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View south across the Weald of Kent as seen from the North Downs Way near Detling. The Weald (/ ˈ w iː l d /) is an area of South East England between the parallel chalk escarpments of the North and the South Downs. It crosses the counties of Hampshire, Surrey, West Sussex, East Sussex, and Kent.
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, 294 metres (965 ft), at Leith Hill in Surrey—the second highest point in south-east England , while another hill in its range, Blackdown , is ...
The High Weald National Landscape is in south-east England. Covering an area of 1,450 square kilometres (560 sq mi), it takes up parts of Kent, Surrey, East Sussex, and West Sussex. [1] It is the fourth largest Area of Outstanding Natural Beauty (AONB) in England and Wales. It has an attractive landscape with a mosaic of small farms and ...
The Wealdway, Kent and East Sussex, is a public footpath that runs for 83 miles / 134 km from Gravesend, Kent on the Thames estuary, to the A259 at Eastbourne, 3 km north of Beachy Head. [ 2 ] Interrelation with other long-distance routes
High Rocks is a key geomorphological site for sandstone weathering features developed on the highest cliffs in the Weald.The Ardingly Sandstone has suffered gentle deformation, and joints have opened out to form spectacular gulls (tension cracks) which are wide enough in places for a person to enter.
The term 'downs' is from Old English dūn, meaning 'hill'.The word acquired the sense of 'elevated rolling grassland' around the 14th century. [7] These hills are prefixed 'south' to distinguish them from another chalk escarpment, the North Downs, which runs roughly parallel to them about 30 mi (48 km) away on the northern edge of the Weald.
Section across southern England showing the inverted nature of the Weald Basin. The Weald Basin (/ ˈ w iː l d /) is a major topographic feature of the area that is now southern England and northern France from the Triassic to the Late Cretaceous. Its uplift in the Late Cretaceous marked the formation of the Wealden Anticline.
Sedlescombe is a village and civil parish in the Rother district of East Sussex, England. The village is on the B2244 road, about 6 miles (10 km) north of Hastings. The parish includes the hamlet of Kent Street, which is on the A21 road. The parish is in the High Weald Area of Outstanding Natural Beauty.
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