Cateran Hole
Cateran Hole is a circa 35m length cave set in the Gritstone of Cateran Hill in Northumberland. It lies about 4 miles due north of Eglingham, and can be reached by lining up the tall mast behind the farm with the left-hand end of the wood to the side of the Quarry House farm (to the north of the cave), then walking on this bearing. A shallow crater with cut steps leads down into an easy rift passage which ultimately chokes. After the initial steepness of the steps, the passage is roomy with a slight downward tilt, running between two large planes of Gritstone which close in above. After about 30m a block, protruding downwards from the ceiling, reduces the route to a crawl into a small chamber which is choked by large blocks ahead. This crawl is sandy and often completely dry, although in very wet weather it occasionally sumps. The main fault, however, continues, and it is likely that this cave could be extended by concerted digging (a dangerous activity), although it is difficult ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cateran Hole Interior
The term cateran (from the Goidelic languages, Gaelic ''ceathairne'', a collective word meaning "peasantry") historically referred to a band of fighting men of a Scotland Scottish Highlands, Highland clan; hence the term applied to the Highland, and later to any, Banditry, marauders or Cattle raiding, cattle-lifters. An individual member is a ceithernach or catanach, but Walter Scott calls an individual a cateran (e.g. in ''Rob Roy (novel), Rob Roy'', ''Chronicles of the Canongate''). According to Randy Lee Eichoff it derives from Old Celtic 'cat' (battle, war) and 'nach' (man, fellow) Catanach means war-man, warrior. Its plural is ceithern or ceithrenn or caithereine or kettering or kettenring and several other spellings. They are mentioned in the Dunkeld Litany: Magnus Magnusson states that some Highland chieftains retained substantial private armies of professional soldiers, known as 'ceatharn', to be used against their neighboursMagnusson, Magnus (2000) ''Scotland, The Sto ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cave
Caves or caverns are natural voids under the Earth's Planetary surface, surface. Caves often form by the weathering of rock and often extend deep underground. Exogene caves are smaller openings that extend a relatively short distance underground (such as rock shelters). Caves which extend further underground than the opening is wide are called endogene caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called Caving, ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganisms, pressure, and atmospheric influences. Isotopic dating techniques can be applied to cave sedime ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Gritstone
Gritstone or grit is a hard, coarse-grained, siliceous sandstone. This term is especially applied to such sandstones that are quarried for building material. British gritstone was used for millstones to mill flour, to grind wood into pulp for paper and for grindstones to sharpen blades. "Grit" is often applied to sandstones composed of angular sand grains. It may commonly contain small pebbles. "Millstone Grit" is an informal term for a succession of gritstones which are to be found in the Pennines (including the Peak District) of northern England. These sediments were laid down in the late (upper) Paleozoic era, in the Carboniferous period, in deltaic conditions. The Millstone Grit Group is a formal stratigraphic term for this sequence of rocks. The gritstone edges of the Peak District The Peak District is an Highland, upland area in central-northern England, at the southern end of the Pennines. Mostly in Derbyshire, it extends into Cheshire, Greater Manchester, Sta ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Northumberland
Northumberland ( ) is a ceremonial counties of England, ceremonial county in North East England, on the Anglo-Scottish border, border with Scotland. It is bordered by the North Sea to the east, Tyne and Wear and County Durham to the south, Cumbria to the west, and the Scottish Borders council area to the north. The town of Blyth, Northumberland, Blyth is the largest settlement. Northumberland is the northernmost county in England. The county has an area of and a population of 320,274, making it the least-densely populated county in England. The south-east contains the largest towns: Blyth, Northumberland, Blyth, Cramlington, Ashington, Bedlington, and Morpeth, Northumberland, Morpeth, the last of which is the administrative centre. The remainder of the county is rural, the largest towns being Berwick-upon-Tweed in the far north and Hexham in the south-west. For local government purposes Northumberland is a Unitary authorities of England, unitary authority area. The county Histo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Eglingham
Eglingham is a village in Northumberland, England, situated about north-west of Alnwick and from Wooler. It lies in the sheltered valley of the Eglingham Burn, a tributary of the River Aln, about above sea level, in a rural conservation area set amongst rolling countryside, within of the Cheviot Hills. The village is surrounded by mainly arable farmland, moorland and woodland, including an arboretum and some commercial forestry. The village has about 60 dwellings and a population of about 100, most situated either side of the through-road, and including the local manorial property, Eglingham Hall. Eglingham is also a parish, about in length by four and a half in breadth, with an area of . It comprises 2 villages: South Charlton and Eglingham; and 4 settlements – Bassington, Ditchburn, Harehope, Shipley – and several smaller places. The River Breamish, which rises in the Cheviots, runs through the parish. The geological composition of the parish includes ric ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chillingham Castle
Chillingham Castle is a medieval castle in the village of Chillingham, Northumberland, Chillingham in the northern part of Northumberland, England. It was the seat of the Baron Grey of Werke, Grey and Earl of Tankerville#Earls of Tankerville, Third Creation (1714), Bennet (later Earls of Tankerville) families from the 15th century until the 1980s, when it became the home of Humphry Wakefield, Sir Edward Humphry Tyrrell Wakefield, 2nd Baronet, who is married to a member of the original Grey family. A large enclosed park in the castle grounds is home to the Chillingham cattle, a rare breed, consisting of about 130 head of white cattle. The castle is a Grade I listed building. In addition to the castle itself, a number of structures on the grounds of the castle are listed Listed building#England and Wales, Grade II on the National Heritage List for England. These include the West Lodge and gateway, the garden wall to the west, the gateway and garden wall to the north, the gateway a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hepburn, Northumberland
Hepburn is a hamlet and former civil parish, now in the parish of Chillingham in the county of Northumberland, England. In 1951 the parish had a population of 43. Etymology The standard authorities give ''Hepburn'' as in origin an Old English name deriving from ''heah'' 'high' + ''byrgen'' 'burial mound'. Governance Hepburn was formerly a township in the parish of Chillingham, in 1866 Hepburn became a separate civil parish, on 1 April 1955 the parish was abolished and merged with Chillingham. From 1974 to 2009 it was in Berwick-upon-Tweed Berwick-upon-Tweed (), sometimes known as Berwick-on-Tweed or simply Berwick, is a town and civil parish in Northumberland, England, south of the Anglo-Scottish border, and the northernmost town in England. The 2011 United Kingdom census recor ... district. See also * Bewick and Beanley Moors SSSI References External links Hamlets in Northumberland Former civil parishes in Northumberland {{Northumberland-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bewick And Beanley Moors
__NOTOC__ Bewick and Beanley Moors is the name given to a Site of Special Scientific Interest (SSSI) in north Northumberland, in the north-east of England. The moors are asserted to be of national importance by Natural England for the extent, quality and diversity of upland types including heaths, fens, wet grassland, flushes, mires and blanket bogs, together creating an extensive mosaic habitat supporting an exceptional community of amphibians. The moors are important, too, for their relict juniper woodland and scrub. Designated in 2010, Bewick and Beanley Moors incorporates within its boundaries two now denotified SSSIs, Hannah's Hill, Harehope (first notified in 1968) and Quarryhouse Moor Ponds (first notified in 1986). Location and natural features Bewick and Beanley Moors, as defined for the purposes of the SSSI, are three distinct and non-contiguous moorland areas in north Northumberland, located to the north and north-west of Alnwick, and to the south-east of Wooler, exte ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |