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Henfield

Horsham DistrictVillages in West Sussex
Henfield aerial
Henfield aerial

Henfield is a large village and civil parish in the Horsham District of West Sussex, England. It lies 41 miles (66 km) south of London, 12 miles (19 km) northwest of Brighton, and 30 miles (48 km) east northeast of the county town of Chichester at the road junction of the A281 and A2037. The parish has a land area of 4,285 acres (1,734.1 ha). In the 2001 census 5,012 people lived in 2,153 households, of whom 2,361 were economically active. Other nearby towns include Burgess Hill to the east and Shoreham-by-Sea to the south. The population at the 2011 Census was 5,349.Just west of the town, the two branches of the River Adur, the western Adur and the eastern Adur, meet at Betley Bridge. From Henfield the Adur flows on into the English Channel at Shoreham-by-Sea.Henfield was already a large village, of 52 households, at the time of Domesday (1086).

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

Geographical coordinates (GPS)

Latitude Longitude
N 50.933 ° E -0.277 °
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Address

Church Lane
BN5 9NY
England, United Kingdom
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Henfield aerial
Henfield aerial
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Nearby Places

Horton Clay Pit
Horton Clay Pit

Horton Clay Pit is a 0.4-hectare (0.99-acre) geological Site of Special Scientific Interest in Small Dole in West Sussex. It is a Geological Conservation Review site. It was once much bigger and a popular area for looking for fossils and many marine creatures have been found in the Gault Clay by professional and amateur fossil hunters alike, especially molluscs - ammonites and belemnites, bivalves and gastropods.This site displays a thick and stratigraphically important sequence of rocks dating to the Folkestone Beds of the Early Cretaceous. It shows evidence of a major structural basin which controlled sedimentation in the western Weald.In 1913 a series of beetle fossils were recovered from its peaty bed. Researchers have used these fossils to suggest a detailed picture of the local environment during the Weichselian glaciation period and have concluded that a sour pool existed here in open heathland with a few coniferous trees. Through Mutual Climatic Range analysis they have predicted that although July was only a mean 1 degree cooler, January was 6 degree cooler.In 1991, the clay pit was granted planning consent for restoration using landfilling. The landfill lies on one side of a shallow excavation with the SSSI lying on the other side. More recently plans have been drawn to bury the SSSI with inert infill to prevent further erosion. This has been agreed in principle by Natural England if the Gault Clay is protected by a marker layer. Additional grassland and woodland planting have been promised that will enable habitat linkages across the restored landfill.