Recent from talks
River Lymn
Knowledge base stats:
Talk channels stats:
Members stats:
River Lymn
The River Lymn is a river in Lincolnshire, England. It rises in the Wolds on the eastern slope of Castcliffe Hill in Fulletby parish. It flows south-eastwards to the Lincolnshire Marsh, where it becomes known as the Steeping River on the boundary of Great Steeping parish. The main channel is supplemented by the Wainfleet Relief Channel as it passes Wainfleet All Saints, and the relief channel is joined by the old course of the Lymn. Once the two channels rejoin, there are three flood defence structures to protect the region from flooding by the North Sea. The river flows into the North Sea at Gibraltar Point.
The river rises on the southern slope of Belchford Hill, to the east of Belchford and close to the 300-foot (91 m) contour. It flows to the south and then to the east to reach Tetford, where there is a grade II listed water mill and mill house. It was built in the late eighteenth century, but shows evidence that it was built around an earlier structure. The much-repaired water wheel, dating from the seventeenth century, and the corn milling machinery are still intact. Beyond Tetford the river is joined by Double Dike, and flows south through woodland, passing to the west of Somersby and Bag Enderby. Here it is joined by a second stream, which rises on the eastern slope of Castcliffe Hill in Fulletby, close to the 280-foot (85 m) contour. It flows through a large lake and is joined by a stream from Holbeck Manor before passing through Salmonby. By the time the two streams join, they are below the 130-foot (40 m) contour.
It continues to the south-east and has dropped by another 33 feet (10 m) by the time it reaches the millpond of Stockwith Mill, beyond which is Stockwith Mill Bridge. The A158 road crosses at Aswardby Bridge, and the site of Aswardby Mill is below that. The next crossing is at Sausthorpe Bridge, which carries a minor road towards Sausthorpe, and the river drops below the 65-foot (20 m) contour at this point. The course continues to the east, passing under the A16 road between Spilsby and Partney at Partney Bridge, by Mill Farm, where there is a weir with a footbridge over the top. Beyond Spilsby, it turns to the south, crossing under a minor road at Northorpe Bridge and the B1195 road at Halton Bridge, to the east of Halton Holegate. Mill Bridge carries another minor road over the channel, but by the time the river reaches it, the river is in the Fens, the channel is embanked on both sides, and it crosses the 16-foot (5 m) contour.
The River Lymn is joined by another embanked channel, Lady Wath's Beck, as it passes between Great Steeping to the north and Little Steeping to the south, and takes the name Steeping River. The railway line between Boston and Skegness crosses to the north bank, and then follows the course of the river to below Wainfleet All Saints. The next bridge is Clough's Bridge, carrying a minor road over the main channel. Just before it, the old course of the Lymn leaves the straight channel of the Steeping River. It is no longer connected to the Steeping River, but is maintained as a drainage ditch by the Internal Drainage Board (IDB). Warth's Bridge and Thorpe Culvert Bridge follow, both roads leading to Thorpe Culvert railway station. Thorpe Culvert pumping station, owned by the IDB, is located just before the second bridge, and after it, the Wainfleet Relief Channel turns off, passing under the railway almost immediately. There are two more bridges as the main channel crosses Wainfleet Common, Bycroft's Bridge and Crow's Bridge. Crow's Bridge has an elliptical arch constructed of red bricks, and was designed by the engineer John Rennie in 1812. Salem Bridge carries the B1195 road to Wainfleet railway station, and the A52 road crosses to the east of Wainfleet All Saints. The channel is now also called Wainfleet Haven, and both names are used to describe it until it reaches the sea.
The Wainfleet Relief Channel is also crossed by the B1195 road, and shortly afterwards, the Lymn joins it. Cowcroft Drain, which joins the Lymn from the north, and the Lymn below the junction are both designated as main rivers, and are the responsibility of the Environment Agency, as is Croft Lane pumping station, which pumps the water from the Lymn into the relief channel. Croft Lane bridge is next, after which the A52 and the Boston to Skegness railway cross, and the relief channel rejoins Wainfleet Haven. The final section contains three flood defence structures. Haven House Sluice is first, after which the channel splits. Wainfleet Clough Outfall is on the western channel, which is tidal below the sluice. The Burgh Sluice Relief Channel is to the east, and Burgh Sluice protects it from the sea just before the two channels rejoin. Cow Bank Drain was excavated in 1812, as part of the last land reclamation scheme in the area. Cow Bank pumping station, owned by the IDB, pumps the drain into the outfall.
Below the outfall, Gibraltar Point National Nature Reserve is located to the east among the dunes and saltings. It is a Site of Special Scientific Interest (SSSI) and a Ramsar site, which provides a diverse habitat for birds such as grey plover and knot, plants including brackish water crowfoot and insects including the red-banded sand-wasp, among others. Gibraltar Point Sailing Club is located at Gibraltar Point, and the east bank of the river channel is used for mooring yachts. Now called Wainfleet Harbour, the channel crosses sand and mudflats to reach Wainfleet Swatch, an area of water protected from the North Sea by the Inner Knock sandbank at low water. The area to the south of Wainfleet Harbour is called Wainfleet Sand and is a danger area. It has been used for artillery practice since at least 1890, but may have been used for cannon and musketry practice long before that. More recently, it was part of RAF Wainfleet, and was used for weaponry practice by aircraft, until the closure of the range in December 2009.
There is a layer of sandstone rock beneath the whole of the catchment of the River Lymn, which is largely covered by a layer of chalk. The sandstone outcrops in only a few places, and where it does, springs provide the base flow for the river. As the layers of rock continue to dip to the east, they are covered by boulder clay, gravel and alluvium.
Flow on the upper river is measured by a gauging station at Partney Mill, consisting of a Crump weir with a 16-foot (5 m) crest. The catchment area of the river above this point is 23.8 square miles (61.6 km2), and this area received annual rainfall of 27.4 inches (696 mm) in the 1960s. This produces an average daily flow of 9.5 million gallons (43.2 Megalitres (Ml)), although a peak flow of 253M gallons (1149 Ml) was recorded in April 1981.
Hub AI
River Lymn AI simulator
(@River Lymn_simulator)
River Lymn
The River Lymn is a river in Lincolnshire, England. It rises in the Wolds on the eastern slope of Castcliffe Hill in Fulletby parish. It flows south-eastwards to the Lincolnshire Marsh, where it becomes known as the Steeping River on the boundary of Great Steeping parish. The main channel is supplemented by the Wainfleet Relief Channel as it passes Wainfleet All Saints, and the relief channel is joined by the old course of the Lymn. Once the two channels rejoin, there are three flood defence structures to protect the region from flooding by the North Sea. The river flows into the North Sea at Gibraltar Point.
The river rises on the southern slope of Belchford Hill, to the east of Belchford and close to the 300-foot (91 m) contour. It flows to the south and then to the east to reach Tetford, where there is a grade II listed water mill and mill house. It was built in the late eighteenth century, but shows evidence that it was built around an earlier structure. The much-repaired water wheel, dating from the seventeenth century, and the corn milling machinery are still intact. Beyond Tetford the river is joined by Double Dike, and flows south through woodland, passing to the west of Somersby and Bag Enderby. Here it is joined by a second stream, which rises on the eastern slope of Castcliffe Hill in Fulletby, close to the 280-foot (85 m) contour. It flows through a large lake and is joined by a stream from Holbeck Manor before passing through Salmonby. By the time the two streams join, they are below the 130-foot (40 m) contour.
It continues to the south-east and has dropped by another 33 feet (10 m) by the time it reaches the millpond of Stockwith Mill, beyond which is Stockwith Mill Bridge. The A158 road crosses at Aswardby Bridge, and the site of Aswardby Mill is below that. The next crossing is at Sausthorpe Bridge, which carries a minor road towards Sausthorpe, and the river drops below the 65-foot (20 m) contour at this point. The course continues to the east, passing under the A16 road between Spilsby and Partney at Partney Bridge, by Mill Farm, where there is a weir with a footbridge over the top. Beyond Spilsby, it turns to the south, crossing under a minor road at Northorpe Bridge and the B1195 road at Halton Bridge, to the east of Halton Holegate. Mill Bridge carries another minor road over the channel, but by the time the river reaches it, the river is in the Fens, the channel is embanked on both sides, and it crosses the 16-foot (5 m) contour.
The River Lymn is joined by another embanked channel, Lady Wath's Beck, as it passes between Great Steeping to the north and Little Steeping to the south, and takes the name Steeping River. The railway line between Boston and Skegness crosses to the north bank, and then follows the course of the river to below Wainfleet All Saints. The next bridge is Clough's Bridge, carrying a minor road over the main channel. Just before it, the old course of the Lymn leaves the straight channel of the Steeping River. It is no longer connected to the Steeping River, but is maintained as a drainage ditch by the Internal Drainage Board (IDB). Warth's Bridge and Thorpe Culvert Bridge follow, both roads leading to Thorpe Culvert railway station. Thorpe Culvert pumping station, owned by the IDB, is located just before the second bridge, and after it, the Wainfleet Relief Channel turns off, passing under the railway almost immediately. There are two more bridges as the main channel crosses Wainfleet Common, Bycroft's Bridge and Crow's Bridge. Crow's Bridge has an elliptical arch constructed of red bricks, and was designed by the engineer John Rennie in 1812. Salem Bridge carries the B1195 road to Wainfleet railway station, and the A52 road crosses to the east of Wainfleet All Saints. The channel is now also called Wainfleet Haven, and both names are used to describe it until it reaches the sea.
The Wainfleet Relief Channel is also crossed by the B1195 road, and shortly afterwards, the Lymn joins it. Cowcroft Drain, which joins the Lymn from the north, and the Lymn below the junction are both designated as main rivers, and are the responsibility of the Environment Agency, as is Croft Lane pumping station, which pumps the water from the Lymn into the relief channel. Croft Lane bridge is next, after which the A52 and the Boston to Skegness railway cross, and the relief channel rejoins Wainfleet Haven. The final section contains three flood defence structures. Haven House Sluice is first, after which the channel splits. Wainfleet Clough Outfall is on the western channel, which is tidal below the sluice. The Burgh Sluice Relief Channel is to the east, and Burgh Sluice protects it from the sea just before the two channels rejoin. Cow Bank Drain was excavated in 1812, as part of the last land reclamation scheme in the area. Cow Bank pumping station, owned by the IDB, pumps the drain into the outfall.
Below the outfall, Gibraltar Point National Nature Reserve is located to the east among the dunes and saltings. It is a Site of Special Scientific Interest (SSSI) and a Ramsar site, which provides a diverse habitat for birds such as grey plover and knot, plants including brackish water crowfoot and insects including the red-banded sand-wasp, among others. Gibraltar Point Sailing Club is located at Gibraltar Point, and the east bank of the river channel is used for mooring yachts. Now called Wainfleet Harbour, the channel crosses sand and mudflats to reach Wainfleet Swatch, an area of water protected from the North Sea by the Inner Knock sandbank at low water. The area to the south of Wainfleet Harbour is called Wainfleet Sand and is a danger area. It has been used for artillery practice since at least 1890, but may have been used for cannon and musketry practice long before that. More recently, it was part of RAF Wainfleet, and was used for weaponry practice by aircraft, until the closure of the range in December 2009.
There is a layer of sandstone rock beneath the whole of the catchment of the River Lymn, which is largely covered by a layer of chalk. The sandstone outcrops in only a few places, and where it does, springs provide the base flow for the river. As the layers of rock continue to dip to the east, they are covered by boulder clay, gravel and alluvium.
Flow on the upper river is measured by a gauging station at Partney Mill, consisting of a Crump weir with a 16-foot (5 m) crest. The catchment area of the river above this point is 23.8 square miles (61.6 km2), and this area received annual rainfall of 27.4 inches (696 mm) in the 1960s. This produces an average daily flow of 9.5 million gallons (43.2 Megalitres (Ml)), although a peak flow of 253M gallons (1149 Ml) was recorded in April 1981.
Recent media