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. [1] It forms part of the Jurassic Coast.
Freshwater Bay takes its name from a freshwater spring which emerged at the bottom of the cliff. An Admiralty pumping station was built on the clifftop in the 19th century for supplying fresh water to the naval base and to the harbour's breakwaters during their construction. Cheyne House was built for the attendant of the station. The man-made tunnel for the pumped water was known as Cheyne Tunnel, and in 2011 this was blocked by a rockfall. [2]
For many decades and through to the second half of the 20th century the bay was in regular use by commercial fishermen. [3]
The Great Southwell Landslip, Britain's second largest recorded historical landslide, occurred in 1734, between Durdle Pier and Freshwater Bay, along a length of 1.5 miles (2.4 km). [4]
Freshwater Bay is reputed to be one of the best places on Portland for fossil locating. [5] [6] The area is known to be popular for fishing, [7] and the cliffs of the bay are also popular with rock climbers. [8]
Above Freshwater Bay is Cheyne House and its grounds which were used, along with other locations across Portland and Weymouth, in the 1963 film The Damned .
The Isle of Portland is a 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.
Kimmeridge is a small village and civil parish on the Isle of Purbeck, a peninsula on the English Channel coast in Dorset, England. It is situated about 4.5 miles (7.2 km) south of Wareham and 7 miles (11 km) west of Swanage. In 2013 the estimated population of the civil parish was 90.
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.
Southwell is a small coastal village in Tophill on the Isle of Portland, Dorset. As Portland and Dorset's southern-most village, it lies between Portland Bill and the villages of Easton and Weston. Though close to the Bill, the village is sheltered by hills on three sides. It is the only village on Portland not to be designated a conservation area.
Church Ope Cove is a small secluded beach on the sheltered eastern side of the Isle of Portland in Dorset, southern England and is part of the Jurassic Coast. It is found close to the village of Wakeham. The beach has many unusual features for the Isle of Portland. The beach used to be sandy, but quarry debris now covers the sand, and has been worn into rounded pebbles. The pebbles cover a small stream which runs to the sea, which is one of the few active streams remaining on the Isle of Portland.
Pulpit Rock is a coastal feature at Portland Bill, the southern tip of the Isle of Portland, Dorset, England. Representing an open bible leaning on a pulpit, Pulpit Rock was formed in the 1870s after a natural arch was cut away by quarrymen at Bill Quarry. As a quarrying relic, the rock is similar to that of Nicodemus Knob, another quarrying landmark on the island.
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.
Kimmeridge Bay is a bay on the Isle of Purbeck, a peninsula on the English Channel coast in Dorset, England, close to and southeast of the village of Kimmeridge, on the Smedmore Estate. The area is renowned for its fossils, with The Etches Collection in the village of Kimmeridge displaying fossils found by Steve Etches in the area over a 30-year period. It is a popular place to access the coast for tourists. To the east are the Kimmeridge Ledges, where fossils can be found in the flat clay beds.
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.
Balaclava Bay is a bay situated on the edge of Portland Harbour, where the breakwater meets the island, at the northern end of the Isle of Portland, Dorset, in southern England. The bay is part of the Jurassic Coast, a World Heritage Site. The bay is overlooked by the Victorian East Weare Battery, built in the 1860s to protect the harbour. The nearest road within the dockyard of Portland Port is named Balaclava Road.
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.
Hallelujah Bay is a bay located on the west side of the Isle of Portland, Dorset, England. The bay is situated below West Weares, with Clay Ope, Blacknor Point and Mutton Cove further south. Near the cove is a large mound of rock and earth beneath the clifftops known locally as the Green Hump.
Durdle Pier is a disused 17th-century stone shipping quay, located on the Isle of Portland, Dorset, England; part of the Jurassic Coast. It is found close by Yeolands Quarry, on the east side of the island within the area of East Weares and Penn's Weare.
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.
Culverwell Mesolithic Site is a Mesolithic settlement, located on the Isle of Portland, Dorset, England. It is found in the local area known as Culverwell, along the Portland Bill Road. It is within an area of unspoiled countryside, with no past quarrying. The site is maintained by the Association for Portland Archaeology – a small group dedicated to researching, investigating and excavating on Portland.
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.
NCI Portland Bill is a National Coastwatch Institution (NCI) lookout station on the Isle of Portland, Dorset, England. The station is situated 50 metres above sea level on the cliff edge, half a mile north of the tip of Portland Bill. It is located close to the Old Higher Lighthouse.
Southwell Business Park is a business park on the Isle of Portland, Dorset, England. It is housed at the former Admiralty Underwater Weapons Establishment, which closed in 1995 and became the Southwell Business Park in 1997.