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Geological Formation

Cheshire Plain

Sedimentary and Stratigraphic Formations

The Cheshire Plain is a flat lowland in the county of Cheshire in North West England, extending south into Shropshire between the hills of North Wales, the foothills of the Pennines and the Shropshire Hills. It is the surface expression of the Cheshire Basin, a deep sedimentary basin, and took its present form as the last glacial period's ice sheets melted between about 20,000 and 15,000 years ago, leaving a thick cover of glacial till and glacio-fluvial sand and gravel. 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: Cheshire Plain

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: Cheshire Plain
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Cheshire Plain
Sources
Cheshire Plain (Wikipedia)
  • Lead section
    The Cheshire Plain is a relatively flat expanse of lowland within the county of Cheshire in North West England but extending south into Shropshire.
  • In Group: Lowland Plains, Lead sentence
    The Cheshire Plain is a relatively flat expanse of lowland within the county of Cheshire in North West England but extending south into Shropshire.
View the Source
Wikidata: Cheshire Plain
Wikidata Q2880633, class allow-list match (w-wdresolver-0926)View the Source
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