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Geological Formation

Tanana Valley

Valleys

The Tanana Valley is a lowland region of central Alaska on the north side of the Alaska Range, where the Tanana River emerges from the mountains. Much of the valley is underlain by permafrost, and its surrounding plains turn boglike in summer and are dotted with pingos, ice-cored mounds pushed up by freezing groundwater. Winters bring temperature inversions and thick fog, along with a katabatic wind known locally as the Tanana Valley Jet, which blows from the southeast to the northwest. It is the most populated part of Alaska north of the Alaska Range, centered on Fairbanks, and is home to the Tanana Athabaskans; sites such as Broken Mammoth and Swan Point, dated to roughly 12,000 to 14,000 years ago, contain some of Alaska's earliest evidence of human occupation. 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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Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Tanana Valley

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Tanana Valley
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Tanana Valley
Sources
Tanana Valley (Wikipedia)
Lead section
Quote, Lead section
The Tanana Valley is a lowland region in central Alaska in the United States, on the north side of the Alaska Range, where the Tanana River emerges from the mountains.
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Wikidata: Tanana Valley
Wikidata Q841915, class allow-list match (w-wdresolver-0926)View the Source
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