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 erstwhile Central stations, opened in 1876, remains closed. In 2009 Network Rail installed a 12-car turnback siding just south of Tunbridge Wells station between the Grove Hill and Strawberry Hill tunnels to facilitate a more frequent service and to allow restricted types of London trains starting or terminating at Tunbridge Wells to be operated in 12-car formations. Previously such services were 11-car at most. Average daily passenger flows on trains between Tunbridge Wells and London have increased from about 10,000 in 1999 to over 12,500 in 2008, a compound growth rate of about 2.5 % per year. Average daily passenger