Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Colne Valley

Valleys

The Colne Valley is a steep-sided valley on the eastern flank of the Pennine Hills in West Yorkshire, England, named for the River Colne, which rises above Marsden and flows east toward Huddersfield before joining the River Holme. The valley contains the villages of Marsden, Slaithwaite, Linthwaite, Milnsbridge, Scapegoat Hill, Longwood and Golcar, and lies within the Kirklees metropolitan borough. During the Industrial Revolution the valley's waterways and canals powered a shift from hand-loom weaving to water-powered textile manufacturing, connecting it to Britain's wider industrial network. 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: Colne 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: Colne Valley
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Colne Valley
Sources
Colne Valley (Wikipedia)
Lead section
Quote, Lead section
The Colne Valley is a steep sided valley on the east flank of the Pennine Hills in the English county of West Yorkshire.
View the Source
Wikidata: Colne Valley
Wikidata Q5147770, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.