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Great Wold Valley
The Great Wold Valley is the largest and broadest of the valleys cutting into the Yorkshire Wolds in northern England. It carries the Gypsey Race, an intermittent stream, which runs from its source near Wharram-le-Street eastwards along and through the northern Yorkshire Wolds to reach the sea at Bridlington. It is known that the Great Wold Valley was an important place of worship during Neolithic times and there are a number of scheduled monuments in the valley. There are two dramatic right angle bends in the course of the Gypsey Race, one turning to the south at Burton Fleming then another turning eastwards again at Rudston. This intermittent and irregular watercourse is believed to be affected by a siphoning action in underground reservoirs and can come into flood apparently regardless of recent rainfall in the local vicinity. This seemingly 'magical' property is thought to be responsible for the number of significant Neolithic sites along its course, including the Rudston Monol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gypsey Race
The Gypsey Race is a winterbourne stream that rises to the east of Wharram-le-Street and flows through the villages of Duggleby, Kirby Grindalythe, West Lutton, East Lutton, Helperthorpe, Weaverthorpe, Butterwick, Foxholes, Wold Newton, Burton Fleming, Rudston and Boynton. The stream flows into the North Sea in Bridlington harbour. It is the most northerly of the Yorkshire chalk streams. The Gypsey Race rises in the Great Wold Valley through a series of springs and flows intermittently between Duggleby and West Lutton where it runs underground in the chalk aquifer before re-surfacing in Rudston. It has been known during very wet conditions for the stream to re-appear at Wold Newton some north-west of Rudston. Water from the aquifer running between West Lutton and Wold Newton also heads south to re-appear at Elmswell feeding West Beck and the River Hull. According to folklore, when the Gypsey Race is flowing in flood (The Woe Waters), bad fortune is at hand. It was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of The East Riding Of Yorkshire
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordnance Datum
In the British Isles, an ordnance datum or OD is a vertical datum used by an ordnance survey as the basis for deriving altitudes on maps. A spot height may be expressed as AOD for "above ordnance datum". Usually mean sea level (MSL) is used for the datum. In particular: * In Great Britain, OD for the Ordnance Survey is ODN (Ordnance Datum Newlyn), defined as the MSL as recorded by the tidal gauge at Newlyn in Cornwall between 1915 and 1921. **Prior to 1921, OD was defined as MSL as recorded in the Victoria Dock, Liverpool, during a short period in 1844 (ODL). * In Northern Ireland, OD for the Ordnance Survey of Northern Ireland is Belfast Ordnance Datum, the MSL at Clarendon Dock, Belfast, between 1951 and 1956. * In the Republic of Ireland, OD for the Ordnance Survey of Ireland is Malin Ordnance Datum: the MSL at Portmoor Pier, Malin Head, County Donegal, between 1960 and 1969. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boynton, East Riding Of Yorkshire
Boynton is a village and civil parish in the East Riding of Yorkshire, England. It is situated approximately west of the town of Bridlington and lies on the B1253 road. According to the 2001 UK census, the parish had a population of 161, however the 2011 census grouped the parish with Grindale (2001 pop. 98), giving a total of 229. The parish church of St Andrew's is a Grade I listed building. It includes a 15th-century tower, as well as memorials to the Strickland, later Cholmley, later Strickland-Constable Baronets, of Boynton (1641), whose seat was at Boynton Hall, which is also Grade I listed. From the mediaeval era until the 19th century Boynton was part of Dickering Wapentake. Between 1894 and 1974 Boynton was a part of the Bridlington Rural District, in the East Riding of Yorkshire. Between 1974 and 1996 it was part of the Borough of North Wolds (later Borough of East Yorkshire, in the county of Humberside Humberside () was a non-metropolitan and ceremonia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sparganium
''Sparganium'' (bur-reed) is a genus of flowering plants, described as a genus by Linnaeus in 1753. It is widespread in wet areas in temperate regions of both the Northern and Southern Hemispheres. The plants are perennial marsh plants that can grow to 3.5 m (depending on the species), with epicene flowers. It was previously placed alone in the family Sparganiaceae. ''Sparganium'' is closely related to the Typhaceae and the APG III system (2009) includes ''Sparganium'' in that family. It has been determined from phylogenetic analysis to be the closest living relative of the genus '' Typha'' (cat-tail). Summary ''Sparganium'', commonly known as the bur-reed, is a genus of aquatic plants of shallow marshes, ponds and streams. There are 9 species found in the United States and Canada. The stem, which may be floating or emergent, emerges from a buried rhizome, which like many wetland plants, is dependent upon aerenchyma to transport oxygen to the rooting zone. The leaves are st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enclosure
Enclosure or Inclosure is a term, used in English landownership, that refers to the appropriation of "waste" or " common land" enclosing it and by doing so depriving commoners of their rights of access and privilege. Agreements to enclose land could be either through a formal or informal process. The process could normally be accomplished in three ways. First there was the creation of "closes", taken out of larger common fields by their owners. Secondly, there was enclosure by proprietors, owners who acted together, usually small farmers or squires, leading to the enclosure of whole parishes. Finally there were enclosures by Acts of Parliament. The primary reason for enclosure was to improve the efficiency of agriculture. However, there were other motives too, one example being that the value of the land enclosed would be substantially increased. There were social consequences to the policy, with many protests at the removal of rights from the common people. Enclosure riots a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Argam
Argam, or Argham (sometimes Ergam, or Ergham), was a civil parish and village in the East Riding of Yorkshire, England. The site is listed in many historical documents, but was deserted by the early 19th century, now being part of the civil parish of Grindale. The village was depopulated, becoming one of the known deserted Medieval villages in Yorkshire. History Argam is mentioned in the Domesday Book as being part of the Hundred or Torbar. Torbar was later joined with the hundreds of Burton and Huntou to form the wapentake of Dickering. The parish was bisected along a north-east/south-west axis by Argham Dykes (or Ergham Dykes), a Bronze Age earthwork that extends from Reighton in the north-east, to Rudston in the south west. The dyke, which was historically called the ''Argham Cursus'', is now a scheduled monument. The dyke is believed to be pre-Roman, however in 1869, some Roman coins were unearthed from the dyke inside a mole-hill, which led to some assuming a Roman-built ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cursus
250px, Stonehenge Cursus, Wiltshire 250px, Dorset Cursus terminal on Thickthorn Down, Dorset Cursuses are monumental Neolithic structures resembling ditches or trenches in the islands of Great Britain and Ireland. Relics found within them indicate that they were built between 3400 and 3000 BC, making them among the oldest monumental structures on the islands. The name 'cursus' was suggested in 1723 by William Stukeley, the antiquarian, who compared the Stonehenge cursus to a Roman chariot-racing track, or circus. Cursuses range in length from to almost . The distance between the parallel earthworks can be up to . Banks at the terminal ends enclose the cursus. Over fifty have been identified via aerial photography while many others have doubtless been obliterated by farming and other activities. The Stonehenge Cursus is a notable example within sight of the more famous Stonehenge stone circle. Other examples are the four cursuses at Rudston in Yorkshire, that at Fornham A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vale Of York
The Vale of York is an area of flat land in the northeast of England. The vale is a major agricultural area and serves as the main north–south transport corridor for Northern England. The Vale of York is often supposed to stretch from the River Tees in the north to the Humber Estuary in the south. More properly it is just the central part of this area which is truly the Vale of York, with the Vale of Mowbray to its north and the Humberhead Levels to its south. It is bounded by the Howardian Hills and Yorkshire Wolds to the east and the Pennines to the west. The low-lying ridge of the Escrick moraine marks its southern boundary. York lies in the middle of the area. Geography Climate As part of Great Britain, the Vale of York generally has cool summers and relatively mild winters. Weather conditions vary from day to day as well as from season to season. The latitude of the area means that it is influenced by predominantly westerly winds with depressions and their associated ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wensleydale
Wensleydale is the dale or upper valley of the River Ure on the east side of the Pennines, one of the Yorkshire Dales in North Yorkshire, England. It is one of only a few Yorkshire Dales not currently named after its principal river, but the older name, Yoredale, can still be seen on some maps and as the Yoredale Series of geological strata. The dale takes its name from the village of Wensley, once its market town. The valley is famous for its cheese, with the main commercial production at Hawes. Also famous are its ales from Theakston Brewery and Black Sheep Brewery in Masham. Most of the dale is within the Yorkshire Dales National Park. Part of lower Wensleydale, below East Witton, is within the Nidderdale Area of Outstanding Natural Beauty. Addlebrough, a fell, dominates the landscape of the upper dale, and Penhill at is prominent in the lower dale. History Wensleydale was the home of one of Yorkshire's most famous clans, the Metcalfes, after they emigrated from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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