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. [1] Fossils can be found in the Upper Oxford Clay in this area. [2]
England is a country that is part of the United Kingdom. It shares land borders with Wales to the west and Scotland to the north-northwest. The Irish Sea lies west of England and the Celtic Sea lies to the southwest. England is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight.
Weymouth is a seaside town in Dorset, England, situated on a sheltered bay at the mouth of the River Wey on the English Channel coast. The town is 11 kilometres (7 mi) south of Dorchester and 8 kilometres (5 mi) north of the Isle of Portland. The town's population is 52,323 (2011). Weymouth has a metropolitan population of 71,083 (2016). The town is the third largest settlement in Dorset after Bournemouth and Poole.
Dorset is a county in South West England on the English Channel coast. The ceremonial county comprises the unitary authority areas of Bournemouth, Christchurch and Poole and Dorset. Covering an area of 2,653 square kilometres (1,024 sq mi), Dorset borders Devon to the west, Somerset to the north-west, Wiltshire to the north-east, and Hampshire to the east. The county town is Dorchester which is in the south. After the reorganisation of local government in 1974 the county's border was extended eastward to incorporate the Hampshire towns of Bournemouth and Christchurch. Around half of the population lives in the South East Dorset conurbation, while the rest of the county is largely rural with a low population density.
The cliff looks over to the Isle of Portland. It is so-called because of the red colouring of the cliffs at this point. [3]
The Isle of Portland is a limestone tied island, 4 miles (6 km) long by 1.7 miles (2.7 km) wide, in the English Channel. Portland is 5 miles (8 km) south of the resort of Weymouth, forming the southernmost point of the county of Dorset, England. A barrier beach called Chesil Beach joins it to the mainland. The A354 road passes down the Portland end of the beach and then over the Fleet Lagoon by bridge to the mainland. Portland and Weymouth together form the borough of Weymouth and Portland. The population of Portland is 12,400.
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.
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.
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.
Bran Point is a small headland on the Dorset coast in southern England, about half way 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.
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.
Chalk is a soft, white, porous, sedimentary carbonate rock, a form of limestone composed of the mineral calcite. Calcite is an ionic salt called calcium carbonate or CaCO3. It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite shells (coccoliths) shed from micro-organisms called coccolithophores. Flint (a type of chert) is very common as bands parallel to the bedding or as nodules embedded in chalk. It is probably derived from sponge spicules or other siliceous organisms as water is expelled upwards during compaction. Flint is often deposited around larger fossils such as Echinoidea which may be silicified (i.e. replaced molecule by molecule by flint).
Durdle Door is a natural limestone arch on the Jurassic Coast near Lulworth in Dorset, England.
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.
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.
Greenhill is a suburb to the northeast of Weymouth in Dorset, England, with a sand and shingle beach.
Worbarrow Bay is a large broad and shallow bay just to the east of Lulworth Cove on the Isle of Purbeck, Dorset, England.
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.
Pondfield Cove is a small, secluded, south-facing cove immediately to the east of Worbarrow Tout and west of Gad Cliff on the south coast of the Isle of Purbeck, in Dorset, England. It is about 6 kilometres (3.7 mi) south of Wareham and about 16 kilometres (10 mi) west of Swanage.
Jordan Hill is located near the coast close to the village of Preston, just to the east of Weymouth, Dorset, England. The hill leads down to Furzy Cliff on the coast to the south. Close by to the east is Bowleaze Cove. The hill figure of the Osmington White Horse can be seen from the hill to the north.
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.
Dorset is a county located in the middle of the south coast of England. It lies between the latitudes 50.512°N and 51.081°N and the longitudes 1.682°W and 2.958°W, and occupies an area of 2,653 km². It spans 90 kilometres (56 mi) from east to west and 63 kilometres (39 mi) from north to south.
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.
Wallsend 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, further south from Mutton Cove, and situated between Southwell Business Park and Portland Bill. The cliff tops above the cove are part of the South West Coast Path.
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.
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.
Coordinates: 50°38′00″N2°24′32″W / 50.6333°N 2.4089°W
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.