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Geological Formation

Coe Glacier

Glaciers and Ice Formations

Coe Glacier lies on the north slope of Mount Hood in the Cascade Range of Hood River County, Oregon, between about 10,500 and 6,400 feet (3,200 and 2,000 meters) in elevation, and is named for Henry C. Coe. Between 1907 and 2004 it lost 15 percent of its surface area and its terminus, now moraine and talus, retreated 390 meters; as of 2004 it covered about 296 acres (120 hectares). This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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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: Coe 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: Coe Glacier
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Sources
Coe Glacier (Wikipedia)
Wikidata: Coe Glacier
Wikidata Q5140490, class allow-list match (w-wdresolver-0926)View the Source
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