Royal Tunbridge Wells

Royal Tunbridge Wells is a large affluent town in western Kent, England, about 40mi south-east of central London by road, 34. 5mi by rail. The town is close to the border of the county of East Sussex. It is situated at the northern edge of the High Weald, the sandstone geology of which 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 had its heyday as a tourist resort under Beau Nash when the Pantiles and its chalybeate spring attracted visitors who wished to take the waters. Though its popularity waned with the advent of sea bathing, the town remains popular and derives some 30 percent of its income from the tourist industry. The town has a population of around 56, 500 and is the administrative centre of Tunbridge Wells Borough and the UK parliamentary constituency of Tunbridge Wells. HistoryEvidence suggests that during the Iron Age people farmed the fields and mined the iron-rich rocks in the Tunbridge Wells area, and excavations in 1940 and 1957–61 by James Money at High Rocks uncovered the remains of a defensive hill-fort. It is thought that the site was occupied into the era of Roman Britain, and the area continued to be part of the Wealden iron industry until its demise in the late eighteenth century—indeed, an iron forge remains in the grounds of Bayham Abbey, in use until 1575 and documented until 1714.

Royal Tunbridge Wells is a large affluent town in western Kent, England, about 40mi south-east of central London by road, 34. 5mi by rail. The town is close to the border of the county of East Sussex. It is situated at the northern edge of the High Weald, the sandstone geology of which 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 had its heyday as a tourist resort under Beau Nash when the Pantiles and its chalybeate spring attracted visitors who wished to take the waters. Though its popularity waned with the advent of sea bathing, the town remains popular and derives some 30 percent of its income from the tourist industry. The town has a population of around 56, 500 and is the administrative centre of Tunbridge Wells Borough and the UK parliamentary constituency of Tunbridge Wells. HistoryEvidence suggests that during the Iron Age people farmed the fields and mined the iron-rich rocks in the Tunbridge Wells area, and excavations in 1940 and 1957–61 by James Money at High Rocks uncovered the remains of a defensive hill-fort. It is thought that the site was occupied into the era of Roman Britain, and the area continued to be part of the Wealden iron industry until its demise in the late eighteenth century—indeed, an iron forge remains in the grounds of Bayham Abbey, in use until 1575 and documented until 1714.