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Geological Formation

Dovedale

Gorges and Canyons

Dovedale is a limestone valley in the Peak District of England, extending just over three miles between Milldale and a wooded ravine near Thorpe Cloud. Its bedrock formed from the fossilized remains of sea creatures that lived in a shallow sea over the area during the Carboniferous period, about 350 million years ago. During past ice ages, glacial meltwater carved the limestone into distinctive rocky formations and dry caves, producing features such as the Dove Holes caves and the isolated 942-foot limestone hill Thorpe Cloud. The River Dove, a 45-mile trout stream, runs through the valley, crossed in places by stepping stones, and the site is owned largely by the National Trust, drawing about a million visitors a year. 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: Dovedale

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: Dovedale
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Dovedale
Sources
1. Dovedale (Wikipedia)
  • Lead section
    Dovedale is a valley in the Peak District of England.
  • Article text
    Dovedale became a national nature reserve in 2006 in recognition that it is "one of England's finest wildlife sites" with diverse plant life and interesting rock formations.
View the Source
Wikidata: Dovedale
Wikidata Q5302426, class allow-list match (w-wdresolver-0926)View the Source
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