Download Our Weardale Visitors Network Browser Here
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Wearhead Weardale Way Stanhope A689
. s n g i s k l a W e s o r m i r p s d y 0 5 1 s d y 0 0 1 s d y 0 5 s y e l l a V l a r e n i M e h t w o l l o F 0 m 0 5 1 m 0 0 1 m 0 5 : E L A C S . l e v e l a e s e v o b a t e e f e n o h p e l e T s t e l i o T y a W e l a d r a e W k l a w e g a l l i v 2 5 4 2 s i h c i h w T A E S E P O H N R U B f o t s e w h t u o s : Y E K e h t o t s e i . r l e t n d i w n r a e v l o e o t v e l - a e s e . n o i t c e r i d y l r e t s e w a n i n r u B v d n o u o b r a g r e t w e o l e o f t n 4 e 0 k 1 a 1 t e s b i n e h e t g a l l i v e h d l T e p o h n r u B w o l l o f d n a e g d i r b e h t f o u . -
Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from Gravity Survey and Structural Inversion
ESSOAr | https:/doi.org/10.1002/essoar.10501104.1 | CC_BY_NC_ND_4.0 | First posted online: Mon, 11 Nov 2019 01:27:37 | This content has not been peer reviewed. Geometry of the Butterknowle Fault at Bishop Auckland (County Durham, UK), from gravity survey and structural inversion Rob Westaway 1,*, Sean M. Watson 1, Aaron Williams 1, Tom L. Harley 2, and Richard Middlemiss 3 1 James Watt School of Engineering, University of Glasgow, James Watt (South) Building, Glasgow G12 8QQ, UK. 2 WSP, 70 Chancery Lane, London WC2A 1AF, UK. 3 School of Physics, University of Glasgow, Kelvin Building, Glasgow G12 8QQ, UK. * Correspondence: [email protected]; Abstract: The Butterknowle Fault is a major normal fault of Dinantian age in northern England, bounding the Stainmore Basin and the Alston Block. This fault zone has been proposed as a source of deep geothermal energy; to facilitate the design of a geothermal project in the town of Bishop Auckland further investigation of its geometry was necessary and led to the present study. We show using three-dimensional modelling of a dense local gravity survey, combined with structural inversion, that this fault has a ramp-flat-ramp geometry, ~250 m of latest Carboniferous / Early Permian downthrow having occurred on a fault surface that is not a planar updip continuation of that which had accommodated the many kilometres of Dinantian extension. The gravity survey also reveals relatively low-density sediments in the hanging-wall of the Dinantian fault, interpreted as porous alluvial fan deposits, indicating that a favourable geothermal target indeed exists in the area. -
Durham Dales Map
Durham Dales Map Boundary of North Pennines A68 Area of Outstanding Natural Barleyhill Derwent Reservoir Newcastle Airport Beauty Shotley northumberland To Hexham Pennine Way Pow Hill BridgeConsett Country Park Weardale Way Blanchland Edmundbyers A692 Teesdale Way Castleside A691 Templetown C2C (Sea to Sea) Cycle Route Lanchester Muggleswick W2W (Walney to Wear) Cycle Killhope, C2C Cycle Route B6278 Route The North of Vale of Weardale Railway England Lead Allenheads Rookhope Waskerley Reservoir A68 Mining Museum Roads A689 HedleyhopeDurham Fell weardale Rivers To M6 Penrith The Durham North Nature Reserve Dales Centre Pennines Durham City Places of Interest Cowshill Weardale Way Tunstall AONB To A690 Durham City Place Names Wearhead Ireshopeburn Stanhope Reservoir Burnhope Reservoir Tow Law A690 Visitor Information Points Westgate Wolsingham Durham Weardale Museum Eastgate A689 Train S St. John’s Frosterley & High House Chapel Chapel Crook B6277 north pennines area of outstanding natural beauty Durham Dales Willington Fir Tree Langdon Beck Ettersgill Redford Cow Green Reservoir teesdale Hamsterley Forest in Teesdale Forest High Force A68 B6278 Hamsterley Cauldron Snout Gibson’s Cave BishopAuckland Teesdale Way NewbigginBowlees Visitor Centre Witton-le-Wear AucklandCastle Low Force Pennine Moor House Woodland ButterknowleWest Auckland Way National Nature Lynesack B6282 Reserve Eggleston Hall Evenwood Middleton-in-Teesdale Gardens Cockfield Fell Mickleton A688 W2W Cycle Route Grassholme Reservoir Raby Castle A68 Romaldkirk B6279 Grassholme Selset Reservoir Staindrop Ingleton tees Hannah’s The B6276 Hury Hury Reservoir Bowes Meadow Streatlam Headlam valley Cotherstone Museum cumbria North Balderhead Stainton RiverGainford Tees Lartington Stainmore Reservoir Blackton A67 Reservoir Barnard Castle Darlington A67 Egglestone Abbey Thorpe Farm Centre Bowes Castle A66 Greta Bridge To A1 Scotch Corner A688 Rokeby To Brough Contains Ordnance Survey Data © Crown copyright and database right 2015. -
Larias Games: Weardale and Teesdale Scenario Pack
LARIAS GAMES: WEARDALE AND TEESDALE SCENARIO PACK Table of Contents Pg3: WVR 1.01: 1058 Wearhead to Durham Pg4: WVR 1.02: Coal from Brandon Pg5: WVR 1.03: Cattle for Heighington Pg6: WVR 1.04: 1820 Bishop Auckland to Middleton in Teesdale Pg7: WVR 1.05: Stormin' Northbound Pg8: WVR 1.06: Maintaining Lands Viaduct Pg9: WVR 1.07: Middleton Shuttle Pg10: WVR 1.08: Railtour Detour Pg11: WVR 1.09: Spenny Transfer Pg12: WVR 1.10: Helping Out Pg13: Credits WVR 1.01: 1058 Wearhead to Durham Duration: 70 Minutes Traction: Class 101 Requirements: Weardale and Teesdale Route Description: You have been tasked with taking the 1058 Wearhead to Durham all the way to Durham. Your timetable calls for stops at St John’s Chapel, Westgate, Eastgate, Stanhope, Frosterley, Wolsingham, Harperley, Witton Le Wear, Bishop Auckland, Hunwick, Willington, Brancepeth, Brandon Colliery, and Durham. Make sure to stick to the tight timetable. WVR 1.02: Coal from Brandon Duration: 35 Minutes Traction: Class 08 Requirements: Weardale and Teesdale Route Description: Two rakes of loaded coal hoppers have been loaded at the Brandon Coillery and now need to be taken to the Brandon sidings so they can be picked up. Along with the loaded hoppers, several empties have been prepared and need to be taken into the Coillery. Your job is to shunt the loaded wagons into the sidings and move the several rakes of empties to the coal loading area. WVR 1.03: Cattle for Heighington Duration: 40 Minutes Traction: Class 25 Requirements: Weardale and Teesdale Route Descripton: A rake of empty cattle vans have been stored in the Barnard Castle goods siding, located just south of the main station. -
St John's Chapel Closed but the Facades Are Still Visible Along Hood Street Giving the Impression of a Once Busy Village
W A NETWORK OF WALKS OFF THE WEARDALE WAY Outer route: 7 miles/11km Starting from Each village loop approximately St John’s Chapel 3 miles/5km or Ireshopeburn The Forest of Weardale Our walks take us through the ‘forest’ of Weardale, an area set aside by the Prince Bishops of Durham in the early Norman period for the hunting of roe and red deer and boar. It was an uncultivated wilderness of open fell on the uplands with wooded valley sides and floor and very little, if any, settlement. red deer Apart from the steep sided tributary denes there is little sign today of the medieval woodland. Deforestation began from mid 13th century when the Bishop created a walled deer park further down the valley, allowing land in upper Weardale to be leased out for cattle farming and mining. Initially the valley floor land was The F leased out to stockmen who cleared irst Farms the woodland to create meadow and pasture for cattle, deer and sheep. Place names such as Daddry Shield, Hunshieldford and Saugh Shield remind us that these were summer only farms or ‘shielings’. From time to time attempts have been made to grow root crops and grain in upper Weardale but the cool wet upland climate severely limits the growing season and today’s farming activities are still dominated by the rearing of beef cattle and sheep together with the growing of hay as winter feed. Hay Meadows Traditional farming methods, including the late cutting of hay and use of manure helped to preserve Upper Weardale hay meadows, which are now regarded as an important landscape feature supporting many species of wild flowers and upland breeding birds. -
County Durham Plan (Adopted 2020)
County Durham Plan ADOPTED 2020 Contents Foreword 5 1 Introduction 7 Neighbourhood Plans 7 Assessing Impacts 8 Duty to Cooperate: Cross-Boundary Issues 9 County Durham Plan Key Diagram and Monitoring 10 2 What the County Durham Plan is Seeking to Achieve 11 3 Vision and Objectives 14 Delivering Sustainable Development 18 4 How Much Development and Where 20 Quantity of Development (How Much) 20 Spatial Distribution of Development (Where) 29 5 Core Principles 71 Building a Strong Competitive Economy 71 Ensuring the Vitality of Town Centres 78 Supporting a Prosperous Rural Economy 85 Delivering a Wide Choice of High Quality Homes 98 Protecting Green Belt Land 124 Sustainable Transport 127 Supporting High Quality Infrastructure 138 Requiring Good Design 150 Promoting Healthy Communities 158 Meeting the Challenge of Climate Change, Flooding and Coastal Change 167 Conserving and Enhancing the Natural and Historic Environment 185 Minerals and Waste 212 Appendices A Strategic Policies 259 B Table of Superseded Policies 261 C Coal Mining Risk Assessments, Minerals Assessments and Minerals and/or Waste 262 Infrastructure Assessment D Safeguarding Mineral Resources and Safeguarded Minerals and Waste Sites 270 E Glossary of Terms 279 CDP Adopted Version 2020 Contents List of County Durham Plan Policies Policy 1 Quantity of New Development 20 Policy 2 Employment Land 30 Policy 3 Aykley Heads 38 Policy 4 Housing Allocations 47 Policy 5 Durham City's Sustainable Urban Extensions 61 Policy 6 Development on Unallocated Sites 68 Policy 7 Visitor Attractions -
Northeast England – a History of Flash Flooding
Northeast England – A history of flash flooding Introduction The main outcome of this review is a description of the extent of flooding during the major flash floods that have occurred over the period from the mid seventeenth century mainly from intense rainfall (many major storms with high totals but prolonged rainfall or thaw of melting snow have been omitted). This is presented as a flood chronicle with a summary description of each event. Sources of Information Descriptive information is contained in newspaper reports, diaries and further back in time, from Quarter Sessions bridge accounts and ecclesiastical records. The initial source for this study has been from Land of Singing Waters –Rivers and Great floods of Northumbria by the author of this chronology. This is supplemented by material from a card index set up during the research for Land of Singing Waters but which was not used in the book. The information in this book has in turn been taken from a variety of sources including newspaper accounts. A further search through newspaper records has been carried out using the British Newspaper Archive. This is a searchable archive with respect to key words where all occurrences of these words can be viewed. The search can be restricted by newspaper, by county, by region or for the whole of the UK. The search can also be restricted by decade, year and month. The full newspaper archive for northeast England has been searched year by year for occurrences of the words ‘flood’ and ‘thunder’. It was considered that occurrences of these words would identify any floods which might result from heavy rainfall. -
Hamsterley Forest 1 Weardalefc Picture Visitor Library Network / John Mcfarlane Welcome to Weardale
Welcome to Weardale Things to do and places to go in Weardale and the surrounding area. Please leave this browser complete for other visitors. Image : Hamsterley Forest www.discoverweardale.com 1 WeardaleFC Picture Visitor Library Network / John McFarlane Welcome to Weardale This bedroom browser has been compiled by the Weardale Visitor Network. We hope that you will enjoy your stay in Weardale and return very soon. The information contained within this browser is intended as a guide only and while every care has been taken to ensure its accuracy readers will understand that details are subject to change. Telephone numbers, for checking details, are provided where appropriate. Acknowledgements: Design: David Heatherington Image: Stanhope Common courtesy of Visit England/Visit County Durham www.discoverweardale.com 2 Weardale Visitor Network To Hexham Derwent Reservoir To Newcastle and Allendale Carlisle A69 B6295 Abbey Consett River Blanchland West Muggleswick A 692 Allen Edmundbyers Hunstanworth A 691 River Castleside East Allen North Pennines Area of Outstanding Natural Beauty Lanchester A 68 B6278 C2C C2C Allenheads B6296 Heritage C2C Centre Hall Hill B6301 Nenthead Farm C2C Rookhope A 689 Lanehead To Alston Tunstall Penrith Cowshill Reservoir M6 Killhope Lead Mining The Durham Dales Centre Museum Wearhead Stanhope Eastgate 3 Ireshopeburn Westgate Tow Law Burnhope B6297 Reservoir Wolsingham B6299 Weardale C2C Frosterley N Museum & St John’s Chapel Farm High House Trail Chapel Weardale Railway Crook A 689 Weardale A 690 Ski Club Weardale -
Exploring the River Wear-Part 1
Armchair Adventurers Explore The River Wear G eog rap Part 1 from the Pennines to the outskirts of Durham hy A period. On the sea bed a limy ooze full of the rch y aeo eolog log G decaying skeletons of sea creatures built up. y Rivers washed down sand and gravel building His up deltas, and forests flourished on the deltas tory and swampy margins. Periodically the seas rose, drowned the deltas and forests and more Geology ooze was deposited; then sea levels dropped The River Wear rises in the North Pennines and and the deltas and forests returned. This cycle flows in an easterly direction to empty in the with compression gave rise to sedimentary North Sea at Sunderland. Weardale is in an rocks. The oozes became limestone, the sands, gravels and muds became shale and sandstone, and the forests became coal. Limestone and sandstone are resistant to erosion, whereas the softer shales wear away more easily. This contrast has produced the terraced hillsides which are characteristic of the whole area and the hard limestone outcrops form waterfalls created by the erosion. area designated for it’s Outstanding Natural Beauty. It is also a UNESCO Global Geopark. A Geopark is a place of outstanding geological heritage which is used to support sustainable development through conservation, education, interpretation and nature tourism. High Force Waterfall Limestone is the dominant rock in Upper The landscape has evolved over 500 million Weardale. Its main constituent, calcium years. During that time the valley has been carbonate, is soluble in rainwater which is liquid molten rock, desert,tropical sea,swamps, acidic and has eroded it to form sink holes, and an ice sheet. -
Barn for Conversion to the East of Laneside Farm
BARN FOR CONVERSION TO THE EAST OF LANESIDE FARM WEARHEAD ▪ BISHOP AUCKLAND ▪ COUNTY DURHAM ▪ DL13 1EB BARN FOR CONVERSION TO THE EAST OF LANESIDE FARM WEARHEAD ▪ BISHOP AUCKLAND ▪ COUNTY DURHAM ▪ DL13 1EB Stanhope 9 Miles ▪ Alston 11 Miles ▪ Hexham 22 Miles Exciting development opportunity • Planning permission approved for a two bedroom detached property • Off road parking • Enclosed lawned garden • Picturesque Dales location Guide Price £65,000 Wolsingham 01388 529579 [email protected] The Area Notes The picturesque village of Wearhead is situated in the heart of 1. The purchaser will be responsible for the maintenance upper Weardale, which is an area of Outstanding Natural and installation of the access track from the public Beauty. It is home to a primary school with a regular bus highway. service linking the village with the rest of the dale. Hexham is 2. The access track will be situated over land belonging to one of the nearest towns which also benefits from a railway a third party, however a right of access will be granted. station and a good range of local amenities, Penrith is also an hours drive from Wearhead and is ideal for a perfect retreat to Planning The Lake District. Full details for the planning permission for this development can be accessed through the Durham County Council A little further down the dale, the village of St John’s Chapel planning portal using reference number DM/17/03385/FPA. offers a basic range of amenities including a Doctor’s Surgery, The permission is due for expiry on 7th December 2020. -
Regional Lead Isotope Study of a Polluted River Catchment
1 Regional lead isotope study of a polluted river 2 catchment: River Wear, Northern England, UK 3 4 Thomas J. Shepherd a*, Simon R.N.Chenery b, Vanessa Pashley c, Richard 5 A. Lord d, Louise E. Ander b, Neil Breward b, Susan F. Hobbs b, Matthew 6 Horstwood c, Benjamin A. Klinck b, Fred Worralla 7 8 a Department of Earth Sciences, University of Durham, Science Laboratories, Durham DH1 3LE, UK 9 b British Geological Survey, Nicker Hill, Keyworth, Nottingham NG12 5GG, UK 10 c NERC Isotope Geosciences Laboratory, Kingsley Dunham Centre, Keyworth, Nottingham NG12 11 5GG, UK 12 d School of Science and Technology, University of Teesside, Middlesbrough, Tees Valley TS1 3BA, UK 13 _________________________________________________________ 14 Abstract 15 16 High precision, lead isotope analyses of archived stream sediments from the River Wear catchment, 17 northeast England (1986-88), provide evidence for three main sources of anthropogenic lead pollution; 18 lead mining, industrial lead emissions and leaded petrol. In the upper catchment, pollution is totally 19 controlled and dominated by large lead discharges from historic mining centres in the North Pennine 20 Orefield (208Pb/206Pb, 207Pb/206Pb ratios range from 2.0744 - 2.0954 and 0.8413 - 0.8554 respectively). 21 In the lower catchment, co-extensive with the Durham Coalfield and areas of high population density, 22 pollution levels are lower and regionally more uniform. Isotope ratios are systematically higher than in 23 the upper catchment (208Pb/206Pb, 207Pb/206Pb ratios range from 2.0856 -2.1397 and 0.8554 - 0.8896 24 respectively) and far exceed values determined for the geogenic regional background. -
Cllr Mrs a Humble Chairman
STANHOPE PARISH COUNCIL At a meeting of the Council held in the Dales Centre, Stanhope on 7th March 2018 PRESENT: Cllr Mrs A Humble Chairman Cllr M Brewin, Cllr Miss J Carrick, Cllr D Craig, Cllr D Ellwood, Cllr Miss F Graham, Cllr Mrs H Maddison, Cllr Mrs D Sutcliff, Cllr B Thompson Also Present: PC G Moore Andrea Wakefield and Charlene Burdis – Wolsingham School Parents 9864 Apologies for Absence Cllr L Blackett, Cllr A Fishburn, Cllr Mrs S Thompson, Cllr Mrs K Hutchinson 9865 To Receive any Declarations of Interest from Members None received 9866 Minute of the meeting held on 7th February 2018 Page 3 should read Weardale Motor Service not Arriva Page 3 should read stay in Education and not stay at school Minutes were moved as a true and correct record and were signed by the Chairman 9867 Police and the Community PC G Moore attended the meeting as PC B Crampsie is on leave and sends his apologies. Since January there have been 45 incidents reported. Vans have been targeted with tools in and scrap metal vehicles have been stopped. A van was stopped with a trailer of wood and building materials on it which turned out to be stolen. Large denomination counterfeit currency has been passed in the shops. Cllr Craig mentioned that two empty tool boxes were reported which could have been from the thefts, PC Moore would investigate this. Cllr Mrs Humble mentioned that the traffic lights were still off at Ireshopeburn and she asked if the cameras were benefiting the Police.