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  2. Weald Basin - Wikipedia

    en.wikipedia.org/wiki/Weald_Basin

    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.

  3. Vale of Kent - Wikipedia

    en.wikipedia.org/wiki/Vale_of_Kent

    The High Weald is in lime green (9a); the Low Weald, darker green (9). Chalk Downs, pale green (6) Geological section from north to south: High and Low Weald shown as one The Weald is the eroded remains of a geological structure, an anticline , a dome of layered Lower Cretaceous rocks cut through by erosion to expose the layers as sandstone ...

  4. Ohio State Route 66 - Wikipedia

    en.wikipedia.org/wiki/Ohio_State_Route_66

    State Route 66 (SR 66) is a north–south state highway in the northwestern portion of the U.S. state of Ohio. Its southern terminus is at U.S. Route 36 (US 36) in Piqua, and its northern terminus is at US 20 in Fayette. South of Defiance it generally follows the route of the former Miami and Erie Canal.

  5. 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.

  6. Wadhurst Clay Formation - Wikipedia

    en.wikipedia.org/wiki/Wadhurst_Clay_Formation

    The Wadhurst Clay Formation is a geological unit which forms part of the Wealden Group and the middle part of the now unofficial Hastings Beds.These geological units make up the core of the geology of the High Weald in the English counties of West Sussex, East Sussex and Kent.

  7. Ashdown Formation - Wikipedia

    en.wikipedia.org/wiki/Ashdown_Formation

    The Ashdown Formation is a geological unit, which forms part of the Wealden Group and the lowermost and oldest part of the now unofficial Hastings Beds.These geological units make up the core of the Weald in the English counties of East Sussex and Kent.

  8. 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 ...

  9. File:KentGeologyWealdenDomeSimple.svg - Wikipedia

    en.wikipedia.org/wiki/File:KentGeologyWealden...

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