Kelsall is a village and civil parish in the unitary authority of

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 str ...

and the ceremonial county of

Cheshire Cheshire ( ) is a ceremonial and historic county in North West England, bordered by Wales to the west, Merseyside and Greater Manchester to the north, Derbyshire to the east, and Staffordshire and Shropshire to the south. Cheshire's county t ...

, England. It is located around east of

Chester Chester is a cathedral city and the county town of Cheshire, England. It is located on the River Dee, close to the English–Welsh border. With a population of 79,645 in 2011,"2011 Census results: People and Population Profile: Chester Loca ...

, west of

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 ...

and north west of Tarporley. The village is situated on Kelsall Hill, a part of the

Mid-Cheshire Ridge The Mid Cheshire Ridge is a range of low sandstone hills which stretch north to south through Cheshire in North West England. The ridge is discontinuous, with the hills forming two main blocks, north and south of the "Beeston Gap". The main mass ...

, the broken line of sandstone hills that divide the west Cheshire Plain from its eastern counterpart. The ridge includes other hills including

Peckforton Peckforton is a scattered settlement (centred at ) and civil parish in the unitary authority of Cheshire East and the ceremonial county of Cheshire, England. The settlement is located to the north east of Malpas and to the west of Nantwich. Th ...

, 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, The Morris Dancer (formerly The Lord Binning) and The Royal Oak (previously The Oak)—a hotel ( Willington Hall Hotel*), a farm shop (Willington Fruit Farm Shop*, a family-run business established over 50 years ago) and a nursing and residential home. Establishments marked with an asterisk are technically in neighbouring Willington. The village also hosts the annual Chester Folk Festival every May. The £3.82m, two-mile A54 bypass opened in October 1986.

KADRAS

Kelsall and District Rural Amenities Society (KADRAS) was formed in the late 1960s in order to stimulate public interest in the care and development of Kelsall's history, beauty and character. The society also aims to encourage the development of general public amenities and features of public interest in Kelsall. KADRAS achieves these goals by charitable means, and through lecturers, study groups, exhibitions and publications. Their magazine, entitled KADRAS is published every two months and encourages contributions from the community in the form of letters, articles and poetry.

Geology

Bedrock geology

The western part of the parish (west of the Peckforton Fault) is underlain by the Wilmslow Sandstone Formation. East of the fault, the bedrock is largely Tarporley

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, p ...

with the underlying Helsby Sandstone occurring in some areas.

Superficial deposits

The lower ground in the west is largely covered by glacial till whilst higher ground in the east is free of superficial deposits. A small area of glacio-fluvial sands and gravels is mapped in the centre of the parish. A narrow strip of alluvium is associated with Salter's Brook.

Geological structure

The Peckforton Fault runs into the parish from the SE then turns north. It downthrows to the east. Two parallel unnamed faults, both downthrowing to the west, run NNE–SSW through Kelsall village, their southern ends terminating at the Peckforton Fault. They terminate against a short ENE–WSW aligned fault with a northerly downthrow at the northern end of the parish. The Clotton Fault which downthrows to the east runs NNW–SSE through the western part of the parish. The rocks within the faulted blocks have a gentle to moderate easterly dip.British Geological Survey 1:50K map sheet 109 Chester

References

External links

Kelsall website
{{authority control Villages in Cheshire Civil parishes in Cheshire