Kelsall

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Kelsall
Cheshire
The Lord Binning, Kelsall (geograph 2664026).jpg
The Lord Binning, a pub in the village centre
Location
Grid reference: SJ525680
Location: 53°12’25"N, 2°42’43"W
Data
Population: 2,609  (2011)
Post town: Tarporley
Postcode: CW6
Dialling code: 01829
Local Government
Council: Cheshire West & Chester
Parliamentary
constituency:
Eddisbury

Kelsall is a village and civil parish in Cheshire. It is located around eight miles east of Chester, eight miles west of Northwich and four miles 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,[1] increasing to 2,609 at the 2011 census.[2]

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 Lord Binning (previously The Morris Dancer) and The Royal Oak (previously The Oak)—a hotel (Willington Hall Hotel*) and a farm shop (Willington Fruit Farm Shop*, a family-run business established over 50 years ago[3]). Establishments marked with an asterisk are technically in neighbouring Willington.

The village also hosts the annual Chester Folk Festival every May.[4] The £3.82m, two-mile A54 bypass opened in October 1986.

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 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 south-east 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.[5]

References

Outside links

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