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Eagle Peak (Wyoming): Difference between revisions

Coordinates: 44°19′15″N 110°01′40″W / 44.32083°N 110.02778°W / 44.32083; -110.02778
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| photo_caption = Eagle Peak
| photo_caption = Eagle Peak
| elevation_ft = 11372
| elevation_ft = 11372
| elevation_ref = <ref name=pb>{{cite peakbagger|pid=5305|name=Eagle Peak, Wyoming|accessdate=June 15, 2013}}</ref>{{NAVD88}}
| elevation_ref = <ref name=pb>{{cite peakbagger|pid=5305|name=Eagle Peak, Wyoming|access-date=June 15, 2013}}</ref>{{NAVD88}}
| prominence_ft = 1847
| prominence_ft = 1847
| prominence_ref = <ref name=pb/>
| prominence_ref = <ref name=pb/>
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| map_caption = Location in Wyoming##Location in the United States
| map_caption = Location in Wyoming##Location in the United States
| coordinates = {{coord|44|19|15|N|110|01|40|W|type:mountain_region:US-WY_scale:100000|format=dms|display=inline,title}}
| coordinates = {{coord|44|19|15|N|110|01|40|W|type:mountain_region:US-WY_scale:100000|format=dms|display=inline,title}}
| coordinates_ref = <ref name=gnis>{{cite gnis|id=1587990|name=Eagle Peak|accessdate=June 15, 2013}}</ref>
| coordinates_ref = <ref name=gnis>{{cite gnis|id=1587990|name=Eagle Peak|access-date=June 15, 2013}}</ref>
| topo = [[United States Geological Survey|USGS]] Eagle Peak
| topo = [[United States Geological Survey|USGS]] Eagle Peak
| type = [[Stratovolcano]]
| volcanic_arc/belt = [[Absaroka Range]]
| first_ascent =
| first_ascent =
| easiest_route =
| easiest_route =
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==Geology==
==Geology==
Eagle Peak is part of the [[Absaroka Range]] and is formed of [[Eocene]] age [[volcaniclastic]] rocks.<ref name=Geology>{{Cite web|url=http://www.wsgs.uwyo.edu/research/stratigraphy/AbsarokaRange/Default.aspx|title=Absaroka Range|publisher=Wyoming State Geological Survey|access-date=27 June 2013}}</ref><ref>{{cite book|url=https://books.google.com/books?id=ywolAQAAIAAJ&pg=SL3-PA28 |title=Stratigraphic Framework of the Absaroka Volcanic Supergroup in the Yellowstone National Park Region |author=Harry W. Smedes and Harold J. Prostka |publisher=U.S. Geological Survey Professional Paper 729-C |year=1972}}</ref> In the last ice age, the area was covered by an ice cap over {{convert|1600|ft}} thick. [[Glacial deposit]]s remain in some locations on the mountain.{{sfn|Richmond|1976|p=20}}
Eagle Peak is part of the [[Absaroka Range]] and is formed of [[Eocene]] age [[volcaniclastic]] rocks.<ref name=Geology>{{Cite web|url=http://www.wsgs.uwyo.edu/research/stratigraphy/AbsarokaRange/Default.aspx|title=Absaroka Range|publisher=Wyoming State Geological Survey|access-date=27 June 2013|archive-date=29 June 2013|archive-url=https://archive.today/20130629084650/http://www.wsgs.uwyo.edu/research/stratigraphy/AbsarokaRange/Default.aspx|url-status=dead}}</ref><ref>{{cite book|url=https://books.google.com/books?id=ywolAQAAIAAJ&pg=SL3-PA28 |title=Stratigraphic Framework of the Absaroka Volcanic Supergroup in the Yellowstone National Park Region |author=Harry W. Smedes and Harold J. Prostka |publisher=U.S. Geological Survey Professional Paper 729-C |year=1972}}</ref> In the last ice age, the area was covered by an ice cap over {{convert|1600|ft}} thick. [[Glacial deposit]]s remain in some locations on the mountain.{{sfn|Richmond|1976|p=20}} Eagle Peak is a remnant of an Absaroka [[stratovolcano]]. <ref>{{cite web | url=https://www.nationalparkstraveler.org/2021/02/yellowstones-volcanic-neighbors-absarokas | title=Yellowstone's Volcanic Neighbors: The Absarokas! }}</ref>


==Geography==
==Geography==
Located in the [[Absaroka Range]], on the park boundary with [[Shoshone National Forest]] in northwestern [[Wyoming]], the mountain rises about {{convert|6|mi|abbr=on}} east of the southeast arm of [[Yellowstone Lake]].<ref name="GM">{{Google maps | url =https://maps.google.com/maps?ll=44.320833,-110.027778&q=loc:44.320833,-110.027778&hl=en&t=h&z=12 | accessdate =16 June 2013}}</ref><ref name=Brit>{{Cite web|url= http://www.britannica.com/EBchecked/media/169439/Eagle-Peak-in-the-Absaroka-Range-the-highest-point-in|title= Eagle Peak|access-date=18 June 2013|publisher=Encyclopædia Britannica}}</ref> The mountain is also one of the highest points in the [[Washakie Wilderness]] area of Shoshone National Forest. Eagle Peak is of a similar height to several other local mountains; there is a ridge which gradually gets higher as it heads southeast culminating in several summits - [[Mount Schurz]], to the immediate northwest is shorter,<ref name=map/> and [[Pinnacle Mountain (Wyoming)|Pinnacle Mountain]],{{sfn|Spencer|1916|p=60}} to the immediate southeast, is taller, but outside of the park boundary.{{Sfn|Kelsey|2001|p=917}}
Located in the [[Absaroka Range]], on the park boundary with [[Shoshone National Forest]] in northwestern [[Wyoming]], the mountain rises about {{convert|6|mi|abbr=on}} east of the southeast arm of [[Yellowstone Lake]].<ref name="GM">{{Google maps | url =https://maps.google.com/maps?ll=44.320833,-110.027778&q=loc:44.320833,-110.027778&hl=en&t=h&z=12 | access-date =16 June 2013}}</ref><ref name=Brit>{{Cite web|url= http://www.britannica.com/EBchecked/media/169439/Eagle-Peak-in-the-Absaroka-Range-the-highest-point-in|title= Eagle Peak|access-date=18 June 2013|publisher=Encyclopædia Britannica}}</ref> The mountain is also one of the highest points in the [[Washakie Wilderness]] area of Shoshone National Forest. Eagle Peak is of a similar height to several other local mountains; there is a ridge which gradually gets higher as it heads southeast culminating in several summits - [[Mount Schurz]], to the immediate northwest is shorter,<ref name=map/> and [[Pinnacle Mountain (Wyoming)|Pinnacle Mountain]],{{sfn|Spencer|1916|p=60}} to the immediate southeast, is taller, but outside of the park boundary.{{Sfn|Kelsey|2001|p=917}}


Several creeks flow through the mountain and the surrounding area and they become a vehicle for cold melt water. The [[Gardner River]] flows to the east of the summit.<ref name="Erfurt-CooperCooper2010">{{cite book|last1=Erfurt-Cooper|first1=Patricia|last2=Cooper|first2=Malcolm|title=Volcano and Geothermal Tourism: Sustainable Geo-resources for Leisure and Recreation|url=https://books.google.com/books?id=RjWPbnRuWk8C&pg=PA111|access-date=16 June 2013|year=2010|publisher=Earthscan|isbn=978-1-84977-518-2|page=111}}</ref> Some of the runoff is fed by the melting of the two major snowfields found in the shadows of the north face of the mountain.<ref name="GM"/> The range to the east drains into the [[Yellowstone River]] via the [[Bighorn River]], but the southern slopes drain into [[Yellowstone Lake]] via Mountain Creek.<ref name=map>{{Cite web|url=http://hfc.nps.gov/carto/PDF/YELLmap1.pdf|title=Yellowstone Map|access-date=19 June 2013|publisher=National Park Service}}</ref>
Several creeks flow through the mountain and the surrounding area and they become a vehicle for cold melt water. The [[Gardner River]] flows to the east of the summit.<ref name="Erfurt-CooperCooper2010">{{cite book|last1=Erfurt-Cooper|first1=Patricia|last2=Cooper|first2=Malcolm|title=Volcano and Geothermal Tourism: Sustainable Geo-resources for Leisure and Recreation|url=https://books.google.com/books?id=RjWPbnRuWk8C&pg=PA111|access-date=16 June 2013|year=2010|publisher=Earthscan|isbn=978-1-84977-518-2|page=111}}</ref> Some of the runoff is fed by the melting of the two major snowfields found in the shadows of the north face of the mountain.<ref name="GM"/> The range to the east drains into the [[Yellowstone River]] via the [[Bighorn River]], but the southern slopes drain into [[Yellowstone Lake]] via Mountain Creek.<ref name=map>{{Cite web|url=http://hfc.nps.gov/carto/PDF/YELLmap1.pdf|title=Yellowstone Map|access-date=19 June 2013|publisher=National Park Service}}</ref>
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==Wildlife==
==Wildlife==
[[File:EaglePeakYNPca1890.jpg|thumb|right|Eagle Peak, c.1890]]
[[File:EaglePeakYNPca1890.jpg|thumb|right|Eagle Peak, c.1890]]
Eagle Peak wildlife are in the [[alpine tundra]] zone and may be threatened by global climate change—the gradual shift of montane fauna and flora upwards could lead to the permanent loss of some species from the park.<ref>{{Cite journal|author1=Romme, William H. |author2=Turner, Monica G. |title=Implications of Global Climate Change for Biogeographic Patterns in the Greater Yellowstone Ecosystem|journal=Conservation Biology|volume=5 |number=3|pages=373–386|date=September 1991|doi=10.1111/j.1523-1739.1991.tb00151.x|doi-access=free}}</ref> To the south, on the boundary of the park is [[Eagle Pass (Wyoming)|Eagle Pass]] and the [[Thorofare Plateau]], which has a population of elk, moose, deer, bear, bighorn sheep and others and lies along an important north-south migration route for the elk. Flora includes sedges and rushes, and [[tufted hairgrass]] in alpine meadows.{{sfn|Meagher|Houston|1999|p=206}}
Eagle Peak wildlife are in the [[alpine tundra]] zone and may be threatened by global climate change—the gradual shift of montane fauna and flora upwards could lead to the permanent loss of some species from the park.<ref>{{Cite journal|author1=Romme, William H. |author2=Turner, Monica G. |title=Implications of Global Climate Change for Biogeographic Patterns in the Greater Yellowstone Ecosystem|journal=Conservation Biology|volume=5 |number=3|pages=373–386|date=September 1991|doi=10.1111/j.1523-1739.1991.tb00151.x|bibcode=1991ConBi...5..373R |doi-access=free}}</ref> To the south, on the boundary of the park is [[Eagle Pass (Wyoming)|Eagle Pass]] and the [[Thorofare Plateau]], which has a population of elk, moose, deer, bear, bighorn sheep and others and lies along an important north–south migration route for the elk. Flora includes sedges and rushes, and [[tufted hairgrass]] in alpine meadows.{{sfn|Meagher|Houston|1999|p=206}}


==See also==
==See also==
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[[Category:Mountains of Park County, Wyoming]]
[[Category:Mountains of Park County, Wyoming]]
[[Category:Highest points of United States national parks]]
[[Category:Highest points of United States national parks]]
[[Category:Volcanoes of Wyoming]]
[[Category:Volcanoes of the United States]]

Latest revision as of 02:48, 8 May 2024

Eagle Peak
Eagle Peak
Highest point
Elevation11,372 ft (3,466 m)[1] NAVD 88
Prominence1,847 ft (563 m)[1]
Coordinates44°19′15″N 110°01′40″W / 44.32083°N 110.02778°W / 44.32083; -110.02778[2]
Geography
Eagle Peak is located in Wyoming
Eagle Peak
Eagle Peak
Location in Wyoming
Eagle Peak is located in the United States
Eagle Peak
Eagle Peak
Location in the United States
LocationPark County, Wyoming, U.S.
Parent rangeAbsaroka Range
Topo mapUSGS Eagle Peak
Geology
Mountain typeStratovolcano
Volcanic arc/beltAbsaroka Range

Eagle Peak is a mountain in the Absaroka Range in the U.S. state of Wyoming and at 11,372 feet (3,466 m) is the highest point in Yellowstone National Park.[1][3][4] It is located about 6 miles (9.7 km) east of the southeast arm of Yellowstone Lake.

Etymology[edit]

According to Lee Whittlesey, Eagle Peak was named in 1885 by geologist Arnold Hague for its resemblance to a "spread eagle".[5] Another source states that it was named in 1878 by Jack Newell, who killed a golden eagle on the mountain that year.[6]

History[edit]

Up until the 1930s, most park officials and geologists believed that Electric Peak near Gardiner, Montana was the park's highest peak, not Eagle Peak.[5] It is ranked as the 218th highest peak in Wyoming and the 2252nd highest peak in the United States.[7] During the historic Yellowstone fires of 1988, the south slopes of Eagle Peak were affected by the Mink Fire.[8]

Geology[edit]

Eagle Peak is part of the Absaroka Range and is formed of Eocene age volcaniclastic rocks.[9][10] In the last ice age, the area was covered by an ice cap over 1,600 feet (490 m) thick. Glacial deposits remain in some locations on the mountain.[11] Eagle Peak is a remnant of an Absaroka stratovolcano. [12]

Geography[edit]

Located in the Absaroka Range, on the park boundary with Shoshone National Forest in northwestern Wyoming, the mountain rises about 6 mi (9.7 km) east of the southeast arm of Yellowstone Lake.[13][14] The mountain is also one of the highest points in the Washakie Wilderness area of Shoshone National Forest. Eagle Peak is of a similar height to several other local mountains; there is a ridge which gradually gets higher as it heads southeast culminating in several summits - Mount Schurz, to the immediate northwest is shorter,[15] and Pinnacle Mountain,[16] to the immediate southeast, is taller, but outside of the park boundary.[17]

Several creeks flow through the mountain and the surrounding area and they become a vehicle for cold melt water. The Gardner River flows to the east of the summit.[18] Some of the runoff is fed by the melting of the two major snowfields found in the shadows of the north face of the mountain.[13] The range to the east drains into the Yellowstone River via the Bighorn River, but the southern slopes drain into Yellowstone Lake via Mountain Creek.[15]

Eagle Peak is one of the most prominent features of the Eagle Peak Quadrangle, a USGS division used for surveying purposes.[8] Other nearby peaks are Mount Humphreys, Table Mountain, Mount Schurz, Pinnacle Mountain, Turret Mountain and Colter Peak.

Access[edit]

The mountain is fairly inaccessible, being a 15-mile (24 km) hike from any of the park roads. From outside the park, the peak can be ascended by hiking up the Fish Hawk Creek valley, which is around 25 kilometres (16 mi) one-way.[19] It is also climbed from inside the park, by sailing to the southeasternmost tip of Yellowstone Lake, hiking down the Yellowstone River valley, and then turning to the east for the ascent.

Wildlife[edit]

Eagle Peak, c.1890

Eagle Peak wildlife are in the alpine tundra zone and may be threatened by global climate change—the gradual shift of montane fauna and flora upwards could lead to the permanent loss of some species from the park.[20] To the south, on the boundary of the park is Eagle Pass and the Thorofare Plateau, which has a population of elk, moose, deer, bear, bighorn sheep and others and lies along an important north–south migration route for the elk. Flora includes sedges and rushes, and tufted hairgrass in alpine meadows.[21]

See also[edit]

References[edit]

  1. ^ a b c "Eagle Peak, Wyoming". Peakbagger.com. Retrieved June 15, 2013.
  2. ^ "Eagle Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved June 15, 2013.
  3. ^ "Yellowstone Fact Sheet". National Park Service. Retrieved June 15, 2013.
  4. ^ Eagle Peak, WY (Map). TopoQwest (United States Geological Survey Maps). Retrieved June 15, 2013.
  5. ^ a b Whittlesey 1988, p. 49.
  6. ^ Urbanek, Mae Bobb (1988). Wyoming Place Names. Mountain Press Publishing Company, Incorporated. p. 59. ISBN 978-0-87842-204-3. Retrieved 16 June 2013.
  7. ^ "Eagle Peak (Wyoming)". Peakery.com. Retrieved 18 June 2013.
  8. ^ a b "Fire Growth Maps for the 1988 Greater Yellowstone Area Fires" (PDF). USDA. January 1994. Archived from the original (PDF) on 19 September 2013. Retrieved 16 June 2013.
  9. ^ "Absaroka Range". Wyoming State Geological Survey. Archived from the original on 29 June 2013. Retrieved 27 June 2013.
  10. ^ Harry W. Smedes and Harold J. Prostka (1972). Stratigraphic Framework of the Absaroka Volcanic Supergroup in the Yellowstone National Park Region. U.S. Geological Survey Professional Paper 729-C.
  11. ^ Richmond 1976, p. 20.
  12. ^ "Yellowstone's Volcanic Neighbors: The Absarokas!".
  13. ^ a b Google (16 June 2013). "Eagle Peak (Wyoming)" (Map). Google Maps. Google. Retrieved 16 June 2013.
  14. ^ "Eagle Peak". Encyclopædia Britannica. Retrieved 18 June 2013.
  15. ^ a b "Yellowstone Map" (PDF). National Park Service. Retrieved 19 June 2013.
  16. ^ Spencer 1916, p. 60.
  17. ^ Kelsey 2001, p. 917.
  18. ^ Erfurt-Cooper, Patricia; Cooper, Malcolm (2010). Volcano and Geothermal Tourism: Sustainable Geo-resources for Leisure and Recreation. Earthscan. p. 111. ISBN 978-1-84977-518-2. Retrieved 16 June 2013.
  19. ^ Kelsey 2001, p. 916.
  20. ^ Romme, William H.; Turner, Monica G. (September 1991). "Implications of Global Climate Change for Biogeographic Patterns in the Greater Yellowstone Ecosystem". Conservation Biology. 5 (3): 373–386. Bibcode:1991ConBi...5..373R. doi:10.1111/j.1523-1739.1991.tb00151.x.
  21. ^ Meagher & Houston 1999, p. 206.

Bibliography[edit]