Old Harry Rocks are a series of chalk sea stacks located at the eastern end of the Jurassic Coast, near Studland and Swanage in Dorset. They mark the transition between the Jurassic Coast and the chalk formations of the Isle of Purbeck. The site is a well-known geological feature and forms a prominent landmark along this section of coastline.
The rocks stand just offshore beneath Ballard Down, with white chalk cliffs extending inland along the ridge. The stacks are the result of coastal erosion, where cracks in the chalk have widened over time to form isolated pillars. From the clifftop, visitors can see views across Poole Bay and along the coastline towards Swanage. The surrounding area consists of open grassland and exposed cliff edges.
Access is via footpaths from Studland, with the most common route starting near the South Beach or National Trust car parks. The walk to Old Harry Rocks is relatively straightforward, following established paths along the clifftop. There are no facilities directly at the site, though services are available in Studland and Swanage. There is no entry fee, but parking charges may apply at nearby car parks.
The site can be visited throughout the year, with clear conditions offering the best visibility. Summer is the busiest period, particularly during weekends and holidays. The area is suitable for walkers, though care is required near cliff edges due to unstable ground and sheer drops. Paths are generally manageable but can be uneven in places.
Nearby locations include Studland Bay, which offers a series of sandy beaches and access points along the coast. Swanage lies to the south, providing a larger town with facilities and a sheltered beach. Durlston Country Park offers additional coastal walking routes, while Kimmeridge provides access to a quieter and more rugged section of the Jurassic Coast.