The Disappearing River Caldew, April/May 2020
The yellow arrow indicates the location of the April/May 2020 Swallow Hole.
The River Caldew passes close to the village of MILLHOUSE in it's junior stage,  sourcing on the eastern face of Skiddaw, on Skiddaw forest,  terminating into the river Eden near the Sheep Mount sports ground, at the lower end of Bitts Park in Carlisle, which in turn feeds into the channel of the River Esk, with a final destination of the Solway Firth.
It also passes close-by to the villages Mosedale, Haltcliff Bridge, Hesket Newmarket, Sebergham, Dalston and Cummersdale, before making it's way through the western side of the city of Carlisle.

Our stretch of the Caldew has a very unique feature.    During periods of low rain fall there are lengthy stretches of the river between Haltcliff Bridge and Hesket Newmarket which completely dry-up and cease to flow.  The smaller volume of river during these times is literally swallowed up by open limestone crevices in the river bed, locally named  "Swallow Holes".   Extensive research, (several years ago) by specialists, has proven that the water taken in by these "swallow holes" actually flows underground in limestone caverns for a distance of more than 5 miles, the majority reappearing back into the Caldew at Howgill just upstream from the village of Sebergham. but has also been proven to reappear as far downstream as Bridge End, Dalston.
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