Royal Tunbridge Wells small districts, "named after the hills on which they stand, Mount Ephraim, Mount Pleasant and Mount Sion; the other is called the Wells..." The 1680s saw a building boom in the town: carefully planned shops were built beside the long Pantiles promenade (then known as the Walks), and the Mount Sion road, on which lodging house keepers were to build, was laid out in small plots. Tradesmen in the town dealt in the luxury goods demanded by their patrons, which would certainly have included Tunbridge ware, a kind of decoratively inlaid woodwork. "They have made the wells very commodious by
Tunbridge Wells Sand Formation Tunbridge Wells Sand Formation The Tunbridge Wells Sand Formation is a geological unit which forms part of the Wealden Group and the uppermost and youngest part of the unofficial Hastings Beds. These geological units make up the core of the geology of the Weald in the English counties of West Sussex, East Sussex and Kent. The other component formations of the Hastings Beds are the underlying Wadhurst Clay Formation and the Ashdown Formation. The Hastings Beds in turn form part of the Wealden Group which underlies much of southeast England. The sediments of the Weald, including the Tunbridge Wells Sand