The Alaska Range is a relatively narrow, 600-mile-long (950km) mountain range in the southcentral region of the U.S. state of Alaska, from Lake Clark at its southwest end[1] to the White River in Canada's Yukon Territory in the southeast. The highest mountain in North America, Denali, is in the Alaska Range. It is part of the American Cordillera.
North American mountain range
Alaska Range
Mount Hunter, Mount Huntington and other rugged peaks of the Alaska Range near Denali
The Alaska range is one of the higher ranges in the world after the Himalayas and the Andes.
Description and history
Mt. Hayes and the eastern Alaska Range mountains View from Denali State Park
The range forms a generally east–west arc with its northernmost part in the center, and from there trending southwest towards the Alaska Peninsula and the Aleutian Islands, and trending southeast into British Columbia and the Pacific Coast Ranges. The mountains act as a high barrier to the flow of moist air from the Gulf of Alaska northwards, and thus have some of the harshest weather in the world. The heavy snowfall also contributes to a number of large glaciers, including the Cantwell, Castner, Black Rapids, Susitna, Yanert, Muldrow, Eldridge, Ruth, Tokositna, and Kahiltna Glaciers. Four major rivers cross the Alaska Range, including the Delta and Nenana Rivers in the center of the range and the Nabesna and Chisana Rivers to the east.
Alaska Range Glacier
The range is part of the Pacific Ring of Fire, and the Denali Fault that runs along its southern edge is responsible for many major earthquakes. Mount Spurr is a stratovolcano located at the northeastern end of the Aleutian Volcanic Arc which has two vents, the summit and nearby Crater Peak.
Parts of the Alaska Range are protected within Wrangell-St. Elias National Park and Preserve, Denali National Park and Preserve, and Lake Clark National Park and Preserve. The George Parks Highway from Anchorage to Fairbanks, the Richardson Highway from Valdez to Fairbanks, and the Tok Cut-Off from Gulkana Junction to Tok, Alaska pass through low parts of the range. The Alaska Pipeline parallels the Richardson Highway.
Naming history
The name "Alaskan Range" appears to have been first applied to these mountains in 1869 by naturalist W. H. Dall. The name eventually became "Alaska Range" through local use. In 1849 Constantin Grewingk applied the name "Tschigmit" to this mountain range. A map made by the General Land Office in 1869 calls the southwestern part of the Alaska Range the "Chigmit Mountains" and the northeastern part the "Beaver Mountains".[2] However, the Chigmit Mountains are now considered part of the Aleutian Range.
The Denali Highway passes through the Alaska Range and offers travelers a close up-look at some of the lower peaks
Mentasta Lake to Kitchatna Mountains (1981): Scott Woolums, George Beilstein, Steve Eck, and Larry Coxen by skis: first traverse. 375 miles (604km) in 45 days.[3]
Canada to Lake Clark (1996): Roman Dial, Carl Tobin, and Paul Adkins by mountain bike and packraft: first full-length traverse. 775 miles (1,247km) in 42 days.[4]
Tok to Lake Clark (1996): Kevin Armstrong, Doug Woody, and Jeff Ottmers by snowshoe, foot, and packraft: first foot traverse. 620 miles (1,000km) in 90 days.[5]
Lake Clark to Mentasta Lake (2016): Gavin McClurg by paraglider and foot: first vol-biv (fly/camp) traverse. 466 miles (750km) in 37 days.[6]
Cantwell/Yakutat to Unimak Island (2020): Quoc Nguyen and Dan Binde by foot and packraft. 2,500 miles (4,023 km) in 120 days.[7]
Gulkana Glacier flows from the ice fields of the Alaska Range
Sources differ as to the exact delineation of the Alaska Range. The Board on Geographic Names entry is inconsistent; part of it designates Iliamna Lake as the southwestern end, and part of the entry has the range ending at the Telaquana and Neacola Rivers. Other sources identify Lake Clark, in between those two, as the endpoint. This also means that the status of the Neacola Mountains is unclear: it is usually identified as the northernmost subrange of the Aleutian Range, but it could also be considered the southernmost part of the Alaska Range.
Wikimedia Commons has media related to Alaska Range.
Churkin, M., Jr., and C. Carter. (1996). Stratigraphy, structure, and graptolites of an Ordovician and Silurian sequence in the Terra Cotta Mountains, Alaska Range, Alaska [U.S. Geological Survey Professional Paper 1555]. Washington, D.C.: U.S. Department of the Interior, U.S. Geological Survey.
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