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Anglezarke Reservoir
Anglezarke Reservoir is the largest reservoir in the Rivington chain to the west of Anglezarke in Lancashire, England. Anglezarke Reservoir has three embankments: the Charnock Embankment, the longest, is long and high, the Knowsley Embankment is long and high and the Heapey Embankment is long and high. It is fed by the River Yarrow, which has been diverted from its original course which is now covered by the Knowsley Embankment. It served the city of Liverpool before its current status as a supply mainly for Wigan. The original `Rivington Pike Scheme' was undertaken by Thomas Hawksley between 1850 and 1857 for the Liverpool Corporation Waterworks. The scheme was to construct five reservoirs and a water treatment works at the south end of Lower Rivington with a pipeline to storage reservoirs at Prescot. Water from two higher level reservoirs, Rake Brook and Lower Roddlesworth, was carried south in `The Goit', a channel connecting them to the reservoirs. In November 199 ...
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Rivington
Rivington is a village and civil parish of the Borough of Chorley, Lancashire, England, occupying . It is about southeast of Chorley and about northwest of Bolton. Rivington is a rural area consisting primarily of agricultural grazing land, moorland, with hill summits including Rivington Pike and Winter Hill within the West Pennine Moors. The area has a thriving tourist industry centred around reservoirs created to serve Liverpool in the Victorian era and Lever Park created as a public park by William Lever at the turn of the 20th century, with two converted barns, a replica of Liverpool Castle and open countryside. Rivington and Blackrod High School is located here. Rivington and its village had a population of 109 at the 2011 Census. History Toponymy The name Rivington is made up of three elements: ''riv'' is from the Old English ''hrēof'' meaning rough or rugged; ''ing'' is a place name forming suffix that seems to have crept in over the years; the last is the Old Eng ...
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Stratum
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and '' lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. ...
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Drinking Water Reservoirs In England
Drinking is the act of ingesting water or other liquids into the body through the mouth, proboscis, or elsewhere. Humans drink by swallowing, completed by peristalsis in the esophagus. The physiological processes of drinking vary widely among other animals. Most animals drink water to maintain bodily hydration, although many can survive on the water gained from their food. Water is required for many physiological processes. Both inadequate and (less commonly) excessive water intake are associated with health problems. Methods of drinking In humans When a liquid enters a human mouth, the swallowing process is completed by peristalsis which delivers the liquid through the esophagus to the stomach; much of the activity is abetted by gravity. The liquid may be poured from the hands or drinkware may be used as vessels. Drinking can also be performed by acts of inhalation, typically when imbibing hot liquids or drinking from a spoon. Infants employ a method of suction ...
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West Pennine Moors
The West Pennine Moors is an area of the Pennines covering approximately of moorland and reservoirs in Lancashire and Greater Manchester, England. It is a Site of Special Scientific Interest. The West Pennine Moors are separated from the main Pennine range by the Irwell Valley to the east. The moorland includes Withnell, Anglezarke and Rivington Moors in the extreme west, Darwen and Turton Moors, Oswaldtwistle Moors and Holcombe Moors. These moors are lower in height than the main spine of the South Pennines. At , the highest point is at Winter Hill. The area is of historical importance with archaeological evidence of human activity from Neolithic times. The area is close to urban areas, the dramatic backdrop to Bolton, Blackburn and Bury and neighbouring towns affording panoramic views across the Lancashire Plain and the Greater Manchester conurbation. The moorland is surrounded by the towns of Bolton, Chorley, Darwen, Horwich, Ramsbottom, Haslingden and Oswaldtwistle. No ...
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Healey Nab
Healey Nab or "The Nab" is an area of countryside owned partly by Lancashire County Council containing rolling hills, moorland, woodland, ponds and streams to the east of Chorley, Lancashire, between the M61 and the West Pennine Moors. To its southeast is Anglezarke Reservoir and to its northeast is White Coppice. The name "Healey Nab" is derived from (high) and (woodland). "Nab" is believed to derive from the Middle-English , meaning promontory or headland. The area is popular with walkers; a network of hiking trails criss-crosses it. It has two small man-made lakes: Bottom Lodge, and Top Lodge, a private fishing lake. They used to be linked to Lower Healey Bleach Works, a finishing works of the town's cotton industry, whose remaining structure has been incorporated into the site's conversion into a small industrial estate. The summit is Grey Heights, and near it is a disused quarry known as Devil's Rock. Its highest point is Grey Heights, at 682 feet, with views of Chorley ...
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Upper Rivington Reservoir
Upper Rivington Reservoir is situated centrally in the Rivington chain of reservoirs, on the West Pennine Moors in Lancashire, England, between Rivington and Anglezarke. The engineer for the Rivington reservoirs was Thomas Hawksley and construction for Liverpool Corporation Waterworks took place between 1852 and 1857. The two dams of the Upper Rivington reservoir are the Horrobin Embankment that separates it from the lower reservoir and carries a road into the village from the west, and the long, high Yarrow Embankment. There is an island. A bridleway and residence, The Street are on the side of the reservoir. It is a popular walking destination, between Anglezarke Reservoir to the north, Lower Rivington Reservoir to the south, and Yarrow reservoir Yarrow Reservoir - named after the River Yarrow - is a reservoir in the Rivington chain in Anglezarke, Lancashire, England, and has a storage capacity second to Anglezarke Reservoir. Construction of the reservoir, designed ...
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High Bullough Reservoir
High Bullough Reservoir is the oldest of all the reservoirs in the Rivington chain, having been authorised by an Act of Parliament obtained in 1846 and completed in 1850. It was built for Chorley Waterworks by the engineer John Frederick Bateman, who had estimated the cost of the project while working for Edwin Chadwick's Towns Improvement Company, and had then acted as Engineer for the project. The outlet consisted of a pipe running through the dam, and supported by two masonry piers where it ran through the central clay puddle. The outlet valve was at the downstream end of the dam, and although this configuration is no longer thought to be good practice, there have been no serious issues with the reservoir throughout its operational life. The earth dam had a maximum height of , was long and impounded of water. Popular with walkers, it forms part of the Anglezarke trail, although it is also accessible from Manor House. It was originally named Chorley Reservoir. There are a n ...
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White Coppice
White Coppice is a hamlet near Chorley, Lancashire, England. It was the most populated part of the township of Anglezarke in the 19th century. Close to the settlement in the early 19th century were quarries and small coal mines. The hamlet lies to the north of Anglezarke Reservoir in the Rivington reservoir chain built to provide water for Liverpool in the mid 19th century. To the south west is a hill known as Healey Nab. White Coppice had a cotton mill at the start of the Industrial Revolution. Its mill lodge provided water for a steam engine, and before that the mill was powered by a waterwheel on the Black Brook. Around 1900 the mill was owned by Alfred Ephraim Eccles, a supporter of the Temperance movement. Notable residents * Walter Haworth was born here on 19 March 1883 and won a Nobel Prize in chemistry. * Sir Henry Tate, 1st Baronet was born on 11 March 1819 in White Coppice. He was an English sugar merchant and philanthropist, noted for establishing the Tate G ...
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Tudorbethan Architecture
Tudor Revival architecture (also known as mock Tudor in the UK) first manifested itself in domestic architecture in the United Kingdom in the latter half of the 19th century. Based on revival of aspects that were perceived as Tudor architecture, in reality it usually took the style of English vernacular architecture of the Middle Ages that had survived into the Tudor period. The style later became an influence elsewhere, especially the British colonies. For example, in New Zealand, the architect Francis Petre adapted the style for the local climate. In Singapore, then a British colony, architects such as R. A. J. Bidwell pioneered what became known as the Black and White House. The earliest examples of the style originate with the works of such eminent architects as Norman Shaw and George Devey, in what at the time was considered Neo-Tudor design. Tudorbethan is a subset of Tudor Revival architecture that eliminated some of the more complex aspects of Jacobethan in favour ...
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Watermans Cottage
Watermans or Waterman's may refer to: * Watermans Arts Centre, arts centre in London, England, UK * Watermans Bay, Western Australia Watermans Bay is a northern coastal suburb of Perth, the capital city of Western Australia. Its local government area is the City of Stirling. History The area originally formed part of the Hamersley Estate, which also included the suburbs n ..., suburb of Perth, Australia * Waterman’s Museum, Yorktown, Virginia, USA See also * Waterman (other) * Waterman's knot * * * * * * * * * {{disambiguation ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur o ...
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White Brook
White Brook is a tributary of Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through North Branch Township and Forkston Township, in Wyoming County, Pennsylvania, in the United States. The stream's watershed has an area of . The stream is classified as a High-Quality Coldwater Fishery. It has a small waterfall and a hiking path is located nearby. Course White Brook begins near the edge of a plateau in North Branch Township. It flows south-southwest for a few tenths of a mile, heading into a valley. The stream then turns south-southeast for several tenths of a mile before entering Forkston Township and reaching the valley floor, where it receives an unnamed tributary from the right. It then turns east-southeast for several tenths of a mile before turning east-northeast for several tenths of a mile and exiting the valley. Here, the stream flows east for several tenths of a mile in the Mehoopany Creek valley before reachin ...
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