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Geological Formation

Forge Valley

Valleys

Forge Valley is a national nature reserve of more than 63 hectares in the North York Moors National Park in North Yorkshire, England, following the route of the River Derwent. It was formed by meltwater at the end of the last ice age, and its woodland cover is roughly 6,000 years old. The valley takes its name from historical iron production, when charcoal was cut from its forests for use in forges, including a foundry that operated north of the valley from 1798; it is designated a Site of Special Scientific Interest and is managed by Raincliffe Woods Community Enterprise CIC. 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
National Park or Reserve 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: Forge 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: Forge Valley
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Forge Valley
Sources
1. Forge Valley (Wikipedia)
Lead section
Quote, Lead section
Forge Valley is a national nature reserve in North Yorkshire, England, located within the North York Moors National Park on the East Ayton / Hackness road. The valley follows the route of the River Derwent and was formed by melting ice water at the end of the last ice age.
View the Source
Wikidata: Forge Valley
Wikidata Q5469597, class allow-list match (w-wdresolver-0926)View the Source
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