Durlston Bay (also known as Durdlestone Bay) [1] is a small bay next to a country park of the same name, just south of the resort of Swanage, on the Isle of Purbeck in Dorset, England. It has been a renowned site for Lower Cretaceous fossils since the initial discovery of fragments there by Samuel Beckles in the 1850s. [2]
Swanage is a coastal town and civil parish in the south east of Dorset, England. It is at the eastern end of the Isle of Purbeck and one of its two towns, approximately 6+1⁄4 miles (10 km) south of Poole and 25 miles (40 km) east of Dorchester. In the 2011 census the civil parish had a population of 9,601. Nearby are Ballard Down and Old Harry Rocks, with Studland Bay and Poole Harbour to the north. Within the parish are Durlston Bay and Durlston Country Park to the south of the town. The parish also includes the areas of Herston, just to the west of the town, and Durlston, just to the south.
A discordant coastline occurs where bands of different rock types run perpendicular to the coast.
The Isle of Purbeck is a peninsula in Dorset, England. It is bordered by water on three sides: the English Channel to the south and east, where steep cliffs fall to the sea; and by the marshy lands of the River Frome and Poole Harbour to the north. Its western boundary is less well defined, with some medieval sources placing it at Flower's Barrow above Worbarrow Bay. According to writer and broadcaster Ralph Wightman, Purbeck "is only an island if you accept the barren heaths between Arish Mell and Wareham as cutting off this corner of Dorset as effectively as the sea." The most southerly point is St Alban's Head.
Durdle Door is a natural limestone arch on the Jurassic Coast near Lulworth in Dorset, England. Although privately owned by the Lulworth Estate, it is open to the public.
Purbeck was a local government district in Dorset, England. The district was named after the Isle of Purbeck, a peninsula that forms a large proportion of the district's area. However, it extended significantly further north and west than the traditional boundary of the Isle of Purbeck which is the River Frome. The district council was based in the town of Wareham, which is itself north of the Frome.
Durlston Country Park is a 320-acre country park and nature reserve stretching along the coast of the Isle of Purbeck on the outskirts of Swanage in Dorset, England. The park is a popular destination for tourists to enjoy the walks, views, visitor centre, climbing, and wildlife, including Durlston Castle, the Great Globe, Tilly Whim Caves, and Anvil Point Lighthouse. It is a gateway to the Jurassic Coast World Heritage Site, forms part of the 630 mile South West Coast Path, and is owned by Dorset Council.
The Purbeck Hills, also called the Purbeck Ridge or simply the Purbecks, are a ridge of chalk downs in Dorset, England. It is formed by the structure known as the Purbeck Monocline. 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.
Purbeck Marble is a fossiliferous limestone found in the Isle of Purbeck, a peninsula in south-east Dorset, England. It is a variety of Purbeck stone that has been quarried since at least Roman times as a decorative building stone.
Durlston is an area of Swanage, in Dorset, England. The area was developed by George Burt as a residential suburb, and includes many large Victorian villas as well as modern developments.
Man o' War Cove lies on the Dorset coast in southern England and is flanked by the rocky, steep and slightly projecting headlands of Durdle Door to the west and Man O War Head to the east.
Tilly Whim Caves consists of three stone quarries in Durlston Country Park, 1 mile (1.6 km) south of Swanage, on the Isle of Purbeck, in Dorset, southern England. The Tilly Whim Caves are a part of the Jurassic Coast.
Purbeck stone refers to building stone taken from a series of limestone beds found in the Upper Jurassic to Lower Cretaceous Purbeck Group, found on the Isle of Purbeck, Dorset in southern England. The best known variety of this stone is Purbeck Marble. The stone has been quarried since at least Roman times up to the present day.
Mupe Bay is a bay with a shingle beach to the east of Lulworth Cove in Dorset, England, and is part of the Jurassic Coast World Heritage Site.
Worbarrow Tout is a promontory at the eastern end of Worbarrow Bay on Isle of Purbeck in Dorset on the south coast of England, about 6 kilometres (3.7 mi) south of Wareham and about 16 kilometres (10 mi) west of Swanage. Immediately to its east is Pondfield Cove.
Cow Corner is the north-western end of Worbarrow Bay, a small secluded bay on the south coast of the Isle of Purbeck, in Dorset England.
Anvil Point is part of the Jurassic Coast on the Isle of Purbeck in Dorset, England. It is within the grounds of Durlston Country Park and is about 3 kilometres (1.9 mi) from Swanage town centre. Anvil Point Lighthouse is located on the point.
The Great Globe at Swanage is one of the largest stone spheres in the world and stands at Durlston Castle within Durlston Country Park, a 113-hectare (280-acre) country park and nature reserve. It is constructed of Portland stone, weighs about 40 tonnes and is 3 metres (10 ft) in diameter.
Durlston Castle stands within Durlston Country Park, a 1.13 square-kilometre (280-acre) country park and nature reserve stretching along the coastline south of Swanage, on the Isle of Purbeck in Dorset.
The Lulworth Formation is a geologic formation in England. It dates from the late Tithonian to the mid Berriasian. It is a subunit of the Purbeck Group. In Dorset, it consists of three members, which are in ascending order, the Mupe Member, the Ridgway Member, and the Warbarrow Tout Member. The Mupe Member is typically 11 to 16 m thick and largely consists of marls and micrites with interbeds of calcareous mudstone. The Ridgeway Member is about 3 to 7 m thick and consists of in its western portion carbonaceous muds, marls and micrites, in the east the muds are replaced by micritic limestone. The Warbarrow Tout Member is 17 to 39 m thick and consists of limestone at the base and micrite and mudstone for the rest of the sequence, this member is the primary source of the vertebrate fossils within the formation. Elsewhere the unit is undifferentiated.
Coordinates: 50°36′04″N1°56′55″W / 50.60111°N 1.94861°W
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