Bering Glacier is a glacier in Alaska that terminates in Vitus Lake about 10 kilometers south of Wrangell-St. Elias National Park, named for the explorer Vitus Bering. Combined with the Bagley Icefield, where the snow that feeds it accumulates, the Bering Glacier system is the largest glacier in North America. It has retreated roughly 12 kilometers since 1900 due to warming temperatures and changing precipitation, though it also undergoes periodic surge events, advancing rapidly about every 20 years, most recently in the winter of 1994 to 1995. The glacier releases an estimated 30 cubic kilometers of meltwater a year, more than double the flow of the Colorado River, draining through the Seal River into the Gulf of Alaska. 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 StatusNational Park or Reserve 1 Connections
Caused By
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: Bering 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: Bering Glacier
In the Other Atlases
Sources
1. Bering Glacier (Wikipedia)
Entity description, protection designationQuote, Entity description, protection designation
a that terminates in Vitus Lake about 10 kilometers south of Wrangell-St. Elias National Park, named for the explorer Vitus Bering. Combined with the Bagley Icefield, where
View the Source Wikidata: Bering Glacier
Wikidata Q2669909, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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