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Geological Formation

Fraser Valley

Valleys

The Fraser Valley is a geographical region in southwestern British Columbia, Canada, extending from just west of Hope to the Pacific Ocean, bounded by the North Shore Mountains near Vancouver in the north and the area south of Bellingham, Washington in the south. It is built around the Fraser River, which flows through the valley to the Strait of Georgia. During the last ice age the area lay under glaciers; as the ice retreated, land once buried beneath it was submerged by water and then slowly rose above it, forming the basin that exists today. The valley extends roughly 80 kilometers east from the built-up Vancouver area to Chilliwack and Agassiz, and it contains the Fraser Delta, the largest landform of the Lower Mainland ecoregion. 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

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: Fraser 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: Fraser Valley
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Fraser Valley
Sources
Fraser Valley (Wikipedia)
Lead section
Quote, Lead section
The Fraser Valley is a geographical region in southwestern British Columbia, Canada and northwestern Washington State.
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Wikidata: Fraser Valley
Wikidata Q3554074, class allow-list match (w-wdresolver-0926)View the Source
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