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Swindale Beck
Swindale Beck is a stream in Cumbria, England. It is formed at Swindale Head where Mosedale Beck, from the slopes of Tarn Crag, joins Hobgrumble Beck from Selside Pike. The stream flows north-east along Swindale and joins the River Lowther near Rosgill between Shap and Bampton. Its waters then flow via the
River Eamont into the Solway Firth.
Prior to 1859, it had been straightened to clear land for grazing.[1][2] In 2016, 750 metres (2,460 ft) of straightened channel was replaced with 890 m (2,920 ft) of a new sinuous channel, reconnecting the stream to its surrounding floodplain.[1][3] This resulted in a rapid and marked improvement in its diversity.[4] In 2022, the project was awarded the European Riverprize.[4]
^"Swindale Beck restored bends benefit breeding fish". BBC News. 6 January 2017. Retrieved 8 June 2021.
^Schofield, Lee. "The Shining River - RSPB England - Our work - The RSPB Community". community.rspb.org.uk. Retrieved 8 June 2021.
^ abLaville, Sandra (26 December 2022). "Diversity returns to Lakeland stream after restoration puts its bends back". The Guardian. Retrieved 26 December 2022.
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Keswick and Penrith Railway in this valley The valley of Mosedale Beck (Swindale), running between Branstree and Tarn Crag, Cumbria, England The valley...
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were brought to the site from the adjoining valleys of Heltondale and Swindale. When the valley was flooded, the dam raised the water level by 29 m (95 ft)...
Introduction. Cambridge University Press. pp. 197–201. ISBN 9781108440493. Ian Swindale, using the chronology of Andonis Vasilakis in his book on Minoan Crete...
Rennie, Senior Principal, Department of the Environment. Edward Thorold Swindale Roberts, lately Principal, Department of Transport. Ernest William Charles...
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