QRA Top 50 Sites Booklet
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Varve-Related Publications in Alphabetical Order (Version 15 March 2015) Please Report Additional References, Updates, Errors Etc
Varve-Related Publications in Alphabetical Order (version 15 March 2015) Please report additional references, updates, errors etc. to Arndt Schimmelmann ([email protected]) Abril JM, Brunskill GJ (2014) Evidence that excess 210Pb flux varies with sediment accumulation rate and implications for dating recent sediments. Journal of Paleolimnology 52, 121-137. http://dx.doi.org/10.1007/s10933-014-9782-6; statistical analysis of radiometric dating of 10 annually laminated sediment cores from aquatic systems, constant rate of supply (CRS) model. Abu-Jaber NS, Al-Bataina BA, Jawad Ali A (1997) Radiochemistry of sediments from the southern Dead Sea, Jordan. Environmental Geology 32 (4), 281-284. http://dx.doi.org/10.1007/s002540050218; Dimona, Jordan, gamma spectroscopy, lead-210, no anthropogenic contamination, calculated sedimentation rate agrees with varve record. Addison JA, Finney BP, Jaeger JM, Stoner JS, Norris RN, Hangsterfer A (2012) Examining Gulf of Alaska marine paleoclimate at seasonal to decadal timescales. In: (Besonen MR, ed.) Second Workshop of the PAGES Varves Working Group, Program and Abstracts, 17-19 March 2011, Corpus Christi, Texas, USA, 15-21. http://www.pages.unibe.ch/download/docs/working_groups/vwg/2011_2nd_VWG_workshop_programs_and_abstracts.pdf; ca. 60 cm marine sediment core from Deep Inlet in southeast Alaska, CT scan, XRF scanning, suspected varves, 1972 earthquake and tsunami caused turbidite with scouring and erosion. Addison JA, Finney BP, Jaeger JM, Stoner JS, Norris RD, Hangsterfer A (2013) Integrating satellite observations and modern climate measurements with the recent sedimentary record: An example from Southeast Alaska. Journal of Geophysical Research: Oceans 118 (7), 3444-3461. http://dx.doi.org/10.1002/jgrc.20243; Gulf of Alaska, paleoproductivity, scanning XRF, Pacific Decadal Oscillation PDO, fjord, 137Cs, 210Pb, geochronometry, three-dimensional computed tomography, discontinuous event-based marine varve chronology spans AD ∼1940–1981, Br/Cl ratios reflect changes in marine organic matter accumulation. -
ANTEVS: a Quantitative Varve Sequence Cross- Correlation Technique with Examples from the Northeastern USA John A
This article was downloaded by: [Frederick Vollmer] On: 02 July 2013, At: 13:34 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK GFF Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/sgff20 ANTEVS: a quantitative varve sequence cross- correlation technique with examples from the Northeastern USA John A. Rayburn a & Frederick W. Vollmer a a Department of Geological Science , State University of New York at New Paltz , New Paltz , NY , 12561 , USA E-mail: Published online: 01 Jul 2013. To cite this article: GFF (2013): ANTEVS: a quantitative varve sequence cross-correlation technique with examples from the Northeastern USA, GFF, DOI: 10.1080/11035897.2013.801924 To link to this article: http://dx.doi.org/10.1080/11035897.2013.801924 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content. -
Application of Non-Destructive Techniques on a Varve Sediment Record from Vouliagmeni Coastal Lake, Eastern Gulf of Corinth, Greece
applied sciences Article Application of Non-Destructive Techniques on a Varve Sediment Record from Vouliagmeni Coastal Lake, Eastern Gulf of Corinth, Greece Alexandros Emmanouilidis 1 , Ingmar Unkel 2 , Joana Seguin 2, Kleoniki Keklikoglou 3,4 , Eleni Gianni 1 and Pavlos Avramidis 1,* 1 Department of Geology, University of Patras, 26504 Rio Patras, Greece; [email protected] (A.E.); [email protected] (E.G.) 2 Institute for Ecosystem Research, Christian-Albrechts-University, 24118 Kiel, Germany; [email protected] (I.U.); [email protected] (J.S.) 3 Hellenic Centre for Marine Research, Institute of Marine Biology, Biotechnology and Aquaculture, 71500 Heraklion, Greece 4 Department of Biology, University of Crete, 71500 Heraklion, Greece; [email protected] * Correspondence: [email protected] Received: 18 October 2020; Accepted: 19 November 2020; Published: 21 November 2020 Abstract: During the last few decades, X-ray attenuation systems have been established as standard techniques in geosciences and as excellent scientific tools for the analysis of sedimentary facies and structures. In the present study, we use two non-destructive and high-resolution systems (computed tomography, X-ray fluorescence) to address all sedimentological facies and structural characteristics on a 6 m long, partly laminated sediment record, from Vouliagmeni lake, located at the eastern part of the Corinth Gulf, Greece. Vouliagmeni lake is the deepest coastal lake in Greece, and its location is of great importance since it is located in one of the most tectonically active regions in the world. The chronological framework of the retrieved sediment sequence spans the last 12,000 years, with alternations of laminated and non-laminated sections. -
Mapping Known and Potential Karst Areas in the Northwest Territories, Canada
Mapping Known and Potential Karst Areas in the Northwest Territories, Canada Derek Ford, PGeo., PhD, FRSC. Emeritus Professor of Geography and Earth Sciences, McMaster University [email protected] For: Environment and Natural Resources, Government of the Northwest Territories August 2009 (i) Executive Summary The Goal of this Report is to Produce Maps of the Known and Potential Karst Landform Sites in the Northwest Territories (NWT) Karst landforms are those created by the dissolution of comparatively soluble rocks and the routing of the water (from rain or snowmelt) underground via caves rather than at the surface in river channels. The principal karst rocks are salt (so soluble that it is scarcely seen at the surface in the NWT), gypsum and anhydrite (solubility around 2500 mg/l of water), and limestone and dolomite (solubility around 250 -350 mg/l). All of these rock types are common and widespread amongst the sedimentary strata in the NWT. Surface karst landforms include: a) karren, which are spreads of individually small solution pits, shafts, and runnels that, collectively, may cover many hectares (limestone pavements); b) sinkholes of solutional, collapse, or other origin that can be tens to hundreds of metres in diameter and proportionally as deep. Sinkholes are considered the diagnostic karst landform worldwide; c) larger topographically closed depressions that may flood or drain seasonally, poljes if flat-floored, otherwise turloughs; d) extensive dry valleys and gorges, dry because their formative waters have been captured underground. All water sinking underground via karst landforms of all sizes drain quickly in comparison with all other types of groundwater because they are able to flow through solutionally enlarged conduits, termed caves where they are of enterable size. -
Oliva Vieira 2017.Pdf
Catena 149 (2017) 637–647 Contents lists available at ScienceDirect Catena journal homepage: www.elsevier.com/locate/catena Soil temperatures in an Atlantic high mountain environment: The Forcadona buried ice patch (Picos de Europa, NW Spain) Jesús Ruiz-Fernández a,⁎,MarcOlivab, Filip Hrbáček c, Gonçalo Vieira b, Cristina García-Hernández a a Department of Geography, University of Oviedo, Oviedo, Spain b Centre for Geographical Studies, Institute of Geography and Spatial Planning, Universidade de Lisboa, Lisbon, Portugal c Department of Geography, Masaryk University, Brno, Czech Republic article info abstract Article history: The present study focuses on the analysis of the ground and near-rock surface air thermal conditions at the Received 15 February 2016 Forcadona glacial cirque (2227 m a.s.l.) located in the Western Massif of the Picos de Europa, Spain. Temperatures Received in revised form 13 June 2016 have been monitored in three distinct geomorphological and topographical sites in the Forcadona area over the Accepted 27 June 2016 period 2006–11. The Forcadona buried ice patch is the remnant of a Little Ice Age glacier located in the bottom of a Available online 1 August 2016 glacial cirque. Its location in a deep cirque determines abundant snow accumulation, with snow cover between 8 and 12 months. The presence of snow favours stable soil temperatures and geomorphic stability. Similarly to Keywords: fi Soil temperatures other Cantabrian Mountains, the annual thermal regime of the soil is de ned by two seasonal periods (continu- Cirque wall temperatures ous thaw with daily oscillations and isothermal regime), as well as two short transition periods. -
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. -
News Snippets
The newsletter of the CAMBRIDGE QUATERNARY ISSUE 36 LENT 2007 News Snippets Dr Steve Boreham recently appeared on Ray Mears’ BBC series ‘Wild Food’. For the full story see the newspaper article on page 6 of this issue. Core team in photograph: Steve Boreham, Julie Miller, Ray Mears and Chris Rolfe The Encyclopedia of Quaternary Science , edited by Scott Elias, was released in November 2006 and a copy has recently arrived in the department. The four volume work provides broad-ranging, up-to-date articles on all of the major topics in the field of Quaternary Science and is aimed at the undergraduate-level but also provides easily accessible, expert information for active researchers. Prof Phil Gibbard (University of Cambridge, UK) and Dr Juergens Ehlers (Geologisches Landesamt, Germany) wrote a section entitled ‘The History of Quaternary Glaciations’. The work is also available online via ScienceDirect. 1 Welcome! The Quaternary Palaeoenvironments Group welcomes Antii Pasanen from the University of Oulu, Finland. Antii has funding from the Vilho, Yrjö and Kalle Väisälä Foundation and from the Academy of Finland to conduct part of his PhD based at the University of Cambridge. His study focuses on the internal structures of glaciofluvial sediments, including glaciotectonic structures, and his study sites are in western Finland, north eastern Russia and East Anglia. He will be conducting sedimentological, tectonic and clast fabric analyses, and will be using ground penetrating radar methods. When he is not working, he enjoys sport, especially floorball (which is played in Cambridge!) and ice hockey. Seminar Dates February QDG talks to be held at 5:30 Fri 23 rd TBA pm in the Lloyd Room at QDG Christ’s College Cambridge. -
Ref: LCAA1820
Ref: LCAA5959 Offers around £595,000 Higher Botrea Farm, Newbridge, Penzance, West Cornwall FREEHOLD A detached former farmhouse providing 4 bedroomed accommodation with additional 2 bedroomed annexe, gardens, stone barn, detached two storey garage, stable block and adjacent paddocks. The whole extending to about 5 acres. Situated in one of Cornwall’s most beautiful, rugged and untouched locations with potential to convert the outbuildings to further accommodation, subject to all necessary consents. 2 Ref: LCAA5959 SUMMARY OF ACCOMMODATION Ground Floor: entrance hall, study/bedroom 4, sitting room, kitchen/dining/breakfast room, utility room, cloakroom/wc. First Floor: 3 bedrooms and 2 bathrooms. Second Floor Annexe: accessed separately from the main house with accommodation including open-plan kitchen/dining/living room, 2 bedrooms and bathroom. Outside: plenty of parking, detached double garage with studio area over, separate barn (ripe for conversion – subject to all requisite consents), detached stable block. Large walled courtyard with decked area and further large lawn bordered by natural stone hedging. Paddocks approaching 3.1 acres. In all, approaching 5 acres. DESCRIPTION A superb and flexible farmhouse providing four bedroomed accommodation with an additional two bedroomed annexe. With the benefit of separate outbuildings, garage and stabling. Higher Botrea Farm offers exceptional rural living with plenty of scope and potential to either modernise the current accommodation or extend and develop the outbuildings, subject to requisite consents. The main house benefits from spacious living accommodation whilst retaining many of its original character features. The annexe is approached via exterior wooden steps and commands excellent rural and coastal views to the Isle of Scilly on a clear day. -
Proceedings of the Ussher Society
Proceedings of the Ussher Society Research into the geology and geomorphology of south-west England Volume 6 Part 3 1986 Edited by G.M Power The Ussher Society Objects: To promote research into the geology and geomorphology of south- west England and the surrounding marine areas; to hold Annual Conferences at various places in South West England where those engaged in this research can meet formally to hear original contributions and progress reports and informally to effect personal contacts; to publish, proceedings of such Conferences or any other work which the Officers of the Society may deem suitable. Officers: Chairman Dr. C.T. Scrutton Vice-Chairman Dr. E. B. Selwood Secretary Mr M.C. George Treasurer Mr R.C. Scrivener Editor Dr. G.M. Power Committee Members Dr G. Warrington Mr. C. R. Morey Mr. C.D.N. Tubb Mr. C. Cornford Mr D. Tucker Membership of the Ussher Society is open to all on written application to the Secretary and payment of the subscription due on January lst each year. Back numbers may be purchased from the Secretary to whom correspondence should be directed at the following address: Mr M. C. George, Department of Geology, University of Exeter, North Park Road, Exeter, Devon EX4 4QE Proceedings of the Ussher Society Volume 6 Part 3 1986 Edited by G.M. Power Crediton, 1986 © Ussher Society ISSN 0566-3954 1986 Typeset, printed and bound bv Phillips & Co., The Kyrtonia Press, 115 High Street, Crediton, Devon EXl73LG Set in Baskerville and Printed by Photolithography Proceedings of the Ussher Society Volume 6, Part 3, 1986 Papers D.L. -
Quaternary Geology & Geomorphology Division Officers
Quaternary Geologist & Geomorphologist Newsletter of the Quaternary Geology and Geomorphology Division http://rock.geosociety.org/qgg Spring 2006 Vol. 47, No. 1 Are these boulders part of an old moraine or a mass wasting deposit? The granite boulders are located on Table Mountain, near Sinks Canyon State Park (over man’s right shoulder), southwest of Lander, Wyoming. J.D. Love related this material to the Paleocene-Eocene ‘unroofing’ of the Wind River Range (skyline) and assigned it to a coarse-grained (near-source) facies of the Eocene White River Fm (1970, USGS Professional Paper 495-C). Recent preliminary 10Be/26Al age interpretations from similar boulders on Table Mountain (back, left) suggest these may be associated with mid-late Pleistocene glacial activity in the Wind River Range (Photo & preliminary data, Dahms). 1 Quaternary Geology & Geomorphology Division Officers Newsletter Editor and Panel Members -- 2006 and Webmaster: Dennis E. Dahms Officers – 6 Members, three of whom serve one-year Dept of Geography terms: Chair, First Vice-Chair, and Second Vice-Chair; Sabin Hall 127 and three of whom serve two-year terms: Secretary, University of Northern Iowa Treasurer, and Newsletter Editor/Webmaster. Cedar Falls, IA 50614-0406 [email protected] Management Board – 8 Members: Division officers and the Chair of the preceding year; also includes the Historian as an ex officio member. Past Chair: Alan R. Gillespie Chair: University of Washington John E. Costa Dept Earth & Space Sciences U.S. Geological Survey PO Box 351310 10615 SE Cherry Blossom Dr. Seattle, WA 98195-1310 Portland, OR 97216-3103 [email protected] [email protected] Historian: (Appointed by the Chair in consultation with 1st Vice-Chair: the Management Board) John (Jack) F. -
Geology of London, UK
Geology of London, UK Katherine R. Royse1, Mike de Freitas2,3, William G. Burgess4, John Cosgrove5, Richard C. Ghail3, Phil Gibbard6, Chris King7, Ursula Lawrence8, Rory N. Mortimore9, Hugh Owen10, Jackie Skipper 11, 1. British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. [email protected] 2. Imperial College London SW72AZ, UK & First Steps Ltd, Unit 17 Hurlingham Studios, London SW6 3PA, UK. 3. Department of Civil and Environmental Engineering, Imperial College London, London, SW7 2AZ, UK. 4. Department of Geological Sciences, University College London, WC1E 6BT, UK. 5. Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, UK. 6. Cambridge Quaternary, Department of Geography, University of Cambridge CB2 3EN, UK. 7. 16A Park Road, Bridport, Dorset 8. Crossrail Ltd. 25 Canada Square, Canary Wharf, London, E14 5LQ, UK. 9. University of Brighton & ChalkRock Ltd, 32 Prince Edwards Road, Lewes, BN7 1BE, UK. 10. Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK. 11. Geotechnical Consulting Group (GCG), 52A Cromwell Road, London SW7 5BE, UK. Abstract The population of London is around 7 million. The infrastructure to support this makes London one of the most intensively investigated areas of upper crust. however construction work in London continues to reveal the presence of unexpected ground conditions. These have been discovered in isolation and often recorded with no further work to explain them. There is a scientific, industrial and commercial need to refine the geological framework for London and its surrounding area. This paper reviews the geological setting of London as it is understood at present, and outlines the issues that current research is attempting to resolve. -
Igc): Australia 2012
FOURTH CIRCULAR and FIELD TRIP GUIDE TRIP FIELD and CIRCULAR FOURTH 34th International Geological Congress (IGC): AUSTRALIA 2012 Unearthing Our Past And Future – Resourcing Tomorrow Brisbane Convention and Exhibition Centre (BCEC) Queensland, Australia 5 - 10 August, 2012 www.34igc.org 34th IGC CIRCULARS General distribution of this and subsequent Circulars for the 34th IGC is by email. The latest Circular is always available for download at www.34igc.org. The Fifth Circular and Final Program will be released in July 2012. AUSTRALIA 2012 An unparalleled opportunity for all to experience the geological and other highlights “downunder” MAJOR SPONSOR AND GEOHOST SPONSOR MAJOR SPONSORS 2 34th IGC AUSTRALIA 2012 | Fourth Circular Message from the President and Secretary General As the congress draws ever closer, we are pleased to release more information to assist you in making arrangements for your participation at the 34th IGC in Brisbane. This Fourth Circular includes a full guide to the Field Trips and full itineraries for each of these trips are provided. Updates have also been made to the scientific program. The response to the Super Early Bird registration offer was excellent. Delegates are now taking advantage of the Early bird registration fees of $550 for students and $995 for members (a member of any national geological organisation worldwide qualifies for the members rate). It is important to note that all 34th IGC registration fees include refreshments and lunch every day of the program, the welcome reception and all congress materials. Every effort has been made to keep the fees to the minimum and it is only because of the support of our sponsors and supporters that these fees have been achievable.