place

Knapps Brook

Bedfordshire geography stubsEngland river stubsLea catchmentLutonRivers of Bedfordshire
Tributaries of the River LeaUse British English from June 2015
Knapps Brook in Leagrave, Luton LU4
Knapps Brook in Leagrave, Luton LU4

Knapps Brook is a minor tributary of the River Lea in Bedfordshire, England. The source of the river Lea is on Leagrave Common in Luton. It forms from a combination of brooks from East End, Houghton Regis and from the Lewsey Estate near the old Lewsey Farm. It joins the River Lea from culverts under the railway embankment and Toddington Road in Leagrave.The brook is most easily viewed from footpaths alongside Toddington Road or footpaths running through the nearby Hockwell Ring estate. Nearby Nappsbury Road in Leagrave takes its name from the former Napps Nursery that occupied the site. The nursery name being a corruption of the brook that runs adjacent to the site.

Excerpt from the Wikipedia article Knapps Brook (License: CC BY-SA 3.0, Authors, Images).

Knapps Brook
Sundon Park Road,

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Knapps BrookContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 51.90845 ° E -0.46034 °
placeShow on map

Address

Sundon Park Road
LU3 2RZ , Marsh Farm
England, United Kingdom
mapOpen on Google Maps

Knapps Brook in Leagrave, Luton LU4
Knapps Brook in Leagrave, Luton LU4
Share experience

Nearby Places

Waulud's Bank
Waulud's Bank

Waulud's Bank is a possible Neolithic henge in Leagrave, Luton dating from 3,000BC. The Waulud's Bank earthworks are in the North of Luton and are situated on the edge of Leagrave common, with Central Leagrave to the south east and Marsh Farm to the west. The River Lea runs alongside on the western side, its source located within the vicinity of the surrounding marsh. Archaeological excavations in 1953, 1971 and 1982 date the site to around 3000 BC, in the Neolithic period, although there was evidence of earlier mesolithic hunter/fisher activity in the immediate area. The 'D' shape of the earthwork is almost identical to that of Marden in Wiltshire, both sites have a river forming one side, and each produced neolithic grooved-ware pottery. Waulud's Bank lies on a glacial ridge near which runs the prehistoric Icknield Way. Initially it was probably a domestic enclosure used for cattle herding. It has been suggested that it later became a henge monument, although the position of its surrounding ditch outside its timber-faced bank would be unusual. Evidence suggests that the site was briefly re-used in the Iron Age, during the Roman occupation and in medieval times. The enclosure consists of a bank and external ditch of around 7 hectares with a turf-revetted chalk and gravel bank faced by a wooden stockade. No entrances have been identified. Most external features have been destroyed by a 19th-century gravel quarry on the south, and the irresponsible dumping of tons of chalk and top-soil along the eastern side during building construction of Marsh Farm in the 1970s. Geophysical surveys in July 1985 and January 2009 failed to reveal any very positive indications of internal features. The bank still stands 2.6 m high in places and on the north side the excavated ditch was 9.2 m wide and 2.1 m deep. Finds included neolithic pottery, animal bones and flint arrow heads (some are on display at Stockwood Heritage Centre, Luton Museum). The building at the edge of Waulud's Bank was a one time farmhouse called Marsh Farm House, the occupants of which owned the area that later became Marsh Farm.