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This article is within the scope of WikiProject Lancashire and Cumbria, a collaborative effort to improve the coverage of Lancashire and Cumbria on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.Lancashire and CumbriaWikipedia:WikiProject Lancashire and CumbriaTemplate:WikiProject Lancashire and CumbriaLancashire and Cumbria
This article is within the scope of WikiProject Rivers, a collaborative effort to improve the coverage of Rivers on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.RiversWikipedia:WikiProject RiversTemplate:WikiProject RiversRiver
Latest comment: 2 years ago2 comments1 person in discussion
Article says ”The river is formed at Chalkfoot near East Curthwaite, where water from Cardew Mires is joined by the Chalk Beck. Chalk Beck rises close to Wavergillhead and runs north, meeting Iron Gill and proceeding through a wooded clough to Chalkfoot” but Ordnance Survey, and the quarry application source, show the Wampool starting at Cardew Mires, which is downstream of Chalkfoot. Assuming there are no counterarguments, I’ll replace the text with something that matches the sources better, but maybe folks with local knowledge think the text is correct as it is, in which case please add some sources. (I will, in any case, rephrase to distinguish between the Chalk Beck and the Wampool.) Thanks all! --Northernhenge (talk) 16:31, 24 March 2024 (UTC)Reply
