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Kelsall Lodge, Delamere
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 Farmer ...
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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 It superseded the boroughs of Ellesmere Port and Neston, Vale Royal and the Chester (district), City of Chester; its council assumed the functions and responsibilities of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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Ward (country Subdivision)
A ward is a local authority area, typically used for electoral purposes. In some countries, wards are usually named after neighbourhoods, thoroughfares, parishes, landmarks, geographical features and in some cases historical figures connected to the area (e.g. William Morris Ward in the London Borough of Waltham Forest, England). It is common in the United States for wards to simply be numbered. Origins The word “ward”, for an electoral subdivision, appears to have originated in the Wards of the City of London, where gatherings for each ward known as “wardmotes” have taken place since the 12th century. The word was much later applied to divisions of other cities and towns in England and Wales and Ireland. In parts of northern England, a ''ward'' was an administrative subdivision of a historic counties of England, county, very similar to a hundred (country subdivision), hundred in other parts of England. Present day In Australia, Canada, New Zealand, Sri Lanka, South Afr ...
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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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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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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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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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Willington, Cheshire
Willington is a village and civil parish from Chester in Cheshire, England. At the 2011 census, the population was 277. The village contains a public house (The Boot), farm shop and hotel (Willington Hall). History The placename means "village of a woman called Winflǣd", from the Old English personal name Winflǣd, and the suffix ''tun'' for farm or village. The name was recorded in the Domesday Book as ''Winfletone'', (under the ownership of Walter de Vernon and consisting of only two households), and then as ''Wynlaton'' in the 12th century. Willington was previously an extra-parochial area in Eddisbury Hundred, which became a civil parish in 1866. From 1894 the civil parish was within Tarvin Rural District, transferring to the Chester district in 1974. Landmarks The Boot Inn occupies a row of red-brick and sandstone cottages that were built in 1815. Behind the pub is Boothsdale, also known as 'Little Switzerland', accessible by a well-used footpath. Willington Hal ...
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Willington Hall
Willington Hall is a former country house in the parish of Willington, Cheshire, England. It was extended in 1878, but reduced in size in the 1950s, and has since been in use as a hotel. History The house was built in 1829 by Major William Tomkinson on land purchased in 1827 from Lord Alvanley. Designed by Nantwich architect George Latham, in 1878 a new east front was added for William's son James Tomkinson. At the same time a new wing and stable blocks were added, and in the 1920s a laundry block was built. Although it escaped the fate of the destruction of country houses in 20th-century Britain, during the 1950s it was reduced in size, removing the 1878 east front and some of the outbuildings. In 1955 a portico was added, and it has since been in use as a hotel. The house is recorded in the National Heritage List for England as a designated Grade II listed building. Architecture Willington Hall is constructed in orange brick with buff sandstone dressings and ...
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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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