Purbeck Hills

East along the top of the Purbeck ridge

Chalk cliffs at the eastern end of Bindon Hill

The Purbeck Hills, also called the Purbeck Ridge, are a ridge of chalk downs in Dorset. The ridge extends from Lulworth Cove in the west to Old Harry Rocks in the east, where it meets the sea. The hills are part of a system of chalk downlands in southern England formed from the Chalk Group which also includes Salisbury Plain and the South Downs.

For most of their length the chalk of the Purbeck Hills is protected from coastal erosion by a band of resistant Portland limestone. Where this band ends, at Durlston Head, the clay and chalk behind has been eroded, creating Poole Bay and the Solent. The ridge of steeply dipping chalk that forms the Purbeck Hills continues further east on the Isle of Wight.

The height of the chalk ridge and proximity to Poole Harbour and the south coast have made the hills of strategic importance. There are a number of Iron Age, Roman and Saxon archaeological sites, such as Nine Barrow Down. At Corfe Castle the hills are broken twice leaving a steep round hill between the ridges on which stood a mediæval castle, guarding the only easy route through the hills, until the Civil War of the 17th century, after which it was slighted by order of Parliament.

Some of the ridge, around the village of Tyneham, near Lulworth, has been closed to the public for use by the army as a firing range. This has protected them from damage from farming and development, and these areas are now nature reserves. At the eastern end Ballard Down is a National Trust nature reserve which is managed for its calcareous grassland habitat.

Named hills

• Nine Barrow Down (653 feet)
• Ridgeway Hill (653 feet)
• Creech Barrow Hill (633 feet)
• Bindon Hill (551 feet), overlooking Lulworth Cove