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  2. Weald - Wikipedia

    en.wikipedia.org/wiki/Weald

    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.

  3. Greensand Ridge - Wikipedia

    en.wikipedia.org/wiki/Greensand_Ridge

    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 ...

  4. High Weald National Landscape - Wikipedia

    en.wikipedia.org/wiki/High_Weald_National_Landscape

    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 ...

  5. Sedlescombe - Wikipedia

    en.wikipedia.org/wiki/Sedlescombe

    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.

  6. Tunbridge Wells Sand Formation - Wikipedia

    en.wikipedia.org/wiki/Tunbridge_Wells_Sand_Formation

    The Tunbridge Wells Sand Formation is a geological unit which forms part of the Wealden Group and the uppermost and youngest part of the unofficial Hastings Beds.These geological units make up the core of the geology of the Weald in the English counties of West Sussex, East Sussex and Kent.

  7. Geology of East Sussex - Wikipedia

    en.wikipedia.org/wiki/Geology_of_East_Sussex

    The geology of East Sussex is defined by the Weald–Artois anticline, a 60 kilometres (37 mi) wide and 100 kilometres (62 mi) long fold within which caused the arching up of the chalk into a broad dome within the middle Miocene, [1] which has subsequently been eroded to reveal a lower Cretaceous to Upper Jurassic stratigraphy.

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  9. Ashdown Forest - Wikipedia

    en.wikipedia.org/wiki/Ashdown_Forest

    The Weald, of which Ashdown Forest is the largest remaining part, stretched for 30 miles (48 km) between the chalk escarpments of the North and South Downs and for over 90 miles (140 km) from east to west from Kent into Hampshire. [62]