Burning Cliff

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.

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.

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.

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.

White Nothe (meaning "White Nose") 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. A zigzag path up the cliff is believed to be one of the locations alluded to as a smuggler's path in the British children's book Moonfleet by J. Meade Falkner. Walking to the base of White Nothe along the shore from Ringstead Bay is possible, but it is cut off at high tide, so much care should be taken. At the top of the Smugglers path, a protruding nose shape comes out of the white cliff, giving the name to the area. The area is partly owned by the National Trust. From the top of White Nothe, to the east, the chalk headland of Bat's Head can be viewed. Walking east along a clifftop path below the summit of Chaldon Hill is possible to Durdle Door and Lulworth Cove. The Isle of Portland can be seen to the southwest across the sea. Immediately to the northwest of White Nothe is the Burning Cliff, which from 1826 smouldered with an underground fire for several years due to the bituminous shale. Situated at the top of White Nothe is a World War II pillbox, constructed in 1940–41 of brick and concrete, as part of the anti-invasion measures. Unusually, the structure is also fitted with a Royal Observer Corps observation post built on top, which was to spot and report aircraft. There is also a row of former coastguards' cottages. White Nothe has featured in artworks.

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.

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.

Chaldon Hill, also called Chaldon Down, is one of the highest hills, 178 metres (584 ft), on South Dorset's Jurassic Coast in England. The summit is about 1.5 miles (2.4 km) west of Durdle Door. A bridleway crosses the hill just below the summit, whilst the South West Coast Path makes its way down the steep hillside to the beach heading for Durdle Door. At the summit is a tumulus and trig point. There are navigation beacons about 200 metres (220 yd) to the southeast. The hill is flanked by two coastal headlands: White Nothe and Bat's Head.

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.

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.