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Geological Formation

Great Appalachian Valley

Structural and Tectonic Formations

The Great Appalachian Valley is one of the major landform features of eastern North America, a vast trough of connected valley lowlands that forms the central feature of the Appalachian Mountains system. It runs roughly 1,200 miles from Quebec in the north to Alabama in the south, crossing Vermont, New York, Pennsylvania, New Jersey, Maryland, Virginia, West Virginia, Tennessee and North Carolina along the way. It marks the eastern edge of the Ridge and Valley physiographic province and has long served as a natural north-south travel corridor, used since prehistoric times. Different sections of the valley carry their own regional names, the Shenandoah Valley among them. 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

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: Great Appalachian 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: Great Appalachian Valley
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Great Appalachian Valley
Sources
Great Appalachian Valley (Wikipedia)
Lead section
Quote, Lead section
The Great Appalachian Valley, also called The Great Valley or Great Valley Region, is one of the major landform features of eastern North America.
View the Source
Wikidata: Great Appalachian Valley
Wikidata Q3816357, class allow-list match (w-wdresolver-0926)View the Source
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