DOCSLIB.ORG

Glossop Conservation Area Character Appraisal Supplementary Planning Document

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Glossop Conservation Area Character Appraisal Supplementary Planning Document Glossop Conservation Area Character Appraisal Supplementary Planning Document LDFGlossop 3 Conservation Area Character Appraisal Supplementary Planning Document Adopted 1 LDF 3 March 2006 CONTENTS Introduction 5 Summary 6 Historic Context 7 1. Industrial Context 7 2. Early Origins 7 3. Expansion 8 4. Consolidation 11 5. Decline 12 6. The End of the Mills 12 The Boundary 14 Character Appraisal 15 1. Architectural Quality 15 2. Street Pattern 21 3. Spaces 23 4. Scale and Density 25 5. Setting 27 6. Traditional Building Materials 29 7. Floorscape 31 8. Shopfronts and Advertisements 33 9. Contribution 0f Trees and Planting 34 10. Negative Factors 36 Appendices 1. Map of Town Centre Conservation Area 2. THI Stage 2 Bid Needs Assessment 3. Listed Buildings 2 INTRODUCTION Glossop has significant historical associations with the development of the textile industry in Derbyshire, which together with the special character of its streets and its unique mix of building styles has led the Borough Council to designate four conservation areas covering the town centre. Each designation aims to preserve or enhance the special character of the area and protect significant elements of its historical evolution. This analysis has been prepared to inform the continued development of the town whilst preserving those aspects, which make it special. It will identify the particular qualities and character of the area as well as the features detracting from its appeal. For the purpose of the appraisal the town centre conservation areas have not been separately defined as the town developed as a whole entity and the analysis of each component of the townscape relates equally to all areas to a greater or lesser extent. This appraisal is not exhaustive and any building, feature or site not mentioned will not mean that it is of little or no significant interest to the character of the conservation area. This document has been prepared with reference to Policy BC5 (Conservation Areas and Their Settings) of the Adopted High Peak Local Plan, March 2005. It will give certainty to developers, planners and the general public that development proposals will respect the characteristic features of the Conservation Area, therefore protecting its character. 3 SUMMARY The origin of Glossop as a centre for the cotton industry defines its character in the modern day. A range of 19th century workers cottages, 19th century industrial mills and publicly donated fine buildings are the surviving evidence of Glossop's development during a period where the textile industry dominated the local economy. The centre of Glossop is also characterised by a range of commercial buildings, housing a wide range of small independent shops, and financial institutions clustered around the crossroads. Interspersed between them are large-scale two and three storey administrative and public buildings. Residential areas are located around the commercial core and at the edges of the High Street. Currently Glossop has a few problem buildings and sites and with these exceptions the vast majority of buildings have a beneficial role to play in preserving or enhancing the character of the town. 4 1. HISTORIC CONTEXT 1.0 Industrial Context The original industrial settlement in the area Old Glossop lies a mile to the east of the present day town. Old Glossop was the original ‘Glossop’, a small agricultural settlement, which developed as the medieval market town and administrative centre for Glossopdale; a dispersed agricultural community based around six hillside communities. 1.1 The damp climate and proximity to flowing water that encouraged this early settlement was also to be responsible for its further development and expansion in the 17th and 18th centuries, when, from the wool spinning of yeoman farmers, (Old) Glossop became a thriving industrial textile town. Its location, close to a supply of fast running streams and in relatively close proximity to Manchester, contributed towards its rapid growth. As elsewhere, textile production at that time focused on domestic spinning. 1.2 The end of the 18th century witnessed the transformation industry nationally from a cottage industry to a factory system of mass production. The introduction of steam power required more plentiful supplies of water and between 1785 and 1831 a significant number of new larger cotton mills were built. By the 1830’s, 46 mills had been built extending due west along the watercourses along the valley bottom and away from (Old) Glossop. 1.3 Early Origins (1793 – 1830) Until 1792 the population travelled between townships of the dale along farm lanes, many of which survive as footpaths. In 1793 the turnpike from Chapel- en-le-Frith to Enterclough Bridge (Woodhead Road) was laid followed in 1803 by the road from Marple Bridge to Glossop, (later extended to form the Snake Turnpike) which linked the mills along the valley bottom. The crossroads of the two roads became the natural focus for the new industrial settlement. In 1807 the Howard Arms, originally a farmhouse selling ale, was rebuilt as a coaching inn further consolidating the centre. A new community started to develop and in 1811 the Littlemoor Chapel was built on Victoria Street. 1.4 The great and sustained burst of building after 1780 was on a scale not previously experienced. The valley had everything needed to encourage and sustain population growth. The Glossop quarries1 produced millstones, freestones and flagstones for paving or roofing. Early fuel was from local peat and wood. By the 19th century there were coal mines at Bore Lane, Chisworth, Combs Charlesworth, Ludworth and Simmondly. In 1801 at the first ever census there were 2,759 people in the eight townships of the dale, a doubling since 1740. By 1821 the population had almost doubled again to 5,135. 1 The quarries had possibly developed following the great rebuilding of the 17th century 5 1.5 From 1782 to 1820 carding and spinning mills were built along every brook in the dale. In 1815 Matthew Ellison, agent for the Duke of Norfolk, built Wren Nest Mill in High Street West. In the same year, John Wood came to Glossop from Marsden in Yorkshire, and rented two vacant mills in (Old) Glossop. By 1819 he had moved to Bridge End and extended an old Fulling Mill. 1.6 By 1820 the Shelf Brook area had nine mills, there were five on Hurst Brook, eight on Chunal brook, eight on Glossop Brook, six on Padfield Brook and six on the Glossop side of the River Etherow. The longest stretch without any textile mills was the length of Glossop Brook near Manor Park (the grounds to the former seat of the Howard’s) being as it was, in close proximity to the Howard family home. Most mills were for cotton spinning, a few span wool and a smaller number paper making. The names of some mills, such as Wren Nest, reflected on the once rural character of the area. Others, such as Woods Mill, were simply named after the owner. 1.7 The ‘new’ town, known by then as ‘Howard Town’2 grew rapidly as rows of stone cottages were built to house the many mill workers and managers. “The cottages were small and low by modern standards, not served by piped water or gas...and with primitive sewerage facilities. They were however solid and weatherproof, close to the mills, neighbours and the growing shops....Ground floors were stone flagged and probabaly scrubbed refularly and sanded, and in the best cottages the open fire place was replaced by cast iron ovens....which provided cooking facilities and hot water...” Farey (1817) 1.8 Expansion (1830-1860) Between the start of the 19th century and 1850 the population grew six fold as the continued growth of large individual mills was spurred on by the development of the steam engine. By 1842, Howard Town Mill, Wren Nest Mill and Sidebottom's in Hadfield stood out from the rest. The majority of mills employed less than 100 people3. At that time Howard Town employed 1,256 people, Wren Nest 513 and Sidebottom's 835. The Howard Town Mills of John Wood and Brothers Limited was the largest textile mill site in north- west Derbyshire and at its peak was one of the largest integrated cotton mills in the country. 1.9 The town was also taking shape at this time. In 1837 Norfolk Square was laid out. As would be expected, the earliest development of the town concentrated along the Marple Bridge Road that linked the mills along the valley floor. 2 After Bernard Edward Howard the 12th Duke of Norfolk 3 Below these 3 were 9 smaller units employing between 100 and 200 people. The remainder comprised over 30 mills. 6 1.10 The building of the Town Hall started in 1838. The original design comprised the arcaded Town Hall building with a symmetrical row of shops either side, which culminated in domed pavilions at either end where it turned the corner. At that time it housed a lock up prison, underneath the town hall on the east side of the arcade. By 1844 a savings bank was held in the Town Hall on Mondays. The building also housed the Glossop County Court. Building continued with the 13th Duke. 1.11 By 1860 a number of areas of smaller streets had been set out off the turnpike roads. One area focused directly to the south of Howard Town Mill, another to the south of Wren Nest Mill and another around the railway station to the north of the town centre. 1.12 The town’s expansion resulted in the extension of local quarries. The sled roads from Glossop Low and Shelf Benches along which horses hauled the stone survive to the present day.
Load more

Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Geology of Todmorden Moor 2 Background
    GEOLOGY OF TODMORDEN MOOR 2 BACKGROUND 1) THE CARBONIFEROUS SERIES OF ROCKS • The rocks of the Todmorden district are of the Carboniferous Series and were first laid down in an ancient sea, which covered most of England. The shells of marine animals in this sea accumulated on the sea floor to form thick beds of chalk-like ooze, which formed Carboniferous Limestone. • An upward movement of the land made the sea shallower bringing the limestone beds closer to a new shoreline. As a result, sand and mud brought down by the continental rivers became sandstones and shales. They tend to be laid in alternating layers, usually with the shales thicker than the sandstones. • Shales are very weak rocks, and grade into mudstones, which are even weaker. Sandstones are much stronger, but again vary considerably in character, some being easily crumbled, some massive but varying in hardness, while others are compressed into layers of hard flag. Sometimes sand and silt have been mixed and form intermediate shaley mudstones. • Some sandstones are so coarse that they are called Millstone Grit. Some of the grits are called Kinderscout grit, because a fine example occurs at Kinderscout in Derbyshire, while other beds of sandstone have names such as Todmorden Grit, Middle Grits, Gorpley Grit, Hazel Greave Grit, &c. according to location or position. There are also many other layers of shale and sandstone that have no special characteristics that enable them to be named specifically. The last of the layers of the Millstone Grit series is a bed of particularly coarse sandstone known as Rough Rock.
    [Show full text]
  • The Growth of Geological Knowledge in the Peak District Trevor D
    The Growth of Geological Knowledge in the Peak District Trevor D. Ford Abstract: The development of geological knowledge in the Peak District from the 18th century to the present day is reviewed. It is accompanied by a comprehensive bibliography. Introduction lead miners made practical use of geological principles as early as the 17th century (Rieuwerts, Geology has changed in the last two centuries from 1984). In the 18th century the course of the initial a largely amateur “gentleman’s” science to a part of Cromford Sough followed the strike of the professional vocation. The results of professional limestone/shale contact where excavation was easier investigation in the Peak District have been built on through shale. The position of the contact was the amateur foundation and the works cited in this obtained by down-dip projection from the outcrop review demonstrate the change in approach. The showing that the soughers had some appreciation of Geological Survey commenced a professional concealed geology. The lead miners also used the approach in the 1860-1880 period, continued basic principles of stratigraphy and structure to during World War I and in the 1950s, but it was not predict whether or not they would intersect until the 1970s that some intensive economic toadstones in driving other soughs in the 18th investigations were pursued. The Geological century (Fig. 1). Survey’s activities in the 20th century were concurrent with the development of Geology Whilst most of the lead miners’ knowledge was Departments in the nearby Universities, where never written down, some of it has been preserved in research grew slowly after World War I and more the appendix to “An Inquiry into The Original State rapidly after World War II.
    [Show full text]
  • Baseline Report Series: 18
    Baseline Report Series: 18. The Millstone Grit of Northern England Groundwater Systems and Water Quality Commissioned Report CR/05/015N Science Group: Air, Land & Water Technical Report NC/99/74/18 i The Natural Quality of Groundwater in England and Wales A joint programme of research by the British Geological Survey and the Environment Agency BRITISH GEOLOGICAL SURVEY Commissioned Report CR/05/015N ENVIRONMENT AGENCY Science Group: Air, Land & Water Technical Report NC/99/74/18 This report is the result of a study jointly funded by the British Baseline Report Series: Geological Survey’s National Groundwater Survey and the 18. The Millstone Grit of Northern Environment Agency Science Group. No part of this work may be England reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, C Abesser, P Shand & J Ingram without the prior permission of the copyright proprietors. All rights are reserved by the copyright Contributors proprietors. Disclaimer R Hargreaves (GIS), M Moreau (Sampling), P Sapey The officers, servants or agents of (Illustrations) both the British Geological Survey and the Environment Agency accept no liability whatsoever for loss or damage arising from the interpretation or use of the information, or reliance on the views contained herein. Environment Agency Dissemination status Internal: Release to Regions External: Public Domain Project No. NC/99/74 ©Environment Agency, 2005 Statement of use This document forms one of a series of reports describing the baseline chemistry of selected reference aquifers in England and Wales. Cover illustration Sandstone of the Pendle Grit ii Formation in a 20 m face in a disused quarry [SD 6143 3796] Key words Environment Agency Project Manager: Baseline, Millstone Grit, Yorkshire, Lancashire, Pennines, water quality, hydrogeochemistry, UK Dr Rob Ward / Jonathan Smith/ Alwyn Hart aquifer.
    [Show full text]
  • REGIONAL GEOLOGY by C
    CHAPTER II REGIONAL GEOLOGY by C. Roger Bristow TOPOGRAPHY The grain-size terminology is based on Wentworth (1922) which distinguishes five sandstone categories: Geographically, the counties of Derbyshire and Staf- very fine 0.032–0.125 mm, fine 0.125–0.25 mm; fordshire extend from the high ground (up to 636 m medium 0.25–0.5 mm; coarse 0.5–1.0 mm and very OD at Kinderscout) of the Peak District in the north, coarse 1.0–2.0 mm. The term ‘granule’ refers to grains down to about 30 m in the Trent Basin in the south east. between 2 and 4 mm; ‘pebbly’ refers to clasts/grains This topographic range is largely a reflection of the > 4.0 mm. underlying geology with the harder, Carboniferous, The qualification of the term ‘sorting’ as used rocks forming the higher ground in the north, and the herein does not follow the strict geological definition somewhat less well cemented, commonly reddened, as no grain-size analysis was undertaken. ‘Well sorted’ Triassic sandstones and softer Mercia Mudstone means that most of the grains are of approximately occupying the lower ground in the south. the same size; ‘poor’ is the opposite, with a wide In the south, the River Trent, a major transport variation in grain size; ‘moderate’ falls between the route, flows dominantly south-eastwards until it is two preceding definitions. joined by the north-flowing River Tame and the west- The colours and their numeric reference used to flowing River Mease just east of Alrewas and then describe the carved stones are taken from the Rock- swings north-eastwards up through Burton where it Color Chart produced by the Geological Society of is joined by the eastward-flowing River Dove, and America, 1963.
    [Show full text]
  • HWR Chatsworth Paper Vsept07 Unformatted.Doc 28/07/2008
    HWR Chatsworth paper vSept07 unformatted.doc 28/07/2008 REGIONAL EVOLUTION OF A FLUVIODELTAIC CYCLIC SUCCESSION IN THE MARSDENIAN (LATE NAMURIAN STAGE, PENNSYLVANIAN) OF THE CENTRAL PENNINE BASIN, UK. 1 2 3 4 C.N. WATERS , J.I. CHISHOLM , A.C. BENFIELD and A.M. O’BEIRNE 1 British Geological Survey, Keyworth, Nottingham NG12 5GG, UK [email protected] 2 4 Park Street, Loughborough, Leicestershire LE11 2EG, UK 3 24 Gascoigne Avenue, Barwick-in-Elmet, Leeds LS15 4LW, UK 4 32 Hemberton Road, London SW9 9LJ, UK SUMMARY: Basinwide analysis of sedimentary facies, isopachytes and palaeocurrents for two late Marsdenian (Pennsylvanian) sedimentary cycles within part of the Millstone Grit Group, has led to a new sequence-stratigraphic interpretation for the relationships between its constituent sandstone units (currently named Huddersfield White Rock, Chatsworth Grit, Brooksbottoms Grit, Holcombe Brook Grit, Brown Edge Flags and Redmires Flags). The Bilinguites superbilinguis (R2c1) and Verneulites sigma (R2c2) marine bands related to fourth-order marine highstands show faunal variations possibly reflecting fifth-order sea-level fluctuations. The lower R2c1 cycle consists entirely of deep water mudstone. The overlying R2c2 cycle shows an upward regressive passage through pro-delta and delta-slope deposits to mouthbar and channel sandstones. The latter comprises an ‘eastern inflow’ of northerly provenance, the distribution of which was not influenced by the underlying basement configuration, and a ‘southern inflow’ sourced from the Wales-Brabant High. Falling sea-levels resulted in progressive narrowing of the fluvial pathway within the main sandstone body of the ‘eastern inflow’, with a concomitant increase in flow velocities and grainsize.
    [Show full text]
  • Walk the Way in a Day Walk 49 Kinder Scout from Hayfield
    Walk the Way in a Day Walk 49 Kinder Scout from Hayfield A splendid hill-walk retracing the route of the famous 1965 - 2015 mass trespass onto Kinder Scout. Heading up William Clough, the Pennine Way is followed along the plateau edge, passing the dramatic Kinder Downfall and visiting Kinder Low before returning by an old pack-horse route. Length: 9 miles (14½ kilometres) Ascent: 1,641 feet (500 metres) Highest Point: 2,077 feet (633 metres) Map(s): OS Explorer OL Map 1 (‘The Peak District - Dark Peak’) (West Sheet) Starting Point: Bowden Bridge car park, near Hayfield (SK 047 868) Facilities: Public toilets. Full range of facilities at Hayfield. Website: http://www.nationaltrail.co.uk/pennine-way/route/walk- way-day-walk-49-kinder-scout-hayfield William Clough The starting point is reached by following Kinder Road as it heads east from the village centre. As well as the ‘pay and display’ car park at Bowden Bridge, there is limited roadside parking near the Sportsman pub. There are public toilets opposite the car park, beside the entrance to Hayfield Campsite. The first part of the walk follows the route of the mass trespass, 2¾ miles (4½ kilometres) onto Kinder Scout. From the car park, turn left and continue along Kinder Road, following a leafy lane running parallel to the River Kinder. Crossing the river, a finger sign marks a left turn through a gate. Hayfield Hayfield is an attractive village of narrow streets located on the River Walk 49: Kinder Scout from Hayfield page 1 Sett. There has been a settlement here since at least Anglo-Saxon demolished in 1900.
    [Show full text]