River Rase | |
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![]() River Rase near Middle Rasen | |
Location | |
Country | United Kingdom |
Country within the UK | England |
Counties | Lincolnshire |
Town | Market Rasen |
Villages | Tealby, Middle Rasen, West Rasen |
Physical characteristics | |
Source | |
• location | Churn Water Heads, Tealby, Lincolnshire |
• coordinates | 53°24′57″N0°15′24″W / 53.4159°N 0.2566°W |
• elevation | 118 m (387 ft) |
Mouth | |
• location | River Ancholme near Snitterby, Lincolnshire |
• coordinates | 53°26′20″N0°28′00″W / 53.4390°N 0.4667°W |
• elevation | 4 m (13 ft) |
Length | 25 km (16 mi) [1] |
Basin size | 67 km2 (26 sq mi) [2] |
Discharge | |
• location | Bishopbridge [2] |
• average | 0.48 m3/s (17 cu ft/s) [2] |
Basin features | |
Tributaries | |
• right | Brimmer Beck, The Dale |
Progression : Rase — Ancholme — Humber — North Sea |
The River Rase is a 16 mile (25 km) long tributary of the River Ancholme that flows through Lincolnshire, in the east of England.
The source of the river is a series of springs known as Churn Water Heads, that occur on Bully Hill north of Tealby in the Lincolnshire Wolds. These springs occur where the permeable chalk geology of the Wolds meets the impermeable mudstone and clays that underlie most of the Rase catchment. [3] [4]
The river flows in a south-westerly direction through the village of Tealby, where it is crossed by the Viking Way, a long-distance footpath that crosses the Wolds. To the west the Rase reaches the market town of Market Rasen, from which the river takes its name, and where it meets a tributary that flows through the local racecourse. The river continues through the villages of Middle Rasen and then West Rasen, where it is spanned by a packhorse bridge. At the hamlet of Bishopbridge the river changes character, becoming an artificial drainage channel that runs in parallel with the Ancholme. As it flows further north the river also loses its identity becoming the East Drain, when it is joined by the Kingerby Beck. The waters of the Rase and the Ancholme eventually join together near Harlam Hill, to the south of Snitterby Carr. [4] [5] [6]
The River Ancholme is a river in Lincolnshire, England, and a tributary of the Humber. It rises at Ancholme Head, a spring just north of the village of Ingham and immediately west of the Roman Road, Ermine Street. It flows east and then north to Bishopbridge west of Market Rasen, where it is joined by the Rase. North of there it flows through the market town of Brigg before draining into the Humber at South Ferriby. It drains a large part of northern Lincolnshire between the Trent and the North Sea.
West Lindsey is a local government district in Lincolnshire, England. Its council is based in Gainsborough, the district's largest town. The district also includes the towns of Caistor and Market Rasen, along with numerous villages and surrounding rural areas. The east of the district includes part of the Lincolnshire Wolds, a designated Area of Outstanding Natural Beauty.
Market Rasen is a market town and civil parish within the West Lindsey district of Lincolnshire, England. The River Rase runs through it east to west, approximately 13 miles (21 km) north-east from Lincoln, 18 miles (29 km) east from Gainsborough, 14 miles (23 km) west of Louth, and 16 miles (26 km) south-west from Grimsby. It lies on the main road between Lincoln and Grimsby, the A46, and is famous for its racecourse. In 2001, the town had a population of 3,200. In the 2011 census, the population of the civil parish was 3,904.
The Caistor Canal was a 4-mile (6.4 km) canal in Lincolnshire, England, constructed between 1793 and 1798. It fell into disuse sometime after 1850 and was legally abandoned in 1936. It ran from the River Ancholme, near South Kelsey toward Caistor through six locks, terminating at Moortown, 3.5 miles (5.6 km) away from its intended terminus at Caistor. Parts of it were dredged in 2010, to aid flood defences in South Kelsey.
The Lincolnshire Wolds are a range of low hills in the county of Lincolnshire, England which run roughly parallel with the North Sea coast, from the Humber Estuary in the north-west to the edge of the Lincolnshire Fens in the south-east. A large part of the Wolds are a designated Area of Outstanding Natural Beauty (AONB), and form the highest land in eastern England between Yorkshire and Kent.
The River Bain is a river in Lincolnshire, England, and a tributary of the River Witham.
The Viking Way is a long distance trail in England running 147 miles (237 km) between the Humber Bridge in North Lincolnshire and Oakham in Rutland.
Toft Newton is a civil parish in the West Lindsey district of Lincolnshire, England. It consists of the small villages of Toft next Newton and Newton by Toft, and the hamlet of Newtoft. It is 4 miles (6 km) west from Market Rasen. According to the 2001 Census it had a population of 522, decreasing to 457 at the 2011 census.
The River Freshney is a river in the English county of North East Lincolnshire. The town of Grimsby stands on its banks. It rises from at least four springs on the edge of the Lincolnshire Wolds, although local folklore and oral tradition has it springing from Welbeck Hill. Originally it entered the tidal Humber estuary at Pyewipe, north west of Grimsby, but has been re-routed and now supplies Grimsby Docks. There was an existing haven within the borough of Grimsby but this suffered greatly with silting problems so in 1669 landowners agreed to the diversion of the Freshney through the town to the haven to provide fresh water and improve the flow. It is believed the work was completed in the very early 18th century.
Barlings Eau is a small river near Barlings, Lincolnshire, England. It is a tributary of the River Witham, joining it near Short Ferry. It acts as the central spine for a number of other small rivers, which drain the low-lying land to either side. Most of its course is within the area managed by the Witham Third District IDB, an Internal Drainage Board responsible for land drainage. One of their pumping stations is on the banks of the river.
The A631 is a road running from Sheffield, South Yorkshire to Louth, Lincolnshire in England. It passes through the counties of South Yorkshire, Nottinghamshire and Lincolnshire. The road has many towns on its route including Rotherham, Maltby, Gainsborough and Market Rasen. It is mostly single road throughout its length but has some stretches of dual carriageway as well.
Ludford is a village and civil parish in the East Lindsey district of Lincolnshire, England. The parish is composed of the villages of Ludford Magna and Ludford Parva.
Osgodby is a village and civil parish in the West Lindsey district of Lincolnshire, England. The population of the civil parish, including Kingerby, Kirkby and Usselby, and West Rasen in its own civil parish, was 660 at the 2011 census.
The River Foulness is a river in the East Riding of Yorkshire, England. Its name is derived from Old English fūle[n] ēa, meaning “dirty water”. Maintenance responsibilities for the river transferred from the Environment Agency to the Market Weighton Drainage Board on 1 October 2011. Market Weighton Drainage Board subsequently amalgamated with the Lower Ouse Internal Drainage Board on 1 April 2012 to create the Ouse and Humber Drainage Board. The river discharges into the Humber Estuary via Market Weighton Canal. Water levels within the river, its tributaries and the canal are managed and controlled by the Environment Agency. The river lies in an area known as the Humberhead Levels.
The River Swift is a 14-mile (23 km) long tributary of the River Avon that rises in south Leicestershire, and flows through the town of Lutterworth before joining the Avon at its confluence at Rugby in Warwickshire in the English Midlands.
The River Eau is a 15-mile-long (24 km) tributary of the River Trent that flows through Lincolnshire, England.
Pauper’s Drain is a small tributary of the River Trent in North Lincolnshire, England, and is 9 km long.
The River Brant is a 14 mi-long (23 km) tributary of the River Witham that flows entirely in the county of Lincolnshire, in the east of England.
The geology of Lincolnshire in eastern England largely consists of an easterly dipping succession of Mesozoic age sedimentary rocks, obscured across large parts of the county by unconsolidated deposits dating from the last few hundred thousand years of the present Quaternary Period.
The River Till is a river in the county of Lincolnshire in England and is ultimately a tributary of the River Witham. Its upper reaches drain the land east of Gainsborough. The middle section is embanked, as the water level is higher than that of the surrounding land, and pumping stations pump water from low level drainage ditches into the river. Its lower reaches from the hamlet of Odder near Saxilby into the city of Lincoln were canalised, possibly as early as Roman times, as part of the Foss Dyke.