Water in Turner's Yorkshire
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Malhamdale and Southern/South Western Dales Fringes
Malhamdale and Southern/South Western Dales Fringes + Physical Influences Malhamdale The landscape of Malhamdale is dominated by the influence of limestone, and includes some of the most spectacular examples of this type of scenery within the Yorkshire Dales National Park and within the United Kingdom as a whole. Great Scar limestone dominates the scenery around Malham, attaining a thickness of over 200m. It was formed in the Carboniferous period, some 330 million years ago, by the slow deposition of shell debris and chemical precipitates on the floor of a shallow tropical sea. The presence of faultlines creates dramatic variations in the scenery. South of Malham Tarn is the North Craven Fault, and Malham Cove and Gordale Scar, two miles to the south, were formed by the Mid Craven Fault. Easy erosion of the softer shale rocks to the south of the latter fault has created a sharp southern edge to the limestone plateau north of the fault. This step in the landscape was further developed by erosion during the various ice ages when glaciers flowing from the north deepened the basin where the tarn now stands and scoured the rock surface between the tarn and the village, leading later to the formation of limestone pavements. Glacial meltwater carved out the Watlowes dry valley above the cove. There are a number of theories as to the formation of the vertical wall of limestone that forms Malham Cove, whose origins appear to be in a combination of erosion by ice, water and underground water. It is thought that water pouring down the Watlowes valley would have cascaded over the cove and cut the waterfall back about 600 metres from the faultline, although this does not explain why the cove is wider than the valley above. -
Lichen Flora of the Malham Tarn Area
Field Studies, 10, (2001) 57 - 92 LICHEN FLORA OF THE MALHAM TARN AREA M. R. D. SEAWARD Department of Environmental Science, University of Bradford, Bradford BD7 1DP AND A. PENTECOST Division of Life Sciences, King's College London, Franklin-Wilkins Building, 150 Stamford Street, London SE1 8WA ABSTRACT A checklist of lichens, lichenicolous fungi and associated fungi recorded from an area within 5 km of the Malham Tarn Field Centre, Yorkshire is accompanied by background information on the ecology and the history of recording there. In all, 346 taxa (including Lecidea obluridata Nyl., new to Britain) have been recorded from the area; 48 are based on old records, most of which are presumed extinct, but some are questionable in the absence of supporting herbarium material. COLLECTORS The earliest lichen records from Malham are attributable to Richard Richardson (1663- 1741) of North Bierley, the first Yorkshireman to collect lichens; his localised material, used by Johann Jacob Dillenius (1684-1747) for his revision of Ray's Synopsis (1724) and his own Historia Muscorum (1742), is to be found in the Dillenian and Sherardian Herbaria at Oxford University (OXF). Other botanists contributing to our knowledge of Malham lichens in the 18th and 19th centuries include John G. Baker (1834-1920), William Borrer (1781-1862), Benjamin Carrington (1827-1893), Samuel Hailstone (1768-1851), Thomas Hebden (1849-1931), William Hudson (1734-1793), Frederic A. Lees (1847-1921), John Nowell (1802-1867), Abraham Shackleton (1830-1916), Abraham Stansfield (1802-1880), William West (1848- 1914) and John Windsor (1787-1868). Hailstone's Malham records appear in Whitaker (1805), but many are unlocalised, being expressed as occurring in 'the Craven area'. -
Water Framework Directive) (England and Wales) Directions 2009
The River Basin Districts Typology, Standards and Groundwater threshold values (Water Framework Directive) (England and Wales) Directions 2009 The Secretary of State and the Welsh Ministers, with the agreement of the Secretary of State to the extent that there is any effect in England or those parts of Wales that are within the catchment areas of the rivers Dee, Wye and Severn, in exercise of the powers conferred by section 40(2) of the Environment Act 1995(a) and now vested in them(b), and having consulted the Environment Agency, hereby give the following Directions to the Environment Agency for the implementation of Directive 2000/60/EC of the European Parliament and of the Council establishing a framework for Community action in the field of water policy(c): Citation and commencement and extent 1.—(1) These Directions may be cited as the River Basin Districts Typology, Standards and Groundwater threshold values (Water Framework Directive) (England and Wales) Direction 2009 and shall come into force on 22nd December 2009. Interpretation 2.—(1) In these Directions— ―the Agency‖ means the Environment Agency; ―the Groundwater Directive‖ means Directive 2006/118/EC of the European Parliament and of the Council on the protection of groundwater against pollution and deterioration(d); ―the Priority Substances Directive‖ means Directive 2008/105/EC of the European Parliament and of the Council on environmental quality standards in the field of water policy(e); ―threshold value‖ has the same meaning as in the Groundwater Directive; and ―the Directive‖ means Directive 2000/60/EC of the European Parliament and of the Council of 23rd October 2000 establishing a framework for Community action in the field of water policy. -
21. Yorkshire Dales Area Profile: Supporting Documents
National Character 21. Yorkshire Dales Area profile: Supporting documents www.gov.uk/natural-england 1 National Character 21. Yorkshire Dales Area profile: Supporting documents Introduction National Character Areas map As part of Natural England’s responsibilities as set out in the Natural Environment 1 2 3 White Paper , Biodiversity 2020 and the European Landscape Convention , we North are revising profiles for England’s 159 National Character Areas (NCAs). These are East areas that share similar landscape characteristics, and which follow natural lines in the landscape rather than administrative boundaries, making them a good Yorkshire decision-making framework for the natural environment. & The North Humber NCA profiles are guidance documents which can help communities to inform their West decision-making about the places that they live in and care for. The information they contain will support the planning of conservation initiatives at a landscape East scale, inform the delivery of Nature Improvement Areas and encourage broader Midlands partnership working through Local Nature Partnerships. The profiles will also help West Midlands to inform choices about how land is managed and can change. East of England Each profile includes a description of the natural and cultural features that shape our landscapes, how the landscape has changed over time, the current key London drivers for ongoing change, and a broad analysis of each area’s characteristics and ecosystem services. Statements of Environmental Opportunity (SEOs) are South East suggested, which draw on this integrated information. The SEOs offer guidance South West on the critical issues, which could help to achieve sustainable growth and a more secure environmental future. -
Stargazing in the Yorkshire Dales National Park
l a wa s n w t in a q g n u a g r i t e n r i b g b o Looking south c When’s the best r u e s s c e n These stars change throughout the year t time to look? f n u l e l but you could see the constellations of Orion, w m The sky doesn’t o m o o n o Pegasus and the Summer Triangle or even n usually get dark Stargazing enough in high our Galaxy, the Milky Way. t n w e a in the Yorkshire Dales c x s i n e summer, so the best r g c g g i b n i b x o a u r s w time to view the stars National Park e t r a u South q t s r i f is from mid-August through to early May. S S S It’s also easiest to see the stars if there is no Moon – look out for new Moon phases. Spring is Top tips best for Be patient – Autumn planets as your eyes is best for the Milky Way and adjust to the darkness, the shooting stars Winter S S S more you will see. is best for star Try to avoid looking at any clusters and lights as it can take up to constellations 20 minutes for your night Further information vision to come back. For details of dark sky events, when to Take care, there might be hazards hidden see shooting stars or the northern lights by the dark. -
Site Improvement Plan Craven Limestone Complex
Improvement Programme for England's Natura 2000 Sites (IPENS) Planning for the Future Site Improvement Plan Craven Limestone Complex Site Improvement Plans (SIPs) have been developed for each Natura 2000 site in England as part of the Improvement Programme for England's Natura 2000 sites (IPENS). Natura 2000 sites is the combined term for sites designated as Special Areas of Conservation (SAC) and Special Protected Areas (SPA). This work has been financially supported by LIFE, a financial instrument of the European Community. The plan provides a high level overview of the issues (both current and predicted) affecting the condition of the Natura 2000 features on the site(s) and outlines the priority measures required to improve the condition of the features. It does not cover issues where remedial actions are already in place or ongoing management activities which are required for maintenance. The SIP consists of three parts: a Summary table, which sets out the priority Issues and Measures; a detailed Actions table, which sets out who needs to do what, when and how much it is estimated to cost; and a set of tables containing contextual information and links. Once this current programme ends, it is anticipated that Natural England and others, working with landowners and managers, will all play a role in delivering the priority measures to improve the condition of the features on these sites. The SIPs are based on Natural England's current evidence and knowledge. The SIPs are not legal documents, they are live documents that will be updated to reflect changes in our evidence/knowledge and as actions get underway. -
The Ecology of Cowside Beck, a Tributary of the River Skirfare in the Malham Area of Yorkshire
The ecology of Cowside Beck, a tributary of the River Skirfare in the Malham area of Yorkshire Oliver Gilbert, Helen Goldie, David Hodgson, Margaret Marker, Allan Pentecost, Michael Proctor and Douglas Richardson Dedicated to the memory of Oliver Lathe Gilbert 7th September 1936 - 15th May 2005 Published by Field Studies Council, Malham Tarn Field Centre, Settle, North Yorkshire BD24 9PU. Tel: 01729-830331 E-mail: [email protected] www.field-studies-council.org Copies of this report may be purchased from the Field Centre. This report can also be consulted on the website above. Contributors The late Oliver L. Gilbert (formerly Department of Landscape, University of Sheffield) Helen Goldie (Department of Geography, University of Durham) 2 Springwell Road, Durham DH1 4LR David Hodgson (The Craven Pothole Club) 9 Craven Terrace, Settle, North Yorkshire BD24 9DF Margaret Marker (formerly School of Geography and Environmental Science, Oxford University) 5 Wytham Close, Eynsham, Oxon OX29 4NS Adrian Norris (formerly The Leeds Museum Resource Centre) 17 West Park Drive, Leeds LSl6 5BL Allan Pentecost School of Health and Life Sciences, Kings College, University of London, 150 Stamford Street, London SE1 9NH Michael C. F. Proctor School of Biosciences, University of Exeter, Hatherly Laboratories, Prince of Wales Road, Exeter EX4 4PS Douglas T. Richardson (formerly Department of Earth Sciences, University of Leeds) 5 Calton Terrace, Skipton, North Yorkshire BD23 2AY If you would like to be involved in this work please contact: Cowside Beck -
The Malhamdale Plan
THE MALHAMDALE PLAN November 2005 Kirkby Malham Parish Council Airton Parish Meeting Calton Parish Meeting Otterburn Parish Meeting Malhamdale Initiative Scosthrop Parish Meeting Acknowledgements The Steering Group would like to take this opportunity to thank the following who have given assistance, support and contributions to help bring the Plan together: Chris Hall, Bob Hart, Annie Heseltine, Sally Heseltine, Mike Holden, Susie Holden, Alan Mercer, Bernadette Schutte, Johnnie Towler Nita Hart who has acted as treasurer to the Steering Group Leeds Metropolitan University for assistance in analysing the survey results Gemma Astin who gave several days of her time to enter survey results onto computer while on secondment to the Malham Tarn Field Centre preparing a final year dissertation on Malhamdale Initiative for her BA course in Human Geography at the University of Wales We would also like to thank members of the following organisations who have given their time and valuable advice Yorkshire Dales National Park Authority Craven District Council North Yorkshire County Council The National Trust The Steering Group comprises: Chris Wildman (Chairman), Sandy Tod (Secretary), Rob Hudson, Simon Maufe, Tony Robinson, Mark Throup, David Whittaker, John Varney THE MALHAMDALE PLAN Table of contents Page Number SECTION 1 Executive Summary ………………………………….. 2 SECTION 2 Introduction to Malhamdale ………………………… 3 SECTION 3 Location ………………………………………………... 4 SECTION 4 Preparing the Malhamdale Plan ……………………… 5 SECTION 5 Summary of Results …………………………………… 6 SECTION 6 Malhamdale Plan - the Vision ………………………… 7 SECTION 7 The Community 7.1 The Community Generally …………………….. 9 7.2 Activities and Facilities ………………………… 10 7.3 Education, Training and Young People ………. 11 7.4 Housing ………………………………………….. 12 7.5 Traffic and Transport ………………………….. -
THE SCENIC HIGHLIGHTS of the PENNINE WAY Discover the True Spirit of the North on England’S Original National Trail
ENGLAND’S GREAT WALKING TRAILS | THE PENNINE WAY LIMESTONE AND LEGEND: THE SCENIC HIGHLIGHTS OF THE PENNINE WAY Discover the true spirit of the North on England’s original National Trail Steeped in history and traversing spectacular upland landscapes in some of England’s most popular National ParKs, the Pennine Way is the most iconic of England’s Great WalKing Trails. Stretching for 268 miles (435Km) across England’s wild northern uplands, with a combined ascent that eXceeds the height of Mount Everest, it’s also arguably the toughest. OVERVIEW • Distance: 74 miles/120km • Start/Finish: Skipton/Appleby-in-Westmorland • Number of Days: 8 • Grade: Challenging • Theme: History / Geology • Landscape: Type High Hills & Moorland Opened in 1965, the Pennine Way blazed a trail for public access to some of England’s wildest landscapes – hitherto the sole preserve of a wealthy elite. Conceived by founder member of The Ramblers Tom Stephenson and popularised by the legendary Alfred Wainwright, the full route follows the rocky spine of England – stretching from the hills of the Derbyshire Peak District, through the Yorkshire Dales and onwards through Durham and Northumberland to the Scottish Border. Roughly following the line of the watershed from which great rivers like the Tyne and the Tees, the Lune and the Eden, flow east and west respectively, the bulk of this legendary trail lies at more than 1,000ft/305m above sea level. Our shortened 8-day itinerary explores the striking limestone landscapes of Malham in the Yorkshire Dales before climbing up onto the lonely massif of Cross Fell, where the Lakeland Fells are clearly visible across the Eden Valley. -
Freshwater Algae in Britain and Ireland - Bibliography
Freshwater algae in Britain and Ireland - Bibliography Floras, monographs, articles with records and environmental information, together with papers dealing with taxonomic/nomenclatural changes since 2003 (previous update of ‘Coded List’) as well as those helpful for identification purposes. Theses are listed only where available online and include unpublished information. Useful websites are listed at the end of the bibliography. Further links to relevant information (catalogues, websites, photocatalogues) can be found on the site managed by the British Phycological Society (http://www.brphycsoc.org/links.lasso). Abbas A, Godward MBE (1964) Cytology in relation to taxonomy in Chaetophorales. Journal of the Linnean Society, Botany 58: 499–597. Abbott J, Emsley F, Hick T, Stubbins J, Turner WB, West W (1886) Contributions to a fauna and flora of West Yorkshire: algae (exclusive of Diatomaceae). Transactions of the Leeds Naturalists' Club and Scientific Association 1: 69–78, pl.1. Acton E (1909) Coccomyxa subellipsoidea, a new member of the Palmellaceae. Annals of Botany 23: 537–573. Acton E (1916a) On the structure and origin of Cladophora-balls. New Phytologist 15: 1–10. Acton E (1916b) On a new penetrating alga. New Phytologist 15: 97–102. Acton E (1916c) Studies on the nuclear division in desmids. 1. Hyalotheca dissiliens (Smith) Bréb. Annals of Botany 30: 379–382. Adams J (1908) A synopsis of Irish algae, freshwater and marine. Proceedings of the Royal Irish Academy 27B: 11–60. Ahmadjian V (1967) A guide to the algae occurring as lichen symbionts: isolation, culture, cultural physiology and identification. Phycologia 6: 127–166 Allanson BR (1973) The fine structure of the periphyton of Chara sp. -
Yorkshire Union
December 2019 Volume 144 Number 1102 Yorkshire Union Yorkshire Union The Naturalist Vol. 144 No. 1102 December 2019 Contents Page YNU visit to Fountains Abbey, 6th May 2016 - a reconstruction of a 161 YNU event on 6 May 1905 Jill Warwick The Lady’s-Slipper Orchid in 1930: a family secret revealed 165 Paul Redshaw The mite records (Acari: Astigmata, Prostigmata) of Barry Nattress: 171 an appreciation and update Anne S. Baker Biological records of Otters from taxidermy specimens and hunting 181 trophies Colin A. Howes The state of the Watsonian Yorkshire database for the 187 aculeate Hymenoptera, Part 3 – the twentieth and twenty-first centuries from the 1970s until 2018 Michael Archer Correction: Spurn Odonata records 195 D. Branch The Mole on Thorne Moors, Yorkshire 196 Ian McDonald Notable range shifts of some Orthoptera in Yorkshire 198 Phillip Whelpdale Yorkshire Ichneumons: Part 10 201 W.A. Ely YNU Excursion Reports 2019 Stockton Hermitage (VC62) 216 Edlington Pit Wood (VC63) 219 High Batts (VC64) 223 Semerwater (VC65) 27th July 230 North Duffield Carrs, Lower Derwent Valley (VC61) 234 YNU Calendar 2020 240 An asterisk* indicates a peer-reviewed paper Front cover: Lady’s Slipper Orchid Cypripedium calceolus photographed in 1962 by John Armitage FRPS. (Source: Natural England Archives, with permission) Back cover: Re-enactors Charlie Fletcher, Jill Warwick, Joy Fletcher, Simon Warwick, Sharon Flint and Peter Flint on their visit to Fountains Abbey (see p161). YNU visit to Fountains Abbey, 6th May 2016 - a reconstruction of a YNU event on 6 May 1905 Jill Warwick Email: [email protected] A re-enactment of a visit by members of the YNU to Fountains Abbey, following the valley of the River Skell through Ripon and into Studley Park, was the idea of the then President, Simon Warwick, a local Ripon resident. -
River Response to Recent Environmental Change in the Yorkshire Ouse Basin, Northern England
River response to recent environmental change in the Yorkshire Ouse basin, northern England. Sean Anthony Longfield, B.Sc. (H ons) 'N/ Submitted in accordance with the requirements for the degree of Doctor of Philosophy The University of Leeds School of Geography July 1998 The candidate confirms that the work submitted is his own and that appropriate credit has been given where reference has been made to the w'ork of others II A b s t r a c t Longfield, S.A. 1998. River response to recent environmental change in the Yorkshire Ouse basin, northern England. University of Leeds, Ph.D. This study examines historical variations in flood frequency and magnitude in the Yorkshire Ouse basin, northern England, over the last 900 years. The causes of temporal and spatial variations in flooding are evaluated through investigation of climatic and land-use controls. Documentary evidence of flooding and climate suggests that a series of large floods between 1263 and 1360 were associated with climatic deterioration from the Medieval Optimum. A shift to generally milder conditions between 1361 and 1549 resulted in no floods being documented in the Ouse basin The frequency of large magnitude floods increased dramatically between 1550 and 1680, as a result of low temperatures, increased surface wetness, more frequent snowfall and a southward shift of prevailing storm tracks over middle latitudes, associated with the onset of the "Little Ice Age’. In contrast, during a wanner phase of the Little Ice Age, between 1681 and 1763, the frequency of localised summer flooding increased in the Ouse basin due to more frequent high intensity, short duration convective storms.