Perry Ledge

Bran Point is a small headland on the Dorset coast in southern England, about halfway between the small villages of Ringstead to the east and Osmington Mills to the west. There is a picturesque cliff-top path between the two villages via Bran Point. The name derives from the brown colouring of the rock forming the cliffs of the headland, caused in part by residual oil deposits. The geology of the area is particularly interesting. The coastline in the area is formed from rocks and shingle with exposed cliffs behind. The Middle White Oolite of the Osmington Oolite more visible to the west has descended to beach level here. At the middle of the cliff, there is nodular rubble consisting of calcitized sponge spicules. Higher in the cliff are reddish brown beds containing Trigonia clavellata fossils.

West Ringstead is a deserted medieval village located on the coast in Dorset, southern England. The village lies on the Jurassic Coast and is located west of the modern village of Ringstead. This medieval village with a church is located in a field to the west of the current Ringstead settlement. It is mentioned in the Domesday Book. It was most likely abandoned after the arrival of the Black Death at Weymouth in 1348. All that can be seen now are variations in the ground level. The site is listed on the National Heritage List for England as a Scheduled Monument (no. 1019393), listed on 15 January 1960.What remains of the village church now forms part of Glebe Cottage, immediately north of the main village site. It has walls consisting of local rubble and the roof covered with modern tiles. Only the chancel and its arch survive from the original medieval church building. The village site is in the parish of Osmington. There was a separate parish of Ringstead until at least the late 15th century. There are four different Ringsteads listed in the Domesday Book, each apparently a separate settlement. One was later given the name "West Ringstead". Another, later known as "Up Ringstead", may have been at the site of the present Upton House to the east above Ringstead Bay towards White Nothe. The location of "Middle Ringstead" is not known. The name of "East Ringstead" survived as a field name on an 1829 Tithe Map in the east of the parish. The location of West Ringstead is just inland from the South West Coast Path. To the east are Ringstead Bay and the headland of White Nothe. To the west are Bran Point and the village of Osmington Mills.

Ringstead is a small seaside village located on the coast in Dorset, southern England. The area lies on the Jurassic Coast and is known for its natural environment and fossils. Ringstead Bay and White Nothe are to the east. Bran Point and Osmington Mills are to the west.

Osmington Mills is a coastal hamlet in the English county of Dorset. It lies within the civil parish of Osmington 5 miles (8.0 km) northeast of Weymouth.

RAF Ringstead is a former Royal Air Force radar station at Ringstead Bay, Dorset, England. It is notable for having served three separate functions: first as a Chain Home early-warning radar station during WWII and then, during the Cold War, as a Rotor station and then, finally, as a USAF Tropospheric scatter station. The first of these functions commenced in 1942; the last of the functions ceased in 1974. The structural remains were Grade II listed in 2020.

Burning Cliff is a cliff under the White Nothe headland at the eastern end of Ringstead Bay, in Dorset, England. The area is well known for its geology and fossils. The cliff is to the northwest of White Nothe. From 1826, the cliff smouldered with an underground fire for several years due to bituminous shale, hence the name.Geologically, Burning Cliff is on a Kimmeridge Clay outcrop. It is immediately west of the fault and Holworth House. The cliff was originally named Holworth Cliff. Today, the cliff consists of landslide, scrubland plants, with the Kimmeridge Clay partially visible. The Kimmeridge Clay above a fault connecting it with the Purbeck Formation to the east under Holworth House. There is a footpath on the cliff. The 1826 fire in the bituminous shale continued for several years. The fire is thought to have been started by heat caused by decomposing pyrite, common in bituminous shale. It emitted sulphurous fumes. At the top of the cliff is a Church of England church, St Catherine-by-the-Sea, Holworth. The cliff lies on the South West Coast Path and forms part of the Jurassic Coast World Heritage Site. The surrounding area is owned by the National Trust.

Ringstead Bay, with the small village of Ringstead at the eastern end and the prominent headland of White Nothe at the western end, is located on the coast in Dorset, southern England. The area lies on the Jurassic Coast and is known for its natural environment and fossils.Ringstead Bay has a pebble and shingle beach with some sand. There are offshore reefs approximately 0.6 kilometres (0.37 mi) in length at the western end opposite the village that are uncovered at low tide. This forms is intertidal zone between the low cliffs to the north and the English Channel to the south. The Ringstead Coral Bed a geological formation exposed at Ringstead Bay, hence the name. It preserves fossils dating back to the Jurassic period. Immediately to the east are the white chalk cliffs of White Nothe, dominating the bay. Below is Burning Cliff. It is possible to walk to the top of White Nothe and back, with views of the bay and across to the Isle of Portland. It is also possible to walk to Ringstead Bay on a circular walk from Lulworth Cove to the east, via Durdle Door and White Nothe.Ringstead Bay also has a nudist beach that is a 20-minutes walk east of the main Ringstead beach.

St Catherine-by-the-Sea is a Church of England church in Holworth, Dorset, England. The small wooden church, which forms part of the Watercombe Benefice, holds a service on the fourth Sunday of the month.

St John's Church was a Church of England church in Poxwell, Dorset, England. It was built in 1867–68 as a replacement to an earlier church and was demolished in 1969.

Poxwell (; sometimes written Pokeswell) is a hamlet and civil parish in the county of Dorset in southwest England. It is located 6 miles (9.7 km) east of Weymouth. The current population of the parish is around 50.

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.The headland faces out over to the Isle of Portland. It is so-called because of the black colouring of the cliffs at this point. To the west along the coast are Redcliff Point and Bowleaze Cove. To the east are the coastal village of Osmington Mills and beyond that Bran Point.

Osmington is a village and civil parish within Dorset, England, situated on the Jurassic Coast 4 miles (6.4 km) north-east of Weymouth. In the 2011 census the parish—which includes the small settlements of Upton, Ringstead and Osmington Mills—had a population of 673.