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Geological Formation

Davis Valley

Valleys

Davis Valley is an ice free dry valley just east of Floridas Ridge in the northeast Dufek Massif of the Pensacola Mountains, Antarctica, mapped by the United States Geological Survey from surveys and United States Navy air photographs taken between 1956 and 1966. It is one of the most southerly dry valley systems on the continent, valued scientifically for what it can reveal about past glacial events and regional climate history, and is protected as Antarctic Specially Protected Area No. 119 under the Antarctic Treaty System. 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 Status
Locally or Regionally Protected 1
Connections

Caused By

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: Davis 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: Davis Valley
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Sources
1. Davis Valley (Wikipedia)
Lead section
Quote, Lead section
It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Edward H.
View the Source
Wikidata: Davis Valley
Wikidata Q5241982, class allow-list match (w-wdresolver-0926)View the Source
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