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River Slea
River in Lincolnshire, England
River in Lincolnshire, England
| Field | Value |
|---|---|
| name | River Slea |
| image | Weir below bridge in Sleaford town centre-Geograph-1876760-by-Mick-Lobb.jpg |
| image_caption | Slea in Sleaford |
| pushpin_map | Lincolnshire |
| pushpin_map_caption | Location of the mouth within Lincolnshire |
| subdivision_type1 | Country |
| subdivision_name1 | England |
| subdivision_type2 | County |
| subdivision_name2 | Lincolnshire |
| length | 36.4 km |
| discharge1_location | Leasingham Mill |
| discharge1_avg | 0.55 m3/s |
| source1_location | West Willoughby |
| mouth_location | River Witham at Chapel Hill |
| mouth_coordinates |
The River Slea is a 36.4 km tributary of the River Witham, in Lincolnshire, England. In 1872 the river was described as "a never-ending source of pure water", and was a trout river renowned throughout the East coast of England. But in the late 1960s, the Anglian Water Authority took control of the river, and thereafter it became rapidly degraded, due mostly to over-abstraction of water for use in farming.
Course
The Slea rises near West Willoughby, two miles south-west of Ancaster, at an altitude of 70 metres. The river descends 30 metres in the first 3 km of its course through Ancaster before flowing past a Site of Special Scientific Interest (alongside Sleaford Golf Club) into Sleaford.
Through Sleaford it flows above ground in two separate courses, and then curves around the foot of The Hub where a new riverside sculpture walk follows it. Leaving Sleaford, it passes Haverholme and runs down through South Kyme where it is known as the Kyme Eau to join the River Witham at Chapel Hill.
References
References
- Combined lengths of Slea and Kyme Eau
- Johnson, Lou. "Riverside walk at Spalding - print walk - Walking Britain".
- "Slea". Environment Agency.
- "Kyme Eau". Environment Agency.
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
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