User:Huligan0/Brandy Bay
on the south coast of the Isle of Purbeck
Brandy Bay is a small secluded southwest-facing bay, with an Oil shale and shingle beach immediately below Gad Cliff and Tyneham Cap, to the east of Worbarrow Bay and to the west of Hobarrow Bay on the south coast of the Isle of Purbeck, in Dorset, England.
Location[edit]
Brandy Bay is located about one kilometre southeast of the ghost village Tyneham, is six kilometres south of Wareham and about 16 kilometres west of Swanage.
Admission to the beach of Brandy Bay is prohibited. Access is solely possible by foot from the South West Coast Path via Hobarrow Bay or by boat. The area around Brandy Bay is owned by the Ministry of Defence (MoD). Lulworth Military Range is part of the Armoured Fighting Vehicles Gunnery School. The 7,500-acre (30 km2) range lies within an Area of Outstanding Natural Beauty and stretches along the coastline between Lulworth Cove to just west of Kimmeridge. Because tanks and Armoured vehicles are used in this area, safety warnings about explosives and unexploded shells are posted around the area by the MoD, visitors are advised to keep to official footpaths and abide to local site notices.[1]
Brandy Bay once had a Roman settlement, but the name derives from the frequent smuggling activities that were taking place here during the 17th and 18th centuries. [2]
Jurassic Coast[edit]
The Jurassic Coast is a UNESCO World Heritage Site. The coastal exposures along the coastline provide a continuous sequence of Triassic, Jurassic and Cretaceous rock formations spanning approximately 185 million years of the Earths history. The Jurassic Coast stretches over a distance of 153 kilometres (95 mi), from Orcombe Point near Exmouth, in the west, to Old Harry Rocks in the east.[3] Brandy Bay is part of the Jurassic Coast.
Geology[edit]
The geology of the Isle of Purbeck is very complex and this is shown very clearly along this stretch of coast. The extreme angular layers of rock seen in the cliffs visibly demonstrate the complex sedimentary folding that affected this area some 30 million years ago. The foldings were caused by the tectonic pressures as the African and European continents collided. During this period, the sediments were twisted horizontally, this is why the younger Cretaceous formations are found further back at the rear of Worbarrow Bay. Brandy Bay lies entirely within the Kimmeridge Clay Formation. Between Brandy Bay and Hobarrow Bay is a wide ledge of the Dolostone (Flats Dolomite Bed) which is called Long Ebb.
See also[edit]
References[edit]
- ^ Ministry of Defence (2003). "Safety and access restrictions: Lulworth ranges". Ministry of Defence. Retrieved 2010-11-16.
{{cite web}}: Cite has empty unknown parameter:|month=(help) - ^ Bruce, Peter (2008). Inshore Along the Dorset Coast. Page 69: Boldre Marine. ISBN 978-1871680416.
{{cite book}}: CS1 maint: location (link) - ^ "Dorset and East Devon Coast". UNESCO World Heritage Centre. 2001. Retrieved 2010-11-16.
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