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Subject Guide 1 – Records Relating to Inclosure
Durham County Record Office County Hall Durham DH1 5UL Telephone: 03000 267619 Email: [email protected] Website: www.durhamrecordoffice.org.uk Subject Guide 1 – Records Relating to Inclosure Issue no. 19 July 2020 Contents Introduction 1 Organisation of List 2 Alphabetical List of Townships 2 A 2 B 2 C 3 D 4 E 4 F 4 G 4 H 5 I 5 K 5 L 5 M 6 N 6 O 6 R 6 S 7 T 7 U 8 W 8 Introduction Inclosure (occasionally spelled “enclosure”) refers to a reorganisation of scattered land holdings by mutual agreement of the owners. Much inclosure of Common Land, Open Fields and Moor Land (or Waste), formerly farmed collectively by the residents on behalf of the Lord of the Manor, had taken place by the 18th century, but the uplands of County Durham remained largely unenclosed. Inclosures, to consolidate land-holdings, divide the land (into Allotments) and fence it off from other usage, could be made under a Private Act of Parliament or by general agreement of the landowners concerned. In the latter case the Agreement would be Enrolled as a Decree at the Court of Chancery in Durham and/or lodged with the Clerk of the Peace, the senior government officer in the County, so may be preserved in Quarter Sessions records. In the case of Parliamentary Enclosure a Local Bill would be put before Parliament which would pass it into law as an Inclosure Act. The Acts appointed Commissioners to survey the area concerned and determine its distribution as a published Inclosure Award. -
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. -
County Durham Landscape Character Assessment: Classification
LANDSCAPE CHARACTER THE LANDSCAPE CLASSIFICATION The Landscape Classification The County Durham Landscape Character Assessment identifies landscape types and character areas at three different levels - the regional, the sub-regional and the local. Regional County Character Areas Sub-regional Broad Landscape Types Broad Character Areas See Table 1 Local Local Landscape Types See Table 2 Local Sub-types County Character Areas. County Character Areas are based on Natural England’s Countryside Character Areas. There are 6 Countryside Character Areas in County Durham, all of which extend beyond its administrative boundaries. County Character Areas are effectively those parts of Countryside Character Areas lying within the County. The boundaries of County Character Areas are more precisely drawn than those of Countryside Character Areas as they are based on a more detailed level of assessment. In reality the boundaries between these broad landscape zones are often gradual and progressive and difficult to identify precisely on the ground. The character of County Character Areas may differ in some ways from that of the larger Countryside Character Areas to which they belong. The descriptions of County Character Areas given here in the Landscape Assessment may therefore be slightly different to the descriptions given in other publications for Countryside Character Areas. Broad Landscape Types and Character Areas Broad Landscape Types are landscapes with similar patterns of geology, soils, vegetation, land use, settlement and field patterns identified at a broad sub-regional level. As with County Character Areas, the boundaries between Broad Landscape Types are not always precise, as the change between one landscape and another can be gradual and progressive. -
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. -
Der Europäischen Gemeinschaften Nr
26 . 3 . 84 Amtsblatt der Europäischen Gemeinschaften Nr . L 82 / 67 RICHTLINIE DES RATES vom 28 . Februar 1984 betreffend das Gemeinschaftsverzeichnis der benachteiligten landwirtschaftlichen Gebiete im Sinne der Richtlinie 75 /268 / EWG ( Vereinigtes Königreich ) ( 84 / 169 / EWG ) DER RAT DER EUROPAISCHEN GEMEINSCHAFTEN — Folgende Indexzahlen über schwach ertragsfähige Böden gemäß Artikel 3 Absatz 4 Buchstabe a ) der Richtlinie 75 / 268 / EWG wurden bei der Bestimmung gestützt auf den Vertrag zur Gründung der Euro jeder der betreffenden Zonen zugrunde gelegt : über päischen Wirtschaftsgemeinschaft , 70 % liegender Anteil des Grünlandes an der landwirt schaftlichen Nutzfläche , Besatzdichte unter 1 Groß vieheinheit ( GVE ) je Hektar Futterfläche und nicht über gestützt auf die Richtlinie 75 / 268 / EWG des Rates vom 65 % des nationalen Durchschnitts liegende Pachten . 28 . April 1975 über die Landwirtschaft in Berggebieten und in bestimmten benachteiligten Gebieten ( J ), zuletzt geändert durch die Richtlinie 82 / 786 / EWG ( 2 ), insbe Die deutlich hinter dem Durchschnitt zurückbleibenden sondere auf Artikel 2 Absatz 2 , Wirtschaftsergebnisse der Betriebe im Sinne von Arti kel 3 Absatz 4 Buchstabe b ) der Richtlinie 75 / 268 / EWG wurden durch die Tatsache belegt , daß das auf Vorschlag der Kommission , Arbeitseinkommen 80 % des nationalen Durchschnitts nicht übersteigt . nach Stellungnahme des Europäischen Parlaments ( 3 ), Zur Feststellung der in Artikel 3 Absatz 4 Buchstabe c ) der Richtlinie 75 / 268 / EWG genannten geringen Bevöl in Erwägung nachstehender Gründe : kerungsdichte wurde die Tatsache zugrunde gelegt, daß die Bevölkerungsdichte unter Ausschluß der Bevölke In der Richtlinie 75 / 276 / EWG ( 4 ) werden die Gebiete rung von Städten und Industriegebieten nicht über 55 Einwohner je qkm liegt ; die entsprechenden Durch des Vereinigten Königreichs bezeichnet , die in dem schnittszahlen für das Vereinigte Königreich und die Gemeinschaftsverzeichnis der benachteiligten Gebiete Gemeinschaft liegen bei 229 beziehungsweise 163 . -
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. -
Teesdale Local Plan Chapter 5 Population and Housing
Teesdale Local Plan – Adopted June 2002 CHAPTER 5 POPULATION & HOUSING Teesdale Local Plan – Adopted June 2002 5) POPULATION & HOUSING 5.0 INTRODUCTION 5.0.1 The projected population of the district is inextricably linked to the District’s future housing requirements. The maintenance of a stable population is a realistic goal for the next ten years. Due to the ageing demographic structure of the district, in–migration would be required to achieve this goal. 5.1 POPULATION PROJECTIONS & HOUSING REQUIREMENTS 5.1.1 The housing requirements of the plan are calculated on the basis of Durham County Structure Plan Policy. Policy 7 of the Structure Plan states that Teesdale will require about 1,000 more dwellings between 1991 – 2006. As this Plan extends to 2010 the housing requirement calculation will need to make an estimate for the building requirement between 2006 and 2010. This is achieved by taking the Structure Plan figure, converting that to an annual building rate and thereby providing an estimate for the period 2006-2010. The housing requirement will also need to take into account those dwellings completed between 1991 – 1998. 5.1.2 According to the published 1991 census figures the Population of Teesdale is 24,068 of which 306 are in communal establishments, Population projections based on 1997 estimates show the population is expected to increase slightly to 24,193 by 2010, with the number of persons in communal establishments expected to remain constant, this would lead to 23,887 requiring housing. 5.1.3 As previously mentioned above, latest projections show a slight increase in population added to that the reduction in the average household size would result in the need for additional dwellings. -
The London Gazette, 2 January, 1934 69
THE LONDON GAZETTE, 2 JANUARY, 1934 69 DISEASES OF ANIMALS ACTS, 1894 TO 1927—continued. SHEEP SCAB MOVEMENT AREAS— continued. thence in a south-easterly direction along the road to Bennetston Hall and thence north- easterly along the road to Sparrowpit; thence in an east-south-easterly direction along the road via Peak Forest, Lane Head, Wardlow Mires, Stony Middleton, Calver and Bridge End to Nether End; thence in an easterly direction along the road via Robinhood, Bleak House, Freebirch, Ingmanthorpe and Cutthorpe to Dunston Hall; thence in a general northerly direction along the road via Instone, Dronfield, Little Norton to Norton Woodseats; thence along Woodseats Road till it meets the London Midland and Scottish Railway that runs from Dore and Totley Station to Sheffield; thence in a north- easterly direction along the said railway to a point near to Victoria Station, Sheffield, where the London and North Eastern Railway lines, which run through Sheffield to Penistone, are carried over the said railway; thence in a north-westerly direction along the London and North Eastern Railway as far as Oughtibridge Station; thence in a westerly direction along the road between Grenoside and Oughtibridge to Oughtibridge; thence in a north-westerly direction via Wharncliffe Side, Deepcar, Stocksbridge, Sheephouse Wood, Langsett to Flouch Inn; thence in a westerly direction via Fiddlers Green and Salters- brook Bridge, to the point where the road crosses the London and North Eastern Railway from Penistone to Glossop near the western end of Woodhead Tunnel and thence along the London and North Eastern Railway via Growden to Glossop and the point of commence- ment. -
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. -
Map 19 Teeside, Tyneside and Wearside, 100-Km Grid Square NZ (Axis Numbers Are the Coordinates of the National Grid) © Crown Copyright
Alwinton ALNWICK 0 0 6 Elsdon Stanton Morpeth CASTLE MORPETH Whalton WANSBECK Blyth 0 8 5 Kirkheaton BLYTH VALLEY Whitley Bay NORTH TYNESIDE NEWCASTLE UPON TYNE Acomb Newton Newcastle upon Tyne 0 GATESHEAD 6 Dye House Gateshead 5 Slaley Sunderland SUNDERLAND Stanley Consett Edmundbyers CHESTER-LE-STREET Seaham DERWENTSIDE DURHAM Peterlee 0 Thornley 4 Westgate 5 WEAR VALLEY Thornley Wingate Willington Spennymoor Trimdon Hartlepool Bishop Auckland SEDGEFIELD Sedgefield HARTLEPOOL Holwick Shildon Billingham Redcar Newton Aycliffe TEESDALE Kinninvie 0 Stockton-on-Tees Middlesbrough 2 Skelton 5 Loftus DARLINGTON Barnard Castle Guisborough Darlington Eston Ellerby Gilmonby Yarm Whitby Hurworth-on-Tees Stokesley Gayles Hornby Westerdale Faceby Langthwaite Richmond SCARBOROUGH Goathland 0 0 5 Catterick Rosedale Abbey Fangdale Beck RICHMONDSHIRE Hornby Northallerton Leyburn Hawes Lockton Scalby Bedale HAMBLETON Scarborough Pickering Thirsk 400 420 440 460 480 500 The shading indicates the maximum requirements for radon protective measures in any location within each 1-km grid square to satisfy the guidance in Building Regulations Approved Document C. The requirement for an existing building with a valid postal address can be obtained for a small charge from www.ukradon.org. The requirement for a site without a postal address is available through the British Geological Survey GeoReports service, http://shop.bgs.ac.uk/GeoReports/. Level of protection required Settlements Roads National Grid None Sunderland Motorways 100-km 10-km Basic Primary Roads Other Features Peterlee Full A Roads LOCAL ADMINISTRATIVE DISTRICT Yarm B Roads Water features Slaley Map 19 Teeside, Tyneside and Wearside, 100-km grid square NZ (axis numbers are the coordinates of the National Grid) © Crown copyright.