Biostrome
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Biostrome
A reef knoll is a land-based landform that comprises an immense pile of calcareous material that accumulated on a previously existing ancient sea floor. At the time of its accumulation it may have had enough structure from organisms such as sponges to have been free-standing and to withstand the sea currents as material accumulated, and was likely an atoll. Another possibility is the remains of deep water coral. Such structures are thus often fossil-rich. A bioherm is a sedimentary rocky landform enclosed or surrounded by rock of different origin. A biostrome is a distinctly bedded or broadly lenticular sedimentary rocky landform. Krumbein defines these terms as types of stromatolites: "Distinctly bedded, widely extensive, blanketlike build-ups are biostromes. Nodular, biscuit-like, dome-shaped or columnar stromatolites are also referred to as bioherms". England Examples on the Derbyshire/Staffordshire border include Thorpe Cloud and Bunster Hill in southern Dovedale, and also ...
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Calcareous
Calcareous () is an adjective meaning "mostly or partly composed of calcium carbonate", in other words, containing lime or being chalky. The term is used in a wide variety of scientific disciplines. In zoology ''Calcareous'' is used as an adjectival term applied to anatomical structures which are made primarily of calcium carbonate, in animals such as gastropods, i.e., snails, specifically about such structures as the operculum, the clausilium, and the love dart. The term also applies to the calcium carbonate tests of often more or less microscopic Foraminifera. Not all tests are calcareous; diatoms and radiolaria have siliceous tests. The molluscs are calcareous, as are calcareous sponges ( Porifera), that have spicules which are made of calcium carbonate. In botany ''Calcareous grassland'' is a form of grassland characteristic of soils containing much calcium carbonate from underlying chalk or limestone rock. In medicine The term is used in pathology, for example i ...
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Parkhouse Hill
Parkhouse Hill is a small but distinctive hill in the Peak District National Park of the Hartington Middle Quarter civil parish, in the English county of Derbyshire. It lies on the north side of the River Dove, close to the border with Staffordshire. Geologically, the hill is the remains of an atoll (a 'reef knoll') which is believed to have existed during the Carboniferous period when what is now the Peak District was covered by a tropical sea. Together with its higher but less distinctive neighbour, Chrome Hill, it forms the Chrome and Parkhouse Hills SSSI, cited for their geology and limestone flora. The walk over Chrome Hill and Parkhouse Hill is known as the Dragon's Back ridge. For many years access to Parkhouse Hill was difficult, as there was no right of way to the summit. Access is now possible under the Countryside and Rights of Way Act 2000, as the hill is a designated access area. A double sunset can sometimes be seen against Parkhouse Hill from nearby Glutton Gr ...
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Three Reef Knolls, From Ne, 6265
3 is a number, numeral, and glyph. 3, three, or III may also refer to: * AD 3, the third year of the AD era * 3 BC, the third year before the AD era * March, the third month Books * ''Three of Them'' (Russian: ', literally, "three"), a 1901 novel by Maksim Gorky * ''Three'', a 1946 novel by William Sansom * ''Three'', a 1970 novel by Sylvia Ashton-Warner * ''Three'' (novel), a 2003 suspense novel by Ted Dekker * ''Three'' (comics), a graphic novel by Kieron Gillen. * ''3'', a 2004 novel by Julie Hilden * ''Three'', a collection of three plays by Lillian Hellman * ''Three By Flannery O'Connor'', collection Flannery O'Connor bibliography Brands * 3 (telecommunications), a global telecommunications brand ** 3Arena, indoor amphitheatre in Ireland operating with the "3" brand ** 3 Hong Kong, telecommunications company operating in Hong Kong ** Three Australia, Australian telecommunications company ** Three Ireland, Irish telecommunications company ** Three UK, British teleco ...
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Clitheroe
Clitheroe () is a town and civil parish in the Borough of Ribble Valley, Lancashire, England; it is located north-west of Manchester. It is near the Forest of Bowland and is often used as a base for tourists visiting the area. In 2018, the Clitheroe built-up area had an estimated population of 16,279. The town's most notable building is Clitheroe Castle, which is said to be one of the smallest Norman keeps in Great Britain. Several manufacturing companies have sites here, including Dugdale Nutrition, Hanson Cement, Johnson Matthey and Tarmac. History The name ''Clitheroe'' is thought to come from the Anglo-Saxon for "Rocky Hill", and was also spelled ''Clyderhow'' and ''Cletherwoode'', amongst others. The town was the administrative centre for the lands of the Honour of Clitheroe. The Battle of Clitheroe was fought in 1138 during the Anarchy. These lands were held by Roger de Poitou, who passed them to the De Lacy family, from whom they passed by marriage in 1310 or 1311 to ...
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Downham, Lancashire
Downham is a village and civil parish in Lancashire, England. It is in the Ribble Valley district and at the United Kingdom 2001 census had a population of 156. The 2011 Census includes neighbouring Twiston giving a total for both parishes of 214. The village is on the north side of Pendle Hill off the A59 road about from Clitheroe. Much of the parish, including the village is part of the Forest of Bowland Area of Outstanding Natural Beauty (AONB). It adjoins the Ribble Valley parishes of Rimington, Twiston, Worston, Chatburn and Sawley, and the Pendle parish of Barley-with-Wheatley Booth. History The manor was originally granted to the de Dinelay family in the fourteenth century by Henry of Grosmont, 1st Duke of Lancaster. It ceased to be a part of the Honour of Clitheroe in 1558 when it was purchased by the Assheton family. It still remains in Assheton ownership today but was reincorporated into the Honour of Clitheroe in 1945 when Ralph Assheton, later 1st Baron Clit ...
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Worston
Worston is a small linear village and civil parish in Lancashire, England. The village is north-west of Pendle Hill, east of Clitheroe, and is in the Ribble Valley district. As it is only a small village, with a population of 76 at the 2001 census, it has no parish council, but instead has a parish meeting. The parish meeting is shared with Mearley. From the 2011 Census population information for both Mearley and Worston is included within the civil parish of Pendleton. The village has a public house "The Calf's Head". The single road that passes through the village continues as a single track road to Downham. Worston is bypassed to the west by the A59 road, which passes through the edge of the parish. Slightly further north is the route of a Roman road, which forms part of the parish boundary. Worston was once a township in the ancient parish of Whalley. This became a civil parish in 1866, forming part of the Clitheroe Rural District from 1894 till 1974. Along with Wisw ...
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Settle, North Yorkshire
Settle is a market town and civil parish in the Craven district of North Yorkshire, England. Historically in the West Riding of Yorkshire, it is served by Settle railway station located near the town centre, and Giggleswick railway station which is a mile away. It is from Leeds Bradford Airport. The main road through Settle is the B6480, which links to the A65, connecting Settle to Leeds, Ilkley, Skipton and Kendal. The town had a population of 2,421 in the 2001 Census, increasing to 2,564 at the 2011 Census. History Settle is thought to have 7th-century Anglian origins, its name being the Angle word for settlement. Craven in the ''Domesday Book'' shows that until 1066 Bo was the lord of Settle but after the Harrying of the North (1069–1071) the land was granted to Roger de Poitou. In 1249 a market charter was granted to Henry de Percy, 7th feudal baron of Topcliffe by Henry III. A market square developed and the main route through the medieval town was aligned on ...
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Malham
Malham is a village and civil parish in the Craven district of North Yorkshire, England. Before 20th century boundary changes, the village was part of the Settle Rural District, in the historic West Riding of Yorkshire. In the ''Domesday Book'', the name is given as Malgun, meaning "settlement by the gravelly places". In 2001 the parish had a population of approximately 150. Malham parish increased in size geographically (to include Malham Moor) and so at the 2011 Census had a population of 238. Malham lies at the upper end of the valley of the River Aire, known above Airton as Malhamdale, in the Yorkshire Dales. The surrounding countryside is well known for its limestone pavements and other examples of limestone scenery. Tourist attractions include Malham Tarn, Malham Cove, Gordale Scar, Janet's Foss and the Dry Valley. In the 1950s the village gave its name to a Ham class minesweeper, HMS Malham. Governance Malham has a joint parish council, Kirkby Malhamdale Parish Counci ...
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Thorpe, North Yorkshire
Thorpe is a village and civil parish in the Craven district of North Yorkshire, England. It is south of Grassington and north of Skipton. The population of the parish was estimated at 40 in 2010. At the 2011 the population remained less than 100. Details are included in the civil parish of Burnsall Burnsall is a village and civil parish in the Craven district of North Yorkshire, England. It is situated on the River Wharfe in Wharfedale, and is in the Yorkshire Dales National Park. The village is approximately south-east from Grassington .... References External links * Villages in North Yorkshire Civil parishes in North Yorkshire Wharfedale {{craven-geo-stub ...
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Craven Fault System
The Craven Fault System is the name applied by geologists to the group of crustal faults in the Pennines that form the southern edge of the Askrigg Block and which partly bounds the Craven Basin. Sections of the system's component faults which include the North, Middle and South Craven faults and the Feizor FaultBritish Geological Survey 1:50,000 scale geological map (England and Wales) sheet 60 ''Settle'' are evident at the surface in the form of degraded faults scarps where Carboniferous Limestone abuts millstone grit. The fault system is approximately coincident with the southwestern edge of the Yorkshire Dales National Park and the northeastern edge of the Bowland Fells. Location The Craven Faults are major crustal fractures across the Pennines. These faults constitute a zone crossing the backbone of England from west to east commencing near Leck, Lancashire at then branching three ways: * The North Craven Fault extends about to . * The Mid Craven Fault extends about ...
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Yorkshire Dales
The Yorkshire Dales is an upland area of the Pennines in the Historic counties of England, historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954. The Dales comprise river valleys and the hills rising from the Vale of York westwards to the hilltops of the Pennine Drainage divide, watershed. In Ribblesdale, Dentdale and Garsdale, the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the River Ouse, Yorkshire, Ouse and the Humber. The extensive limestone cave systems are a major area for caving in the UK and numerous walking trails run through the hills and dales. Etymology The word ''Dale (landform), dale'', like ''dell'', is derived from the Old English word ''dæl''. It has cognates in the North Germanic languages, Nordic/Germanic languages, Germanic words for valley (''dal'', ''tal''), and occurs in valley names across Yorkshire and Northern England. Usage here may have ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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