Middlewich Revised Archaeological Assessment 2013
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Meeting of the Parish Council
Clerk: Carol Jones Tel: 01270 262636 Email: [email protected] Web: www.shavingtononline.co.uk Parish Councillors are summoned to a MEETING OF THE PARISH COUNCIL DAY/DATE: WEDNESDAY, 3 FEBRUARY 2021 TIME: 7.30 PM MEETING TO BE HELD REMOTELY, VIA VIDEO-LINK PLATFORM: ZOOM ACCESS: Please click the link below. https://us02web.zoom.us/webinar/register/WN_DLGbiCxIRwSKhQNwGWUXYQ Enquiries to: Clerk: Carol Jones Issue date: 29 January 2021 Phone: 01270 262636 Signed: C M Jones To: Members of the Parish Council Councillors V Adams, L Buchanan, N Cooper, B Gibbs (Chairman), K Gibbs, J Hassall, M Ferguson, R Hancock, G McIntyre and R Moore Notes for Members of the Public: a) This meeting is being held remotely in accordance with regulations made under S.78 of the Coronavirus Act 2020. There are, therefore, no paper copies of the agenda or the accompanying documents. b) All documents (other than those which are restricted) can be accessed from the Parish Council’s website - www.shavingtononline.co.uk. c) If you wish to observe the meeting or make a statement under the Public Question Time slot, please ensure that you register using the link above. The system can accommodate a maximum of 100 attendees. Therefore, registration will be on a ‘first come, first served’ basis. Shavington-cum-Gresty Parish Council Agenda – (Meeting – 3 February 2021) A G E N D A 1 APOLOGIES 2 DECLARATION OF INTERESTS Members to declare any (a) disclosable pecuniary interest; (b) personal interest; or (c) prejudicial interest which they have in any item of business on the agenda, the nature of that interest, and in respect of disclosable interests and prejudicial interests, to withdraw from the meeting prior to the discussion of that item. -
The Archaeology of Mining, and Quarrying, for Salt and the Evaporites (Gypsum, Anhydrite, Potash and Celestine)
The archaeology of mining, and quarrying, for Salt and the Evaporites (Gypsum, Anhydrite, Potash and Celestine) Test drafted by Peter Claughton Rock salt, or halite (NaCl- sodium chloride), has been mined since the late 17th century, having been discovered during exploratory shaft sinking for coal at Marbury near Northwich, Cheshire, in November 1670. Prior to that the brine springs of Cheshire and those at Droitwich in Worcestershire were the source of salt produced by evaporation, along with production from a large number of coastal sites using seawater. Alabaster, fine grained gypsum (CaSO4. 2H2O - hydrated calcium sulphate), has however been quarried in the East Midlands for use in sculpture since at least the 14th century (Cheetham 1984, 11-13) and the use of gypsum for making plaster dates from about the same period. Consumption The expansion of mining and quarrying for salt and the other evaporites came in the 19th century with the development of the chemical industry. Salt (sodium chloride) was a feedstock for the production of the chlorine used in many chemical processes and in the production of caustic soda (sodium hydroxide) and soda ash (sodium carbonate). Anhydrite (anhydrous calcium sulphate) was used in the production of sulphuric acid. Salt or halite (rock salt) was first mined at Winsford in Cheshire (the site of the only remaining active rock salt mine in England) in 1844. Production expanded in the late 19th century to feed the chemical industry in north Cheshire (together with increasing brine production from the Northwich salt fields). The Lancashire salt deposits, on the Wyre estuary at Fleetwood and Preesall, not discovered until 1872 whilst boring in search of haematite (Landless 1979, 38), were a key to the development of the chemical industry in that area. -
William Furmval, H. E. Falk and the Salt Chamber of Commerce, 1815-1889: "Ome Chapters in the Economic History of Cheshire
WILLIAM FURMVAL, H. E. FALK AND THE SALT CHAMBER OF COMMERCE, 1815-1889: "OME CHAPTERS IN THE ECONOMIC HISTORY OF CHESHIRE BY W. H. CHALONER, M.A., PH.D. Read 17 November 1960 N the second volume of his Economic History of Modern I Britain (p. 145), Sir John Clapham, writing of the chambers of commerce and trade associations which multiplied rapidly after 1860, suggested that between 1850 and 1875 "there was rather less co-operation among 'capitalist' producers than there had been in the more difficult first and second quarters" of the nineteenth century. He mentioned that in the British salt industry there had been price-fixing associations "based on a local monopoly" in the early nineteenth century, and added that after 1825 the industry "witnessed alternations of gentle men's agreements and 'fighting trade' " until the formation of the Salt Union in 1888. This combine has been called "the first British trust", but to the salt proprietors of the time it was merely "a new device, made easier by limited liability, for handling an old problem". (1) The purpose of this study is to examine in greater detail the business organisation of the natural local monopoly enjoyed by the Cheshire saltmakers in the nineteenth century and to trace the part played by "The Coalition" and the Salt Chamber of Commerce in fostering price regulation and output restriction between the end of the Napoleonic Wars and 1889.< 2 > 111 Op. cit., pp. 147-8; see also Accounts and Papers, 1817, III, 123, p. 22, and E. Hughes, Studies in Administration and Finance, 1558-1825 (1934), pp. -
Victorian Salt Pans and Rock Salt Mining
Victorian Salt Pans Cheshire became dominant in salt making because of its easy access to strong natural brine and rock salt and good communica- tions. But this came at a cost to the environ- ment until the change to controlled brine pumping and vacuum evaporation. Salt was skimmed into salt moulds - originally Salt blocks were sold complete, or crushed to Brine was pumped to a brine tank ready to be baskets, later cooper made cones, then make fine salt. gravity fed to the salt pans. wooden boxes. Images from AF Calvert – Salt in Cheshire, London, 1913 Lump Crushing Storage & Packing Trap doors Brine A fine pan described in the Illustrated London Drying Area News 1850. Fishery pans could be much Brine 200°F Flues and ditches larger and made coarser crystals in pans set Firing Area up outdoors to replicate ‘Bay Salt’. The surviving brine pump at Murgatroyd’s Pan House Stove House Salt Works, Middlewich. Open pan salt works made fine salt and block Flues carried heat and fumes from the salt in a Pan House with an attached Stove furnace underneath the Stove House to a Rock Salt Mining House. Coal was burnt under the iron pan. chimney. Rising heat dried the salt when it Refineries Rock salt itself was not found until 1670, Salt was skimmed into boxes and barrowed was ‘lofted’ to the warehouse floor above. ‘There was a growth in rock salt refineries when William Jackson discovered it into the Stove House. after 1670 but Acts of Parliament restricted whilst prospecting for coal. their construction. -
Roadside Hedge and Tree Maintenance Programme
Roadside hedge and tree maintenance programme The programme for Cheshire East Higways’ hedge cutting in 2013/14 is shown below. It is due to commence in mid-October and scheduled for approximately 4 weeks. Two teams operating at the same time will cover the 30km and 162 sites Team 1 Team 2 Congleton LAP Knutsford LAP Crewe LAP Wilmslow LAP Nantwich LAP Poynton LAP Macclesfield LAP within the Cheshire East area in the following order:- LAP = Local Area Partnership. A map can be viewed: http://www.cheshireeast.gov.uk/PDF/laps-wards-a3[2].pdf The 2013 Hedge Inventory is as follows: 1 2013 HEDGE INVENTORY CHESHIRE EAST HIGHWAYS LAP 2 Peel Lne/Peel drive rhs of jct. Astbury Congleton 3 Alexandra Rd./Booth Lane Middlewich each side link FW Congleton 4 Astbury St./Banky Fields P.R.W Congleton Congleton 5 Audley Rd./Barley Croft Alsager between 81/83 Congleton 6 Bradwall Rd./Twemlow Avenue Sandbach link FW Congleton 7 Centurian Way Verges Middlewich Congleton 8 Chatsworth Dr. (Springfield Dr.) Congleton Congleton 9 Clayton By-Pass from River Dane to Barn Rd RA Congleton Congleton Clayton By-Pass From Barn Rd RA to traffic lights Rood Hill 10 Congleton Congleton 11 Clayton By-Pass from Barn Rd RA to traffic lights Rood Hill on Congleton Tescos side 12 Cockshuts from Silver St/Canal St towards St Peters Congleton Congleton Cookesmere Lane Sandbach 375199,361652 Swallow Dv to 13 Congleton Dove Cl 14 Coronation Crescent/Mill Hill Lane Sandbach link path Congleton 15 Dale Place on lhs travelling down 386982,362894 Congleton Congleton Dane Close/Cranberry Moss between 20 & 34 link path 16 Congleton Congleton 17 Edinburgh Rd. -
A Walk from Church Minshull
A Walk to Church Minshull Aqueduct Marina photo courtesy of Bernie Stafford Aqueduct Marina, the starting point for this walk, was opened in February 2009. The marina has 147 berths, a shop and a café set in beautiful Cheshire countryside. With comprehensive facilities for moorers, visiting boaters and anyone needing to do, or have done, any work on their boat, the marina is an excellent starting point for exploring the Cheshire canal system. Starting and finishing at Church Minshull Aqueduct Marina, this walk takes in some of the prettiest local countryside as well as the picturesque village of Church Minshull and the Middlewich Branch of the Shropshire Union Canal. Some alternative routes are also included at the end to add variation to the walk which is about five or six miles, depending on the exact route taken. Built to join the Trent and Mersey Canal with the Chester Canal, the Middlewich Branch carried mainly coal, salt and goods to and from the potteries. Built quite late in the canal building era, like so many other canals, this canal wasn’t as successful as predicted. Today, however, it is a very busy canal providing an essential link between the Trent and Mersey Canal at Middlewich and the Llangollen Canal as well as being part of the Four Counties Ring and linking to the popular Cheshire Ring boating route. The Route Leaving the marina, walk to the end of the drive and turn north (right) onto the B5074 Church Minshull road and walk to the canal bridge. Cross the canal and turn down the steps on the right onto the towpath, then walk back under the bridge, with the canal on your left. -
Holmes Chapel Settlement Report
Cheshire East Local Plan Site Allocations and Development Policies Document Holmes Chapel Settlement Report [ED 33] August 2020 OFFICIAL Contents 1. Introduction .......................................................................................................... 1 2. Holmes Chapel .................................................................................................... 2 Introduction .................................................................................................... 2 Neighbourhood Development Plan ................................................................ 2 Strategy for development in Holmes Chapel ................................................. 2 3. Development needs at Homes Chapel ................................................................ 4 4. Site selection ....................................................................................................... 5 Introduction .................................................................................................... 5 Stage 1: Establishing a pool of sites for Holmes Chapel ............................... 5 Stage 2: First site sift ..................................................................................... 5 Stage 3: Decision point – the need for sites in Holmes Chapel ..................... 6 Stage 4: Site assessment, Sustainability Appraisal and Habitats Regulations Assessment ................................................................................................... 6 Stages 5 to 7: Evaluation and initial recommendations; -
Middlewich Before the Romans
MIDDLEWICH BEFORE THE ROMANS During the last few Centuries BC, the Middlewich area was within the northern territories of the Cornovii. The Cornovii were a Celtic tribe and their territories were extensive: they included Cheshire and Shropshire, the easternmost fringes of Flintshire and Denbighshire and parts of Staffordshire and Worcestershire. They were surrounded by the territories of other similar tribal peoples: to the North was the great tribal federation of the Brigantes, the Deceangli in North Wales, the Ordovices in Gwynedd, the Corieltauvi in Warwickshire and Leicestershire and the Dobunni to the South. We think of them as a single tribe but it is probable that they were under the control of a paramount Chieftain, who may have resided in or near the great hill‐fort of the Wrekin, near Shrewsbury. The minor Clans would have been dominated by a number of minor Chieftains in a loosely‐knit federation. There is evidence for Late Iron Age, pre‐Roman, occupation at Middlewich. This consists of traces of round‐ houses in the King Street area, occasional finds of such things as sword scabbard‐fittings, earthenware salt‐ containers and coins. Taken together with the paleo‐environmental data, which hint strongly at forest‐clearance and agriculture, it is possible to use this evidence to create a picture of Middlewich in the last hundred years or so before the Romans arrived. We may surmise that two things gave the locality importance; the salt brine‐springs and the crossing‐points on the Dane and Croco rivers. The brine was exploited in the general area of King Street, and some of this important commodity was traded far a‐field. -
The Changing Technology of Post Medieval Sea Salt Production in England
1 Heritage, Uses and Representations of the Sea. Centro de Investigação Transdisiplinar Cultura, Espaço e Memoría (CITCEM) Porto, Faculdade de Letras da Universidade do Porto, 20-22 October 2011. The changing technology of post medieval sea salt production in England Jeremy Greenwood Composition of seawater Sea water contains 3.5% evaporites of which salt (sodium chloride) comprises 77.8%. The remainder is known as bittern as it includes the bitter tasting, aperient and deliquescent sulphates of magnesium (Epsom salt) and sodium (Glauber’s salt) as well as about 11% magnesium chloride. 2 Successful commercial salt making depends on the fractional crystallisation of seawater producing the maximum amount of salt without contamination by bittern salts. As seawater is evaporated, very small amounts of calcium carbonate are precipitated followed by some calcium sulphate. This is followed by the crystallisation of sodium chloride but before this is complete, bitter Epsom salt appears; something that needs to be avoided.1 In Continental Europe, evaporation of sea water is achieved solely by the energy of the wind and sun but this is not possible in the English climate so other techniques were developed. 1 http://www.solarsaltharvesters.com/notes.htm SOLAR SALT ENGINEERING 3 Evaporation vessel Briquetage The earliest known English method of coastal saltmaking has been found in the late Bronze Age. This involved boiling seawater in crude clay dishes supported by clay firebars (briquetage) and was widespread in Europe. This technique continued into the Iron Age and into the Roman period with variations inevitably occurring in the industry, although the dating of saltworks is very problematical.2 Detailed interpretation continues to be a matter of dispute. -
Open Spaces Summary Report: Congleton 1 Socio-Economic Profile
Contents 1 Socio-Economic Profile 2 2 PPG17 Typology Summary 3 Type 1: Parks & Gardens 3 Type 2: Natural & Semi-Natural Urban Greenspaces 4 Type 3: Green Corridors 5 Type 4: Outdoor Sports Facilities 6 Type 5: Amenity Greenspace 8 Type 6: Provision for Children & Teenagers 9 Type 7: Allotments, Community Gardens & Urban Farms 11 Type 8: Cemeteries & Churchyards 11 Type 9: Accessible Countryside in Urban Fringe Areas 12 Type 10: Civic Spaces 13 3 Conclusion 14 Appendices A Quality Report 16 B Outdoor Sports Facilities Report (Type 4) 17 C Provision for Children & Teenagers Report (Type 6) 20 D Potential Future Site Upgrade Information 22 Open Spaces Summary Report: Congleton 1 Socio-Economic Profile 1 Socio-Economic Profile 1.1 Congleton is a historic market town with a population of 26,580. It lies on the River Dane in the east of the Borough. In its early days it was an important centre of textile production, today, however, it is important for light engineering. The town also acts as a dormitory settlement for Manchester, Macclesfield and Stoke-on-Trent. 1.2 Congleton has a reasonably vibrant town centre. It is served by several bus routes, has its own train station with direct services between Stoke-on-Trent and Manchester and the M6 is a short distance away. 1.3 Congleton is surrounded by Green Belt to the south and east and the Jodrell Bank Telescope Consultation Zone applies to the countryside to the north east of the town. There are flood risk areas along the River Dane, Dane-in-Shaw Brook and Loach Brook. -
Submission July 2015 Brereton Parish Neighbourhood Plan Brereton Neighbourhood Plan
Brereton Neighbourhood Plan Submission July 2015 Brereton Parish Neighbourhood Plan Brereton Neighbourhood Plan “What you hear from the people of the parish and what you can see with your own eyes is how fortunate we are to live here. With our surrounding local towns expanding by the day we have a responsibility to preserve the best of what we have whilst meeting the needs of current and future generations.” John Charlesworth, Brereton resident and Neighbourhood Plan team member. Page 1 Brereton Parish Neighbourhood Plan About This Document Brereton Parish Neighbourhood Plan Submission This document is the Submission version of the Brereton Parish Neighbourhood Plan (the Plan). Regulation 15 of The Neighbourhood Planning (General) Regulations 2012, directs that the Submission of the Neighbourhood Plan is used to submit to Cheshire East Council for formal consideration and wider consultation. In January 2013 Brereton Parish Council began to develop the Neighbourhood Plan with the aim of shaping the vision for Brereton Parish until 2030. In consultations over the last two years the whole community has helped to develop the Plan. You have told us what changes you would like to see within the Parish and how we can enhance and preserve the things you value most. This Plan and its proposed polices reflects these community aspirations and views, and will significantly influence future planning decisions for new developments within the Parish. Reference to Supporting Documents is widely used throughout the Plan. These references, for example (ref. SD/B01), relate to the table of Supporting Documents listed in Appendix B. The Plan has been prepared by Brereton Parish Council, the qualifying body responsible for creating the Neighbourhood Plan. -
Active Surface Salt Structures of the Western Kuqa Fold-Thrust Belt, Northwestern China
Active surface salt structures of the western Kuqa fold-thrust belt, northwestern China Jianghai Li1, A. Alexander G. Webb2,*, Xiang Mao1, Ingrid Eckhoff2, Cindy Colón2, Kexin Zhang2, Honghao Wang1, An Li2, and Dian He2,† 1The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China 2Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA ABSTRACT fold-thrust belt display a variety of erosion- dynamics of salt motion. Although geo scientists tectonics interactions, with nuances refl ect- have interpreted thousands of salt sheets in The western Kuqa fold-thrust belt of Xin- ing the low viscosity and high erodibility of more than 35 basins worldwide (Hudec and jiang Province, China, hosts a series of surface salt, including stream defl ections, potential Jackson, 2006, 2007), subaerial preservation of salt structures. Here we present preliminary tectonic aneurysm development, and even halite salt structures is rare (Talbot and Pohjola, analysis of the geometry, kinematics, and sur- an upper-crustal test site for channel fl ow– 2009; Barnhart and Lohman, 2012). A fraction face processes of three of these structures: the focused denudation models. of these subaerial salt structures occur in active Quele open-toed salt thrust sheet, Tuzima- settings, where boundary conditions of ongoing zha salt wall, and Awate salt fountain. The INTRODUCTION deformation can be geodetically characterized. fi rst two are line-sourced, the third appears The Kuqa fold-thrust belt of Xinjiang Prov- to be point-sourced, and all are active. The Among common solid Earth materials, salt is ince, northwestern China, offers a new prospect ~35-km-long, 200-m-thick Quele open-toed distinguished by uncommonly low density, low for subaerial investigation of a range of active salt thrust sheet features internal folding, viscosity, near incompressibility, high solubil- salt structures.