Geology Site Account
London Borough of Waltham Forest, WOODFORD WELLS, Lords Bushes & Knighton Wood, TQ413935, Proposed Local Geological Site
Locate Lords Bushes & Knighton Wood on map
Lord's Bushes and Knighton wood are areas of adjoining oak and hornbeam woodland partly in Essex and partly in The London Borough of Waltham Forest. The woodland sits on an extensive patch of what is known as Woodford Gravel, the origin of which is not entirely clear. The proportion of angular and rounded flint, and in particular of other rock types such as Lower Greensand chert from The Weald, indicate that it was deposited by a northward¬flowing river. This theory is supported by the fact that there are other patches of Woodford Gravel in the vicinity and they decline in elevation northwards. It therefore appears that the Woodford Gravel was deposited by a river flowing from what is now the Weald of Surrey northwards across East London to join the Thames which at that time flowed across north Essex and Suffolk. When this river was in existence is very difficult to determine but it was probably over 700,000 years ago.
Reference: Gibbard 1995 (p.12), Ellison 2004 (p.54-57).
Geology Site Map
Locate Lords Bushes & Knighton Wood on map
Lord's Bushes and Knighton wood are areas of adjoining oak and hornbeam woodland partly in Essex and partly in The London Borough of Waltham Forest. The woodland sits on an extensive patch of what is known as Woodford Gravel, the origin of which is not entirely clear. The proportion of angular and rounded flint, and in particular of other rock types such as Lower Greensand chert from The Weald, indicate that it was deposited by a northward¬flowing river. This theory is supported by the fact that there are other patches of Woodford Gravel in the vicinity and they decline in elevation northwards. It therefore appears that the Woodford Gravel was deposited by a river flowing from what is now the Weald of Surrey northwards across East London to join the Thames which at that time flowed across north Essex and Suffolk. When this river was in existence is very difficult to determine but it was probably over 700,000 years ago.
Lord’s Bushes and Knighton Wood are part of Epping Forest and are accessible at all times.
A bank of gravel on the side of the lake in Knighton Wood. The gravel was probably deposited over 700,000 years ago by a northward-flowing tributary of the ancient pre-diversion Thames. Photo: G. Lucy
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Reference: Gibbard 1995 (p.12), Ellison 2004 (p.54-57).
Geology Site Map