Sources of Stone
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Bus Service Review – Proposals for Implementation
Appendix 1 – Summary of Proposals OFFICIAL Appendix 1 - Summary of Proposals Plan showing indicative routes outlined within the Recommended Network. 1. Summary of Changes for Final Proposals – Ordered by Consulted Upon Routes Proposed Route Current Route Consulted Network Changes from Consulted Network Proposed Routes A - Macclesfield – 19 Macclesfield – Prestbury Hourly weekday and Saturday Timetable adjusted to retain 12:00pm-13:00pm Prestbury service (except 12-1pm) using service with drivers break incorporated during off route of current 19 service. peak periods. Route unchanged. B – Nantwich – 39 – Nantwich – Wybunbury - Retention of existing 39 service Utilising of downtime on service to provide part of Wybunbury - Crewe Crewe with no timetable changes. Nantwich Town Service (to Nantwich Trade Park) to accommodate other proposals for Route G. Service remains two-hourly with minor adjustment to timetable. C - Crewe – Middlewich - 42 – Crewe – Middlewich – Retention of existing 42 service Re-routing of service via Frank Webb Avenue instead Congleton Congleton except diverting via Minshull of Minshull New Road. 85A – Crewe Bus Station – New Road instead of Frank The costs for evening services will be obtained as part Morrisons and onwards to Webb Avenue and passing of procurement of the Recommended Network. Nantwich (known as 1B Crewe Bus Eagle Bridge Medical Centre Station to Morrisons and onwards instead of Victoria Avenue. to Nantwich until September 2017) Service would operate hourly on weekdays and every 90 minutes on a Saturday, finishing earlier. D1 - Macclesfield – Forest 58 – Macclesfield – Forest Cottage Retention of existing 58 and 60 No changes proposed. Cottage – Burbage - – Burbage – Buxton services with no timetable Buxton 60 - Macclesfield – Hayfield changes. -
Regional Geology
CHAPTER III REGIONAL GEOLOGY The area known as the West Riding was an administrative EARLY PALAEOZOIC division of the ancient county of Yorkshire and includes (ORDOVICIAN TO DEVONIAN SYSTEMS) parts of the modern administrative areas of West Ordovician rocks outcrop as small inliers east of Howgill Yorkshire, North Yorkshire, Cumbria and Lancashire. Fells and more extensively in the extreme northwest Geographically the area extends from the high ground around Sedburgh. Historically they were exploited on a (>600m) of the Pennines in the north and west into the local basis for building stone, flagstones and roofing slates. lowland areas marginal to the Vale of York in the east. The Silurian rocks were exploited for flagstones in the These major topographic subdivisions reflect changes Ingleton and Horton-in-Ribblesdale areas and were used in the underlying geological formations (Fig. 6). The locally for grave stones, boundary and milestone markers. high mountainous spine of the Pennine area that crosses The best known of these stones were the Horton Flags the West Riding from north to south, is underlain by which were quarried around Helwith Bridge (from the hard, durable rocks ranging from Precambrian to seventeenth to nineteenth centuries: Mitchell, W. 1985). Namurian (Carboniferous) in age. The lower ground to The massive sandstones of the Austick Grits were also the south-east is underlain by the thick Coal Measure used locally for building. Stones from this succession have successions exposed in the deeply incised valleys of the not so far been identified in the Anglo-Saxon carved Yorkshire Coalfield, extending southwards from Leeds to Sheffield. -
Street Name Street Number Parish Score Alderley Road C420 Mottram
Street Name Street Number Parish Score Alderley Road C420 Mottram St Andrew 0 Alsager Road C609 Betchton 0 Artists Lane C419 Nether Alderley 75 Back Lane C104 Ashley 0 Bailey Crescent UY627 Congleton 0 Barlow Road UW1199 Wilmslow 0 Beatty Drive UY636 Congleton 0 Berkshire Drive UY1858 Congleton 0 Bexton Road UW1230 Knutsford 0 Birch Tree Lane UY1170 Odd Rode 75 Birtles Road UW1235 Macclesfield 0 Black Road UW1238 Macclesfield 0 Blackden Lane C318 Goostrey 0 Blackhill Lane UW1239 Knutsford 35 Blakelow Road UW1241 Macclesfield 50 Bomish Lane UW2493 Goostrey 0 Bond Street UW1251 Macclesfield 25 Bridgemere Lane C535 Hunsterson 25 Brook Street UW1268 Macclesfield 25 Broughton Road C502 Crewe 25 Brownlow Heath Lane C307 Newbold Asbury 0 Browns Lane UW1274 Wilmslow 0 Brunswick Street UY663 Congleton 0 Burleyhurst Lane C106 Mobberley 35 Burleyhurst Lane C106 Wilmslow 35 Buxton Old Road UY667 Congleton 0 Calveley Hall Lane C519 Calveley 25 Calveley Hall Lane UY1391 Calveley 25 Castle Mill Lane C104 Ashley 0 Castle Mill Lane UW2078 Ashley 0 Catherine Street UW1305 Macclesfield 0 Cawley Lane C416 Adlington 50 Chance Hall Lane C306 Moreton cum Alcumlow 0 Chance Hall Lane C306 Odd Rode 0 Chancery Lane UY676 Alsager 0 Chancery Lane UW1310 Bollington 0 Chantry Road UW2709 Disley 25 Chapel Road C420 Alderley Edge 0 Chapel Street UY678 Congleton 0 Chapel Street C304/A/03 Odd Rode 0 Checkley Lane C535 Checkley cum Wrinehill 35 Chelford Road C410 Over Alderley 25 Chelford Road C417 Prestbury 25 Chester Road UW5031 Rostherne 0 Chester Street UY1768 Crewe -
C/R/D Summary Skeleton Document
Application No: 19/3774M Location: LIDGETTS LANE, RAINOW, MACCLESFIELD Proposal: The proposed development includes a new service reservoir, construction compounds and connection pipework to the exiting service reservoir. Applicant: Mr Michael Barton, United Utilities Plc Expiry Date: 14-Feb-2020 SUMMARY The proposed development seeks the erection of a new Service reservoir and associated infrastructure within close proximity to an existing facility in order to allow servicing and maintenance of the existing reservoir and in effect, provide a ‘back-up’ option for the local water supply. The proposal would represent inappropriate development in the Green Belt by reason of its impact upon openness and encroachment. There would also be limited landscape harm created. However, it is deemed that Very Special Circumstances apply that clearly outweigh this harm. More specifically, the significant implications on local water supply if the facility not provided (in event of failure of the existing facility) and the because of the subsequent likely greater landscape implications of the alterative option which is to lay several kilometres of pipework and erect new pumping stations across a greater area. As such, the principle of the proposal is deemed to be acceptable. The scheme is deemed to be of an appropriate functional design that would not create any significant concerns with regards to; highways, amenity, landscape, trees, nature conservation, flooding and drainage, archaeology or Public Rights of Way, subject to conditions where necessary. For the above reasons, the application is recommended for approval. RECOMMENDATION APPROVE subject to conditions REASON FOR REFERRAL The application has been referred to Northern Planning Committee because it relates to a commercial development comprising of a site between 2 and 4 hectares. -
Landscape-Strategy-Dark-Peak.Pdf
www.peakdistrict.gov.uk 3: Dark Peak Peak District National Park Authority Dark Peak Dark Peak open moorland © Peak District National Park Authority Introduction The Dark Peak is a sparsely settled area of gritstone uplands lying at the southern end of the Pennine Hills. The area comprises an extensive upland plateau with steep gritstone slopes, sometimes with rocky edges, that drop away to lower lying slopes, wooded cloughs and deep valleys, some of which have been flooded to create large reservoirs. It contrasts sharply with the adjoining limestone uplands of the White Peak and is named on account of the dark hues created in the landscape by the peat moors and exposed gritstone. Whilst this landscape character area contrasts with the White Peak, the transition to other landscape character areas such as the Dark Peak Eastern and Western Fringe landscapes is much more gradual; these are landscapes of similar character but tend to be lower lying, more settled and more intensively managed than the Dark Peak with enclosed farmland rather than open moorland predominating. The Eastern Moors to the south-east of the Dark Peak are similar to it in character but lower lying with less deep peat creating a landscape that has been more obviously modified by people than the Dark Peak generally has. In the north, the moorland plateau of the Dark Peak continues into the Southern Pennines. 2 Landscape Strategy and Action Plan Peak District National Park Authority 3: Dark Peak such as the golden plover and the dunlin. On the lower moorland Physical influences slopes heather dominates, with varying amounts of bilberry, The Dark Peak is an extensive area of high moorland and adjacent cowberry and crowberry. -
FIGURE 3 Solid Geology of Cheshire and Lancashire, with the Distribution of Stone Types Used for Anglo-Saxon Sculptures in Chesh
10 FIGURE 3 Solid geology of Cheshire and Lancashire, with the distribution of stone types used for Anglo-Saxon sculptures in Cheshire and Lancashire CHAPTER III REGIONAL GEOLOGY by C. Roger Bristow Geographically, the counties of Lancashire and Cheshire METHODOLOGY extend from the high ground (up to 560 m OD in the north in the Forest of Bowland) of the Pennines All the carved stones in the present area have been in the east, to sea level in the west. This topographic examined, in situ, using a hand lens. As the stones could not range is largely a reflection of the underlying geology be ‘hammered’ to produce a fresh surface, examination with the harder, Carboniferous, rocks forming the depended partly on the vagaries of preservation and higher ground in the east, and the somewhat less well location. It means that some stones could not be properly cemented, commonly reddened, Triassic sandstones and examined — for example those with a heavy lime wash softer Mercia Mudstone occupying the lower ground (Hilbre 2 and Whalley 9) or a heavy overgrowth of in the west. These ‘solid’ rocks are in turn overlain by lichen (Wincle Grange 1). The above-mentioned lens extensive, thick, deposits of Quaternary glacial sand and has an in-built graticule which allows the size(s) of the gravel, boulder clay and alluvium and peat. constituent grains to be determined fairly accurately. The Drainage of this area is dominantly by northward- grain-size terminology is based on Wentworth (1922) flowing rivers in the south into the rivers Dee and Mersey. which distinguishes five sandstone categories: very fine In the centre, the principal drainage off the Pennines is 0.032–0.125 mm, fine 0.125–0.25 mm; medium 0.25– southwards before these rivers unite to flow westwards 0.5 mm; coarse 0.5–1.0 mm and very coarse 1.0–2.0 mm. -
Bollington at the Time of the 1911 Census
A Century Ago – Bollington at the time of the 1911 census SOMEWAYS DIFFERENT…SOMEWAYS NOT. The Bollington of 100 years ago was not so very different in appearance from the Bollington of today, give or take wedges of new housing at Bollington Cross, Ingersley Road and elsewhere. The basic physical outline of the village with its stone cottages and houses was already in place alongside the churches, public houses and other community features in that Census year 1911. The aqueduct carrying the Canal across the valley was there, and the railway viaduct with the green sward of the (Gnat Hole) Recreation Ground between them. White Nancy had been standing guard on Kerridge Hill from 1815 onwards. The Cotton Mills (Clarence, Adelphi and Olivers’ Waterhouse Mill) were working and the Paper Mill, Oak Bank, and others. There were, to be sure, many more shops and, other than on foot, by horse, train, and such cars as there were, there was no great back and forth to Macclesfield and beyond. Supermarkets lay in the future and Bollington was much more self-contained than it is now. The skies above were quiet with no Manchester Airport nearby and the main noise (and smell) in the streets came from horses, although cars were beginning to make an appearance. With no radios, TV sets or Internet it was naturally the case that folk knew more about their actual neighbours than “breaking news” about people on the other side of the world and in the country at large. Yet, without a doubt, events national and international could have their impact in Bollington as when the American Civil War had (many years before) shut down our Cotton Mills through lack of raw materials. -
Origin of Carboniferous Sandstones Fringing the Northern Margin of the Wales-Brabant Massif: Insights from Detrital Zircon Ages
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by NERC Open Research Archive Origin of Carboniferous sandstones fringing the northern margin of the Wales-Brabant Massif: insights from detrital zircon ages ANDREW MORTON1,2*, COLIN WATERS3, MARK FANNING4, IAN CHISHOLM5 and MATT BRETTLE6 1 HM Research Associates, 2 Clive Road, Balsall Common, CV7 7DW, UK 2 CASP, University of Cambridge, 181a Huntingdon Road, Cambridge CB3 0DH, UK 3 British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 4 Research School of Earth Sciences, The Australian National University, Canberra ACT0200, Australia 5 4 Park Street, Loughborough, Leicestershire, LE11 2EG, UK 6 Premier Oil UK Limited, 53 Blenheim Place, Aberdeen AB25 2DZ, UK *Correspondence to: Andrew Morton, HM Research Associates, 2 Clive Road, Balsall Common, CV7 7DW, UK. Email: [email protected] ABSTRACT A study of detrital zircon age populations in Namurian-Westphalian (Carboniferous) sandstones in the southern Central Pennine Basin of the UK has revealed considerable complexity in their provenance history. The Pendleian-Marsdenian Morridge Formation, which is known to have been derived from the Wales-Brabant Massif to the south on the basis of palaeocurrent and petrographic information, is dominated by zircons ultimately derived from the Caledonian belt to the north. These zircons were recycled from sandstones of northern origin that had been previously deposited over the massif during Middle to Late Devonian times. The Morridge Formation also includes Late Neoproterozoic zircons of local Wales-Brabant Massif origin. The south lobe of the Yeadonian Rough Rock has been previously interpreted as having a complex provenance including sediment of northern origin interbedded with sediment ascribed to a Wales- Brabant Massif source. -
S a Turd a Y Sund a Y Frid a Y S At
SATURDAY 6.45PM CATHERINE HARDMAN Booths Supermarket THE HOWLING REV THE CATENIAN & FRIENDS MALE VOICE ABIGAIL CHETHAM CHOIR 3.30 - 4.30 7PM Dexter and Jones DRUMROOTS - AFRICAN DRUMMING JAM SESSION WORKSHOP (DROP-IN) FRIDAY 7PM Brook Street Club 4PM Dexter and Jones TOM ATTAH AND MAT WALKLATE HELEN WALFORD THE GRITSTONE CLAYS ASHLEY SHERLOCK 7PM The Courthouse MILES HUNT 7.30PM St Cross Church SAM LYON VALE ROYAL STRING ORCHESTRA THE FINE LINES 7.30PM Knutsford Little Theatre 7.30PM Knutsford Little Theatre PILGRIMS’ WAY MIKE MCGOLDRICK & FRIENDS LUCAS MARKS AMELIA COBURN 8PM The Cross Keys 7.30PM St John’s Church THE MUSIC TRAIN WITH GEOFF TATTON SINGERS HIGGINBOTTOM & ROB CARROLL 8-11PM The Botanist 8PM Old Sessions House ELLIE & SIMON BEN ROTHWELL 12.30-1.15PM & 1.45-2.30PM Lost & Found 8PM-11PM The Botanist LUMINOUS TONY & JOHN 1-5PM Evuna 9PM TIL LATE SUNDAY April’s Kitchen GLENN SHARP DEAN MAC AND THE 105 2-4.30PM The Botanist 12.30PM - 1.30PM Saks Hair RICK W AMY GRACE 3PM Old Sessions House 12.30-1.15PM;1.45-2.30PM Lost & Found BERIAN MILES MODJANGO 3.15 TO 5.15PM The Lord Eldon 1PM SAT The Market Hall KNUTSFORD TRADITIONAL & FOLK CHARLOTTE PETERS ROCK SESSION DAVE VAUGHAN HELEN WILSON 4PM The Courthouse HALLE BRASS 1PM - 3PM April’s Kitchen RNCM ZERBINA DUO SHAMONA 4PM Dexter and Jones 2PM - 3PM Saks Hair CHRIS HOWARTH MARTHA DAWSON 7.30PM Knutsford Little Theatre 2.30 - 4.30 Music on the Moor GREG RUSSELL & CIARAN ALGAR KRAFTY KIDZ MARK RADCLIFFE WITH DAVE RUSSELL EMMA GILMOUR PERFORMS AS ELSA & CHRIS LEE Join us for a laid-back summer celebration of the very best food, TICKET INFO drink and music, hosted by Tom Kerridge THE LAMBING SHED, KNUTSFORD 7 – 9 SEPTEMBER 2018 22-24 JUNE 2018 SOME EVENTS REQUIRE TICKETS WHICH ARE OFFICIAL PROGRAMME AVAILABLE ONLINE AT: WWW.KNUTSFORDMUSICFESTIVAL.COM OR FROM THE COUNCIL OFFICES: TOFT ROAD, KNUTSFORD, WA16 6TA. -
REGIONAL GEOLOGY by Graham K. Lott
CHAPTER II REGIONAL GEOLOGY by Graham K. Lott The ‘quarrying’ and use of local stone in Notting- the Triassic comprises a thick succession of non- hamshire, for both building and decorative purposes, marine, green-grey to reddish brown sandstones, dates back to Roman times. However, the lithological siltstones and mudstones, the latter including thinly units that characterise the geological succession interbedded, grey-green, dolomitic, very fine grained within the county contain only a few beds of stone sandstones (known locally as skerry). In contrast, the suitable for these purposes. This lack of indigenous early Jurassic marine succession is only sporadically stone useful for decorative carving is reflected in the exposed along the northern edge of the low-lying composition of the suite of carved stone fragments Vale of Belvoir and comprises a succession of grey that have been studied as part of this Corpus project. limestones and mudstones (Lias Group). The eastern By far the majority of the stones examined consist part of the county is locally blanketed by extensive of lithologies (primarily sandstones and limestones) tracts of glacial and alluvial sediments (unconsolidated sourced from outside the county border. sands, gravels, clays and muds) of Quaternary age. carboniferous THE GEOLOGY OF NOTTINGHAMSHIRE Pennine Coal Measures Group Nottinghamshire has a relatively simple geological The Carboniferous rocks that crop out in the west of succession comprising a sequence of eastwards- the county form part of the Pennine Coal Measures dipping sedimentary rock units whose outcrops Group. This succession is best known economically extend from north to south across the county (see for its coal reserves but also contains a number of Fig. -
UK FAST CHESHIRE CRICKET LEAGUE DIV's 3 & 4
UK FAST CHESHIRE CRICKET LEAGUE DIV's 3 & 4 2019 wk UKFCCL DIV 3 Umpire Umpire 2019 wk UKFCCL DIV 4 Umpire Umpire SAT 1 JUNE 7 UKFCCL DIV 3 SAT 1 JUNE 7 UKFCCL DIV 4 Over Peover v Chester Co Officers Brian Cheetham John Wheater Bowdon Vale v Trafford MV David Edwardes Aston v Frodsham Chris Hyde Terry Marnick Kerridge v Saughall Ron Tweats Dave Lawson Bunbury v Wirral Tom Grindley Paul Tyrell Malpas v Winsford Mike Boffey Ashleigh Wood Cholmondeley v Knutsford John Bone Phil Goodall Styal v Mossley Ian Barber CH Ladybridge v Old Parkonians Bob Butland Bill Curtis Tranmere Victoria v Glazebury John Edmonds Ian Taylor Holmes Chapel v Audlem Duane Jones Pal Sundaram Westminster Park v Wistaston Terry Johnson Mike Woollard SAT 8 JUNE 8 UKFCCL DIV 3 SAT 8 JUNE 8 UKFCCL DIV 4 Audlem v CH Ladybridge Jeff Langham Chris Hind Glazebury v Malpas Terry Johnson Chester Co Officers v Cholmondeley Keven Johnson Tom Miller Mossley v Tranmere Victoria Andrew Simpson Frodsham v Holmes Chapel Tony Sayle Brian Cheetham Saughall v Bowdon Vale Dave Clayton Geoff Young Knutsford v Aston Steven Foster Chris Moore Trafford MV v Westminster Park Bill Alger Old Parkonians v Bunbury Alan Squibbs Mike Boffey Winsford v Kerridge Ken Simpson Wirral v Over Peover Terry Marnick Wistaston v Styal Ron Tweats Ashleigh Wood SAT 15 JUNE 9 UKFCCL DIV 3 SAT 15 JUNE 9 UKFCCL DIV 4 Over Peover v Old Parkonians Ron Tweats Keith Gardiner Bowdon Vale v Winsford Philip Lowe Roger Seymour Aston v Cholmondeley Don Joy Tom Grindley Kerridge v Malpas Chris Hyde Ashleigh Wood Bunbury v -
Walk the Way in a Day Walk 47 Bleaklow and Old Glossop
Walk the Way in a Day Walk 47 Bleaklow and Old Glossop Following the course of a Roman road (Doctor’s Gate) 1965 - 2015 up onto the Bleaklow plateau, the Pennine Way is joined as it makes its way across difficult moorland terrain and along a cliff-edge path (Torside Clough). The return route includes a railway trail and quiet roads, passing through the suburbs of Glossop. Length: 13¾ miles (22¼ kilometres) Ascent: 2,297 feet (700 metres) Highest Point: 2,077 feet (633 metres) Map(s): OS Explorer OL Map 1 (‘The Peak District - Dark Peak’) (West Sheet) Starting Point: Doctor’s Gate (start), Old Glossop (SK 045 948) Facilities: Public toilets at Manor Park. Inn at Old Glossop. Website: http://www.nationaltrail.co.uk/pennine-way/route/walk- way-day-walk-47-bleaklow-and-old-glossop The Doctor’s Gate There is roadside parking near the start of the Doctor’s Gate, on a side road (Shepley Street) leading to a bus turning circle between some factories and a stream. The first part of the walk follows the Doctor’s Gate for 3¼ miles (5½ kilometres) up the valley of Shelf Brook. A finger sign marks the start of a hardcore track, which is followed east. On the far side of the stream are the wooded slopes of Shire Hill, while dotted about the valley floor are mature oaks and sycamores. As the track veers towards a stone bridge leading to a farm, turn through a gate on the left (1 = SK 060 947). Walk 47: Bleaklow and Old Glossop page 1 The Doctor’s Gate To the west of Glossop is the Roman fort of Ardotalia, known Bleaklow popularly as Melandra Castle.