wilderness is one of the more popular climbing and hiking destinations, and an estimated 200 different climbing routes are located within the peaks that surround the cirque.[80]
There are over 500 lakes in the forest, and 1,000 mi (1,600 km) of streams and rivers.[82] The Clarks Fork of the Yellowstone River is federally-designated as a Wild and Scenic River for 22 mi (35 km) through the forest, with cliffs towering up to 2,000 ft (610 m) as the river winds through a gorge. The forest is on the eastern slopes of the Continental Divide, and the rivers flow into the Atlantic Ocean basin.
Glaciology
According to the U.S. Forest Service, Shoshone National Forest has the greatest number of glaciers of any National Forest in the Rocky Mountains. The forest recreation guide lists 16 named and 140 unnamed glaciers within the forest, all in the Wind River Range. Forty-four of these glaciers are in the Fitzpatrick Wilderness, centered around the highest mountain peaks.[83][37] However, the state water board for Wyoming lists only 63 glaciers for the entire Wind River Range, which includes glaciers in adjacent Bridger-Teton National Forest.[84] Researchers claim that for most of the period that glaciers have been known to exist in the forest, that they have been in a state of general retreat, with glacial mass losses of as much as 25 percent between the years 1985 and 2009.[85]
Reversing the growth of mid-latitude glaciers that occurred during the Little Ice Age (1350–1850), there has been a world-wide reduction of mountain glacial ice since, with some regions losing as much as 50 percent of their peak ice cover. This can be correlated by examining photographic evidence of glaciers taken over time even with an absence of other means of documentation.[86] The behavior of the glaciers of Shoshone National Forest is consistent with this pattern. In one study of Dinwoody and Gannett Glaciers, during the period from 1958-1983, the thickness of these glaciers was reduced 77 and 61 ft (23 and 19 m), respectively.[87]
Gannett Glacier, on the northeast slope of Gannett Peak, is the largest single glacier in the U.S. Rocky Mountains. It has reportedly lost over 50 percent of its volume since 1920 with 25 percent of that occurring between the years 1980-1999.[88] Upper Fremont Glacier has been studied more than any other glacier in the Wind River Range. Scientist have obtained ice cores from the Upper Fremont Glacier and found that there have been measurable changes in the atmosphere over the past several hundred years.[89] The Upper Fremont Glacier and the Quelccaya Ice Cap in the Andes of South America both show nearly identical atmospheric records, which indicate a global linkage of atmospheric conditions over time.[90]
The small glaciers in the forest are less able to resist melting than the great ice sheets of Greenland and Antarctica. Once a glacier begins retreating, it may fall into disequilibrium and be unable to find mass balance (accumulation versus melting rate) at any size. Without a favorable climate change, it will continue to retreat until it disappears.[91] Loss of glacial ice already reduces the summer glacial runoff that supplies water to streams and lakes and provides a cold-water source vital to certain fish and plant species. This, in turn, may have a significant impact on the forest ecosystem over time.[84]
Climate
Wyoming is an arid state, averaging 12.68 inches (32.2 cm) of precipitation annually.[92] However, Shoshone National Forest is located in and near some of the largest mountain ranges in the state, and consequently receives anywhere between 15 and 70 in (380 and 1,780 mm) annually.[68] Higher elevations in the forest not only get more precipitation than lower elevations, but also have lower overall temperatures, with summertime highs around 60 °F (16 °C) and lows near 35 °F (2 °C) while lower elevations may be 20 °F (−7 °C) or more warmer on average.[68] Humidity levels throughout the forest are low, especially at higher altitudes. In the middle of the forest at the Wapiti Ranger Station, which is 30 mi (48 km) west of the forest headquarters in Cody, Wyoming, January high and low temperatures are 35.8 and 13.2 °F (2.1 and −10.4 °C), while the July highs and lows are 81.4 and 49.1 °F (27.4 and 9.5 °C). The annual precipitation at Wapiti is 10.37 in (263 mm).[93]
Most of the precipitation falls in the winter and early spring, while summer is punctuated with widely scattered thunderstorms.[68] The autumn is usually cool and dry. Due to the altitude and dryness of the atmosphere, vigorous radiative cooling occurs throughout the year, and exceptional daily temperature variances are not uncommon.[94] Consequently, the nights range from very cool in the summer to extremely cold in the winter; therefore, visitors should always remember to bring along at least a jacket, even during the summer.[95] Records indicate that the highest temperature ever recorded in the forest was 100 °F (38 °C) in 1978, while the coldest was −49 °F (−45 °C) in 1972.[96]
Recreation
Shoshone National Forest receives an average of over half a million visitors a year.[2] Two visitor centers provide orientation, books, maps, and interpretive displays. One visitor center is at the Wapiti Wayside on the Buffalo Bill Cody Scenic Byway, west of Cody, Wyoming and adjacent to the historic Wapiti Ranger Station while the other visitor center is to the south in Lander, Wyoming.[37] There are 30 vehicle access campgrounds in the forest, with up to 54 individual sites per campground. Approximately half of these campgrounds provide running water and restroom facilities and also provide for handicapped accessibility.[37][97] Referred to as "front country" campgrounds, they also permit recreational vehicle access in most cases. All of the campgrounds are on a first come, first served basis although four campgrounds have sites that can be reserved in advance by contacting the National Reservation Service.[37][97] Due to the presence of grizzly bears, a few of the campgrounds require what is referred to as "hard-sided" camping only, and tent camping is not permitted.[37]
For some visitors the greater solitude of the backcountry requires using hiking trails to backpacking or horseback riding into more remote destinations. There are dozens of trails which total over 1,600 mi (2,600 km) located throughout the forest.[37] Many of the trailheads can be accessed at campgrounds, with shorter day hikes available as well.[98] The Continental Divide Trail has a 20-mile (32 km) section which passes through the forest and crosses the Continental Divide at Sheridan Pass.[99] There is also the Nez Perce National Historic Trail and the Beartooth Loop National Recreation Trail, both of which are in the northern regions of the forest.[100][101] Some remote areas can also be accessed by horseback. Trailheads usually provide enough room for horse and pack animal trailers plus personal vehicles.[37] Along forest access roads, all-terrain vehicles (ATV) are allowed, but since wilderness areas do not permit access by way of motorized transport, those who wish to visit such areas usually do so either by hiking in or on horseback.[102][103]
Hunting and fishing are popular recreational activities permitted throughout the forest. Many of the streams and rivers are considered to be "Blue Ribbon Trout Streams".[104] Though many streams and lakes have excellent opportunities to catch various species of trout, the north and south forks of the Shoshone River, the Greybull River and the Clark's Fork of the Yellowstone, the only federally designated Wild and Scenic River in Wyoming, are a few of the better locations to reign in a trophy level Rainbow or Yellowstone cutthroat trout.[104] 1,000 miles (1,600 km) of streams and a hundred lakes that can be legally fished from provide plenty of elbow room during even the most crowded of fishing seasons. Hunting and fishing licenses are sponsored by the state of Wyoming and are available through the Wyoming Game and Fish Department.[105]
The southern section of the forest in the Wind River Range is the primary destination for mountain climbers. Nine of the highest 10 peaks in Wyoming are here, and the mountains are primarily of granitic rock with countless cliffs and sheer rock walls.[106] The Cirque of the Towers is particularly popular as it has numerous peaks within a relatively short distance of each other. Two particular climbs on the peaks in the cirque are considered amongst the finest climbing adventures available in the U.S.[107] The Absaroka Range also attracts climbers but not of a technical nature since the rocks are not considered solid enough for good anchoring points.[108] For the tallest peaks in the Wind River Range, the entire summiting effort will take even experienced climbers many days due to the inaccessibility of the region and complexity of the climbing effort.[109]
Winter activities include cross-country skiing and snowmobiling, with 48 mi (77 km) of groomed trails for cross-country skiing and over 300 mi (480 km) for use by snowmobilers.[110] The region around Togwotee Pass allows snowmobilers easy access from paved roads and has snow depths of between 6 to 10 ft (1.8 to 3.0 m) annually at elevations of 8,000 to 10,000 ft (2,400 to 3,000 m), which equates to a long season for winter activities.[111]
Scenic roads
Shoshone National Forest forms the eastern boundary of Yellowstone National Park and the northeastern and eastern entrances to the park are both accessed by way of designated scenic roadways. A federally designated National Scenic Byways All-American Road, the Beartooth Highway (U.S. Highway 212), weaves through the forest and serves as the northeastern entranceway to Yellowstone National Park.[112][113] Chief Joseph Scenic Byway (Wyoming Highway 296) connects Cody, Wyoming with the Beartooth Highway and follows the old trail in which Chief Joseph and the Nez Perce tribe attempted to flee the U.S. Cavalry in 1877.[114] South of there, Buffalo Bill Cody Scenic Byway (US 14/16/20) heads west from Cody, Wyoming, passes through the forest and crosses Sylvan Pass as it enters Yellowstone.[115] Lastly, the Wyoming Centennial Scenic Byway (US 26/287) heads northwest from Dubois, Wyoming, over Togwotee Pass and enters Jackson Hole and Grand Teton National Park.[81] Though the Beartooth Highway is the only one of these four roads that is a National Scenic Byway, all four of them have been designated Wyoming State Scenic Byways by the state of Wyoming.[116]
References
- ^ "Land Areas of the National Forest System" (pdf). U.S. Department of Agriculture. September 30, 2011. Retrieved August 31, 2013.
- ^ a b "National Visitor Use Monitoring". U.S. Department of Agriculture. Retrieved August 31, 2013.
- ^ "Wapiti Ranger Station". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved August 31, 2013.
- ^ "Shoshone". Answers. Retrieved March 23, 2013.
- ^ a b c "Welcome to Shoshone National Forest". U.S. Department of Agriculture. Retrieved August 31, 2013.
- ^ "History and Culture". U.S. Forest Service. Retrieved August 31, 2013.
- ^ Hebard, Grace R. (1995). Washakie, Chief of the Shoshones. Bison Books. p. 56. ISBN 978-0803272781. Retrieved August 31, 2013.
- ^ Capace, Nancy (2007). Encyclopedia of Wyoming. Somerset Publishers, Inc. p. 88. ISBN 978-0403096138. Retrieved August 31, 2013.
- ^ Johansen, Bruce E. (July 23, 2007). Encyclopedia of American Indian History. ABC-CLIO. p. 1127. ISBN 978-1851098187. Retrieved August 31, 2013.
{{cite book}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ a b "Mummy Cave". Wyoming State Historic Preservation Office. Retrieved September 29, 2013.
- ^ a b Husted, Wilfred M. (2002). "The Archeology of Mummy Cave, Wyoming: An Introduction to Shoshonean Prehistory" (pdf). National Park Service. Retrieved September 29, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ "National Register Information System". National Register of Historic Places. National Park Service. July 9, 2010.
- ^ a b c Utley, Robert M. (2004). After Lewis and Clark: Mountain Men and the Paths to the Pacific. Bison Books. pp. 15–16. ISBN 978-0803295643. Retrieved August 31, 2013.
- ^ a b Daugherty, John. "The Fur Trappers". A Place Called Jackson Hole. Grand Teton Natural History Association. Retrieved August 31, 2013.
- ^ Burns, Ken. "Private John Colter". Lewis and Clark: The Journey of the Corps of Discovery. PBS. Retrieved August 31, 2013.
- ^ a b Baldwin, Kenneth H. (November 15, 2004). "Terra Incognita: The Raynolds Expedition of 1860". Enchanted Enclosure. U.S. Army. Retrieved August 31, 2013.
- ^ Steen, Harold K. (1991). The beginning of the National Forest System. U.S. Forest Service. Retrieved August 31, 2013.
- ^ "Wapiti Ranger Station". National Historic Landmarks Program. National Park Service. Retrieved August 31, 2013.
- ^ a b McCoy, Michael (2007). Off the Beaten Path Wyoming: A Guide to Unique Places. GPP Travel. pp. 152–153. ISBN 978-0762744312. Retrieved August 31, 2013.
- ^ Reef, Catherine (2010). African Americans in the Military. Facts on File, Incorporated. p. 6. ISBN 9780816078394. Retrieved August 31, 2013.
- ^ "Burial Sites". The Lewis and Clark Journey of Discovery. National Park Service. Retrieved August 31, 2013.
- ^ a b "The History of Kirwin". U.S. Forest Service. Retrieved August 31, 2013.
- ^ "Shoshone National Forest - FAQs". U.S. Forest Service. Retrieved August 31, 2013.
- ^ Otis, Alison T. (1986). The Forest Service and the Civilian Conservation Corps, 1933-42. U.S. Forest Service. pp. 24–26. ISBN 9781236205001. Retrieved August 31, 2013.
- ^ Miller, Char (2013). Atlas of US and Canadian Environmental History. Routledge. p. 138. ISBN 9781136755248. Retrieved August 31, 2013.
- ^ Taylor, David T. (March 21, 2012). "Shoshone National Forest Economic Profile" (pdf). University of Wyoming Department of Agricultural & Applied Economics and the U.S. Forest Service. p. 87. Retrieved September 2, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ "USFS Ranger Districts by State" (pdf). U.S. Forest Service. Retrieved August 31, 2013.
- ^ "Sustainable Operations". U.S. Forest Service. Retrieved September 2, 2013.
- ^ Taylor, David T. (March 21, 2012). "Shoshone National Forest Economic Profile" (pdf). University of Wyoming Department of Agricultural & Applied Economics and the U.S. Forest Service. p. 73. Retrieved September 15, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Bleizeffer, Dustin (August 23, 2013). "Don't count on a rush of drilling rigs in the Shoshone National Forest". WyoFile. Retrieved September 2, 2013.
- ^ Taylor, David T. (March 21, 2012). "Shoshone National Forest Economic Profile" (pdf). University of Wyoming Department of Agricultural & Applied Economics and the U.S. Forest Service. p. 53. Retrieved September 15, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ "Beartooth Front, Wyoming" (pdf). Too Wild to Drill. Wilderness Society. Retrieved September 2, 2013.
- ^ "Analysis of the Management Situation" (pdf). U.S. Forest Service. February 2012. pp. 79–81. Retrieved September 15, 2013.
- ^ Wuerthner, George (1992). "Flora". Yellowstone: A Visitor's Companion (1 ed.). Stackpole Books. p. 65. ISBN 978-0811730785. Retrieved November 2, 2013.
- ^ a b "About the forest". U.S. Department of Agriculture. Retrieved November 2, 2013.
- ^ a b c d e Enright, Kelly (1992). America's Natural Places: Rocky Mountains and Great Plains. Greenwood. p. 137. ISBN 978-0313353154. Retrieved November 2, 2013.
- ^ a b c d e f g h i j k "Shoshone National Forest Visitor Guide" (pdf). U.S. Forest Service. Retrieved January 4, 2014.
- ^ "Rare Plants of Shoshone National Forest (USFS R-2)". Wyoming Rare Plant Field Guide, US Forest Service Rare Plant List. U.S. Geological Survey. Retrieved September 30, 2013.
- ^ a b Houston, Kent E. (October 2001). "A Field Guide for Forest Indicator Plants, Sensitive Plants, and Noxious Weeds of the Shoshone National Forest, Wyoming" (pdf). U.S. Department of Agriculture. pp. 155–171. Retrieved November 2, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ a b "Bark Beetle Epidemic". U.S. Forest Service. Retrieved November 2, 2013.
- ^ a b "Shoshone National Forest – vegetation management projects in 2011" (pdf). U.S. Forest Service. Retrieved November 2, 2013.
- ^ a b "Grizzly Bear Conservation and Recovery" (pdf). U.S. Department of Agriculture. September 2013. Retrieved November 15, 2013.
- ^ a b Moody, David (July 2005). "Wyoming Grizzly Bear Management Plan" (pdf). Wyoming Game and Fish Department. pp. 25–31. Retrieved December 15, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ K.J. Mills and R.F. Trebelcock, eds. (2013). "2012 Wyoming Gray Wolf Population Monitoring and Management Annual Report" (pdf). Wyoming Game and Fish Department. p. 1. Retrieved December 21, 2013.
{{cite web}}
:|author=
has generic name (help) - ^ K.J. Mills and R.F. Trebelcock, eds. (2013). "2012 Wyoming Gray Wolf Population Monitoring and Management Annual Report" (pdf). Wyoming Game and Fish Department. pp. 8–9. Retrieved December 21, 2013.
{{cite web}}
:|author=
has generic name (help) - ^ "Wolves in Wyoming". Wyoming Game and Fish Department. 2013. Retrieved December 21, 2013.
- ^ "Gray Wolf Hunting Seasons" (pdf). Wyoming Game and Fish Commission. 2012. Retrieved December 21, 2013.
- ^ "Mountain Lion Hunting Seasons" (pdf). Wyoming Game and Fish Commission. 2012. Retrieved December 21, 2013.
- ^ Murphy, Kerry (March 2011). "Wolverine Conservation in Yellowstone National Park" (pdf). National Park Service. Retrieved December 21, 2013.
- ^ "Proposed Revision of the Critical Habitat Designation for the Canada Lynx and Revised Definition of the Contiguous United States Distinct Population Segment of Canada Lynx" (pdf). U.S. Fish and Wildlife Service. 2013. Retrieved December 21, 2013.
- ^ a b c d e "Shoshone National Forest Species of Interest Report" (pdf). U.S. Forest Service. April 2009. pp. 65–68. Retrieved December 22, 2013.
- ^ a b c Orabona, Andrea (June 2012). "Atlas of Birds, Mammals, Amphibians and Reptiles in Wyoming" (pdf). Wyoming Game and Fish Department. Retrieved December 21, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ a b c d e "Shoshone National Forest Species of Interest Report" (pdf). U.S. Forest Service. April 2009. pp. 6–11. Retrieved December 22, 2013.
- ^ French, Brett (September 17, 2012). "Montana, Wyoming trying to understand why moose populations are plummeting". Billings Gazette. Retrieved December 21, 2013.
- ^ a b c "Shoshone National Forest Comprehensive Evaluation Report" (pdf). U.S. Forest Service. December 2007. Retrieved December 21, 2013.
- ^ Mlodik, Cory (April 2012). "Risk Analysis of Disease Transmission between Domestic Sheep and Goats and Rocky Mountain Bighorn Sheep" (PDF). U.S. Forest Service. Retrieved December 21, 2013.
- ^ a b "Wyoming Fishing Guide" (pdf). Wyoming Game and Fish Department. 2011. Retrieved December 29, 2013.
- ^ Gresswell, Robert (June 30, 2009). "Yellowstone Cutthroat Trout (Oncorhynchus clarkii bouvieri): A Technical Conservation Assessment" (pdf). U.S. Geological Survey. Retrieved December 29, 2013.
- ^ "Aquatic Invasive Species". U.S. Forest Service. Retrieved December 29, 2013.
- ^ "Wilderness". U.S. Forest Service. Retrieved September 7, 2013.
- ^ Landres, Peter (July 2000). "National Wilderness Preservation System Database: Key Attributes and Trends, 1964 Through 1999" (pdf). U.S. Department of Agriculture. p. 1. Retrieved September 7, 2013.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ "The National Wilderness Preservation System". The Wilderness Act of 1964. Wilderness.net. Retrieved September 7, 2013.
- ^ a b Aplet, Gregory H. (April 2006). "Evolution of Wilderness Fire Policy" (pdf). International Journal of Wilderness. 12 (1): 9–13. Retrieved December 30, 2013.
- ^ "Evolution of Federal Wildland Fire Management Policy" (pdf). Review and Update of the 1995 Federal Wildland Fire Management Policy January 2001. National Park Service, U.S. Forest Service. January 2001. Retrieved December 30, 2013.
- ^ Omi, Phillip N. (May 23, 2005). "Institutionalization of Fire Exclusion". Forest Fires: A Reference Handbook. ABC-CLIO. p. 67. ISBN 978-1851094387.
- ^ Omi, Phillip N. (May 23, 2005). "Institutionalization of Fire Exclusion". Forest Fires: A Reference Handbook. ABC-CLIO. p. 131. ISBN 978-1851094387.
- ^ "Deadliest Incidents Resulting in the Deaths of 8 or More Firefighters". National Fire Protection Association. February 2012. Retrieved December 30, 2013.
- ^ a b c d e f g h "Shoshone National Forest Fire Management Plan - 2012" (pdf). U.S. Forest Service. 2012. pp. 46–49. Retrieved January 4, 2014.
- ^ "Fire and fuels management". U.S. Forest Service. Retrieved December 30, 2013.
- ^ "About the epidemic". U.S. Forest Service. Retrieved December 30, 2013.
- ^ "Washakie Ranger District". U.S. Forest Service. Retrieved January 17, 2014.
- ^ a b "Absaroka Beartooth Wilderness". U.S. Forest Service. Retrieved January 18, 2014.
- ^ "Francs Peak, Wyoming". Peakbagger.com. Retrieved January 4, 2014.
- ^ a b c Antweiler, John C. (984). "Northern part of the Washakie Wilderness and Nearby Roadless Areas, Wyoming". U.S. Geological Survey Professional Paper. 2 (1300). U.S. Geological Survey: 1272–1275. Retrieved January 18, 2014.
{{cite journal}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Larson, T.A. (March 1, 1981). Wyoming: A Guide to Its History, Highways, and People. University of Nebraska Press. p. 429. ISBN 978-0803268548. Retrieved January 18, 2014.
- ^ Adkison, Ron (June 1, 1996). Hiking Wyoming's Wind River Range. Falcon Guides. p. 1. ISBN 978-1560444022. Retrieved January 18, 2014.
- ^ Earth's Oldest Rocks. Elsevier Science. October 26, 2007. pp. 780–781. ISBN 978-0080552477. Retrieved January 18, 2014.
{{cite book}}
: Unknown parameter|editors=
ignored (|editor=
suggested) (help) - ^ "Wind River Range". Wyoming State Geological Survey. 2013. Retrieved January 21, 2014.
- ^ Kelsey, Joe (July 16, 2013). Climbing and Hiking in the Wind River Mountains. Falcon Guides. p. 432. ISBN 978-0762780785. Retrieved January 21, 2014.
- ^ a b Cooper, Ed (November 25, 2008). Soul of the Rockies: Portraits of America's Largest Mountain Range. Falcon Guides. pp. 76–82. ISBN 978-0762749416. Retrieved January 21, 2014.
- ^ a b "Wind River Ranger District". U.S. Forest Service. Retrieved January 21, 2014.
- ^ Dow, Fred (2001). U.S. National Forest Campground Guide Rocky Mountain Region. Authorhouse. p. 507. ISBN 978-0759630239. Retrieved January 21, 2014.
{{cite book}}
: Unknown parameter|coauthor=
ignored (|author=
suggested) (help) - ^ "Fitzpatrick Wilderness". U.S. Forest Service. Retrieved January 11, 2014.
- ^ a b Hutson, Harold J. "Wyoming State Water Plan". Retrieved January 11, 2014.
- ^ Rice, Janine (January 2012). "Climate Change on the Shoshone National Forest, Wyoming: A Synthesis of Past Climate, Climate Projections, and Ecosystem Implications" (pdf). U.S. Forest Service. pp. 24–25. Retrieved January 11, 2014.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Hall, Myrna (February 2003). "Modeled Climate-Induced glacier change in Glacier National Park, 1850–2100" (pdf). 53 (2). Bioscience. Retrieved January 12, 2014.
{{cite journal}}
: Cite journal requires|journal=
(help); Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Pochop, Larry (July 1990). "Glacial Icemelt in the Wind River Range, Wyoming". Water Resources Data System Library. Retrieved January 12, 2014.
{{cite web}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Urbigkit, Cat (September 1, 2005). "Glaciers shrinking". Sublette Examiner. Retrieved January 14, 2014.
- ^ "Glacial Ice Cores Reveal a Record of Natural and Anthropogenic Atmosphere Mercury Deposition for the Last 270 Years". U.S. Geological Survey. June 2002. Retrieved January 14, 2014.
- ^ "Fremont Glacier, Wyoming USA". National Oceanic and Atmospheric Administration. Retrieved January 15, 2014.
- ^ Pelto, Mauri. "The Disequilbrium of North Cascade, Washington Glaciers 1984–2004". Retrieved January 15, 2014.
- ^ "Precipitation" (pdf). The National Atlas of the United States of America. U.S. Department of the Interior. Retrieved January 4, 2014.
- ^ "Monthly Station Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1971 - 2000" (pdf). Wyoming. National Oceanic and Atmospheric Administration (NOAA). February 2002. Retrieved January 4, 2014.
- ^ "Temperature". Wyoming State Climate Office. Retrieved January 4, 2014.
- ^ "Weather Climate". Wyoming Office of Tourism. Retrieved January 4, 2014.
- ^ "Monthly Averages for Wind River Ranger District - Shoshone NF". The Weather Channel. Retrieved January 4, 2014.
- ^ a b "Camping and Cabins". U.S. Forest Service. Retrieved January 5, 2014.
- ^ "Day Hiking". U.S. Forest Service. Retrieved January 5, 2014.
- ^ "Wyoming Access Points". Continental Divide Trail Coalition. Retrieved January 5, 2014.
- ^ "Nez Perce National Historic Trail (NPNHT) FACTS" (pdf). U.S. Forest Service. Retrieved January 5, 2014.
- ^ "Beartooth loop". The National Recreation Trails Program. Retrieved January 5, 2014.
- ^ "Motor Vehicle Use Map" (pdf). U.S. Forest Service. 2012. Retrieved January 8, 2014.
- ^ "Washakie Wilderness Fact Sheet". Wilderness.net. Retrieved January 8, 2014.
- ^ a b Retallic, Ken (February 1, 2012). Flyfisher's Guide to Wyoming: Including Grand Teton and Yellowstone National Parks. Wilderness Adventures Press. pp. 141–172. ISBN 978-1932098105.
{{cite book}}
:|access-date=
requires|url=
(help) - ^ "Wyoming Game and Fish Department Regulations". Wyoming Game and Fish Department. Retrieved January 8, 2014.
- ^ "Wyoming 13,000-foot Peaks". Peakbagger.com. Retrieved January 11, 2014.
- ^ Roper, Steve; Steck, Allen (1979). Fifty Classic Climbs of North America. San Francisco: Sierra Club Books. pp. 171–183. ISBN 0-87156-292-8.
- ^ "Francs Peak". Summitpost. Retrieved January 11, 2014.
- ^ Hunger, Bill (June 3, 2008). Wyoming: 110 of the State's Best Hiking Adventures. Falcon Guides. p. 151. ISBN 978-0762734207. Retrieved January 11, 2014.
- ^ "Shoshone National Forest". Wyoming Office of Tourism. Retrieved January 11, 2014.
- ^ "Continental Divide" (pdf). Wyoming State Trails Program. 2013. Retrieved January 11, 2014.
- ^ "A Wild Road – The Beartooth Highway". Friends of the Beartooth. Retrieved January 4, 2014.
- ^ "Beartooth Highway". Federal Higway Administration. Retrieved January 4, 2014.
- ^ "Chief Joseph Scenic Byway". Wyoming Office of Tourism. Retrieved January 4, 2014.
- ^ "Buffalo Bill Cody Scenic Byway". Wyoming Office of Tourism. Retrieved January 4, 2014.
- ^ "Scenic Byways and Backways". Wyoming Office of Tourism. Retrieved Jauuary 4, 2014.
{{cite web}}
: Check date values in:|accessdate=
(help)
- IUCN Category VI
- 1891 establishments in Wyoming
- Greater Yellowstone Ecosystem
- Landmarks in Wyoming
- National Forests of Wyoming
- Native American archeology
- Shoshone National Forest
- Civilian Conservation Corps in Wyoming
- Protected areas of Park County, Wyoming
- Protected areas of Fremont County, Wyoming
- Protected areas of Hot Springs County, Wyoming
- Protected areas of Sublette County, Wyoming
- Protected areas of Teton County, Wyoming