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Cloth-making was, apart from iron-making, the other large-scale industry carried out on the Weald of Kent and Sussex in medieval times. The ready availability of wool from the sheep of the Romney Marsh, and the immigration from Flanders in the fourteenth century of cloth-workers – places like Cranbrook attracted hundreds of such skilled workers – ensured its place in Kentish industrial ...
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.
Weald of Kent Grammar School, ... Kent College, Pembury; The King's School, ... Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; ...
Geologically, East Sussex is part of southern anticline of the Weald: the South Downs, a range of moderate chalk hills which run across the southern part of the county from west to east and mirrored in Kent by the North Downs. To the north lie parallel valleys and ridges, the highest of which is the Weald itself (the Hastings beds and Wealden ...
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 ...
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.
Wealden is a local government district in East Sussex, England.Its council is based in Hailsham, the district's second largest town.The district also includes the towns of Crowborough, Polegate and Uckfield, along with numerous villages and surrounding rural areas.
These geological units make up the core of the Weald in the English counties of East Sussex and Kent. The other component formations of the Hastings Beds are the overlying Wadhurst Clay Formation and the Tunbridge Wells Sand Formation. The Hastings Beds in turn forms part of the Wealden Supergroup which underlies much of South East England.
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