St Osmund's Church, Osmington

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.

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.

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.

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.

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.

Broadrock is a cliff on the coast in Dorset, southern England. It faces out into Weymouth Bay between Bowleaze Cove and Redcliff Point. There are many landslips on the cliffs at this point.

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.

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.

Riviera Hotel is a hotel at Bowleaze Cove, Weymouth, Dorset, England. Overlooking Weymouth Bay, the hotel was built in 1936–37 and has been a Grade II listed building since 1997. Historic England has remarked that it "epitomises the austere approach of the modernists in the immediate pre-war era, and suggests the designer's acquaintance with contemporary work in Rome and elsewhere".

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.

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. The beach is made up of mainly shingle and shell with some sandy areas. A small pier divides the beach near the River Jordan outflow. The remains of Jordan Hill Roman Temple are located on Jordan Hill, leading down to Bowleaze. The hill figure of the Osmington White Horse can be seen. A coastal cliff walk leads eastwards from Bowleaze, passing the Broadrock cliffs, Redcliff Point, and thence to Osmington Mills.

The River Jordan (archaically known as the River Jordon) is a river in the county of Dorset, England. The river is approximately 3 miles (4.8 km) long, and includes the tributaries of the Osmington Brook and the Preston River. The River Jordan discharges into the English Channel at Bowleaze Cove, northeast of Weymouth.