10. North Pennines Area Profile: Supporting Documents
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The North Pennines Area of Outstanding Natural Beauty Management Plan 2009 – 2014 NORTHUMBERLAND NATIONAL PARK
Part B – Strategy The North Pennines Area of Outstanding Natural Beauty Management Plan 2009 – 2014 NORTHUMBERLAND NATIONAL PARK Haydon Corbridge Haltwhistle A69 Bridge Bardon MIll 9 9 A6 A6 HEXHAM e P yn BRAMPTON W Allen R. T Banks Hallbankgate The Garden Lambley Station Talkin Tarn Viaduct B Highland Country Park 6 Slaley 3 Halton-lea-Gate Whiteld 0 Cattle Centre 6 A Talkin 6 8 t en Cold Fell w Castle Carrock South Whiteld Allendale er . D Tyne Moor R Valley Derwent Geltsdale RSPB East Allen Resr Shotley Beamish Museum Reserve R Valley . A686 Hexhamshire (12 miles) S Bridge R o Ninebanks R . Slaggyford . Common E u R E d t . h W a A CONSETT e s Cumrew B Pow n 6 T e t 8 y s 6 Blanchland 9 n t 2 Hill 9 Edmundbyers e West Allen A B 5 A l Country 6 Valley l Derwent e 4 l 1 l n Park 3 e Valley n Castleside Lanchester Alston 2C Armathwaite Croglin South C Tynedale Allenheads C Railway 2 C & The Hub Killhope A 6 8 6 A689 Museum Rookhope Stanhope 2C 68 C A Nenthead Common Waskerley Resr. Garrigill Nenthead Durham Thortergill Mines Dales Tunstall M Forge Cowshill Resr. 6 Kirkoswald Hartside Centre Lazonby W St John’s Stanhope P Chapel Eastgate Melmerby Fell Tow law Ireshopeburn Frosterley Wolsingham B Melmerby Weardale Westgate 6 4 Museum 1 2 W e a r d a l e Harehope Crook R Quarry Weardale R . T . ees Railway W Sea to Sea Cycle Route (C2C) Cross Fell B e 6 2 a Langwathby 7 r Great Dun Fell 7 Bollihope Common Cow Green B PENRITH 6 Reservoir 2 7 Blencarn 8 Langdon Beck Moor House - A66 Upper Teesdale Bowlees Visitor Centre Hamsterley Forest NNR Newbiggin PW High Force Chapel Rheged Cauldron Low Force Snout Te Middleton-in-Teesdale Woodland BISHOP Dufton e West s d a Auckland AUCKLAND High Cup Nick l e Ark on the Edge A 68 276 Romaldkirk Hilton B6 Grassholme Raby Castle Appleby-in- Resr. -
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. -
Oresome North Pennines: Site Overview
OREsome North Pennines: Site Overview Whitesike and Bentyfield lead mines and ore works Fig. 1: Whitesike and Bentyfield Mines viewed from the B6277 road, looking east SAM list entry number: 1015832 Other designations: Whitesike Mine and Flinty Fell SSSI Grid ref.: NY751425 County: Cumbria District/Parish: Eden, Alston Moor Altitude: 430-460m SAM area: 3.32 hectares Habitats: Narrow valley with sheep pasture, scrub and mine workings Highlights Archaeology: The dressing floors of Whitesike and Bentyfield ore works retain especially deep stratified deposits including areas that are waterlogged, which is ideal for the preservation of organic materials, such as wood and leather. Nationally important remains of 19th century ore processing equipment is considered to survive within these deposits, which will provide very valuable information about ore processing technology. The two linked mines form typical examples of mid-19th century mine complexes and as they are crossed by a footpath, they are an educational resource and public amenity. Botany: This site includes one of the richest calaminarian grassland communities remaining on the North Pennine lead mines, with the full suite of North Pennine metallophyte plants all thriving and a rich diversity of other plants, lichens and bryophytes. Thrift is declining throughout this area and the vigorous population at Whitesike may be the largest and most healthy left in the North Pennines, so it is considered to be of at least regional importance. 1 Geology: There is an exposure of the sponge and coral bearing limestone at location 6 on the geological features map. This bed is widely present across the Northern Pennines, but its location here alongside a footpath makes this an important educational and interpretation resource. -
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. -
Download Chapter In
Flora and vegetation Margaret E Bradshaw The flora of Upper Teesdale is probably more widely known than that of any other area in Britain, and yet perhaps only a few of the thousands who visit the Dale each year realise the extent to which the vegetation and flora contribute to the essence of its character. In the valley, the meadows in the small walled fields extend, in the lower part, far up the south-facing slope, and, until 1957 to almost 570m at Grass Hill, then the highest farm in England. On the north face, the ascent of the meadows is abruptly cut off from the higher, browner fells by the Whin Sill cliff, marked by a line of quarries. Below High Force, the floor of the valley has a general wooded appearance which is provided by the small copses and the many isolated trees growing along the walls and bordering the river. Above High Force is a broader, barer valley which merges with the expansive fells leading up to the characteristic skyline of Great Dun Fell, Little Dun Fell and Cross Fell. Pennine skyline above Calcareous grassland and wet bog, Spring gentian Red Sike Moss © Margaret E Bradshaw © Geoff Herbert Within this region of fairly typical North Pennine vegetation is a comparatively small area which contains many species of flowering plants, ferns, mosses, liverworts and lichens which can be justifiably described as rare. The best known is, of course, the spring gentian (Gentiana verna), but this is only one of a remarkable collection of plants of outstanding scientific value. -
Number 71 October 2013
Number 71 FellFarerthe October 2013 Editorial CLUB OFFICIALS Sometimes you get a photograph that you know just has to be the front page picture. PRESIDENT: Gordon Pitt Tel: 015395 68210 Sometimes you don’t and you struggle to find VICE PRESIDENT: Roger Atkinson Tel: 01539732490 any reasonable picture that will do. Then , perversely, they seem to come along like buses TRUSTEES Vicky Atkinson Tel: 07971 408378 - too many all at the same time. Mick Fox Tel: 01539 727531 Cheryl Smallwood Tel: 01629 650164 That’s how it was this time; I had several Mark Walsh Tel: 01606 891050 photographs that would have all made great front cover shots. So which one to choose? COMMITTEE Well, most of the contenders were of the Chairman: Roger Atkinson Tel: 01539 732490 198, Burneside Road Shinscrapers on the crags around Kendal on Kendal LA96EB Thursday evenings but there was just this one, email: [email protected] a happy accident, taken in the dark at the campsite on the shore of Ullswater. I asked Vice Chairman: Mark Walsh Tel: 01606 891050 20, Knutsford Road the Secretary to choose and she answered Antrobus without hesitation. I was pleased. She was Northwich right so I used it. Cheshire CW9 6JW Thanks you to this issue’s contributers : email: [email protected] John Peat, Paul East, Sarah, Matt and Emma Secretary: Clare Fox Tel: 01539 727531 Jennings, Helen Speed, Alec Reynolds, Joan 50, Gillinggate Abbot, David Birkett, Ruth Joyce, Peter and Kendal Nat Blamire LA94JB email: [email protected] Ed. Cover Photograph: Treasurer: Val Calder Tel: 01539727109 Jess Walsh and Kirsten Ball toasting marshmallows, 86, Vicarage Drive The Water Weekend Kendal LA95BA Side Farm Campsite. -
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. -
Moor View, Hunstanworth, Blanchland, DH8 9UF
Moor View, Hunstanworth, Blanchland, DH8 9UF Moor View, Hunstanworth, Blanchland, DH8 9UF Offers In Region Of: £480,000 An opportunity to acquire this beautiful Grade ll listed, detached, period three bedroom family home. Located within the beautiful Hamlet of Hunstanworth. With half an acre of generous gardens to be fully enjoyed. • Detached family home • Large gardens • Enjoying fabulous views • Three bedrooms • Sitting room, dining room, music room • Study/office • Garage and store rooms DESCRIPTION is a gravelled garden with raised flower beds, bushes and shrubs. Moor view is a beautiful Grade ll listed detached period family home The rear garden enjoys views over the countryside. located with the hamlet of Hunstanworth, 2 miles south west of Blanchland. Situated within the North Penines Area of Outstanding LOCATION Natural Beauty and 3 miles from Derwent Reservoir. The house enjoys Hunstanworth is a North Pennine parish surrounding by green fields fabulous views to the rear over surrounding countryside, and offers and woodland and near to beautiful heather moorlands. It is close to character noteworthy features including fireplaces, beamed ceilings and the Northumberland/County Durham border and just 2 miles South Gothic style windows. The house is approached via paved pathway over West of the historical village of Blanchland and is close to a the front garden, the front door leads into the entrance hall and a particularly beautiful stretch of the River Derwent. 10 miles West of spacious reception hallway with large walk-in cloaks cupboard and doors Consett and 12 miles south of Hexham, 25 west by south of leading off to a cozy living room with wooden fireplace housing an open Newcastle, and 8 miles south-west of Stanhope. -
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. -
Stanhope Churchyard
The Weardale Churchyard Project Prepared by Margaret Manchester on behalf of Weardale Field Study Society St Thomas' Churchyard, Stanhope, Weardale, Co.Durham, England. MEM NO. INSCRIPTION 1 In Affectionate Remembrance/ of/ GEORGE SANDERSON/ BELOVED HUSBAND OF HANNAH SANDERSON/ WHO DIED APRIL 4TH 1881 AGED 54 YEARS/ ALSO CLYDE SON OF THE ABOVE/ DIED MARCH 9TH 1870 AGED 2 YEARS/ ALSO WILLIAM SON OF THE ABOVE/ DIED AUGUST 9TH 1881 AGED 37 YEARS/ ALSO JOHN GEORGE SON OF THE ABOVE/ DIED JANY 20TH 1885 AGED 33 YEARS/ ALSO THOMAS SANDERSON/ WHO DIED JUNE 7TH 1887/ AGED 39 YEARS/ ALSO ROBERT SANDERSON/ WHO DIED MAY 22ND 1888/ AGED 34 YEARS/ ALSO OF THE ABOVE HANNAH SANDERSON/ DIED APRIL 3RD 1902 AGED 74 YEARS/ ALSO OF ANNIE NICHOLSON/ DIED APRIL 26TH 1906 AGED 34 YEARS 2 In/ MEMORY OF/ HANNAH WIFE OF/ JOSEPH DIXON OF EASTGATE/ WHO DEPARTED THIS LIFE/ FEB 21ST 1860 AGED 73 YEARS/ ALSO OF ANN THEIR THIRD/ DAUGHTER WHO DIED/ JULY 1ST 1821 AGED 7 YEARS/ ALSO OF THE ABOVE/ JOSEPH DIXON WHO DIED/ DECEMBER 24TH 1861 AGED 74 YEARS 3 In Loving Memory/ of/ NICHOLAS/ BELOVED HUSBAND/ OF ELIZABETH SANDERSON/ WHO DIED DECR 5TH 1885/ AGED 67 YEARS./ ALSO OF THEIR CHILDREN/ JOHN/ DIED JUNE 3RD 1864 AGED 21 YEARS/ SARAH/ DIED NOVR 10TH 1866 AGED 20 YEARS/ MARY/ DIED DECR 7TH 1882 AGED 23 YEARS/ AND ELIZABETH HIS BELOVED WIFE/ WHO DIED OCT 2ND 1892/ AGED 73 YEARS/ "THY WILL BE DONE"/ ANNIE SMOKER/ DIED NOV 21ST 1927/ AGED 87 YEARS/ FREDERICK SMOKER/ DIED MARCH 9TH 1932/ AGED 83 YEARS 4 In/ Loving Memory of/ Thomas WILSON/ OF SCURFIELD HOUSE/ WHO DIED 25 DEC 1843/ AGED 46 YEARS./ ALSO OF JANE, WIFE OF THE ABOVE/ WHO DIED 26 APRIL 1892,/ AGED 94 YEARS./ ALSO OF/ ISABELLA, THEIR DAUGHTER/ WHO DIED AT BISHOP OAK/ 26 DEC 1902/ AGED 73 YEARS./ ALSO OF ELIZABETH, THEIR DAUGHTER/ WHO DIED AT EAST BIGGINS/ 20 JULY 1908,/ AGED 81 YEARS. -
On the Junction of the Silurian Rocks and Carboniferous Limestone On
Downloaded from http://pygs.lyellcollection.org/ by guest on September 30, 2021 309 JUNCTION OF THE SILURIAN HOCKS WITH THE OVERLYING MOUNTAIN LIMESTONE, AT MOUGHTON FELL, IN RIBBL1S- DALE. BY THE EDITOR. (SEE PHOTOGRAPH.) THE photograph issued with this year's volume of proceedings, illustrates an important section exposed in the valley of the Bibble, nearly opposite the village of Horton. The Silurian rocks, composed of grits, slates and limestones, extend over a large area, bounded by the line of the Pennine Fault, running in a north and south direction, and that of the equally important series of Craven Faults which run eastward from Ingleton, their position being indicated by the precipitous Scars of GiggXeswick, Attermire, Malham, Yordale and Kilnsey. Bounded on the west and south by these Faults, the Silurian rocks underlie all the highest moun• tains in Yorkshire, forming a tolerably even base, with a general dip to the north-east. Sections exposing the junction of these rocks with the superincumbent Mountain Limestone may be seen beneath Whernside and Ingleborough, in the Ingleton and Dale Becks, and in Clapdale; underlying Cross Fell and Mickle Fell, they may be seen at High Cup Gill, and as shown by Mr. Dakyns, at the Pencil Mill, near Cronkley Scar. Penyghent, and the extensive Limestone Fells of Malham and Kilnsey also have a basement of Silurian Grits. Perhaps the finest section, showing the junction of the two formations, anywhere exposed, is the one chosen for the subject of this photograph. The Silurian Rocks have long been quarried, and are locally known as the Horton Flagstones; they are a bluish grey colour, rather coarse structure, and can be obtained of very large size.