Columbia Glacier is a tidewater glacier that descends from the Chugach Mountains into Prince William Sound on the south coast of Alaska. It is among the fastest moving glaciers in the world and has been retreating since the early 1980s; the Harriman Alaska Expedition named it after Columbia University in 1899. The glacier is about fifty one kilometers long, covers roughly 1,000 square kilometers, and reaches about 550 meters thick. Since 1982 its terminus has retreated about sixteen kilometers, at times moving nearly thirty meters a day while shedding icebergs, and it is expected to retreat a further fifteen kilometers in coming decades. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
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: Columbia Glacier (Alaska)
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: Columbia Glacier (Alaska)
In the Other Atlases
Sources
Columbia Glacier (Alaska) (Wikipedia)
Lead sectionQuote, Lead section
The Columbia Glacier, a glacier in Prince William Sound on the south coast of the U.S. state of Alaska, is one of the fastest moving glaciers in the world, and has been retreating since the early 1980s.
View the Source Wikidata: Columbia Glacier (Alaska)
Wikidata Q833807, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.
Sign in to dispute this or suggest a correction.