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Mupe Bay
Mupe Bay is a bay with a shingle beach to the east of Lulworth Cove in Dorset, England, and is part of the Jurassic Coast World Heritage Site. The bay exposes a sequence of Cretaceous rocks from the Bindon Hill Chalk in the north through the Wealden Beds to the Purbeck Beds in the south at Mupe Rocks. Mupe Bay is only accessible when the Lulworth Ranges are open to the public. It can be reached by a walk from the car park at Lulworth Cove. To the south are Mupe Ledges and out to sea Mupe Rocks. Black Rock is located at the eastern end of the bay. See also * List of Dorset beaches This is a list of notable beaches in the United Kingdom. England * Bigbury-on-Sea, Devon * Biggar, Cumbria * Blackpool, Lancashire * Blackpool Sands, Devon * Bournemouth, Dorset * Brean, Somerset * Bridlington, East Riding of Yorkshire * Br ... References External links Ian West's ''Geology of the Wessex Coast'' Field Guide including photographs Bays of Dorset Jurassic Coast [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bindon Hill
Bindon Hill is an extensive Iron Age earthwork enclosing a coastal hill area on the Jurassic Coast near Lulworth Cove in Dorset, England, about west of Swanage, about south west of Wareham, and about south east of Dorchester. It is within an Area of Outstanding Natural Beauty. Hill fort The main rampart and external ditch (univallate) run for over 2 km along an east-west ridge parallel to the coast, which lies about 750 m to the south. The ridge rises to 168 m and the cliffs are 30–120 m high. At the western end, an incomplete series of ramparts curve back to the cliffs of Lulworth Cove. At the eastern end, the main rampart reaches the cliffs on the north side of Mupe Bay. The total enclosed area is about 110 ha. The enormous enclosed area, lack of evidence of settlement in the interior, and the impossibility of effectively defending such a large perimeter, all suggest it was primarily an enclosed pasture for domesticated animals, not a strategic tribal hill fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Dorset Beaches
This is a list of notable beaches in the United Kingdom. England * Bigbury-on-Sea, Devon * Biggar, Cumbria * Blackpool, Lancashire * Blackpool Sands, Devon * Bournemouth, Dorset * Brean, Somerset * Bridlington, East Riding of Yorkshire * Brighton, Sussex * Bude, Cornwall * Burnham-on-Sea, Somerset * Castle Cove, Dorset * Chesil Beach, Dorset * Church Ope Cove, Dorset * Clacton-on-Sea, Essex * Crantock, Cornwall * Dawlish Warren, Devon * Earnse Bay, Cumbria * Exmouth, Devon * Fistral Beach, Cornwall * Goodrington Sands, Devon * Great Yarmouth, Norfolk * Gyllyngvase, Cornwall * Holywell Bay, Cornwall * Lowestoft, Suffolk * Lulworth Cove, Dorset * Lyme Regis, Dorset * Maenporth, Cornwall * Margate, Kent * Minehead, Somerset * Morecambe Bay, Lancashire * Mount's Bay, Cornwall * Newquay, Cornwall * Paignton, Devon * Perranporth, Cornwall * Porthcurno, Cornwall * Saunton Sands, Devon * Scarborough, North Yorkshire * Slapton Sands, Devon * Southend-on-Sea, Essex * St Oswald's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lulworth Ranges
The Lulworth Ranges are military firing ranges located between Wareham and Lulworth in Dorset, England. They cover an area of more than , are leased in a rolling contract from the Weld Estate by the Ministry of Defence and are part of the Armoured Fighting Vehicles Gunnery School based at Lulworth Camp. The ranges were established in 1917. Location The ranges are about west of Swanage and about east of Dorchester. They lie within an Area of Outstanding Natural Beauty and stretches along the coastline between the east of Lulworth Cove to just west of Kimmeridge. The coastline is part of the Jurassic Coast, a UNESCO World Heritage Site. The range includes the ghost village of Tyneham, deserted in 1943 and abandoned permanently following its compulsory purchase by the Army in 1948. Use The ranges are used for static and mobile live-firing practice by tanks and other armoured vehicles. The ranges are cleared for use by tank main armament and other vehicle-mounted heavy weapon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
University Of Southampton
, mottoeng = The Heights Yield to Endeavour , type = Public research university , established = 1862 – Hartley Institution1902 – Hartley University College1913 – Southampton University College1952 – gained university status by royal charter , chancellor = Ruby Wax , vice_chancellor = Mark E. Smith , head_label = Visitor , head = Penny Mordaunt , location = Southampton, Hampshire, England , campus = City Campus , academic_staff = 2,715 (2020) , administrative_staff = 5,001 , students = () , undergrad = () , postgrad = () , colours = Navy blue, light sea green and dark red , endowment = £14.9 million , budget = £578.4 million , affiliations = ACU EUAPort-City University LeagueRussell GroupSES (universities), SESSET ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Purbeck Beds
The Purbeck Group is an Upper Jurassic to Lower Cretaceous lithostratigraphic group (a sequence of rock strata) in south-east England. The name is derived from the district known as the Isle of Purbeck in Dorset where the strata are exposed in the cliffs west of Swanage. The Purbeck Group is famous for its fossils of reptiles and early mammals. This sequence of rocks has gone by various names in the past including amongst others the Purbeck Beds, Purbeck Formation, Purbeck Limestone Formation and Purbeck Stone. Rocks of this age have in the past been called the Purbeckian stage by European geologists. The Purbeckian corresponds with the Tithonian to Berriasian stages of the internationally used geologic timescale. Outcrops The Purbeck Group outcrops follow the line of the Jurassic outcrop from Dorset, through the Vale of Wardour, Swindon, Garsington, Brill and Aylesbury. In East Sussex, the Purbeck Group outcrops at three locations north and northwest west of Battle, East Suss ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wealden Beds
The Wealden Group, occasionally also referred to as the Wealden Supergroup, is a group (a sequence of rock strata) in the lithostratigraphy of southern England. The Wealden group consists of paralic to continental (freshwater) facies sedimentary rocks of Berriasian to Aptian age and thus forms part of the English Lower Cretaceous. It is composed of alternating sands and clays. The sandy units were deposited in a flood plain of braided rivers, the clays mostly in a lagoonal coastal plain.Jackson (2008) The Wealden Group can be found in almost all Early Cretaceous basins of England: its outcrops curve from the Wessex Basin in the south to the Cleveland Basin in the northeast. It is not found in northwest England and Wales, areas which were at the time tectonic highs where no deposition took place. The same is true for the London Platform around London and Essex. Offshore, the Wealden Group can reach a thickness of 700 metres. The terms ''Wealden'' and ''Wealden facies'' are also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Heritage Site
A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for having cultural, historical, scientific or other form of significance. The sites are judged to contain " cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site must be a somehow unique landmark which is geographically and historically identifiable and has special cultural or physical significance. For example, World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains, or wilderness areas. A World Heritage Site may signify a remarkable accomplishment of humanity, and serve as evidence of our intellectual history on the planet, or it might be a place of great natural beauty. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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