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Geological Formation

Jefferson Park Glacier

Glaciers and Ice Formations

Jefferson Park Glacier lies on the northwest slopes of Mount Jefferson in the Cascade Range of Oregon, spanning Linn and Marion counties at elevations between about 7,700 and 9,500 feet. About 0.9 miles long, it is retreating, and its terminus is marked by moraines and talus. 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: Jefferson Park 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: Jefferson Park Glacier
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Sources
Jefferson Park Glacier (Wikipedia)
Wikidata: Jefferson Park Glacier
Wikidata Q6175559, class allow-list match (w-wdresolver-0926)View the Source
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