| Sunrise Glacier | |
|---|---|
  Sunrise Glacier | |
| Type | Valley glacier |
| Location | Denali Borough, Alaska, U.S. |
| Coordinates | 63°21′49″N150°10′06″W / 63.36361°N 150.16833°W |
 | |
Sunrise Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates near Scott Peak, moving northwest. It is the source of Sunrise Creek. Sunset Glacier is nearby. [1] [2]
Kahiltna Glacier is the longest glacier of the Alaska Range in the U.S. state of Alaska. It starts on the southwest slope of Denali near Kahiltna Pass. Its main channel runs almost due south between Mount Foraker to the west and Mount Hunter to the east. The name was first reported as "Car-ilt-nu Glacier" by Alaska Range explorer Lt. J.S. Herron in 1902. An alternate name is Kagheltnu Li'a. Kahiltna Glacier is the longest glacier in the Alaska Range at 44 miles (71 km) in length.
Peters Glacier, also known as Hanna Glacier and Hudeetsedle Toyaane' is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier runs from the Peters Basin icefield in a deep valley to the north of Denali's Wickersham Wall, between Denali and Peters Dome, falling from the icefield via the Tluna Icefall, where it is joined by Jeffery Glacier. It exits the Alaska Range to the north, forming the source of the Muddy River. Peters Glacier was named by A.H. Brooks for U.S. Geological Survey topographer William John Peters, who surveyed in Alaska from 1898 to 1902. Until 1947 it was named Hanna Glacier for U.S. Senator from Ohio Marcus Alonzo Hanna, a friend of President William McKinley.
Jeffery Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range on the north side of Denali directly below the Wickersham Wall, heading northeast to join Peters Glacier after the latter's Tluna Icefall.
Traleika Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates from two forks on either side of Farthing Horn on the east side of Denali. The west fork of the glacier starts in the Thayer Basin to the south of Denali, moving northeast and falling from the basin's 15,000-foot (4,600 m) height via the Traleika Icefall into the west fork between Karsten Ridge and the Farthing Horn. The main fork starts from Denali's east buttress in Traleika Col, joining the West Fork between the Farthing Horn and Mount Silverthrone, then moving northeast to join Muldrow Glacier. Traleika Glacier was named in 1945 by Bradford Washburn, attributing the name to a Susitna name meaning "great one" or "high one.". The form Traleika is an Anglicization of the Dena'ina name Dghelaay Ka'a, denoting Denali.
Brooks Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates on the east face of Mount Silverthrone at Brooks Gap. The 9-mile (14 km) glacier moves northeast, joining Muldrow Glacier between Mount Brooks and Ragged Peak. Brooks Glacier was named by T.G. Gerdine of the U.S. Geological Survey circa 1900 for geologist Alfred Hulse Brooks.
Muldrow Glacier, also known as McKinley Glacier, is a large glacier in Denali National Park and Preserve in the U.S. state of Alaska. Native names for the glacier include, Henteel No' Loo' and Henteel No' Loot.
There are three glaciers named West Fork Glacier in Alaska, two of which are in the Alaska Range. The first West Fork Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates at Anderson Pass, extending to the east and forming the source of the West Fork of the Chulitna River. Traleika Glacier was named in 1945 by Bradford Washburn, attributing the name to a Susitna name meaning "great one" or "high one." GNIS ID 1411870
Cantwell Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The 3-mile (4.8 km) long glacier originates from the crest of the Alaska Range in the eastern part of the park, giving rise to Cantwell Creek. Cantwell Glacier and Cantwell Creek are named for Yukon Valley explorer John C. Cantwell.
Eldridge Glacier is a major glacier in Denali National Park and Preserve in the U.S. state of Alaska. The 30-mile (48 km) long glacier originates on the east side of Explorers Peak, flowing northeast to a basin below Mount Eldridge, gathering flow from several glaciated cirques, then flowing southeast to the valley of the Chulitna River, where it gives rise to the Fountain River. A large unnamed tributary glacier joins Eldridge Glacier a few miles above its terminus.
Caldwell Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains at Gurney Peak and Lewis Peak, moving southwest to become a source of the Kichatna River. Named in 1889 by explorer Lt. J.S. Herron, it is 5 miles (8.0 km) long.
Cul-de-sac Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains on the side of Kichatna Spire, moving north. Its run-off and that of neighboring Shelf and Shadows glaciers feeds the west fork of the Yentna River.
Tatina Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains on the north side of the Cathedral Spires, moving northeast. Its run-off is the source of the Tatina River.
Shelf Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains on the side of Kichatna Spire, moving north. It is a tributary to neighboring Shadows Glacier, which with Cul-de-sac Glacier feeds the west fork of the Yentna River.
Shadows Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains on the north side of the Cathedral Spires, moving north. It receives neighboring Shelf Glacier as a tributary, and together with Cul-de-sac Glacier feeds the west fork of the Yentna River.
Fleischmann Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier lies in the southern Kichatna Mountains above Simpson Pass, moving south. It the source of Morris Creek, which feeds the Kichatna River.
Kanikula Glacier., also known as Little Tokositna Glacier, is an 11-mile (18 km) long glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates in a series of glacial amphitheaters in the south side of the range, moving southeast past Mount Goldie and ending before the valley of Tokositna Glacier. Variant forms and spellings of the name include K'enik'ela Li'a, Kahnicula Glacier, Kanicula Glacier and Little Tokasitna Glacier.
Tokositna Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates in two major arms on the east side of Mount Hunter, moving east until the main arms join, then turning south. Tokositna Glacier is the source of the Tokositna River. Spelling variants and alternate names include Tokasitna Glacier, Tokichitna Glacier and Tuqashitnu Li'a.
Sunset Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates near Scott Peak, moving southwest, then northwest. Sunrise Glacier is nearby.
The Polychrome Glaciers are five glaciers in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glaciers originate in parallel glaciated north-trending valleys in the Alaska Range, opposite Polychrome Mountain across Polychrome Pass.
Scott Peak is an 8,828 ft (2,690 m) glaciated mountain summit located in Denali National Park and Preserve, on the crest of the Alaska Range, in the U.S. state of Alaska. It is situated 9 mi (14 km) southeast of the Eielson Visitor Center, at the head of the Sunset Glacier, and 33.5 mi (54 km) northeast of Denali. This mountain was named in 1953 by Reynold E. (Pete) Isto of the U.S. Geological Survey and Bradford Washburn to honor Lieutenant Gordon D. Scott (1925–1953), a surveyor for the United States Coast and Geodetic Survey who was killed in a plane crash during mapping operations of this area. Scott Peak is set ten miles south of where the crash occurred near the Stony Creek Bridge area of the park road on June 11, 1953. Established climbing routes on Scott Peak include the Northeast Face, Northwest Face, and the Sunset Glacier. The first ascent of this peak was made in 1953 by Bradford Washburn.
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