Osmington Mills

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.

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.

Perry Ledge is a reef west of Ringstead in Dorset, England.The ledge consists of limestone dating from the Jurassic period and is exposed at low tide. It is located close to Bran Point.

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.

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.

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.

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.

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.

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.The cliff looks over to the Isle of Portland. It is so-called because of the red colouring of the cliffs at this point.Close by to the west are the Broadrock cliffs and Bowleaze Cove. To the east are Black Head and the coastal village of Osmington Mills.

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.

The Osmington White Horse is a hill figure cut into the limestone of Osmington Hill just north of Weymouth in Dorset in 1808. It is in the South Dorset Downs in the parish of Osmington.The figure is of King George III riding his horse and can be seen for miles around. The king was a regular visitor to Weymouth and made it 'the first resort'. The figure is 280 feet (85 m) long and 323 feet (98 m) high and is best viewed from the A353 road. In 1989 the figure was restored for a broadcast of the TV show Challenge Anneka, although the work was subsequently criticised by historians for doing more harm than good. Anneka Rice, presenter of the show, stated that planning permission and advice had been sought before the work.In August 2011 pranksters added a 'horn' made from plastic sheeting to make the horse resemble a unicorn.In 2012, it was announced that for the Olympics 2012, the horse would be cleaned and slightly recut to make it look like the original when it was cut in 1808. Restoration was completed on 11 March 2012, and Princess Anne attended a ceremony at which a new plaque made of local stone was revealed. The restoration was done by volunteers, who spent two years carrying out repairs.The figure is designated as a Scheduled Monument.