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 Formation, were deposited during the Early Cretaceous Period, which lasted for approximately 40 million years from 140 to 100 million years ago. The Tunbridge Wells Sands are of Late Valanginian age. The Formation takes its name from the spa town of Tunbridge Wells in Kent. The Tunbridge Wells Sand Formation comprises complex cyclic sequences of siltstones with sandstones and clays, typically fining upwards, and is lithologically similar to the older Ashdown Formation. It has a total thickness typically in the region of about 75 m. However, near Haywards Heath borehole data has proven the formation to be up to 150m