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Essex Field Club
Essex Field Club
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EFC Centre at Wat Tyler Country ParkIn January we are only open to the public at our centre at Wat Tyler Country Park on Wednesdays 10am-4pm.
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Geology Site Account

A-Z Geological Site Index

Bushy Hill, SOUTH WOODHAM FERRERS, Chelmsford District, TQ813986, Potential Local Geological Site

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Bushy Hill, north of South Woodham Ferrers. Grid Reference: TQ 813 986.


Bushy Hill is a prominent landmark and a good example of natural landslips.


Summary of the geological interest:

Bushy Hill is the southernmost point of a ridge of high ground overlooking South Woodham Ferrers. The hill is composed of London Clay capped by Claygate Beds with a relatively thin capping of gravel of unknown age. There are notable landslips on the southern and western slopes.

There are fine views from this ridge across the valley of the Crouch with the Bagshot Beds hills of Rayleigh to the south and the Langdon Hills to the south-west. Although there are no public footpaths to the summit, which is occupied by a radar research station, similar views can be had from the minor road which runs across the ridge to the north (near Edwin’s Hall) and from the public footpath from this road around the western slopes of the hill. To the east of the hill is typical London Clay landscape.

The footpath that traverses the south-eastern slopes of the hill passes hummocky ground from previous landslips. These slips sometimes provide exposures of Claygate Beds.


Scientific interest and site importance

Bushy Hill is a prominent and locally important landscape feature. It is composed of London Clay overlain by Claygate Beds. There are very good examples of landslips on the southern and western slopes that can be seen from aerial photographs. The landslips can also be inspected close to from the public footpath that traverses the south-eastern slopes of the hill. Here there is hummocky ground from previous landslips which sometimes provide exposures of Claygate Beds. The Claygate Beds are found to consist of brown-buff silty clays with seams of silty sand with occasional septarian nodules.

The landslips on Bushy Hill, which are of several different types, have been taking place here for thousands of years and will continue until the slopes reach an angle of about 8 degrees which is required for ultimate stability on London Clay and Claygate Beds. These landslips probably originated in periods of periglacial activity when this part of Essex was close to the southern limit of the Anglian ice sheet, 450,000 years ago. Less than a kilometre (half a mile) north of Bushy Hill is an isolated patch of boulder clay, or till, which indicates that a lobe of ice from the ice sheet briefly penetrated beyond Hanningfield to this point. The slippage is exacerbated by springs emerging from seams of sand in the Claygate Beds.


Other information

Bushy Hill is known locally as ‘Radar Hill’ due to having been visually dominated by the radar station. Before the radar station was built it was known as ‘Landslip Hill’ as the landslips on the south face periodically left a bare escarpment, which was clearly visible from the village.


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Reference: Bristow 1985 (p.71 & 85), Greensmith et al. 1973 (p.33-34), Hutchinson 1965 (p. 26-28).

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