A Geological Fence Diagram for England and Wales
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Pilot Rock - Soda Mountain 6089 Ft Elev
Pilot Rock Cascade-Siskiyou BLM BLM archives Rising 570 ft to an elevation of 5910 ft., Pilot Rock is perhaps the most striking feature of Cascade- Siskyou National Monument. Visible from much of the Shasta Valley in northern California and parts of Oregon’s Rogue Valley, the Rock serves as a friendly beacon to some five million vehicles and their passengers that travel the I-5 corridor annually. Competing Theories Pilot Rock is part of the Cascade Range, a mountain Put simply, a “plug” is an intrusive body formed by mag- range notable for its string of volcanic peaks stretching ma which cooled underground and was later exposed by from British Columbia to northern California’s Lassen erosion. Peak. The Monument’s proclamation refers to Pilot Rock as “a volcanic plug,” describing it as “a remnant of a Recent Research feeder vent left after a volcano eroded away, leaving an Recent research regarding Pilot Rock suggests that 25 outstanding example of the inside of a volcano.” Pilot million years ago, magma oozed through a weak spot Rock is composed mostly of volcanic andesite and has in the earth’s crust, but did not reach the surface. As a sheer, vertical faces with classic columnar jointing created result, some geologists refer to Pilot Rock as technically by the cooling of its andesite composition. a “volcanic plug,” but NOT as defined in the Monument’s proclamation. (The proclamation evidently uses “plug” Plug or a Neck or both? and “neck” interchangeably.) However “plugs”and Many geologists use the terms “neck” and “plug” in- “necks” are defined, what they both have in common is terchangeably, while others believe the terms apply to erosion. -
The Carboniferous Bowland Shale Gas Study: Geology and Resource Estimation
THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION The Carboniferous Bowland Shale gas study: geology and resource estimation i © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Disclaimer This report is for information only. It does not constitute legal, technical or professional advice. The Department of Energy and Climate Change does not accept any liability for any direct, indirect or consequential loss or damage of any nature, however caused, which may be sustained as a result of reliance upon the information contained in this report. All material is copyright. It may be produced in whole or in part subject to the inclusion of an acknowledgement of the source, but should not be included in any commercial usage or sale. Reproduction for purposes other than those indicated above requires the written permission of the Department of Energy and Climate Change. Suggested citation: Andrews, I.J. 2013. The Carboniferous Bowland Shale gas study: geology and resource estimation. British Geological Survey for Department of Energy and Climate Change, London, UK. Requests and enquiries should be addressed to: Toni Harvey Senior Geoscientist - UK Onshore Email: [email protected] ii © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Foreword This report has been produced under contract by the British Geological Survey (BGS). It is based on a recent analysis, together with published data and interpretations. Additional information is available at the Department of Energy and Climate Change (DECC) website. https://www.gov.uk/oil-and-gas-onshore-exploration-and-production. This includes licensing regulations, maps, monthly production figures, basic well data and where to view and purchase data. -
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. -
Written Guide
The tale of a tail A self-guided walk along Edinburgh’s Royal Mile ww.discoverin w gbrita in.o the stories of our rg lands discovered th cape rough w s alks 2 Contents Introduction 4 Route map 5 Practical information 6 Commentary 8 Credits © The Royal Geographical Society with the Institute of British Geographers, London, 2015 Discovering Britain is a project of the Royal Geographical Society (with IBG) The digital and print maps used for Discovering Britain are licensed to the RGS-IBG from Ordnance Survey Cover image: Detail from the Scottish Parliament Building © Rory Walsh RGS-IBG Discovering Britain 3 The tale of a tail Discover the stories along Edinburgh’s Royal Mile A 1647 map of The Royal Mile. Edinburgh Castle is on the left Courtesy of www.royal-mile.com Lined with cobbles and layered with history, Edinburgh’s ‘Royal Mile’ is one of Britain’s best-known streets. This famous stretch of Scotland’s capital also attracts visitors from around the world. This walk follows the Mile from historic Edinburgh Castle to the modern Scottish Parliament. The varied sights along the way reveal Edinburgh’s development from a dormant volcano into a modern city. Also uncover tales of kidnap and murder, a dramatic love story, and the dramatic deeds of kings, knights and spies. The walk was originally created in 2012. It was part of a series that explored how our towns and cities have been shaped for many centuries by some of the 206 participating nations in the 2012 Olympic and Paralympic Games. -
University of Birmingham a Lower Carboniferous (Visean)
University of Birmingham A lower Carboniferous (Visean) tetrapod trackway represents the earliest record of an edopoid amphibian from the UK Bird, Hannah; Milner, Angela; Shillito, Anthony; Butler, Richard DOI: 10.1144/jgs2019-149 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Bird, H, Milner, A, Shillito, A & Butler, R 2020, 'A lower Carboniferous (Visean) tetrapod trackway represents the earliest record of an edopoid amphibian from the UK', Geological Society. Journal, vol. 177, no. 2, pp. 276-282. https://doi.org/10.1144/jgs2019-149 Link to publication on Research at Birmingham portal Publisher Rights Statement: Journal of the Geological Society, 2019, https://doi.org/10.1144/jgs2019-149 © 2019 The Author(s). Published by The Geological Society of London. All rights reserved. General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. -
Volcanoes: a Suitable Home? Lesson Plan
Lesson 5: Volcanoes: a suitable home? Lesson Plan Use the Volcaones PowerPoint presentation in conjunction with the Lesson Plan. The PowerPoint presentation contains photograph and images and follows the sequence of the lesson. The factsheet for teachers, to accompany this lesson also explains some of the key points in more detail. This lesson assumes prior knowledge from Lesson 4: Volcanoes. Remember to use atlases or Google Earth to locate the volcanoes mentioned in the lesson. Key questions and ideas Why do people live on or near volcanoes? To understand that volcanoes produce useful minerals and that these can be extracted. To understand that volcanic soils are fertile and good for agriculture. What is geothermal energy important? Why is the volcanic landscape and environment important for tourism? What are the dangers of living on or near volcanoes? Subject content area Locational knowledge: Using maps to focus on Europe, North and South America, concentrating on key physical and human characteristics, key topographical features and land-use patterns; and understand how some of these have changed over time. Place knowledge: Understand geographical similarities and differences through the study of a region of the United Kingdom, a region in a European Country and a region within North and South America. Physical geography: Describe and understand key aspects of physical geography, including volcanoes. Human geography: Describe and understand key aspects of human geography, including types of settlement and land use, economic activity and the distribution of natural resources including energy, food and minerals. Geographical skills and fieldwork: Use maps and digital/computer mapping to locate countries and describe features studied. -
Northumberland National Park Geodiversity Audit and Action Plan Location Map for the District Described in This Book
Northumberland National Park Geodiversity Audit and Action Plan Location map for the district described in this book AA68 68 Duns A6105 Tweed Berwick R A6112 upon Tweed A697 Lauder A1 Northumberland Coast A698 Area of Outstanding Natural Beauty Holy SCOTLAND ColdstreamColdstream Island Farne B6525 Islands A6089 Galashiels Kelso BamburghBa MelrMelroseose MillfieldMilfield Seahouses Kirk A699 B6351 Selkirk A68 YYetholmetholm B6348 A698 Wooler B6401 R Teviot JedburghJedburgh Craster A1 A68 A698 Ingram A697 R Aln A7 Hawick Northumberland NP Alnwick A6088 Alnmouth A1068 Carter Bar Alwinton t Amble ue A68 q Rothbury o C B6357 NP National R B6341 A1068 Kielder OtterburOtterburnn A1 Elsdon Kielder KielderBorder Reservoir Park ForForestWaterest Falstone Ashington Parkand FtForest Kirkwhelpington MorpethMth Park Bellingham R Wansbeck Blyth B6320 A696 Bedlington A68 A193 A1 Newcastle International Airport Ponteland A19 B6318 ChollerforChollerfordd Pennine Way A6079 B6318 NEWCASTLE Once Housesteads B6318 Gilsland Walltown BrewedBrewed Haydon A69 UPON TYNE Birdoswald NP Vindolanda Bridge A69 Wallsend Haltwhistle Corbridge Wylam Ryton yne R TTyne Brampton Hexham A695 A695 Prudhoe Gateshead A1 AA689689 A194(M) A69 A686 Washington Allendale Derwent A692 A6076 TTownown A693 A1(M) A689 ReservoirReservoir Stanley A694 Consett ChesterChester-- le-Streetle-Street Alston B6278 Lanchester Key A68 A6 Allenheads ear District boundary ■■■■■■ Course of Hadrian’s Wall and National Trail N Durham R WWear NP National Park Centre Pennine Way National Trail B6302 North Pennines Stanhope A167 A1(M) A690 National boundaryA686 Otterburn Training Area ArAreaea of 0 8 kilometres Outstanding A689 Tow Law 0 5 miles Natural Beauty Spennymoor A688 CrookCrook M6 Penrith This product includes mapping data licensed from Ordnance Survey © Crown copyright and/or database right 2007. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Devonian and Carboniferous Stratigraphical Correlation and Interpretation in the East Irish
CR/16/040 Last modified: 2016/05/30 11:40 Carboniferous stratigraphical correlation and interpretation in the Irish Sea Energy and Marine Geoscience Programme Commissioned Report CR/16/040 CR/16/040 Last modified: 2016/05/30 11:40 BRITISH GEOLOGICAL SURVEY ENERGY AND MARINE GEOSCIENCE PROGRAMME COMMISSIONED REPORT CR/16/040 Carboniferous stratigraphical correlation and interpretation The National Grid and other Ordnance Survey data © Crown Copyright and database rights in the Irish Sea 2015. Ordnance Survey Licence No. 100021290 EUL. Keywords O. Wakefield, C. N. Waters and N. J. P Smith Report; Stratigraphy, Carboniferous, East Irish Sea. Front cover View of the Great Orme, Llandudno, North Wales, comprising thick carbonate platform successions typical of the Carboniferous Limestone Supergroup of the Irish Sea and adjacent areas (P007274). ©BGS NERC Bibliographical reference Wakefield, O. Waters, C.N. and Smith, N.J.P. 2016. Carboniferous stratigraphical correlation and interpretation in the Irish Sea. British Geological Survey Commissioned Report, CR/16/040. 82pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is -
Pilot Rock at CSNM
Pilot Rock Cascade-Siskiyou BLM BLM archives Rising 570’ to an elevation of 5,910’, Pilot Rock is perhaps the most striking feature of Cascade-Siskyou National Monument. Visible from much of the Shasta Valley in northern California and parts of Oregon’s Rogue Valley, the Rock serves as a friendly beacon to some five million vehicles and their passengers that travel the I-5 corridor annually. Welcome Recent Research Pilot Rock is part of the Cascade Range, a mountain Recent research regarding Pilot Rock suggests that 25 range notable for its string of volcanic peaks stretching million years ago, magma oozed through a weak spot from British Columbia to northern California’s Lassen in the earth’s crust, but did not reach the surface. As a Peak. The monument’s proclamation refers to Pilot Rock result, some geologists refer to Pilot Rock as technically as “a volcanic plug,” describing it as “a remnant of a a “volcanic plug,” but NOT as defined in the Monument’s feeder vent left after a volcano eroded away, leaving an proclamation. (The proclamation evidently uses “plug” outstanding example of the inside of a volcano.” Pilot and “neck” interchangeably.) However “plugs’ and Rock is composed mostly of volcanic andesite and has “necks” are defined, what they both have in common sheer, vertical faces with classic columnar jointing created is erosion. After the softer rock is eroded, the remain- by the cooling of its andesite composition. ing harder volcanic structure stands up in bold relief to the surrounding landscape as the blockish, irregular, Plug or a Neck or both? columnar structure you see today. -
Dinantian Carbonate Development and Related Prospectivity of the Onshore Northern Netherlands
Dinantian carbonate development and related prospectivity of the onshore Northern Netherlands Nynke Hoornveld, 2013 Author: Nynke Hoornveld Supervisors: Bastiaan Jaarsma, EBN Utrecht Prof. Dr. Jan de Jager, VU University Amsterdam Master Thesis: Solid Earth, (450199 and 450149) 39 ECTS. VU University Amsterdam 01-06-2013 Dinantian carbonate development and related prospectivity of the onshore Northern Netherlands Nynke Hoornveld, 2013 Contents Contents……………………………………………………………………………………………………………………………………………..2 Abstract…………………………………………………………………………………………….………………………………………………..3 Introduction…………………………………………………………………………………………………………….…………………….……4 Geological History of the Netherlands relating to Dinantian development…………………………..……………..7 Tectonic history…………………………………………………………………………………………………………………………..9 Stratigraphy of the Carboniferous…………………………………………………………………………………………….16 Stratigraphic Nomenclature of the Netherlands……………………………………………………………….………23 Methods……………………………………………………………………………………………………………………………………….…..26 Seismic interpretation…………………………………………………………………………………………………………….…27 Time-depth conversion…………………………………………………………………………………………………….……...35 Well correlation……………………………………………………………………………………………………………………..…38 Carbonate production, precipitation and geometries, with a focus on the Dinantian……….………40 Results………………………………………………………………………………………………………………………………….…………..57 Well information, evaluation and reservoir development………………………………………………………..58 Geometry of the Dinantian carbonate build-ups in the Dutch Northern onshore…………..……….75 The geological history -
A Lithostratigraphical Framework for the Carboniferous Successions of Northern Great Britain (Onshore)
A lithostratigraphical framework for the Carboniferous successions of northern Great Britain (onshore) Research Report RR/10/07 HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are bookmarked enabling direct links to be followed to the principal section headings and sub- headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY The National Grid and other Ordnance Survey data are used RESEARCH REPOrt RR/10/07 with the permission of the Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2011. Keywords Carboniferous, northern Britain, lithostratigraphy, chronostratigraphy, biostratigraphy. A lithostratigraphical framework Front cover for the Carboniferous successions View of Kae Heughs, Garleton Hills, East Lothian. Showing of northern Great Britain Chadian to Arundian lavas and tuffs of the Garleton Hills Volcanic Formation (Strathclyde Group) (onshore) exposed in a prominent scarp (P001032). Bibliographical reference M T Dean, M A E Browne, C N Waters and J H Powell DEAN, M T, BROWNE, M A E, WATERS, C N, and POWELL, J H. 2011. A lithostratigraphical Contributors: M C Akhurst, S D G Campbell, R A Hughes, E W Johnson, framework for the Carboniferous N S Jones, D J D Lawrence, M McCormac, A A McMillan, D Millward, successions of northern Great Britain (Onshore).