The Pantiles The Pantiles The Pantiles is a Georgian colonnade in the town of Royal Tunbridge Wells, Kent, England. Formerly known as The Walks and the (Royal) Parade, it leads from the well that gave the town its name. The area was created following the discovery of a chalybeate spring in the early 17th century and is now a popular tourist attraction. The Pantiles today includes a variety of specialist shops, art galleries, cafés, restaurants and bars as well as a Farmers market held outside every other Saturday. Throughout the summer jazz bands play outside on the bandstand attracting hundreds of people.
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