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Geological Formation

Gannett Glacier

Glaciers and Ice Formations

Gannett Glacier is the largest glacier in the Rocky Mountains within the United States, located on the east and north slopes of Gannett Peak, the highest mountain in Wyoming, on the east side of the Continental Divide in the Wind River Range. It is one of dozens of glaciers in the Fitzpatrick Wilderness of Shoshone National Forest. Like many glaciers worldwide it has been shrinking: its area was estimated at 4.6 square kilometers in 1950 and measured at 3.63 square kilometers in 1999, with a depth reduction of 18.6 meters recorded between 1958 and 1983. A 1989 study found that meltwater from Gannett and the neighboring Dinwoody Glacier, which feeds Dinwoody Creek and the Wind River, had been contributing decreasing amounts of water as the glaciers thinned and retreated, especially after 1950. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Glaciation, Processes

Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Gannett Glacier

In Discipline

Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Gannett Glacier
In the Other Atlases
Sources
1. Gannett Glacier (Wikipedia)
Lead section (protected-status)
Quote, Lead section (protected-status)
Gannett is but one of dozens of glaciers located in the Fitzpatrick Wilderness of Shoshone National Forest.
View the Source
Wikidata: Gannett Glacier
Wikidata Q5521432, class allow-list match (w-wdresolver-0926)View the Source
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