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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 Rocks - Wikipedia

    en.wikipedia.org/wiki/High_Rocks

    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.

  5. 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 ...

  6. Southern Sandstone - Wikipedia

    en.wikipedia.org/wiki/Southern_Sandstone

    Steps and rocks at High Rocks outside Tunbridge Wells. Southern Sandstone is a local name for the Ardingly Sandstone of southeast England, a soft sandstone of Cretaceous age separating the Tunbridge Wells Sands from the overlying Grinstead Clay.

  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.

  8. South Downs - Wikipedia

    en.wikipedia.org/wiki/South_Downs

    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.

  9. Crowborough - Wikipedia

    en.wikipedia.org/wiki/Crowborough

    Crowborough is a town and civil parish in East Sussex, England, in the Weald at the edge of Ashdown Forest in the High Weald Area of Outstanding Natural Beauty, 7 miles (11 km) south-west of Royal Tunbridge Wells and 33 miles (53 km) south of London. It had a population 20,607 at the 2011 Census.

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