The North Downs Way National Trail is a long-distance path in southern England, opened in 1978. It runs from Farnham to Dover, past Guildford, Dorking, Merstham, Otford and Rochester, along the Surrey Hills Area of Outstanding Natural Beauty (AONB) and Kent Downs AONB.

Planning for a new Long Distance Path, as they were classified in 1949, began in Kent in 1950. After an extensive survey, it was agreed that a route on "a line which offers the best scenic qualities for the walker" along the ridge of the North Downs, rather than the Pilgrim's Way (which even in the 1960s was predominantly metalled road), was preferred. Working alongside Surrey county Council, plans were eventually submitted in 1966.

The North Downs Way was officially designated by then Minister of Housing and Local Government, Anthony Greenwood, on 14 July 1969, and opened in parts shortly afterwards, becoming fully open in 1978. At that time, it was 141 miles in length, 36 miles of which were newly created Public Rights of Way.

The North Downs are a ridge of chalk hills in south east England that stretch from Farnham in Surrey to the White Cliffs of Dover in Kent.Westerham Heights, at the northern edge of the North Downs, near Bromley, South London, is the highest point in London at an elevation of 245 metres. The North Downs lie within two Areas of Outstanding Natural Beauty (AONBs), the Surrey Hills and the Kent Downs. The North Downs Way National Trail runs along the North Downs from Farnham to Dover.

Etymology

'Downs' is from Old English dun meaning, amongst other things, 'hill'. The word acquired the sense of 'elevated rolling grassland' around the fourteenth century. These hills are prefixed 'north' to distinguish them from the morphologically similar range of hills - the South Downs - which run roughly parallel to them but some 50 km (31 mi) to the south.

Geography

The narrow spine of the Hog's Back between Farnham and Guildford forms the western extremity of the North Downs, whilst the cliffs between Folkestone and Deal terminate the ridge in the east. There are two distinct aspects, the steep south-facing escarpment and the gentle north-facing dip slope. The southern boundary is defined by the foot of the escarpment which gives way to the flat, broad clay lands between the Downs and Greensand Ridge known as the Vale of Holmesdale. The northern boundary is less apparent but occurs where the chalk submerges below the more recent Paleocene deposits.