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
Royal Tunbridge Wells Tunbridge Wells. The town is sited at the head of a valley that runs south-east to Groombridge; like the River Teise, which originates in Tunbridge Wells, the stream in the valley is one of the many tributaries of the River Medway, which runs through a much larger valley north of the High Weald. Nearby villages have been subsumed into the built-up area of the town, so that now it incorporates High Brooms to the north, Hawkenbury to the south, and Rusthall (whose name resonates with the iron content of the rocks) to the west. Royal Tunbridge Wells is twinned with: