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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.
So far only about two dozen sites have been identified where iron was made before the Roman invasion, mostly scattered across East Sussex and the Vale of Kent.A large site at Broadfield, Crawley is the westernmost place where smelting has been ascertained, although there is a possible site associated with an Iron Age enclosure at Piper's Copse near Northchapel in the western Weald.
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 ...
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 ...
The Wealden hall house is a type of vernacular medieval timber-framed hall house traditional in the south east of England. Typically built for a yeoman, it is most common in Kent (hence "Wealden" for the once densely forested Weald) and the east of Sussex but has also been built elsewhere. [1]
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 ...
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.
In Elizabeth's reign, Sussex was open to the older Protestant forms practised in the Weald as well as the newer Protestant forms coming from Continental Europe; combined with a significant Catholic presence, Sussex was in many ways out of step with the rest of southern England.