Devonshire Rigs Sites

Total Page:16

File Type:pdf, Size:1020Kb

Devonshire Rigs Sites Devon County Geological Sites Site reference no. SX77SW2 Name: Leigh Tor District: Teignbridge Parish: Widecombe in the Moor National grid ref: SX 712714 OS sheets: 1:50k 191 1:25k SX67/77 1:10k SX77SW GS 1:50k 338 GridRef x y Lat Long SX711714 271100 71400 50.52814 -3.8199576 Locality description (address): Leigh Tor, 2.2km NNE of Holne Nature of site: Tor with large clitter of loose blocks particularly downslope from the tor. Geological / geomorphological features: Dyke-like body of quartz.-veined tourmalinised hornfels up to about 10m wide. Most of the tor is somewhat disturbed with many large blocks rotated, but the lower part of the tor is mainly in situ. The body cuts Crackington Formation hornfels within the granite aureole and extends west north westwards towards the granite and across it far to the west. It also extends over several kilometres east-south-eastwards in the Carboniferous rocks. It is probably associated with a major regional steep fault structure. The rock consists of a dark matrix of tourmalinised hornfels cut by a dense anastomosing network of cross cutting quartz veins with some drusy cavities into which grow quartz crystals. The structure was probably subjected to repeated movements and brecciation. Much debris of hornfels can be seen to the south and west-south-west of the tor. Reasons for registration as a Regionally Important Geological / Geomorphological Site: A good example of quartz/tourmaline rock occurring outside the granite, most occurring in the granite. It is probably worth more mineralogical study. Site sensitivity: None known Safety: A lot of the rock is slippery particularly in the rain and care has to be exercising in climbing about on it. Interest groups: University. Undergraduate - Research Professional geologists - Amateur geologists - General public. Access and Parking: Only about 200m from the main road and there are small car parks nearby. Date of assessment (V = visited) : V 1998 E C Freshney Site owner : Common Mr J Simpson, Spitchwick Manor, Poundsgate Other comments: References: Reid, C R, Barrow, G., Sherlock, R L., MacAlister, D A., Dewey, H. and Bromehead, C N. 1912. The Geology of Dartmoor, Memoirs of the Geological Survey of England and Wales, London. .
Recommended publications
  • Historical Background of the Contact Between Celtic Languages and English
    Historical background of the contact between Celtic languages and English Dominković, Mario Master's thesis / Diplomski rad 2016 Degree Grantor / Ustanova koja je dodijelila akademski / stručni stupanj: Josip Juraj Strossmayer University of Osijek, Faculty of Humanities and Social Sciences / Sveučilište Josipa Jurja Strossmayera u Osijeku, Filozofski fakultet Permanent link / Trajna poveznica: https://urn.nsk.hr/urn:nbn:hr:142:149845 Rights / Prava: In copyright Download date / Datum preuzimanja: 2021-09-27 Repository / Repozitorij: FFOS-repository - Repository of the Faculty of Humanities and Social Sciences Osijek Sveučilište J. J. Strossmayera u Osijeku Filozofski fakultet Osijek Diplomski studij engleskog jezika i književnosti – nastavnički smjer i mađarskog jezika i književnosti – nastavnički smjer Mario Dominković Povijesna pozadina kontakta između keltskih jezika i engleskog Diplomski rad Mentor: izv. prof. dr. sc. Tanja Gradečak – Erdeljić Osijek, 2016. Sveučilište J. J. Strossmayera u Osijeku Filozofski fakultet Odsjek za engleski jezik i književnost Diplomski studij engleskog jezika i književnosti – nastavnički smjer i mađarskog jezika i književnosti – nastavnički smjer Mario Dominković Povijesna pozadina kontakta između keltskih jezika i engleskog Diplomski rad Znanstveno područje: humanističke znanosti Znanstveno polje: filologija Znanstvena grana: anglistika Mentor: izv. prof. dr. sc. Tanja Gradečak – Erdeljić Osijek, 2016. J.J. Strossmayer University in Osijek Faculty of Humanities and Social Sciences Teaching English as
    [Show full text]
  • Cold-Climate Landform Patterns in the Sudetes. Effects of Lithology, Relief and Glacial History
    ACTA UNIVERSITATIS CAROLINAE 2000 GEOGRAPHICA, XXXV, SUPPLEMENTUM, PAG. 185–210 Cold-climate landform patterns in the Sudetes. Effects of lithology, relief and glacial history ANDRZEJ TRACZYK, PIOTR MIGOŃ University of Wrocław, Department of Geography, Wrocław, Poland ABSTRACT The Sudetes have the whole range of landforms and deposits, traditionally described as periglacial. These include blockfields and blockslopes, frost-riven cliffs, tors and cryoplanation terraces, solifluction mantles, rock glaciers, talus slopes and patterned ground and loess covers. This paper examines the influence, which lithology and structure, inherited relief and time may have had on their development. It appears that different rock types support different associations of cold climate landforms. Rock glaciers, blockfields and blockstreams develop on massive, well-jointed rocks. Cryogenic terraces, rock steps, patterned ground and heterogenic solifluction mantles are typical for most metamorphic rocks. No distinctive landforms occur on rocks breaking down through microgelivation. The variety of slope form is largely inherited from pre- Pleistocene times and includes convex-concave, stepped, pediment-like, gravitational rectilinear and concave free face-talus slopes. In spite of ubiquitous solifluction and permafrost creep no uniform characteristic ‘periglacial’ slope profile has been created. Mid-Pleistocene trimline has been identified on nunataks in the formerly glaciated part of the Sudetes and in their foreland. Hence it is proposed that rock-cut periglacial relief of the Sudetes is the cumulative effect of many successive cold periods during the Pleistocene and the last glacial period alone was of relatively minor importance. By contrast, slope cover deposits are usually of the Last Glacial age. Key words: cold-climate landforms, the Sudetes 1.
    [Show full text]
  • Mystic Mountain © Mendip Hills AONB
    Viewpoint Mystic mountain © Mendip Hills AONB Time: 15 mins Region: South West England Landscape: rural Location: Ebbor Gorge, Somerset, BA5 3BA Grid reference: ST 52649 48742 Getting there: Park at Deer Leap car park and picnic area (on the road between Wookey Hole and Priddy) Keep an eye out for: Buzzards and other birds of prey soaring on the thermals below From this stunning vantage point we have sweeping views south across the flat land of the Somerset Levels. On a clear day, looking east you can see the dark line of hills marking out Exmoor National Park and if you look in a west south-west direction you can even spot the Bristol Channel glistening in the distance. As our eyes pan across the view they rest on a perfectly rounded knoll with a short tower on top. This is Glastonbury Tor. Claimed as the site of the legendary Vale of Avalon and the final resting place of King Arthur, the tor rises up above the flat land surrounding it and is visible for miles around. Why does the mystical Glastonbury Tor rise up out of the surrounding lowlands? First of all look straight ahead and in the middle distance you’ll see three hills which punctuate the flat landscape. From left to right they are Hay Hill, Ben Knowle Hill and Yarley Hill, part of a low ridge just south of the River Axe. Surrounding these hills the Somerset Levels are an area of low-lying farmland. The lowest point is just 0.2 metres above sea level.
    [Show full text]
  • 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.
    [Show full text]
  • Engineering Geology in Washington, Volume I Washington Diviaion of Geology and Euth Resources Bulletin 78
    ENGINEERING GEOLOGY IN WASHINGTON Volume I RICHARD W. GALSTER, Chairman Centennial Volume Committee Washington State Section, Association of Engineering Geologists WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES BULLETIN 78 1989 Prepared in cooperation with the Washington State Section of the A~ociation or Engineering Geologists ''WNatural ASHINGTON STATE Resources DEPARTMENT OF Brian Boyle • Commlssloner 01 Public Lands Ari Stearns - Sup,,rvuor Division of Geology and Earth Resources Raymond LcumanJs. Slate Geologist The use of brand or trade names in this publication is for pur­ poses of identification only and does not constitute endorsement by the Washington Division of Geology and Earth Resources or the Association of Engineering Geologists. This report is for sale (as the set of two volumes only) by: Publications Washington Department of Natural Resources Division of Geology and Earth Resources Mail Stop PY-12 Olympia, WA 98504 Price $ 27.83 Tax 2.17 Total $ 30.00 Mail orders must be prepaid; please add $1.00 to each order for postage and handling. Make checks or money orders payable to the Department of Natural Resources. This publication is printed on acid-free paper. Printed in the United States of America. ii VOLUME I DEDICATION . ................ .. .. ...... ............ .......................... X FOREWORD ........... .. ............ ................... ..... ................. xii LIST OF AUTHORS ............................................................. xiv INTRODUCTION Engineering Geology in Washington: Introduction Richard W. Galster, Howard A. Coombs, and Howard H. Waldron ................... 3 PART I: ENGINEERING GEOLOGY AND ITS PRACTICE IN WASHINGTON Geologic Factors Affecting Engineered Facilities Richard W. Galster, Chapter Editor Geologic Factors Affecting Engineered Facilities: Introduction Richard W. Galster ................. ... ...................................... 17 Geotechnical Properties of Geologic Materials Jon W. Koloski, Sigmund D. Schwarz, and Donald W.
    [Show full text]
  • Pp.01-06 Front Pages Pp. 01-4 Front 21/11/2011 14:25 Page 1
    93049 IMCOS covers 2011.qxd:Layout 1 14/2/11 08:42 Page 4 FINE ANTIQUE MAPS, ATLASES, GLOBES, CITY PLANS&VIEWS journal Winter 2011 Number 127 Paris from Jansson's Theatrum Urbium (1657), complete with 500 plates in eight vols. The largest and most beautiful, early city atlas. Splendid period color throughout; pristine condition. Very rare--one edition only. Visit our beautiful map gallery at 70 East 55th St. (Between Park & Madison Avenue) New York, New York 10022 212-308-0018 • 800-423-3741 (U.S. only) • [email protected] Recent acquisitions regularly added at martayanlan.com Contact us to receive a complimentary printed catalogue or register on our web site. We would be happy to directly offer you material in your collecting area; let us know about your interests. We are always interested in acquiring fine antique maps. GALLERY HOURS: Mon-Fri, 9:30-5:30 and by appointment. For People Who Love Early Maps 93049 IMCOS covers 2011.qxd:Layout 1 14/2/11 08:42 Page 5 THE MAP HOUSE OF LONDON (established 1907) Antiquarian Maps, Atlases, Prints & Globes 54 BEAUCHAMP PLACE KNIGHTSBRIDGE LONDON SW3 1NY Telephone: 020 7589 4325 or 020 7584 8559 Fax: 020 7589 1041 Email: [email protected] www.themaphouse.com pp.01-06 Front pages_ pp. 01-4 Front 21/11/2011 14:25 Page 1 Journal of the International Map Collectors’ Society Founded 1980 Winter 2011 Issue No.127 Features From Observation to Knowledge: The influence of London map and chartmakers 7 by Mary Pedley Revealing Devon History: An unrecorded manuscript atlas 17 by E.H.T.
    [Show full text]
  • A Geomorphic Classification System
    A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals
    [Show full text]
  • The Early Neolithic Tor Enclosures of Southwest Britain
    The Early Neolithic Tor Enclosures of Southwest Britain By Simon R. Davies A thesis submitted to The University of Birmingham For the degree of Ph.D. Funded by the AHRC. i University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. Abstract Along with causewayed enclosures, the tor enclosures of Cornwall and Devon represent the earliest enclosure of large open spaces in Britain and are the earliest form of surviving non-funerary monument. Their importance is at least as great as that of causewayed enclosures, and it might be argued that their proposed associations with settlement, farming, industry, trade and warfare indicate that they could reveal more about the Early Neolithic than many causewayed enclosure sites. Yet, despite being recognised as Neolithic in date as early as the 1920s, they have been subject to a disproportionately small amount of work. Indeed, the southwest, Cornwall especially, is almost treated like another country by many of those studying the Early Neolithic of southern Britain. When mentioned, this region is more likely to be included in studies of Ireland and the Irish Sea zone than studies concerning England.
    [Show full text]
  • ON APPLICATION of GLOTTOCHRONOLOGY for CELTIC LANGUAGES Dedicated to the Memory of Sergei Starostin (March 24, 1953 – September 30, 2005)
    SBORNÍK PRACÍ FILOZOFICKÉ FAKULTY BRNĚNSKÉ UNIVERZITY STUDIA MINORA FACULTATIS PHILOSOPHICAE UNIVERSITATIS BRUNENSIS A 54, 2006 — LINGUISTICA BRUNENSIA PETRA NOVOTNÁ – VÁCLAV BLAŽEK ON APPLICATION OF GLOTTOCHRONOLOGY FOR CELTIC LANGUAGES Dedicated to the memory of Sergei Starostin (March 24, 1953 – September 30, 2005) The present article continues in the series of studies published in this journal, demonstrating the application of lexicostatistics and glottochronology for vari- ous Indo-European branches, namely Germanic (Blažek & Pirochta 2004), Slavic (Novotná & Blažek 2005). Especially in the latter study the various modifications of glottochronology are explained in details. For Celtic languages two main alternative models of their internal classifica- tion were proposed. The traditional, p/q-model, is based especially on phonology, the Insular/Continental dichotomy has been argumented by morphology. Goidelic Goidelic q-Celtic Insular Celtiberian Brittonic Gaulish & Lepontic Gaulish & Lepontic p-Celtic Continental Brittonic Celtiberian (H. Pedersen, K.H. Schmidt) (P. Schrijver, C. Watkins) The lexicostatistic approach for a study of genetic relations of the Celtic lan- guages was introduced by Robert Elsie (1979; 1986; 1990). Applying lexicostatis- tic method with 100–word-list and excluding synonyms, he has got the following results for the Brittonic languages: Breton-Cornish 84.8%, Cornish-Welsh 78.8%, Breton-Welsh 73.7% (Elsie 1979, 48). In the case of the Goidelic languages, Elsie studied in details together 58 various Goidelic dialects and varieties on the basis of 184–word-list. He concludes that Manx is closer to any of the dialect group of Irish than to any of the dialect group of Scottish Gaelic (Elsie 1986, 244). The second attempt to apply the lexicostatistic approach for classification of the Celtic languages was realized, unfortunately not published, by Sergei Staros- tin, who used his own modification of glottochronology.
    [Show full text]
  • Rocks of the Krkonoše Tundra
    Rocks of the kRkonoše tundRa Podpořeno grantem z Islandu, Lichtenštejnska a Norska. Supported by grant from Iceland, Liechtenstein and Norway. Rocks of the Krkonoše Tundra Rocks and rocky outcrops are an unmis- extensive canyons, gorges, castellated takable part of a mountain range, even rocks, cliffs and castle koppies, as well though, according to their type, the char- as individual points of interest, such as acter of their geological development, waterfalls, caves, overhangs, rock towers representation and diversity of minerals, and pinnacles, balanced rocks and many climatic conditions, as well as various others. The rocks are also of importance local conditions, there are mountain for their connections with human activi- ranges which are rich in rocks, while ties, as people have long sought them others are poor. Rocky areas without out for building castles and due to their a cover of weathering products are not landscape dominance, for the construc- only a significant helper for geologists tion of various chapels, tourist chalets and geomorphologists who study these and last but not least, lookout towers mountains, but also play a fundamental and vantage points, often accessed by role for lay tourists and undemanding stairs, ladders, footbridges etc. visitors, because it is the quantity and shape of the rocks which are probably Krkonoše is a very old mountain range the most important factors in determin- and of course this also determines ing the landscape attractiveness of each its relief. Although there are certain region, i. e. its wildness and romantic exceptions, we can generally say that character. Of course there are mountain our developmentally younger moun- ranges with almost no exposed rocks, but tain ranges, where erosion is more they will never be as attractive for visitors rapid and contributes to the shaping as those ranges which are decorated by of the rocks, have a higher number of interesting rock formations.
    [Show full text]
  • Paleostress Reconstruction of Faults Recorded in the Niedźwiedzia Cave (Sudetes): Insights Into Alpine Intraplate Tectonic of NE Bohemian Massif
    International Journal of Earth Sciences https://doi.org/10.1007/s00531-021-01994-1 ORIGINAL PAPER Paleostress reconstruction of faults recorded in the Niedźwiedzia Cave (Sudetes): insights into Alpine intraplate tectonic of NE Bohemian Massif Artur Sobczyk1 · Jacek Szczygieł2 Received: 28 December 2019 / Accepted: 16 January 2021 © The Author(s) 2021 Abstract Brittle structures identifed within the largest karstic cave of the Sudetes (the Niedźwiedzia Cave) were studied to reconstruct the paleostress driving post-Variscan tectonic activity in the NE Bohemian Massif. Individual fault population datasets, including local strike and dip of fault planes, striations, and Riedel shear, enabled us to discuss the orientation of the prin- cipal stresses tensor. The (meso) fault-slip data analysis performed both with Dihedra and an inverse method revealed two possible main opposing compressional regimes: (1) NE–SW compression with the formation of strike-slip (transpressional) faults and (2) WNW–ESE horizontal compression related to fault-block tectonics. The (older) NE-SW compression was most probably associated with the Late Cretaceous–Paleogene pan-regional basin inversion throughout Central Europe, as a reaction to ongoing African-Iberian-European convergence. Second WNW–ESE compression was active as of the Middle Miocene, at the latest, and might represent the Neogene–Quaternary tectonic regime of the NE Bohemian Massif. Exposed fault plane surfaces in a dissolution-collapse marble cave system provided insights into the Meso-Cenozoic tectonic history of the Earth’s uppermost crust in Central Europe, and were also identifed as important guiding structures controlling the origin of the Niedźwiedzia Cave and the evolution of subsequent karstic conduits during the Late Cenozoic.
    [Show full text]
  • Free Event Guide
    FREE EVENT GUIDE 9 - 24 SEPTEMBER 2017 ”Always enjoyable and inspiring” 2 DEVON OPEN STUDIOS 2017 Welcome to Devon Artist Network’s Open Studios 2017 Members of Devon Artist Network are once again opening their studios and homes across this beautiful county to showcase their work to the public. Devon Artist Network’s mission is to support the county’s artists and crafters by organising events, exhibitions, family workshops and more. Do visit the website www.devonartistnetwork.co.uk where you can access the wealth of talent in Devon and find out how to support it. Charlotte Chance venue 83 We are, as ever, grateful to Helpful Holidays, the West Country holiday cottage specialists, for their support both in enabling us to offer our Emerging Artist Bursaries (see page 3) and in sponsoring part of the administration of the whole event. If you are planning a visit to the West Country this year, why not look at their website www.helpfulholidays.com for a comprehensive selection of beautiful Avenda Burnell Walsh venue 124 holiday cottages across the region. DEVON OPEN STUDIOS 2017 3 How to use this free guide Opening Days and Times Over 250 artists working across the stunning county Unless otherwise stated, venues’ standard opening times are: 11am - 6pm. There are two late evenings (Thursday of Devon are waiting to welcome you to their NORTH DEVON 1 NORTH DEVON 14th and 21st), when some venues open from 6 - 8pm. unique workspaces. There is so much to explore: TORRIDGE && MIDTORRIDGE DEVON If the date is shown the venue is open on those evenings.
    [Show full text]