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Kelsall
Kelsall is a village and civil parish in the unitary authority of Cheshire West and Chester and the ceremonial county of Cheshire, England. It is located around east of Chester, west of Northwich and north west of Tarporley. The village is situated on Kelsall Hill, a part of the Mid-Cheshire Ridge, the broken line of sandstone hills that divide the west Cheshire Plain from its eastern counterpart. The ridge includes other hills including Peckforton, Beeston, Frodsham and Helsby. At the 2001 Census the population of Kelsall civil parish was 2,525, increasing to 2,609 at the 2011 census. The total population of the Kelsall local government ward, which also included the village of Ashton Hayes, was recorded as 3,439. This ward had been amalgamated with Tarvin by the time of the 2011 Census. The village contains two churches, one primary school, a community centre, a doctors' surgery, a chemist, a local store, a butchers shop, four public houses—The Boot*, The Farmers Arms, ...
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Listed Buildings In Kelsall
Kelsall is a civil parish in Cheshire West and Chester, England. It contains six buildings that are recorded in the National Heritage List for England as designated listed buildings, all of which are at Grade II. This grade is the lowest of the three gradings given to listed buildings and is applied to "buildings of national importance and special interest". Much of the parish is occupied by the village of Kelsall, with the rest of the parish rural. The listed buildings consist of farmhouses, farm buildings, a church and a lock-up. See also * Listed buildings in Ashton Hayes * Listed buildings in Delamere * Listed buildings in Horton-cum-Peel * Listed buildings in Oakmere * Listed buildings in Tarvin Tarvin is a Civil parishes in England, civil parish in Cheshire West and Chester, England. It contains 27 buildings that are recorded in the National Heritage List for England as designated listed buildings. Of these, one is listed at Grade  ... * Listed buildings ...
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St Philip's Church, Kelsall
St Philip's Church is in the village of Kelsall, Cheshire, England. It is an active Anglican parish church in the deanery of Chester, the archdeaconry of Chester, and the diocese of Chester. The church is recorded in the National Heritage List for England as a designated Grade II listed building. History The church was built in 1860 to a design by Thomas Bower of Nantwich. Architecture St Philip's is constructed in sandstone with a roof of Welsh slates and a red tiled ridge. Its architectural style is Decorated. The plan consists of a four-bay nave with a south porch, and a two-bay chancel with a north vestry. A bellcote stands on the east end of the nave. The windows along the sides of the church are divided by buttresses. In the nave the windows have two-lights with alternating quatrefoil and trefoil heads, and contain plate tracery. The chancel windows are pairs of lancets with trefoil heads. The east window has three lights, and the west window four lights. ...
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Eddisbury (UK Parliament Constituency)
Eddisbury is a constituency in Cheshire represented in the House of Commons of the UK Parliament since 2019 by Edward Timpson, a Conservative. From 2015 to 2019 it was represented by Antoinette Sandbach, a former Conservative member who had the whip removed on 3 September 2019 and joined the Liberal Democrats on 31 October 2019. History The constituency was first created as one of eight single-member divisions of Cheshire under the Redistribution of Seats Act 1885, having previously been part of the larger 2-member Western Division of Cheshire. It was named for the former hundred of Eddisbury and constituted a largely rural area, including Frodsham, Tarporley, Malpas and Audlem. It also included non-resident freeholders of the Parliamentary Borough of Chester. Under the Representation of the People Act 1948, the seat was abolished for the 1950 general election, being distributed to the constituencies of Crewe, Northwich, Runcorn and City of Chester. It was re-const ...
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A54 Road
The A54 road is a road in England linking Chester in Cheshire with Buxton in Derbyshire. Its route through both urban and steep rural areas presents a challenge to Cheshire County Council in maintaining the safety of the road. Many years ago it was the main east–west route in Cheshire. The importance of the A54 through Middlewich and Winsford decreased in the 1970s and 1980s with the building of the M56 motorway and dualling of the A556 at Northwich. The section through Winsford carries approximately 30,000 vehicles per day. History Re-routing of the A54 away from the narrow cobbled streets of Congleton town centre was first proposed in 1935. Before this, at the point where the A34 now meets the A54 an unusual lighthouse was erected in 1924 bearing the words "Dangerous hill – change to low gear", backlit at night, to reduce accidents at the sharp bend. According to a 2007 report by the Road Safety Foundation for the European Road Assessment Programme (EuroRAP), the A54 is o ...
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Cheshire West And Chester
Cheshire West and Chester is a Unitary authorities of England, unitary authority with Borough status in the United Kingdom, borough status in the ceremonial county of Cheshire, England. It was established on 1 April 2009 as part of the 2009 structural changes to local government in England, 2009 local government changes, by virtue of an order under the Local Government and Public Involvement in Health Act 2007. It superseded the boroughs of Ellesmere Port and Neston, Vale Royal and the Chester (district), City of Chester; its council assumed the functions and responsibilities of the former Cheshire County Council within its area. The remainder of ceremonial Cheshire is composed of Cheshire East, Borough of Halton, Halton and Borough of Warrington, Warrington. The decision to create the Cheshire West and Chester unitary authority was announced on 25 July 2007 following a consultation period, in which a proposal to create a single Cheshire unitary authority was rejected. Governan ...
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Tarvin
Tarvin is a village in the unitary authority of Cheshire West and Chester and the ceremonial county of Cheshire, England. It had a population of 2,693 people at the 2001 UK census, rising to 2,728 at the 2011 Census, and the ward covers about . Location and context Tarvin is about east of Chester. The current parish covers Tarvin, Duddon, Clotton, Stapleford, Burton, Hoofield and Oscroft. There are currently 28 listed buildings in Tarvin (one Grade I Listed, two Grade II* Listed, and twenty-five Grade II Listed). The centre of the village is a Conservation Area that was created in 1972, and much of the land surrounding the village is designated Green Belt. Geology The Cheshire Plain (sometimes known as the Cheshire Gap) is a relatively flat expanse of lowland, which supports agricultural use for dairy farming on the medium-scale pastoral fields that surround the village. Tarvin is west of a sandstone ridge that divides the Cheshire Plain. The River Gowy passes to the so ...
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Ashton Hayes
Ashton Hayes is a village and former civil parish, now in the parish of Ashton Hayes and Horton-cum-Peel, in the unitary authority of Cheshire West and Chester and ceremonial county of Cheshire, England. It is located about 8 miles east of Chester on the B5393 road. The nearest villages are Mouldsworth to the north east and Kelsall to the south east. According to the 2011 Census it had a population of 936. The main village in the parish – formerly known as Ashton – was renamed Ashton Hayes following a referendum, to avoid confusion with other places of the same name. The civil parish was abolished in 2015 to form Ashton Hayes and Horton-cum-Peel, part of it also went to Mouldsworth. History In 1086, the village was recorded in the Domesday Book as comprising 12 households and lying within the hundred of Rushton in the county of Cheshire. Medieval pottery kiln In 1933 a pottery kiln, which had been in use between the 13th and 15th century, was discovered in the garden of Sm ...
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Northwich
{{Infobox UK place , static_image_name = Northwich - Town Bridge.jpg , static_image_caption = Town Bridge, the River Weaver and the spire of Holy Trinity Church , official_name = Northwich , country = England , region = North West England , population = 50,531 , population_ref = (2021){{NOMIS2021 , id=E35001305 Overview Profile: Northwich Town Council"; downloaded fro.gov.uk/find_out_more/datasets_and_statistics/statistics/census_2011/population_profiles Cheshire West and Chester: Population Profiles 16 May 2019 , os_grid_reference = SJ651733 , coordinates = {{coord, 53.259, -2.518, display=inline,title , post_town = NORTHWICH , postcode_area = CW , postcode_district = CW8,CW9 , dial_code = 01606 , constituency_westminster = Weaver Vale , constituency_westminster1 = Tatton , civil_pa ...
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Alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ...
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Glacial Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is depos ...
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Siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, pp.381-382 Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses. Description There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock ( clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined a ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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