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The Greensand Ridge, also known as the Wealden Greensand, is an extensive, prominent, often wooded, mixed greensand/sandstone escarpment in south-east England. Forming part of the Weald, a former dense forest in Sussex, Surrey and Kent, it runs to and from the East Sussex coast, wrapping around the High Weald and Low Weald. It reaches its highest elevation, , at Leith Hill in Surrey—the second highest point in south-east England, while another hill in its range, Blackdown, is the highest point in Sussex at . The eastern end of the ridge forms the northern boundary of Romney Marsh.
About 51 per cent of the Wealden Greensand is protected as the South Downs National Park, Kent Downs and Surrey Hills Area of Outstanding Natural Beauty.
The Weald dome consists of a series of geological strata laid down in the Cretaceous that have subsequently been lifted up, formed into a dome (i.e. anticline) and then deformed and faulted. The top-most and therefore youngest layer of the dome is Chalk, laid down in the Upper Cretaceous. Below it lie successively older strata of alternating clays and sandstones laid down in the Lower Cretaceous, namely Upper Greensand, Gault Clay, Lower Greensand, Weald Clay and the Hastings Beds. Differential fluvial erosion has virtually flattened the dome into a series of hills and vales. On the surface the strata of which the dome is composed crop out in a series of concentric circles, shaped like a horseshoe, with the more resistant chalk and sandstones forming hills and ridges (such as the North and South Downs, the Greensand Ridge, and the High Weald), and the weaker clays forming vales (such as the Low Weald) between them. The very resistant rocks of the Lower Greensand, in particular the Hythe Beds, have produced prominent escarpments that form an arc around the northern edge of the Low Weald, running parallel to and just south of the chalk escarpment of the North Downs. This stretch of the Greensand has become the most closely identified with the term "Greensand Ridge", and it includes the second highest point in south-east England, Leith Hill in Surrey. West of the Weald the Lower Greensand has produced a more extensive area of hills and valleys, including the highest point in Sussex, Blackdown. On the south side of the Weald the Lower Greensand also forms another arc of rather less pronounced hills parallel to and just north of the South Downs, which become less prominent the further east one goes.
The Lower Greensand is composed of alternating mudstones (sandy, with clay particles such as smectite) and sandstones, up to a maximum thickness of about , and is composed of a number of distinct formations, namely the Folkestone Beds, Sandgate Beds, Bargate Beds, Hythe Beds and Atherfield Clay.Gallois (1965), p.4.
The Greensand Ridge, capped by the resistant sands and sandstones of the Hythe Beds, reinforced by bands of chert, rises steeply as a series of high, wooded escarpments between Gibbet Hill, Hindhead (), north of Haslemere, and the ridge's highest point, Leith Hill (). It then flattens for several miles, before re-emerging east of Nutfield to run eastwards as a high wooded ridge into an area between Oxted and Sevenoaks known locally as the Chartlands, where it reaches another high point at Toys Hill, Kent (). Here there are views to the south of the Weald from a terrace donated in 1898 by Octavia Hill, one of the founders of the National Trust. The ridge continues eastwards past Sevenoaks, until south-west of Maidstone it is broken by the valley of the Medway. The ridge then continues as far as Pluckley, Kent. From there the land levels until it drops to the old sea-cliff line above Romney Marsh.
In the area around Haslemere local anticlinal features are superimposed on the main axis of the Wealden anticline, causing the outcrop of resistant Hythe Beds to widen from to more than and to produce an escarpment that is particularly marked between Haslemere and Midhurst, where Blackdown rises to , the highest point in Sussex. South of here the Vale of Fernhurst has been eroded down into the Low Weald by what is now a small stream following a line of a gentle west-east trending upfold. This stream, the River Lod, runs parallel to the larger River Rother which flows about 10 km further south in the lee of the chalk escarpment of the South Downs. Valley slope processes in the Vale of Fernhurst have resulted in escarpments to the north and south that are steep enough to have collapsed by land slipping.Friend (2008), pp. 171-172. Further east, the Lower Greensand has not produced any pronounced topographical features.
In many places along the escarpment of the Greensand Ridge erosion by wind and rain, landslips on the steep scarp face, and solifluction in glacial times have further combined to create steep-side coombes, and low hillocks below the scarp.
The Jutes and Saxons who settled in south-east England in the centuries following the collapse of the Roman empire applied the term Weald (a Germanic term for woodland) to the very large, heavily wooded forest that they found lying inland of the coastal lands and river valleys that they initially settled. This forest, difficult to penetrate and settle, and difficult to exploit agriculturally, in due course became an essential part of a system of transhumance whereby each autumn swine would be driven, sometimes over long distances, from the longer-settled areas on the periphery into the Wealden forest to feed on acorns of oak trees and beech mast. For these peoples the term Weald did not include the land cleared of forest and settled earlier, such as the fertile Vale of Holmesdale (which separates the North Downs from the Greensand Ridge), nor the more lightly wooded and open hills found on the sandstones of the Greensand Ridge, which also seem to have been settled earlier.Brandon (2003), pp.13-14. Local people regarded the hills of the Greensand Ridge as overlooking the Weald, rather than forming a part of it, and hence a distinction came to be made between the settlements on the Greensand Ridge, such as Sevenoaks, Sundridge Upland and Boughton Malherbe Upland, and those formed during the later medieval colonisation of the Wealden portion of these parishes, called today Sevenoaks Weald, Sundridge Weald and Boughton Malherbe Weald.Brandon (2003), p.3.
A practice of treating the Greensand Ridge regularly as part of the Weald arose in geology when natural scientists, starting in the late 18th century, began to include it in their analysis of the geological history of the Wealden dome. Geology still confuses by using interchangeably the Weald and the "Wealden Anticline" that embraces all the land bounded by the chalk escarpments of the North and South Downs, including the Greensand hills.
Fuller's earth, which lies interbedded between the Bargate and Sandgate Layers, was much quarried for the cloth industry. The seam, which lies about 20 to 30 feet below the surface between Nutfield and Bletchingley, was considered the best in the country and for several centuries large quantities were excavated. Resources are now running low and little is now extracted.Cowan (1997), p.41.
| Telegraph Hill | 207 | 130 | SU870264 |
| Marley Heights | 216 | 53 | SU890302 |
| Hatch Farm Hill | 211 | 43 | SU898298 |
| Black Down | 280 | 191 | SU919296 |
| Gibbet Hill | 272 | 125 | SU899359 |
| The Warren | 251 | 33 | TQ076424 |
| Pitch Hill | 257 | 85 | TQ082423 |
| Holmbury Hill | 261 | 107 | TQ103429 |
| Leith Hill | 295 | 246 | TQ139431 |
| Crockham Hill | 216 | 41 | TQ445514 |
| Toys Hill | 248 | 117 | TQ469520 |
| Wheatsheaf Hill | 218 | 42 | TQ490516 |
| Raspit Hill | 207 | 34 | TQ577548 |
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