| Tatina Glacier | |
|---|---|
  Tatina Glacier | |
| Type | Valley glacier |
| Location | Matanuska-Susitna Borough, Alaska, U.S. |
| Coordinates | 62°27′03″N152°48′44″W / 62.45083°N 152.81222°W |
 | |
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. [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.
Kantishna is an unincorporated community in Denali Borough, Alaska, United States, within Denali National Park and Preserve. Founded as a gold mining camp in 1905, it endured longer than similar communities in the area, having been constructed nearest to the source of the gold. It lies in the Kantishna Hills at the junction of Eureka Creek and Moose Creek, 3 mi (5 km) northwest of Wonder Lake, and near the mouth of the Kantishna River. Although the community was once also called "Eureka", the Board on Geographic Names officially ruled in favor of "Kantishna" in 1944, the name given to the post office that was built at the site in 1905. Its elevation is 1,696 feet (517 m).
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.
Lacuna Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins on the south side of Mount Foraker in the Alaska Range, moving southwest to join the Yentna Glacier, to which Lacuna is a tributary.
Yentna Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range between Mount Russell and Mount Foraker, moving southwest. It is the source of the east fork of the Yentna River. Lacuna Glacier is a major tributary, and Dall Glacier enters the glacial valley just below Yentna Glacier's present terminus.
Dall 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 Mount Russell, moving southwest, then south to the Yentna River just below the present terminus of Yentna Glacier.
Chedotlothna Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range between Mount Russell and Mount Dall moving northeast, then north. It is the source of the Swift Fork of the Kuskokwim River. The name Chedotlothna was reported as a native name by S.R. Capps in 1925. Alternate spellings include Chedotlothno and Chedotluthna. The glacier is also called Todzolno' Lughwzra'.
Surprise Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range near Mount Dall, moving west. Its terminus is the source of the Tonzona River.
Herron 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 Mount Foraker, moving northwest for 14 miles (23 km). It is the source of the Herron River. The name was given by A.H. Brooks of the U.S. Geological Survey to honor Lt. Joseph S. Herron, who mapped much of the region.
Foraker 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 Mount Foraker, moving northwest for 15 miles (24 km). It is the source of the Foraker River.
Straightaway Glacier, also known as Crosson 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 Mount Crosson, moving northwest. It is a source of the Foraker River.
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.
Buckskin Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates on the east side of The Moose's Tooth, flowing east, then southeast, for 14 miles (23 km) before giving rise to the Hidden River.
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.
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