( I ) North of England Institute of Mining Engineers
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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| CC_BY_NC_ND_4.0 | First posted online: Mon, 11 Nov 2019 01:27:37 | This content has not been peer reviewed.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. -
A Mineralogy of Anthropocene E
1 A Minerology for the Anthropocene Pierre FLUCK Institut Universitaire de France / Docteur-ès-Sciences / geologist and archeologist / Emeritus Professor at Université de Haute-Alsace This essay is a follow-up on « La signature stratigraphique de l’Anthropocène », which is also available on HAL- Archives ouvertes. Table of contents 1. Introduction: neoformation minerals in ancient mining galleries 2. Minerals from burning coal mines 3. Minerals from the mineral processing industry 4 ...and metallurgy 5. Neoformations in slags 6. Speciation of heavy metals in soils 7. Metal objects in their archaeological environment, or affected by fire 8. Neoformations in or on the surface of building stones 9. A mineralogy of materials. The “miracle of the potter”. The minerals in cement 10. A mineralogy of the biosphere? Conclusions Warning. This paper is written to be read by both specialists and a wider audience. However, it contains many mineral names. While these may resonate in the minds of mineralogists or collectors, they may not be as meaningful to less discerning readers. Such readers should not be scared, for they may find excellent encyclopaedic records on the web, including chemical composition, crystallographic properties and description of each of these species. This is why we have decided not to include further information in this paper. Acknowledgements. I would like to thank the mineralogists with whom I have had the opportunity to maintain fruitful exchanges for a long time: my pupil Hubert Bari, Éric Asselborn, Cédric Lheur, François Farges. And I would like to honour the memories of René Weil (1901-1983), my master in descriptive mineralogy, and of Jacques Geffroy (1918-1993), pupil of Alfred Lacroix, my master in metallogeny. -
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 Partnership of Smithson Tennant and William Hyde Wollaston
“A History of Platinum and its Allied Metals”, by Donald McDonald and Leslie B. Hunt 9 The Partnership of Smithson Tennant and William Hyde Wollaston “A quantity of platina was purchased by me a few years since with the design of rendering it malleable for the different purposes to which it is adapted. That object has now been attained. ” WILLIAM HYDE W O L L A S T O N Up to the end of the eighteenth century the attempts to produce malleable platinum had advanced mainly in the hands of practical men aiming at its pre paration and fabrication rather than at the solution of scientific problems. These were now to be attacked with a marked degree of success by two remarkable but very different men who first became friends during their student days at Cam bridge and who formed a working partnership in 1800 designed not only for scientific purposes but also for financial reasons. They were of the same genera tion and much the same background as the professional scientists of London whose work was described in Chapter 8, and to whom they were well known, but with the exception of Humphry Davy they were of greater stature and made a greater advance in the development of platinum metallurgy than their predecessors. Their combined achievements over a relatively short span of years included the successful production for the first time of malleable platinum on a truly com mercial scale as well as the discovery of no less than four new elements contained in native platinum, a factor that was of material help in the purification and treatment of platinum itself. -
Optical Properties of Common Rock-Forming Minerals
AppendixA __________ Optical Properties of Common Rock-Forming Minerals 325 Optical Properties of Common Rock-Forming Minerals J. B. Lyons, S. A. Morse, and R. E. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig. 13-3. A. High Positive Relief Zircon ZrSiO. Tet. (+) 111=1.940 High biref. Small euhedral grains show (.055) parallel" extinction; may cause pleochroic haloes if enclosed in other minerals Sphene CaTiSiOs Mon. (110) (+) 30-50 13=1.895 High biref. Wedge-shaped grains; may (Titanite) to 1.935 (0.108-.135) show (110) cleavage or (100) Often or (221) parting; ZI\c=51 0; brownish in very high relief; r>v extreme. color CtJI\) 0) Gamet AsB2(SiO.la where Iso. High Grandite often Very pale pink commonest A = R2+ and B = RS + 1.7-1.9 weakly color; inclusions common. birefracting. Indices vary widely with composition. Crystals often euhedraL Uvarovite green, very rare. Staurolite H2FeAI.Si2O'2 Orth. (010) (+) 2V = 87 13=1.750 Low biref. Pleochroic colorless to golden (approximately) (.012) yellow; one good cleavage; twins cruciform or oblique; metamorphic. Olivine Series Mg2SiO. Orth. (+) 2V=85 13=1.651 High biref. Colorless (Fo) to yellow or pale to to (.035) brown (Fa); high relief. Fe2SiO. Orth. (-) 2V=47 13=1.865 High biref. Shagreen (mottled) surface; (.051) often cracked and altered to %II - serpentine. Poor (010) and (100) cleavages. Extinction par- ~ ~ alleL" l~4~ Tourmaline Na(Mg,Fe,Mn,Li,Alk Hex. (-) 111=1.636 Mod. biref. -
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 -
ART. IX.-Notes on the Platinum, Metals, and Their 8L'paration from Each Other I by M
1ll. C. Lea on the Platinum Metala. 81 ART. IX.-Notes on the Platinum, Metals, and their 8l'paration from each other i by M. CAREY LEA, Philadelphia.-Part I. (1) FEW branches of inorganic chemistry present difficulties com parable with those involved in the study and separation of the platinum metals. 'rheir close analogy with each other, and the remarkllble manner in which the relations of each to chemical reagents are controlled by the presence of the others, give rise to difficulties in their detection and separation which are only by degrees being surmounted. Much time and unwearied labor on the part of the chemist are required to rench results whith when obtained appear insignificant in proportion to the effort which they cost, and it may ill fnct be said that the platinum metals constitute a chemistry in themselves, governed by special rules and to be studied by special method~. Each step in the simplification of the processes by which the separations are effected, each decisive reaction by which the presence or ab sence of a member of the group may be certainly iuferred, is so much gained toward conquering a complete knowledge of these rare and mteresting bodies. All[. JOUR. BOI.-SEOOND BUlBS, VOL. XXXVIII, No.112.-JuLT, 1864. n 82 M. C. Lea on the Platinum Metals. For much the better half of all we know upon this subject, we are indebted to Dr. Claus, whose method of' separation I have followed up to a certain point, and then have diverged from it, with I think some adva.ntage. -
New Mineral Names*
American Mineralogist, Volume 97, pages 2064–2072, 2012 New Mineral Names* G. DIEGO GATTA,1 FERNANDO CÁMARA,2 KIMBERLY T. TAIT,3,† AND DMITRY BELAKOVSKIY4 1Dipartimento Scienze della Terra, Università degli Studi di Milano, Via Botticelli, 23-20133 Milano, Italy 2Dipartimento di Scienze della Terra, Università di degli Studi di Torino, Via Valperga Caluso, 35-10125 Torino, Italy 3Department of Natual History, Royal Ontario Museum, 100 Queens Park, Toronto, Ontario M5S 2C6, Canada 4Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia IN THIS ISSUE This New Mineral Names has entries for 12 new minerals, including: agardite-(Nd), ammineite, byzantievite, chibaite, ferroericssonite, fluor-dravite, fluorocronite, litochlebite, magnesioneptunite, manitobaite, orlovite, and tashelgite. These new minerals come from several different journals: Canadian Mineralogist, European Journal of Mineralogy, Journal of Geosciences, Mineralogical Magazine, Nature Communications, Novye dannye o mineralakh (New data on minerals), and Zap. Ross. Mineral. Obshch. We also include seven entries of new data. AGARDITE-(ND)* clusters up to 2 mm across. Agardite-(Nd) is transparent, light I.V. Pekov, N.V. Chukanov, A.E. Zadov, P. Voudouris, A. bluish green (turquoise-colored) in aggregates to almost color- Magganas, and A. Katerinopoulos (2011) Agardite-(Nd), less in separate thin needles or fibers. Streak is white. Luster is vitreous in relatively thick crystals and silky in aggregates. Mohs NdCu6(AsO4)3(OH)6·3H2O, from the Hilarion Mine, Lavrion, Greece: mineral description and chemical relations with other hardness is <3. Crystals are brittle, cleavage nor parting were members of the agardite–zálesíite solid-solution system. observed, fracture is uneven. Density could not be measured Journal of Geosciences, 57, 249–255. -
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. -
High Temperature Sulfate Minerals Forming on the Burning Coal Dumps from Upper Silesia, Poland
minerals Article High Temperature Sulfate Minerals Forming on the Burning Coal Dumps from Upper Silesia, Poland Jan Parafiniuk * and Rafał Siuda Faculty of Geology, University of Warsaw, Zwirki˙ i Wigury 93, 02-089 Warszawa, Poland; [email protected] * Correspondence: j.parafi[email protected] Abstract: The subject of this work is the assemblage of anhydrous sulfate minerals formed on burning coal-heaps. Three burning heaps located in the Upper Silesian coal basin in Czerwionka-Leszczyny, Radlin and Rydułtowy near Rybnik were selected for the research. The occurrence of godovikovite, millosevichite, steklite and an unnamed MgSO4, sometimes accompanied by subordinate admixtures of mikasaite, sabieite, efremovite, langbeinite and aphthitalite has been recorded from these locations. Occasionally they form monomineral aggregates, but usually occur as mixtures practically impossible to separate. The minerals form microcrystalline masses with a characteristic vesicular structure resembling a solidified foam or pumice. The sulfates crystallize from hot fire gases, similar to high temperature volcanic exhalations. The gases transport volatile components from the center of the fire but their chemical compositions are not yet known. Their cooling in the near-surface part of the heap results in condensation from the vapors as viscous liquid mass, from which the investigated minerals then crystallize. Their crystallization temperatures can be estimated from direct measurements of the temperatures of sulfate accumulation in the burning dumps and studies of their thermal ◦ decomposition. Millosevichite and steklite crystallize in the temperature range of 510–650 C, MgSO4 Citation: Parafiniuk, J.; Siuda, R. forms at 510–600 ◦C and godovikovite in the slightly lower range of 280–450 (546) ◦C. -
An Exploration of Georgius Agricola's Natural Philosophy in De Re Metallica
Mining Metals, Mining Minds: An Exploration of Georgius Agricola’s Natural Philosophy in De re metallica (1556) By Hillary Taylor Dissertation Submitted to the Faculty of the Graduate School of Vanderbilt University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in History January 31, 2021 Nashville, Tennessee Approved: William Caferro, Ph.D. Lauren R. Clay, Ph.D. Laura Stark, Ph.D. Elsa Filosa, Ph.D. Francesca Trivellato, Ph.D. For my parents, Jim and Lisa ii Acknowledgements I have benefitted from the generosity of many individuals in my odyssey to complete this dissertation. My sincerest thanks go to Professor William Caferro who showed me how to call up documents at the Archivio di Stato in Florence, taught me Italian paleography, read each chapter, and provided thoughtful feedback. It has been a blessing working closely with a scholar who is as great as he is at doing history. I have certainly learned by his example, watching as he spends his own time reading, translating, writing, and editing. I have attempted to emulate his productivity, and I know that I would not have finished the ultimate academic enterprise without his guidance. Professor Caferro pruned my prose without bruising my ego, too badly. I must also extend my warmest thanks to the other members of my committee, Professor Lauren Clay, Professor Laura Stark, Professor Elsa Filosa, and Professor Francesca Trivellato. I am also grateful to Professor Monique O’Connell, my undergraduate advisor at Wake Forest University. Monique was the first to introduce me to the historiographical complexities of Italian history and intellectual thought.