Royal Tunbridge Wells Royal Tunbridge Wells Royal Tunbridge Wells, previously just Tunbridge Wells, is a town in western Kent, England, south-east of central London, close to the border with East Sussex upon the northern edge of the High Weald, whose sandstone geology is exemplified by the rock formations at the Wellington Rocks and High Rocks. The town came into being as a spa in the Restoration and enjoyed its heyday as a fashionable resort in the mid-1700s under Beau Nash when the Pantiles, and its chalybeate spring, attracted significant numbers of visitors who wished to take the waters. Though its popularity as a
Tunbridge Wells Sand Formation of up to 12m. It is particularly well exposed throughout the region between East Grinstead, West Sussex, and Tunbridge Wells, Kent, at localities such as; Stone Farm south of East Grinstead; Chiddinglye Rocks near West Hoathly; Toad Rock, Bull’s Hollow and Happy Valley west of Tunbridge Wells; and Harrisons Rocks, Bowles Rocks and High Rocks near Crowborough. At all of these places the Ardingly Sandstone forms a weathering-resistant layer, relative to the rest of the formation, which has become very popular with rock climbers and is known locally as Southern Sandstone. These are the closest rock climbing crags to London