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White Peak Trails and Cycle Routes
Things to See and Do The High Peak Trail by funded part Project The Countryside The Cromford and High Peak Railway was one of the first The White Peak is a spectacular landscape of open views railways in the world. It was built between 1825 and s www.derbyshire.gov.uk/buse characterised by the network of fields enclosed by dry stone Several Peak District 1830 to link the Peak Forest Canal at Whaley or 2608 608 0870 walls. North and south of Hartington the trails go down into villages have annual Bridge (north of Buxton) to the Traveline from timetables and services other updates, Check the deep valley of the Upper Dove and the steeper gorge at well dressings (a Cromford Canal – a distance of Hire. Cycle Waterhouses and tableau of flower- Beresford Dale. On the lower land are the towns and villages 33 miles. The railway itself was Hire Cycle Ashbourne to Leek and Derby links 108 Travel TM built from local stone in traditional style. based pictures designed like a canal. On the around the village flat sections the wagons were Hire. Cycle Hay Interesting Places wells). Ask at visitor pulled by horses. Large Manifold Track below Thor’s Cave Parsley and Hire Cycle Ashbourne to Buxton links 542 Bowers centres for dates. The Trails and White Peak cycle network have a rich industrial steam powered Centre. Hire Cycle Ashbourne and Hire Cycle Water heritage and railway history. beam engines in The Manifold Track Carsington to Wirksworth and Matlock links 411 Travel TM Look out for the sculpted benches along the Trails and the From Track to Trail And Further Afield ‘engine houses’ This was the Leek and Manifold Valley Light Railway. -
Reconstructing Palaeoenvironments of the White Peak Region of Derbyshire, Northern England
THE UNIVERSITY OF HULL Reconstructing Palaeoenvironments of the White Peak Region of Derbyshire, Northern England being a Thesis submitted for the Degree of Doctor of Philosophy in the University of Hull by Simon John Kitcher MPhysGeog May 2014 Declaration I hereby declare that the work presented in this thesis is my own, except where otherwise stated, and that it has not been previously submitted in application for any other degree at any other educational institution in the United Kingdom or overseas. ii Abstract Sub-fossil pollen from Holocene tufa pool sediments is used to investigate middle – late Holocene environmental conditions in the White Peak region of the Derbyshire Peak District in northern England. The overall aim is to use pollen analysis to resolve the relative influence of climate and anthropogenic landscape disturbance on the cessation of tufa production at Lathkill Dale and Monsal Dale in the White Peak region of the Peak District using past vegetation cover as a proxy. Modern White Peak pollen – vegetation relationships are examined to aid semi- quantitative interpretation of sub-fossil pollen assemblages. Moss-polsters and vegetation surveys incorporating novel methodologies are used to produce new Relative Pollen Productivity Estimates (RPPE) for 6 tree taxa, and new association indices for 16 herb taxa. RPPE’s of Alnus, Fraxinus and Pinus were similar to those produced at other European sites; Betula values displaying similarity with other UK sites only. RPPE’s for Fagus and Corylus were significantly lower than at other European sites. Pollen taphonomy in woodland floor mosses in Derbyshire and East Yorkshire is investigated. -
Parish Council Guide for Residents
CHAPEL-EN-LE-FRITH PARISH WELCOME PACK TITLE www.chapel-en-le-frithparishcouncil.gov.uk PARISH COUNCILGUIDE FOR RESIDENTS Contents Introduction The Story of Chapel-en-le-Frith 1 - 2 Local MP, County & Villages & Hamlets in the Parish 3 Borough Councillors 14 Lots to Do and See 4-5 Parish Councillors 15 Annual Events 6-7 Town Hall 16 Eating Out 8 Thinking of Starting a Business 17 Town Facilities 9-11 Chapel-en-le-Frith Street Map 18 Community Groups 12 - 13 Village and Hamlet Street Maps 19 - 20 Public Transport 13 Notes CHAPEL-EN-LE-FRITH PARISH WELCOME PACK INTRODUCTION Dear Resident or Future Resident, welcome to the Parish of Chapel-en-le-Frith. In this pack you should find sufficient information to enable you to settle into the area, find out about the facilities on offer, and details of many of the clubs and societies. If specific information about your particular interest or need is not shown, then pop into the Town Hall Information Point and ask there. If they don't know the answer, they usually know someone who does! The Parish Council produces a quarterly Newsletter which is available from the Town Hall or the Post Office. Chapel is a small friendly town with a long history, in a beautiful location, almost surrounded by the Peak District National Park. It's about 800 feet above sea level, and its neighbour, Dove Holes, is about 1000 feet above, so while the weather can be sometimes wild, on good days its situation is magnificent. The Parish Council takes pride in maintaining the facilities it directly controls, and ensures that as far as possible, the other Councils who provide many of the local services - High Peak Borough Council (HPBC) and Derbyshire County Council (DCC) also serve the area well. -
The Ultimate Peak District & Derbyshire Bucket List
The Ultimate Peak District & Derbyshire Bucket List: 101 Great Things To Do 1. Embrace the great outdoors in the UK’s first National Park Established in 1951, the Peak District is the country’s oldest National Park. If you love the outdoors, this protected area of natural beauty - which covers 555 square miles in total - offers over 200 square miles of stunning open access land to explore. 2. Visit the ‘jewel in the Peak District’s crown’ at Chatsworth House Home to the Duke and Duchess of Devonshire, Chatsworth is one of the UK’s favourite stately homes. Discover over 30 magnificent rooms, a 105-acre garden, parkland, a farmyard and playground, and one of Britain’s best farm shops. 3. Conquer the tallest ‘Peak’ in the Peak District At 636 metres above sea level, you’ll feel like you’re standing on top of the world when you conquer the Kinder Scout plateau. It’s the highest point in the National Park and was also the site of the 1932 Mass Trespass, a landmark event which sparked a debate about the right to roam in the countryside, leading to the establishment of the Peak District as the first National Park two decades later. 4. Discover the UK’s oldest Ice Age cave art at Creswell Crags Walk in the footsteps of Ice Age hunters, uncover the secrets of early man, discover incredible Ice Age cave art and marvel at the UK’s largest discovery of ritual protection marks at this picturesque limestone gorge on the Derbyshire/Nottinghamshire border. 5. -
Land at Manchester Road Tunstead Milton High Peak Derbyshire
________________________________________________________ LAND AT MANCHESTER ROAD TUNSTEAD MILTON HIGH PEAK DERBYSHIRE ________________________________________________ Proof of Evidence A G Massie BSc (Hons) MRICS IRRV MCIArb Prepared on the instructions of High Peak Borough Council Market Place Buxton Derbyshire SK17 6EL Appeal Ref: APP/H1033/W/16/3147726 NOVEMBER | 2016 LIVERPOOL MANCHESTER GLASGOW LONDON Alabama House Hill Quays 272 Bath Street 26 York Street 6 Rumford Place 14 Commercial Street Glasgow London Liverpool L3 9BY Manchester M15 4PZ G2 4JR W1U 6PZ www.keppiemassie.com Table of Contents 1.0 INTRODUCTION ................................................................................................ 1 2.0 PURPOSE AND CONTENTS OF THE REPORT ........................................................... 2 3.0 THE NATIONAL PLANNING POLICY FRAMEWORK .................................................... 6 4.0 SITES WITH PLANNING PERMISSION AND UNDER CONSTRUCTION .......................... 9 5.0 OTHER SITES WITH PLANNING PERMISSION ...................................................... 19 6.0 LOCAL PLAN ALLOCATIONS AND OTHER IDENTIFIED SITES .................................. 45 7.0 SMALL SITES AND WINDFALL ALLOWANCE ......................................................... 59 8.0 CONCLUSIONS AND DELIVERABLE SUPPLY ......................................................... 62 9.0 DECLARATION ................................................................................................ 64 Appendices (Bound Separately) Appendix 1 North -
New Electoral Arrangements for Derbyshire Dales District Council Draft Recommendations February 2021
New electoral arrangements for Derbyshire Dales District Council Draft Recommendations February 2021 Translations and other formats: To get this report in another language or in a large-print or Braille version, please contact the Local Government Boundary Commission for England at: Tel: 0330 500 1525 Email: [email protected] Licensing: The mapping in this report is based upon Ordnance Survey material with the permission of Ordnance Survey on behalf of the Keeper of Public Records © Crown copyright and database right. Unauthorised reproduction infringes Crown copyright and database right. Licence Number: GD 100049926 2021 A note on our mapping: The maps shown in this report are for illustrative purposes only. Whilst best efforts have been made by our staff to ensure that the maps included in this report are representative of the boundaries described by the text, there may be slight variations between these maps and the large pdf map that accompanies this report, or the digital mapping supplied on our consultation portal. This is due to the way in which the final mapped products are produced. The reader should therefore refer to either the large pdf supplied with this report or the digital mapping for the true likeness of the boundaries intended. The boundaries as shown on either the large pdf map or the digital mapping should always appear identical. Contents Introduction 1 Who we are and what we do 1 What is an electoral review? 1 Why Derbyshire Dales? 2 Our proposals for Derbyshire Dales 2 How will the recommendations affect you? -
Proposed Residential Development, Land at Leek Road, Buxton
LANDSCAPE AND VISUAL IMPACT ASSESSMENT Proposed Residential Development, Land at Leek Road, Buxton. Client: Persimmon Homes (North West) Final Report Prepared by PGLA Landscape Architects September 2016 Quality Checked Document: LEE1511_LVIA01 Revision - Final Report Written by: PGG/KLJ 229 Ducie House Ducie Street Manchester Reviewed by: PGG M1 2JW Tel: 0161 238 9138 Date: September 2016 [email protected] www. pgla.co.uk Land at Leek Road, Buxton Landscape and Visual Impact Assessment TABLE OF CONTENTS Section 1.0 Introduction Page 1 Section 2.0 Methodology Page 3 Section 3.0 Landscape Related Planning Policy Review Page 11 Section 4.0 Baseline Conditions Page 16 Section 5.0 Mitigation Page 30 Section 6.0 Potential Landscape and Visual Effects Page 31 Section 7.0 Summary of Effects Page 38 Section 8.0 Conclusions Page 42 Appendix A – Figures Figure 1 – Access and Circulation Figures 2 to 6 – Landscape Character Areas Figures 7 & 8 – Landscape Designations Figure 9 - Topography Figures 10 & 11 – Zone of Theoretical Visibility Figure 12 – Opportunities and Constraints Figure 13 – Landscape Strategy Figure 14 – Masterplan (e*SCAPE Urbanists) Figure 15 – Viewpoint Locations Appendix B Methodology Tables Table A – Scale of Significance Table B – Likely Significance of Effects Table C - Duration of Overall Effects September 2016 Persimmon PGLA Ltd Page ii Land at Leek Road, Buxton Landscape and Visual Impact Assessment 1 INTRODUCTION This report has been prepared by PGLA Ltd and presents the findings of the Landscape and Visual Impact Assessment (LVIA) and the anticipated effects of the proposed residential development at Leek Road upon the local landscape character and the visual amenity. -
People and Definition of the Landscape Area
People People Residents Taking figures from the 2011 census and adjusting for proportion of residential part of parish/ward within the South West Peak LPS area we can give The South West Peak comprises all or part of a very close estimate of a resident population some 35 parishes or wards; 17 of those have of 12,814 people. Some 6,515 of those live in the more than 80% of their parish within the area. urban fringing wards of Buxton, Whaley Bridge, Despite the large number of parishes in the LPS Chapel-en-le-Frith and Macclesfield which area, the resident population is fairly low and together account for 6,673ha or 18.8% of the land highly dispersed. Whilst there are few centres of area. In the remaining rural 28,720ha, or 81.2% of population there is a strong sense of community, the land area, reside the remaining 6,299 people particularly in subdivisions of the area like the at a population density of 22 people per square Staffordshire Moorlands. kilometre. Figure Unit Total area of the SWP 35,393 ha Total population with adjustment for % or parish/ward in the SWP 12,814 no Total area of the above urban parts in the SWP 6,673 ha % urban parts 19 % People Urban population 6,515 no % urban population (urban parish/ward) 51 % Total area of rural parts in the SWP 28,720 ha % rural parts 81 % Total rural population (excluding Buxton, Whaley Bridge, 6,299 no Chapel-en-le-Frith, Macclesfield) % rural population (rural parish/ward) 49 % Population density urban 98 people/sqkm Population density rural 22 people/sqkm Looking at demographics, the most numerous Statistics, 2015). -
Review of Tufa Deposition and Palaeohydrological Conditions in the White Peak, Derbyshire, UK: Implications for Quaternary Landscape Evolution
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive Review of tufa deposition and palaeohydrological conditions in the White Peak, Derbyshire, UK: implications for Quaternary landscape evolution. Vanessa J. Banks1,2*, Peter F. Jones2, David J. Lowe1, Jonathan R. Lee1, Jeremy Rushton1, and Michael A. Ellis1. 1 British Geological Survey, Kingsley Dunham Centre, Nicker Hill, Keyworth, Nottingham NG12 5GG 2 University of Derby, Geographical, Earth and Environmental Sciences, Kedleston Road, Derby, DE22 1GB * Corresponding author. E‐mail address: [email protected] Abstract. This review considers the geological and geomorphological context of tufa barrages that occupy buried valley settings in the Wye catchment, Derbyshire. It describes the potential relationship of the tufa with locations of hypothesised river captures and inception horizon‐guided groundwater flow paths. Tufa barrage development is associated with steps in the bedrock, which may be related to knick‐point recession during river capture. Broad estimates of valley incision have been calculated from previously dated deposits. These support current interpretations of particularly significant effective base‐level lowering during the Anglian and Devensian stages of the Quaternary and have the potential to add to the knowledge of regional uplift histories. Key words: tufa, Quaternary hydrogeology, inception horizons, incision, landscape evolution. 1. Introduction. Tufa is a terrestrial freshwater accumulation of calcium carbonate (Viles, 2004) that is commonly found in limestone terrain. Also referred to as travertine by some authors (Pentecost, 1999), it is precipitated when water that is saturated with calcium carbonate becomes supersaturated due to degassing of carbon dioxide. This can be caused by: atmospheric absorption of carbon dioxide, increase in temperature, decrease in pressure, physical agitation, aquatic plant photosynthesis (Lorah and Herman, 1988), or microbial processes (Pedley and Rogerson, 2010). -
Part One: Landscape Character Descriptions 2
Part One: Landscape Character Descriptions 2. White Peak Landscape Character Types • Plateau Pastures ..................... 2.5 • Limestone Slopes ..................... 2.13 • Upland Limestone Pastures ... 2.10 • Limestone Dales ....................... 2.17 White Peak Character Area 52 Part 1 - 2.1 White Peak CHARACTER AREA 52 A gently rolling upland, limestone plateau punctuated by steep sided dales, scattered villages and isolated farmsteads within a pastoral setting. Landscape Character Types • Plateau Pastures • Limestone Slopes • Limestone Dales • Upland Limestone Pastures "... it was veined with a network of old stone walls, dividing the fields, and broken here and there with ruins of old lead-mines and works. A sparse stone farm bristled with six naked sharp trees. In the distance was a patch of smoky grey stone, a hamlet .... stone fences under the sky, looking for the curves downward that indicated a drop to one of the underneath, hidden dales.” DH Lawrence ‘The Virgin and the Gypsy’ Introduction neutral or acidic soils. These soils below ground with water finding its are well-drained, dark brown silt- way into faults and fissures, The White Peak character area is loams farmed as pasture and rough creating caves and caverns. Over located in the west of the county, grazing. The soils of the upper time these would collapse to form most is within the Peak District plateau tend to have deeper steep sided slopes of exposed National Park. It stretches from deposits. Here the drift has formed stone. Some dales still have rivers Castleton in the north, to a matrix with the course, resistant and streams meandering through Wirksworth in the south. -
Bakewell, Great Longstone, Baslow, Rowsley Rowsley Baslow, Longstone, Great Bakewell, Ncludes Cycle Hire, Cycle Ncludes I
Refreshments and Visitor Centres Visitor and Refreshments Shops: Bakewell, Great Longstone, Baslow, Rowsley Rowsley Baslow, Longstone, Great Bakewell, ncludes Cycle Hire, Cycle ncludes I Stanton in Peak, Youlgreave Peak, in Stanton Shops: Bakewell 1:50,000 Scale Map Scale 1:50,000 Pubs: Great Longstone, Hassop, Baslow, Beeley, Rowsley, Rowsley, Beeley, Baslow, Hassop, Longstone, Great 7 Pubs: Bakewell, Millers Dale (below trail, by the river) the by trail, (below Dale Millers Bakewell, 8 s: Cafe Hassop Station, Baslow, Edensor, Chatsworth, Beeley, Rowsley Rowsley Beeley, Chatsworth, Edensor, Baslow, Station, Hassop 6 (seasonal) (seasonal) Mill Blackwell and 97% road/3% trail road/3% 97% es: Caf Hassop Station (all year), Millers Dale, Dale, Millers year), (all Station Hassop Grade: Hard 100% trail 100% Ascent: 674m/2211ft Grade: Easy 5 Distance: 29km/18miles Ascent: 148m/487ft (on Monsal Trail) DE45 1NW DE45 Trail) Monsal (on Distance: 29km/18miles /End Point: Point: /End Start Hassop Station Café and Cycle Hire car park park car Hire Cycle and Café Station Hassop Monsal Trail) DE45 1NW DE45 Trail) Monsal (on park car return to the start. start. the to return /End Point: /End Start Hassop Station Café and Cycle Hire Hire Cycle and Café Station Hassop oss the River Wye SA. Take second L signposted Hassop to to Hassop signposted L second Take SA. Wye River the oss Cr 10. n around and follow the trail back the same way. same the back trail the follow and around n Tur 2. taking care through the town centre. town the through care taking 1 and continue on the trail to the end at Blackwell Mill. -
Groundwater in Carboniferous Carbonates
Groundwater in Carboniferous carbonates Field excursion to the Derbyshire "White Peak" District 26th June 2015 John Gunn with contributions from Andy Farrant, Paul Hardwick and Steve Worthington Contents PAGE 1. INTRODUCTION 2 2. THE "WHITE PEAK" DISTRICT 2 3. GEOLOGICAL BACKGROUND 2 4. SURFACE DRAINAGE AND GEOMORPHOLOGY 6 5. THE HYDROGEOLOGY OF THE PEAK DISTRICT LIMESTONES 7 6. CAVES 8 7. ITINERARY 9 STOP 1: THE BULL I'TH'THORN BOREHOLE, HURDLOW 9 STOP 2: THE RIVER WYE AND TUNSTEAD QUARRY 13 STOP 3: ELDON HILL QUARRY 19 STOP 4: ELDON HILL DOLINES 22 STOP 5: DIRTLOW RAKE AND DOLINES 23 STOP 6: CAVE DALE 25 STOP 7: CASTLETON SPRINGS AND PEAK CAVERN 25 STOP 8: WINNATS PASS 30 STOP 9: MAGPIE SOUGH TAIL 31 STOP 10: OLD BATH SPRING 32 8. REFERENCES 32 Acknowledgements The organisers are grateful to: The British Geological Survey for Figures 2 and 19, Maurice Gregory for permission to visit Eldon Hill Quarry, John Harrison for permission to visit Peak Cavern, and Peter Harrison for permission to visit Russet Well. Cover photographs A common perception of the Peak District karst hydrogeology is that it is dominated by sinking streams that feed caves which in turn discharge substantial flows of water from large springs such as Peak Cavern Rising (left). However, over much of the area where limestones crop out there is only dispersed autogenic recharge through a soil cover and surprisingly little evidence of karstic drainage, particularly at depth. During the excavation of stone from Ballidon Quarry in the southern White Peak no caves were encountered and the 100m of limestone exposure (right) shows only an epikarst below which there are no visible conduits and nothing to suggest concentrated drainage.