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Geological Formation

Stikine Icecap

Glaciers and Ice Formations

The Stikine Icecap, also called the Stikine Icefield, is a large icefield in the Boundary Ranges of the Coast Mountains, straddling the Alaska Panhandle and the border between Alaska and British Columbia. On the United States side much of it lies within Tongass National Forest and the Stikine LeConte Wilderness. It feeds the Taku River, which forms its northern edge, and the Stikine River, which forms its southern edge, and it is the parent icefield of glaciers including LeConte and Sawyer on the American side and Great Glacier on the Canadian side. The region is known for technically demanding granite peaks such as Devils Thumb and Burkett Needle, often compared to Patagonia. 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: Stikine Icecap

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: Stikine Icecap
In the Other Atlases
Sources
1. Stikine Icecap (Wikipedia)
  • Lead section
    The Stikine Icecap (sometimes referred to as the Stikine Icefield) is a large icefield straddled on the Alaska-British Columbia boundary in the Alaska Panhandle region.
  • Lead section (protected-status)
    Within the United States, most of it is under the administration of the Tongass National Forest and is part of the Stikine-LeConte Wilderness within the national forest.
View the Source
Wikidata: Stikine Icecap
Wikidata Q2268498, class allow-list match (w-wdresolver-0926)View the Source
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