Exmoor Group
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Exmoor Group
The Exmoor Group is a late Devonian to early Carboniferous lithostratigraphic group (a sequence of rock strata) in southwest England whose outcrop extends from Croyde in north Devon east across Exmoor to Minehead in west Somerset. The group comprises the following formations (in stratigraphic order, i.e., the oldest at the base and the youngest at the top) the: *Pilton Mudstone Formation (Pilton Beds, Pilton Shales) *Baggy Sandstones Formation (Baggy Beds, Marwood Beds) *Upcott Slates Formation *Pickwell Down Sandstones Formation *Morte Slates Formation *Ilfracombe Slates Formation *Hangman Sandstone Formation (Hangman Grits) *Lynton Formation (Lynton Beds, Lynton Slates) Each of these divisions has been given different names by different authors in the past including those shown in brackets above. Some that had been classed as 'formations' (or even in one case as a 'group') are now ' members'. Lynton Formation Extending east from Woody Bay, the Lynton Formation underlies the ...
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Porlock Weir
Porlock Weir is a harbour settlement approximately west of the inland village of Porlock, Somerset, England. "Porlock" comes from the Old English ''port'' '' loca'', meaning an enclosure near a harbour. Porlock Weir refers to the salmon stakes and traps that were situated along the shore. Many cottages date from the 17th century, including the Gibraltar Cottages which have been designated as a grade II listed building. Like most ports in West Somerset, the harbour is tidal and is home to a small flotilla of yachts and is visited by many more in spring and summer. The port has existed for more than a thousand years. The ''Anglo-Saxon Chronicle'' reports that in 1052 Harold Godwinson came from Ireland with nine ships and plundered the area and before that in 866 AD it was raided by Danes. In the 18th and 19th centuries coal from South Wales was the main cargo and in World War II pit props cut in local forests were the return cargo. The ketch ''Lizzy'' was wrecked at Gore Point, ...
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Group (stratigraphy)
In geology, a group is a lithostratigraphic unit consisting of a series of related formations that have been classified together to form a group. Formations are the fundamental unit of stratigraphy. Groups may sometimes be combined into supergroups. Groups are useful for showing relationships between formations, and they are also useful for small-scale mapping or for studying the stratigraphy of large regions. Geologists exploring a new area have sometimes defined groups when they believe the strata within the groups can be divided into formations during subsequent investigations of the area. It is possible for only some of the strata making up a group to be divided into formations. An example of a group is the Glen Canyon Group, which includes (in ascending order) the Wingate Sandstone, the Moenave Formation, the Kayenta Formation, and the Navajo Sandstone. Each of the formations can be distinguished from its neighbor by its lithology, but all were deposited in the same vast ...
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Crowcombe
Crowcombe is a village and civil parish under the Quantock Hills in Somerset, England, southeast of Watchet, and from Taunton. The village has a population of 489. The parish covers the hamlets of Crowcombe Heathfield, Flaxpool, Halsway, Lawford and Triscombe. The village is on the route of the Samaritans Way South West. History The name Triscombe is believed to derive from the Old English words and . The first documentary evidence of the village is by Æthelwulf of Wessex in 854, where it was spelt 'Cerawicombe'. At that time the manor belonged to Glastonbury Abbey. Later Gytha Thorkelsdóttir, wife of Earl Godwin, gave it to the monks of Winchester to make amends for her husband's "treacherous abuses of divers monastic institutions". The Domesday Book of 1086 lists the village as 'Crawcombe', which is believed to come from the Old English words ''craw'' and ''cumb''. The parish of Crowcombe was part of the Williton and Freemanners Hundred. The medieval cross of red s ...
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Quantock Hills
The Quantock Hills west of Bridgwater in Somerset, England, consist of heathland, oak woodlands, ancient parklands and agricultural land. They were England's first Area of Outstanding Natural Beauty, designated in 1956. Natural England have designated the Quantock Hills as a national character area. They are entirely surrounded by another: the Vale of Taunton and Quantock Fringes. The hills run from the Vale of Taunton Deane in the south, for about to the north-west, ending at Kilve and West Quantoxhead on the coast of the Bristol Channel. They form the western border of Sedgemoor and the Somerset Levels. From the top of the hills on a clear day, it is possible to see Glastonbury Tor and the Mendips to the east, Wales as far as the Gower Peninsula to the north, the Brendon Hills and Exmoor to the west, and the Blackdown Hills to the south. The highest point on the Quantocks is Wills Neck, at . Soil types and weather combine to support the hills' plants and animals. In 1970, an ...
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Oare, Somerset
Oare is a village and civil parish on Oare Water on Exmoor in the Somerset West and Taunton district of Somerset, England. It is located east of Lynton and the parish includes the hamlet of Oareford and the village of Culbone which contains its own tiny church. History The village was known as ''Are'' in the Domesday Book of 1086. After the Norman Conquest the manor was granted to Ralph de Pomeray. Later it was held by the Kelly family. Oare was part of the hundred of Carhampton. Governance The parish council has responsibility for local issues, including setting an annual precept (local rate) to cover the council's operating costs and producing annual accounts for public scrutiny. The parish council evaluates local planning applications and works with the local police, district council officers, and neighbourhood watch groups on matters of crime, security, and traffic. The parish council's role also includes initiating projects for the maintenance and repair of parish ...
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Woody Bay, Devon
__NOTOC__ Woody Bay is a bay on the North Devon coast of England, west of Lynton and east of Combe Martin with a stony beach. It lies in the civil parish of Martinhoe at the edge of the Exmoor National Park and is a waypoint on the South West Coast Path. There were once plans to develop the area to become a holiday resort. Access to the remote beach is via a very narrow one mile long steep lane, there is no parking. Around the headland is Lee Abbey Bay that is on the Lee Abbey Estate. This has an accessible beach with parking. History In 1885 the Manor of Martinhoe, including the then-named ''Wooda Bay'', was purchased by Colonel Benjamin Lake, a wealthy solicitor from Orpington in Kent. Perhaps in an effort to emulate Sir George Newnes' efforts in the nearby twin towns of Lynton and Lynmouth, Col. Lake planned to develop the bay as an exclusive resort. He converted Martinhoe Manor House into an Hotel, and in 1894, opened a new golf course at Martinhoe common. Plots of la ...
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Eros Rock - Geograph
In Greek mythology, Eros (, ; grc, Ἔρως, Érōs, Love, Desire) is the Greek god of love and sex. His Roman counterpart was Cupid ("desire").''Larousse Desk Reference Encyclopedia'', The Book People, Haydock, 1995, p. 215. In the earliest account, he is a primordial god, while in later accounts he is described as one of the children of Aphrodite and Ares and, with some of his siblings, was one of the Erotes, a group of winged love gods. Etymology The Greek , meaning 'desire', comes from 'to desire, love', of uncertain etymology. R. S. P. Beekes has suggested a Pre-Greek origin. Cult and depiction Eros appears in ancient Greek sources under several different guises. In the earliest sources (the cosmogonies, the earliest philosophers, and texts referring to the mystery religions), he is one of the primordial gods involved in the coming into being of the cosmos. In later sources, however, Eros is represented as the son of Aphrodite, whose mischievous interventions i ...
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Stratigraphic Unit
A stratigraphic unit is a volume of rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrographic, lithologic or paleontologic features (facies) that characterize it. Units must be ''mappable'' and ''distinct'' from one another, but the contact need not be particularly distinct. For instance, a unit may be defined by terms such as "when the sandstone component exceeds 75%". Lithostratigraphic units Sequences of sedimentary and volcanic rocks are subdivided the basis of their shared or associated lithology. Formally identified lithostratigraphic units are structured in a hierarchy of lithostratigraphic rank, higher rank units generally comprising two or more units of lower rank. Going from smaller to larger in rank, the main lithostratigraphic ranks are Bed, Member, Formation, Group and Supergroup. Formal names of lithostratigraphic units are assigned by geological surveys. Units of formation or hi ...
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Lynton Slates
The Lynton Slates is a geologic formation in England. It preserves fossils dating back to the Devonian period. See also * List of fossiliferous stratigraphic units in England See also *Lists of fossiliferous stratigraphic units in Europe * Lists of fossiliferous stratigraphic units in the United Kingdom References * {{DEFAULTSORT:Fossiliferous stratigraphic units in England England England is a country ... References * Geologic formations of England Devonian System of Europe Devonian England Slate formations {{England-stub ...
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Baggy Sandstones
The Baggy Sandstones is a geologic formation in England. It preserves fossils dating back to the Devonian period. See also * List of fossiliferous stratigraphic units in England See also *Lists of fossiliferous stratigraphic units in Europe * Lists of fossiliferous stratigraphic units in the United Kingdom References * {{DEFAULTSORT:Fossiliferous stratigraphic units in England England England is a country ... References * Geologic formations of England Devonian System of Europe Devonian England Sandstone formations {{England-stub ...
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Formation (stratigraphy)
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness (geology), thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by ...
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Minehead
Minehead is a coastal town and civil parish in Somerset, England. It lies on the south bank of the Bristol Channel, north-west of the county town of Taunton, from the boundary with the county of Devon and in proximity of the Exmoor National Park. The parish of Minehead has a population of approximately 11,981, making it the most populous town in the western part of the Somerset West and Taunton local government district, which in turn, is the worst area in the country for social mobility. This figure includes Alcombe and Woodcombe, suburban villages which have been subsumed into Minehead. There is evidence of human occupation in the area since the Bronze and Iron Ages. Before the Norman conquest, it was held by Ælfgar, Earl of Mercia and after it by William de Moyon and his descendants, who administered the area from Dunster Castle, which was later sold to Sir George Luttrell and his family. There was a small port at Minehead by 1380, which grew into a major trading centre d ...
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