The Jurassic Coast is a World Heritage Site on the English Channel coast of southern England. It stretches from Exmouth in East Devon to Studland Bay in Dorset, a distance of about 96 miles (154 km), and was inscribed on the World Heritage List in mid-December 2001.
Durdle Door is a natural limestone arch on the Jurassic Coast near Lulworth in Dorset, England. It is owned by the Welds, a family who own 12,000 acres (50 km2) in Dorset in the name of the Lulworth Estate. It is open to the public.
Ringstead Bay and the small village of Ringstead are located on the coast in Dorset, southern England. The area lies on the Jurassic Coast and is known for its natural environment and fossils.
Weymouth Bay is a sheltered bay on the south coast of England, in Dorset. It is protected from erosion by Chesil Beach and the Isle of Portland, and includes several beaches, notably Weymouth Beach, a gently curving arc of golden sand which stretches from the resort of Weymouth. Weymouth Bay is situated approximately halfway along the UNESCO Jurassic Coast World Heritage Site.
Church Ope Cove is a small secluded beach on the sheltered eastern side of the Isle of Portland in Dorset, southern England and is part of the Jurassic Coast. It is found close to the village of Wakeham. The beach has many unusual features for the Isle of Portland. The beach used to be sandy, but quarry debris now covers the sand, and has been worn into rounded pebbles. The pebbles cover a small stream which runs to the sea, which is one of the few active streams remaining on the Isle of Portland.
White Nothe is a chalk headland on the English Channel coast at the eastern end of Ringstead Bay, east of Weymouth in Dorset, England. The area is well known for its geology and fossils. Its flanks are the result of prehistoric landslides and the inaccessible slopes of the undercliff provide a secluded wildlife habitat.
Newton's Cove is a small cove with sand, shingle and rock pools, 0.5 kilometres (0.3 mi) south of Weymouth, Dorset, England, overlooking Portland Harbour and next to the Nothe Fort. The beach is mainly used by locals and by tourists who visit the Nothe Gardens and the fort.
Bowleaze Cove is a small sand and shingle beach, near the village of Preston, just to the northeast of Weymouth, Dorset, England. The cove is on the Jurassic Coast and is known for its geology. Just to the west is Furzy Cliff.
Bindon Hill is an extensive Iron Age earthwork enclosing a coastal hill area on the Jurassic Coast near Lulworth Cove in Dorset, England, about 19 kilometres (12 mi) west of Swanage, about 6 kilometres (3.7 mi) south west of Wareham, and about 17 kilometres (11 mi) south east of Dorchester. It is within an Area of Outstanding Natural Beauty.
Redcliff Point is on the south coast of England, to the east of Weymouth in Dorset. It lies just past the eastern end of the sweeping Weymouth Bay on the Jurassic Coast, a UNESCO World Heritage landscape known for its geology. Fossils can be found in the Upper Oxford Clay in this area.
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.
Black Head a headland on the south coast of England, to the east of Weymouth in Dorset. It lies on the Jurassic Coast, a UNESCO World Heritage landscape known for its geology. Fossils can be found in the area.
St Oswald's Bay is located near Lulworth on the Jurassic Coast in Dorset, England.
Dungy Head is a coastal promontory located west of Lulworth Cove on the Jurassic Coast in Dorset, England. It forms the eastern end of St Oswald's Bay. It is composed of Portland stone strata. The surrounding area is popular for coastal walks, which yield impressive views. Cliff-climbing however is dangerous and not recommended.
Furzy Cliff is located on the coast near the village of Preston, just to the east of Weymouth, Dorset, England. It is at the northeastern end of Weymouth Beach, looking out over Weymouth Bay to Portland Harbour and the Isle of Portland. Close by to the east is Bowleaze Cove. Just inland to the north are Jordan Hill and the remains of the Jordan Hill Roman Temple. On the top of the cliff there is a large grass area with good views.
Clay Ope is on the west side of the Isle of Portland in Dorset, England. It forms part of the Jurassic Coast. The geology of the area includes Purbeck Beds, Portland Stone, Portland Sand, and Kimmeridge Clay. Above Clay Ope is West Cliff.
Mutton Cove is a cove, located on the Isle of Portland, Dorset, England; part of the Jurassic Coast. It is found on the west side of Portland. Presumably named after the once-famous Portland sheep, the cove is an erosional indentation just south of the promontory of Blacknor. On the cliff tops of the cove is part of the South West Coast Path and further south is Wallsend Cove and Portland Bill.
Freshwater Bay is a bay on the east side of the Isle of Portland, Dorset, England, south from Church Ope Cove and between the villages of Wakeham and Southwell. It forms part of the Jurassic Coast.
Portland Raised Beach refers to small raised beaches on each side of Portland Bill, on the Isle of Portland, part of the Jurassic Coast in Dorset, England. The main one is known as the West Pleistocene Raised Beach; nearby is the East Pleistocene Raised Beach.
The Great Southwell Landslip occurred in 1734 on the Isle of Portland, Dorset, England near the southerly village of Southwell and extended for a length of 1.5 miles (2.4 km) between Durdle Pier and Freshwater Bay. It remains Britain's second largest recorded historical landslide.
