'Aview from the Hills' in Our Winter Issue, Alf Alderson Visited
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Durham Rare Plant Register 2011 Covering VC66 and the Teesdale Part of VC65
Durham Rare Plant Register 2011 Covering VC66 and the Teesdale part of VC65 JOHN L. DURKIN MSc. MIEEM BSBI Recorder for County Durham 25 May Avenue. Winlaton Mill, Blaydon, NE21 6SF [email protected] Contents Introduction to the rare plants register Notes on plant distribution and protection The individual species accounts in alphabetical order Site Index First published 2010. This is the 2011, second edition. Improvements in the 2011 edition include- An additional 10% records, most of these more recent and more precise. One kilometre resolution maps for upland and coastal species. My thanks to Bob Ellis for advice on mapping. The ―County Scarce‖ species are now incorporated into the main text. Hieracium is now included. This edition is ―regionally aligned‖, that is, several species which are county rare in Northumberland, but were narrowly rejected for the Durham first edition, are now included. There is now a site index. Cover picture—Dark Red Helleborine at Bishop Middleham Quarry, its premier British site. Introduction Many counties are in the process of compiling a County Rare Plant Register, to assist in the study and conservation of their rare species. The process is made easier if the county has a published Flora and a strong Biological Records Centre, and Durham is fortunate to have Gordon Graham's Flora and the Durham Wildlife Trust‘s ―Recorder" system. We also have a Biodiversity project, based at Rainton Meadows, to carry out conservation projects to protect the rare species. The purpose of this document is to introduce the Rare Plant Register and to give an account of the information that it holds, and the species to be included. -
Newsletter Appleby Archaeology
Winter 2011 Appleby Archaeology Heather Edwards, Spring Programme Newsletter AGM and Members’ Evening th 7.00pm Tuesday 10 January Volume 14 Issue 4 Winter 2011 Martin Railton : Altogether Archaeology on Brackenber Moor - Results of the 2011 Excavations at the “Roman Signal Station” Group News quired low level oblique aerial photographs, for example, Round the Museums appear to show an enclosure around the summit, with the cairns lying diagonally across it. Is this feature due to li- Richard Stevens : More on Abbeytown - an I hope you've noticed a subtle change in your Newsletter. I’m not normally much interested in museums but, curi- thology as some have claimed, or archaeology? We think outlying chapel at Holme St. Cuthbert Yes, your Committee has decided that the time has finally ously, I find that I’ve visited no fewer than four local ex- it is time to find out. come for us to switch to colour! I hope you'll agree that hibitions this summer. photographs, in particular, have benefited from the We therefore need to raise funds and support locally to The first was the Dock Museum at Barrow. I only went change. We've decided to try it for a year, at any rate. pay for archaeologists to conduct non-intrusive techniques because this was where Apparch’s annual summer day- Great Langdale Axe Factories Please let us know what you think. of investigation, and for laboratory analyses that we our- trip dropped us on our way to Furness Abbey. But I’m selves cannot provide. Our target is £6500 and have al- Tuesday 14th February Other changes in the pipeline included proposed amend- very glad I did because I thought it was quite wonderful. -
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. -
The North Pennines
LANDSCAPE CHARACTER THE NORTH PENNINES The North Pennines The North Pennines The North Pennines Countryside Character Area County Boundary Key characteristics • An upland landscape of high moorland ridges and plateaux divided by broad pastoral dales. • Alternating strata of Carboniferous limestones, sandstones and shales give the topography a stepped, horizontal grain. • Millstone Grits cap the higher fells and form distinctive flat-topped summits. Hard igneous dolerites of the Great Whin Sill form dramatic outcrops and waterfalls. • Broad ridges of heather moorland and acidic grassland and higher summits and plateaux of blanket bog are grazed by hardy upland sheep. • Pastures and hay meadows in the dales are bounded by dry stone walls, which give way to hedgerows in the lower dale. • Tree cover is sparse in the upper and middle dale. Hedgerow and field trees and tree-lined watercourses are common in the lower dale. • Woodland cover is low. Upland ash and oak-birch woods are found in river gorges and dale side gills, and larger conifer plantations in the moorland fringes. • The settled dales contain small villages and scattered farms. Buildings have a strong vernacular character and are built of local stone with roofs of stone flag or slate. • The landscape is scarred in places by mineral workings with many active and abandoned limestone and whinstone quarries and the relics of widespread lead workings. • An open landscape, broad in scale, with panoramic views from higher ground to distant ridges and summits. • The landscape of the moors is remote, natural and elemental with few man made features and a near wilderness quality in places. -
Discover Mid Teesdale
n o s l i W n o m i S / P A P N © Discover Allendale mid Teesdale Including routes to walk, cycle and ride Area covered by detailed route map © Charlie Hedley/Natural England The Teesdale Railway Path and Public Rights of Way are managed by North Pennines Area of Durham County Council Countryside Group, tel: 0191 383 4144. Outstanding Natural Beauty This leaflet has been produced by the North Pennines AONB Partnership and Mid Teesdale Project Partnership. Funded by: The North Pennines Area of Outstanding Natural Beauty (AONB) is one of the finest landscapes in the country. It was designated in 1988 and at almost 2,000 sq. kilometres is the second largest of the 40 AONBs and is one of the most peaceful Through: and unspoilt places in England. It is nationally and internationally important for its upland habitats, geology and wildlife, with much of the area being internationally designated. The North Pennines AONB became Britain’s first European Geopark in 2003 in recognition of its internationally important geology and local efforts to use North Pennines AONB Partnership, Weardale Business Centre, The Old Co-op Building, 1 Martin Street, it to support sustainable development. A year later it became a founding member Stanhope, Co. Durham DL13 2UY tel: +44 (0)1388 528801 www.northpennines.org.uk email: [email protected] of the UNESCO Global Geoparks Network. For more information about the AONB, call 01388 528801 or visit This publication is printed on Greencoat Plus Velvet paper: 80% recycled post consumer, FSC The North Pennines AONB Partnership certification; NAPM recycled certification; 10%TCF virgin fibre; 10% ECF fibre. -
Mountain Accidents 2015
ISSN 2046-6277 LAKE DISTRICT SEARCH & MOUNTAIN RESCUE ASSOCIATION MOUNTAIN ACCIDENTS 2015 Cambridge Crag and Bowfell from ‘Wainwright’s Southern Fells’ and reproduced by courtesy of the Westmorland Gazette The Lake District Search and Mountain Rescue Association would like to acknowledge the contributions given to this association by all members of the public, public bodies and trusts. In particular, this association gratefully acknowledges the assistance given by Cumbria Constabulary. Contents Introduction ................................................................... 2 Chairman’s Report ........................................................ 3 Incident Details 2015 January ................................................................. 5 February ................................................................ 7 March .................................................................... 12 April ....................................................................... 16 May ....................................................................... 21 June ...................................................................... 26 July ........................................................................ 31 August ................................................................... 35 September ............................................................. 43 October ................................................................. 48 November .............................................................. 54 December ............................................................. -
Waterfalls: Forms, Distribution, Processes and Rates of Recession
QUAESTIONES GEOGRAPHICAE 39(1) • 2020 WATERFALLS: FORMS, DISTRIBUTION, PROCESSES AND RATES OF RECESSION ANDREW S. GOUDIE School of Geography, Centre for the Environment, University of Oxford, Oxford, United Kingdom Manuscript received: December 15, 2019 Revised version: February 2, 2020 GOUDIE A. S., 2020. Waterfalls: forms, distribution, processes and rates of recession. Quaestiones Geographicae 39(1), Bo- gucki Wydawnictwo Naukowe, Poznań, pp. 59–77. 8 figs, 3 tables. ABSTRACT: A waterfall is a very steep (commonly nearly vertical) fall of some magnitude in a river course. Waterfalls are widespread fluvial landforms that have been described from many parts of the world. Thirty-eight World Heritage Properties include waterfalls in their designation. In addition, some waterfalls are actual or potential geomorphosites. Waterfalls occur in almost all climatic environments, though they are particularly common in formerly glaciated areas. They occur on a huge diversity of rock types, although in general, they do not form persistent or large falls on soft or unconsolidated rocks. Waterfalls also occur in a wide range of geomorphological settings: glaciated areas, areas of ac- tive tectonism, areas of sea-cliff retreat and sea-level change, great escarpments on passive margins, basins with river capture, rifted and faulted areas and areas that have been subjected to megaflooding. Multiple processes account for waterfall retreat and varying rates of recession. Although the greatest interest has been in rates of waterfall recession, there are examples of waterfalls that prograde as a result of tufa deposition. KEY WORDS: waterfalls, caprock, knickpoints, plunge pools, tufa Corresponding author: Andrew Goudie, [email protected] Introduction distribution and rates of retreat. -
Landscape Conservation Action Plan Part 1
Fellfoot Forward Landscape Conservation Action Plan Part 1 Fellfoot Forward Landscape Partnership Scheme Landscape Conservation Action Plan 1 Fellfoot Forward is led by the North Pennines AONB Partnership and supported by the National Lottery Heritage Fund. Our Fellfoot Forward Landscape Partnership includes these partners Contents Landscape Conservation Action Plan Part 1 1. Acknowledgements 3 8 Fellfoot Forward LPS: making it happen 88 2. Foreword 4 8.1 Fellfoot Forward: the first steps 89 3. Executive Summary: A Manifesto for Our Landscape 5 8.2 Community consultation 90 4 Using the LCAP 6 8.3 Fellfoot Forward LPS Advisory Board 93 5 Understanding the Fellfoot Forward Landscape 7 8.4 Fellfoot Forward: 2020 – 2024 94 5.1 Location 8 8.5 Key milestones and events 94 5.2 What do we mean by landscape? 9 8.6 Delivery partners 96 5.3 Statement of Significance: 8.7 Staff team 96 what makes our Fellfoot landscape special? 10 8.8 Fellfoot Forward LPS: Risk register 98 5.4 Landscape Character Assessment 12 8.9 Financial arrangements 105 5.5 Beneath it all: Geology 32 8.10 Scheme office 106 5.6 Our past: pre-history to present day 38 8.11 Future Fair 106 5.7 Communities 41 8.12 Communications framework 107 5.8 The visitor experience 45 8.13 Evaluation and monitoring 113 5.9 Wildlife and habitats of the Fellfoot landscape 50 8.14 Changes to Scheme programme and budget since first stage submission 114 5.10 Moorlands 51 9 Key strategy documents 118 5.11 Grassland 52 5.12 Rivers and Streams 53 APPENDICES 5.13 Trees, woodlands and hedgerows 54 1 Glossary -
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Freshwater life Martyn G Kelly, Trevor D Cris, Ben Lamb and Brian Whitton Introduction Without the River Tees there would be no Teesdale and so, whilst much of the attention in this book is focussed on the plant and animal life in the fields and fells, we should not ignore either the river or the numerous tributary streams that feed it. Cow Green Reservoir, too, plays an important part in the story of Upper Teesdale, not just because of the ways in which it has altered the landscape and habitats in the upper valley, but also because the decision to impound the river precipitated many significant ecological studies and, ironically, raised the profile of the Teesdale rarities beyond a small band of botanical cognoscenti. The River Tees was the first British River to receive a detailed biological survey (by Butcher and colleagues in the mid-1930s). This was followed in the 1970s and 1980s by studies of the upper reaches of the main river and its tributaries by Durham University and the Freshwater Biological Association (later Institute of Freshwater Ecology and now Centre for Ecology and Hydrology). Since the previous edition of this book, further studies have investigated a wide range of factors including gravel, heavy metals, availability of salmonid spawning habitat and water colour. The upper tributaries of the Tees range from torrential streams, fed at times of peak flow mainly by surface run-off, to calcareous streams with some or much of their water from limestone springs. Those with the most water from springs are the ones which vary least in flow and have the highest calcium concentrations. -
Magazine Spring 2011 Plan Your Walk
magazine spring 2011 magazine spring 2011 Northern England Northern England 11/02/2011 12:43 03 Hebden Bridge, West Yorkshire 04 Teesdale, County Durham l Distance 11km/7 miles l Time 4hrs l Type Hill, woodland valley, open farmland l Distance 18km/11¼ miles l Time 6hrs l Type Valley and moorland NAVIGATION FITNESS NAVIGATION FITNESS 2 LEVEL 2 3 LEVEL 3 2 LEVEL 2 2/3 LEVEL 2/3 plan your walk plan your walk Forest and l WEST l Firth l Ettersgill YORKSHIRE Denholme Clough l HEBDEN Holwick BRIDGE CO.DURHAM TEESDALE Luddenden P Foot l N l Halifax l Kirkby Stephen TRO L l Cragg Vale l ORGA Sowerby AR B Bridge A Birkdale N l Melbecks EVE M l O T Ripponden l HY: FI HY: HY: S HY: P P Where: Circular walk Where: Circular walk from from Hebden Bridge via Bowlees via Cronkley Fell Heptonstall and Hardcastle and High and Low Force PHOTOGRA Crags. PHOTOGRA waterfalls. Start/end: St George’s The rugged moorland and deep, taking the L-hand track, marked Start/end: Bowlees Visitor The North Pennines, Britain’s 1. START The Bowlees Visitor Square, Hebden Bridge wooded valleys of the South ‘Private road‘. Pass a house on Centre car park (NY907283). second largest AONB, is one of Centre, housed in an old (SD992272). Pennines have long inspired your R and, just before a grassy terrain: Moorland and the most remote and unspoilt Methodist chapel, is worth a visit terrain: Mainly footpaths writers and poets, including the parking area, turn R on to a riverside path. -
Low Force and Holwick Are in the North Pennines Area of Outstanding Natural Beauty (AONB) and Geology and Landscape Around European Geopark
Low Force and Holwick are in the North Pennines Area of Outstanding Natural Beauty (AONB) and Geology and landscape around European Geopark European Geoparks The North Pennines AONB is Britain’s first European Low Force Geopark, a status supported by UNESCO, and a founding member of the Global Geoparks Network. Geoparks are special places with outstanding geology and landscape, and Holwick and where there are strong local efforts to make the most of geological heritage through interpretation, education, conservation and nature tourism. To find out more visit www.europeangeoparks.org A 2½-mile walk exploring landscape, Walk starts from here rocks, fossils and mines North Pennines Moor House – Upper Teesdale National Nature AONB & European Reserve (NNR) Geopark © Crown Copyright. All rights reserved. Part of this walk (south of the River Tees near Low Force) is Durham County Council. LA100049055. 2011. within the Moor House – Upper Teesdale NNR. This large reserve contains an almost complete range of upland For more information please contact: habitats typical of the North Pennines, from hay meadows North Pennines AONB Partnership, +44 (0)1388 528801 and juniper woods to limestone grassland and blanket bog. Weardale Business Centre, [email protected] It also includes the waterfalls of Cauldron Snout and High The Old Co-op Building, www.northpennines.org.uk 1 Martin Street, Stanhope, twitter.com/NorthPennAONB Force. For more information contact the Reserve Base on Bishop Auckland, County Durham facebook.com/NorthPenninesAONB 01833 622374. DL13 2UY Find out more about North Pennine geology This leaflet is one of a series of geological publications about the North Pennines.