An Overview of the Lithostratigraphical Framework for the Quaternary Deposits on the United Kingdom Continental Shelf
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Assessing the Chronostratigraphic Fidelity of Sedimentary Geological Outcrops in the Pliocene–Pleistocene Red Crag Formation, Eastern England
Downloaded from http://jgs.lyellcollection.org/ by guest on September 25, 2021 Research article Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2019-056 Where does the time go? Assessing the chronostratigraphic fidelity of sedimentary geological outcrops in the Pliocene–Pleistocene Red Crag Formation, eastern England Neil S. Davies1*, Anthony P. Shillito1 & William J. McMahon2 1 Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK 2 Faculty of Geosciences, Utrecht University, Princetonlaan 8a, Utrecht 3584 CB, Netherlands NSD, 0000-0002-0910-8283; APS, 0000-0002-4588-1804 * Correspondence: [email protected] Abstract: It is widely understood that Earth’s stratigraphic record is an incomplete record of time, but the implications that this has for interpreting sedimentary outcrop have received little attention. Here we consider how time is preserved at outcrop using the Neogene–Quaternary Red Crag Formation, England. The Red Crag Formation hosts sedimentological and ichnological proxies that can be used to assess the time taken to accumulate outcrop expressions of strata, as ancient depositional environments fluctuated between states of deposition, erosion and stasis. We use these to estimate how much time is preserved at outcrop scale and find that every outcrop provides only a vanishingly small window onto unanchored weeks to months within the 600–800 kyr of ‘Crag-time’. Much of the apparently missing time may be accounted for by the parts of the formation at subcrop, rather than outcrop: stratigraphic time has not been lost, but is hidden. The time-completeness of the Red Crag Formation at outcrop appears analogous to that recorded in much older rock units, implying that direct comparison between strata of all ages is valid and that perceived stratigraphic incompleteness is an inconsequential barrier to viewing the outcrop sedimentary-stratigraphic record as a truthful chronicle of Earth history. -
Neogene Stratigraphy of the Langenboom Locality (Noord-Brabant, the Netherlands)
Netherlands Journal of Geosciences — Geologie en Mijnbouw | 87 - 2 | 165 - 180 | 2008 Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands) E. Wijnker1'*, T.J. Bor2, F.P. Wesselingh3, D.K. Munsterman4, H. Brinkhiris5, A.W. Burger6, H.B. Vonhof7, K. Post8, K. Hoedemakers9, A.C. Janse10 & N. Taverne11 1 Laboratory of Genetics, Wageningen University, Arboretumlaan 4, 6703 BD Wageningen, the Netherlands. 2 Prinsenweer 54, 3363 JK Sliedrecht, the Netherlands. 3 Naturalis, P.O. Box 9517, 2300 RA Leiden, the Netherlands. 4 TN0 B&0 - National Geological Survey, P.O. Box 80015, 3508 TA Utrecht, the Netherlands. 5 Palaeocecology, Inst. Environmental Biology, Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands. 6 P. Soutmanlaan 18, 1701 MC Heerhugowaard, the Netherlands. 7 Faculty Earth and Life Sciences, Vrije Universiteit, de Boelelaan 1085, 1081 EH Amsterdam, the Netherlands. 8 Natuurmuseum Rotterdam, P.O. Box 23452, 3001 KL Rotterdam, the Netherlands. 9 Minervastraat 23, B 2640 Mortsel, Belgium. 10 Gerard van Voornestraat 165, 3232 BE Brielle, the Netherlands. 11 Snipweg 14, 5451 VP Mill, the Netherlands. * corresponding author. Email: [email protected] Manuscript received: February 2007; accepted: March 2008 Abstract The locality of Langenboom (eastern Noord-Brabant, the Netherlands), also known as Mill, is famous for its Neogene molluscs, shark teeth, teleost remains, birds and marine mammals. The stratigraphic context of the fossils, which have been collected from sand suppletions, was hitherto poorly understood. Here we report on a section which has been sampled by divers in the adjacent flooded sandpit 'De Kuilen' from which the Langenboom sands have been extracted. -
How Uniform Was the Old Norse Religion?
II. Old Norse Myth and Society HOW UNIFORM WAS THE OLD NORSE RELIGION? Stefan Brink ne often gets the impression from handbooks on Old Norse culture and religion that the pagan religion that was supposed to have been in Oexistence all over pre-Christian Scandinavia and Iceland was rather homogeneous. Due to the lack of written sources, it becomes difficult to say whether the ‘religion’ — or rather mythology, eschatology, and cult practice, which medieval sources refer to as forn siðr (‘ancient custom’) — changed over time. For obvious reasons, it is very difficult to identify a ‘pure’ Old Norse religion, uncorroded by Christianity since Scandinavia did not exist in a cultural vacuum.1 What we read in the handbooks is based almost entirely on Snorri Sturluson’s representation and interpretation in his Edda of the pre-Christian religion of Iceland, together with the ambiguous mythical and eschatological world we find represented in the Poetic Edda and in the filtered form Saxo Grammaticus presents in his Gesta Danorum. This stance is more or less presented without reflection in early scholarship, but the bias of the foundation is more readily acknowledged in more recent works.2 In the textual sources we find a considerable pantheon of gods and goddesses — Þórr, Óðinn, Freyr, Baldr, Loki, Njo3rðr, Týr, Heimdallr, Ullr, Bragi, Freyja, Frigg, Gefjon, Iðunn, et cetera — and euhemerized stories of how the gods acted and were characterized as individuals and as a collective. Since the sources are Old Icelandic (Saxo’s work appears to have been built on the same sources) one might assume that this religious world was purely Old 1 See the discussion in Gro Steinsland, Norrøn religion: Myter, riter, samfunn (Oslo: Pax, 2005). -
Marine Climate and Hydrography of the Coralline Crag (Early Pliocene, UK): Isotopic Evidence from 16 Benthic Invertebrate Taxa
Marine climate and hydrography of the Coralline Crag (early Pliocene, UK): isotopic evidence from 16 benthic invertebrate taxa. Item Type Article; Research Report Authors Vignols, Rebecca M.; Valentine, Annemarie M.; Finlayson, Alana G.; Harper, Elizabeth M.; Schöne, Bernd R.; Leng, Melanie J.; Sloane, Hilary J.; Johnson, Andrew L. A. Citation Bradshaw, J. et al. (2018). Marine climate and hydrography of the Coralline Crag (early Pliocene, UK): isotopic evidence from 16 benthic invertebrate taxa. Available at: https:// www.sciencedirect.com/science/article/pii/S0009254118302717? via%3Dihub (Accessed: 22 Jan 2019). DOI: 10.1016/ j.chemgeo.2018.05.034 DOI 10.1016/j.chemgeo.2018.05.034 Publisher Elsevier Journal Chemical Geology Rights Archived with thanks to Chemical Geology Download date 06/10/2021 07:06:31 Item License http://creativecommons.org/licenses/by-nc-nd/4.0/ Link to Item http://hdl.handle.net/10545/623343 Chemical Geology xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Marine climate and hydrography of the Coralline Crag (early Pliocene, UK): isotopic evidence from 16 benthic invertebrate taxa Rebecca M. Vignolsa,1, Annemarie M. Valentineb,2, Alana G. Finlaysona,3, Elizabeth M. Harpera, ⁎ Bernd R. Schönec, Melanie J. Lengd, Hilary J. Sloaned, Andrew L.A. Johnsonb, a Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK b School of Environmental Science, University of Derby, Kedleston Road, Derby DE22 1GB, UK -
Nordic American Voices Nordic Museum
Nordic American Voices Nordic Museum Interview of Yngve Hveding ID: 2017.036.001 March 18, 2017 Seattle, Washington Interviewers: Brandon Benson; Marjorie Graf Marjorie Graf: [0:00] This is an interview for the Nordic American Voices oral history project. Today is March 18, 2017, and we will be interviewing Yngve Hveding. We are at the Nordic Heritage Museum in Seattle, Washington. My name is Marjorie Graf, and also here interviewing is— Brandon Benson: [0:22] Brandon Benson. Marjorie Graf: [0:24] So, we’d like you to start by just stating your name and date of birth, and go on with your family history. Yngve Hveding: [0:32] My name is Yngve Hveding. I was born in Tromsø, in northern Norway, in 1945. My grandparents came from Lofoten and Vesterålen, just south of Tromsø. My grandfather’s name was Johann Hveding. He was born in 1867, in Lofoten. And my grandmother was born in 1878. Her name was Hilma Hansen. They were married in 1905 in [unintelligible] Kommune, Nordland, just north of Lofoten. [1:13] They had two kids— my dad, who was also named Johann Hveding, born in 1908, and he had a sister called Gunvor, born in 1911. My dad married my mother, who was from southern Norway. Her name was Fredis Stannis, born in 1908. They met at a place up in Lofoten where my dad was working, and they got married in 1937. A year later, they moved to Tromsø. They lived there before the war started. After a few years, my older sister was born in 1942. -
A Vibrant City on the Edge of Nature 2019/2020 Welcome to Bodø & Salten
BODØ & SALTEN A vibrant city on the edge of nature 2019/2020 Welcome to Bodø & Salten. Only 90 minutes by plane from Oslo, between the archipelago and south, to the Realm of Knut Hamsun in the north. From Norway’s the peaks of Børvasstidene, the coastal town of Bodø is a natural second biggest glacier in Meløy, your journey will take you north communications hub and the perfect base from which to explore via unique overnight accommodations, innumerable hiking trails the region. The town also has gourmet restaurants, a water and mountain peaks, caves, fantastic fishing spots, museums park, cafés and shopping centres, as well as numerous festivals, and cultural events, and urban life in one of the country’s including the Nordland Music Festival, with concerts in a beautiful quickest growing cities, Bodø. In the Realm of Hamsun in the outdoor setting. Hamsun Centre, you can learn all about Nobel Prize winner Knut Hamsun`s life and works, and on Tranøy, you can enjoy open-air This is a region where you can get close to natural phenomena. art installations against the panoramic backdrop of the Lofoten There is considerable contrast – from the sea to tall mountains, mountain range. from the midnight sun to the northern lights, from white sandy beaches to naked rock. The area is a scenic eldorado with wild On the following pages, we will present Bodø and surroundings countryside and a range of famous national parks. Here, you can as a destination like no other, and we are more than happy immerse yourself in magnificent natural surroundings without to discuss any questions, such as possible guest events and having to stand in line. -
Mineral Resource Information in Support of National, Regional and Local Planning
Mineral Resource Information in Support of National, Regional and Local Planning Suffolk Commissioned Report CR/03/076N BRITISH GEOLOGICAL SURVEY COMMISSIONED REPORT CR/03/076N Mineral Resource Information in Support of National, Regional and Local Planning Suffolk D J Harrison, P J Henney, S J Mathers, D G Cameron, N A Spencer, S F Hobbs, D J Evans, G K Lott and D E Highley The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/1999 Key words Suffolk, mineral resources, mineral planning. Front cover Front cover photo: Coastal scenery at Minsmere RSPB reserve, north of Sizewell, Suffolk. Bibliographical reference D J Harrison, P J Henney, D G Cameron, Mathers S J, N A Spencer, S F Hobbs, D J Evans, G K Lott and D E Highley. 2003. Mineral Resource Information in Support of National, Regional and Local Planning. Suffolk. British Geological Survey Commissioned Report, CR/03/076N. Keyworth, Nottingham British Geological Survey 2003 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS Keyworth, Nottingham NG12 5GG Sales Desks at Nottingham and Edinburgh; see contact details 0115-936 3241 Fax 0115-936 3488 below or shop online at www.thebgs.co.uk e-mail: [email protected] The London Information Office maintains a reference collection www.bgs.ac.uk of BGS publications including maps for consultation. Shop online at: www.thebgs.co.uk The Survey publishes an annual catalogue of its maps and other publications; this catalogue is available from any of the BGS Sales Murchison House, West Mains Road, Edinburgh EH9 3LA Desks. -
Camp Cruising
The AshBreezeJournal of the Traditional Small Craft Association Camp Cruising IN THIS ISSUE Youth and Boat Building Making Boat Kits What We Missed VOLUME 41, Number 3 • Fall 2020 • $4.00 The Ash Breeze President’s The Ash Breeze (ISSN 1554-5016) is the quarterly journal of the Traditional Message Small Craft Association, Inc. It is published at Mariner Media, Inc., 131 West 21st Street, Buena Vista, VA David Wyman 24416. Communications concerning Photo by Rosemary Wyman membership or mailings should be addressed to: PO Box 183, West I have been fortunate to have spent much of my life in and Mystic, CT 06388. www.tsca.net around boats of all types and sizes. That said, small traditional Volume 41, Number 3 boats continue to be my passion. I love designing, building, and using small boats and helping others to do the same. Some of Editor: you know me from my involvement in the Downeast Chapter’s Andy Wolfe Small Reach Regatta or from the articles I have written for The [email protected] Ash Breeze. My greatest joy is heading out on the water for an Editors Emeriti: hour, a day, or a multiday adventure either alone or with friends, Richard S. Kolin many of whom I have gotten to know through the TSCA. Sam & Marty King I have given a lot of thought about what I could do to David & Katherine Cockey further our association during my year as president. The word Ralph Notaristefano and concept of communication has come to the forefront. Ken Steinmetz At present, our main form of communication is our wonder John Stratton journal, The Ash Breeze, a Facebook Group with over 4,300 Dan Drath members, and a well-designed website. -
A Maritime Resource Survey for Washington’S Saltwater Shores
A MAritiMe resource survey For Washington’s Saltwater Shores Washington Department of archaeology & historic preservation This Maritime Resource Survey has been financed in part with Federal funds from the National Park Service, Department of the Interior administered by the Department of Archaeology and Historic Preservation (DAHP) and the State of Washington. However, the contents and opinions do not necessarily reflect the views or policies of the Department of the Interior, DAHP, the State of Washington nor does the mention of trade names or commercial products constitute endorsement or recommendation by the Department of the Interior or DAHP. This program received Federal funds from the National Park Service. Regulations of the U.S. Department of Interior strictly prohibit unlawful discrimination in departmental Federally Assisted Programs on the basis of race, color, national origin, age, or handicap. Any person who believes he or she has been discriminated against in any program, activity, or facility operated by a recipient of Federal assistance should write to: Director, Equal Opportunity Program, U.S. Department of the Interior, National Park Service, 1849 C Street, NW, Washington, D.C. 20240. publishing Data this report commissioned by the Washington state Department of archaeology and historic preservation through funding from a preserve america grant and prepared by artifacts consulting, inc. DAHP grant no. FY11-PA-MARITIME-02 CFDa no. 15-904 cover image Data image courtesy of Washington state archives Washington state Department of archaeology and historic preservation suite 106 1063 south capitol Way olympia, Wa 98501 published June 27, 2011 A MAritiMe resource survey For Washington’s Saltwater Shores 3 contributors the authors of this report wish to extend our deep gratitude to the many indi- viduals, institutions and groups that made this report possible. -
Pliocene Dinoflagellate Cyst Stratigraphy, Palaeoecology And
Geol. Mag.: page 1 of 21. c 2008 Cambridge University Press 1 doi:10.1017/S0016756808005438 Pliocene dinoflagellate cyst stratigraphy, palaeoecology and sequence stratigraphy of the Tunnel-Canal Dock, Belgium STIJN DE SCHEPPER∗,MARTINJ.HEAD† & STEPHEN LOUWYE‡ ∗Cambridge Quaternary, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK †Department of Earth Sciences, Brock University, 500 Glenridge Avenue, St. Catharines, Ontario L2S 3A1, Canada ‡Palaeontology Research Unit, Ghent University, Krijgslaan 281 – S8, B-9000 Gent, Belgium (Received 21 November 2007; accepted 8 April 2008) Abstract – Dinoflagellate cysts and sequence stratigraphy are used to date accurately the Tunnel-Canal Dock section, which contains the most complete record of marine Pliocene deposits in the Antwerp harbour area. The Zanclean Kattendijk Formation was deposited between 5.0 and 4.4 Ma during warm- temperate conditions on a shelf influenced by open-marine waters. The overlying Lillo Formation is divided into four members. The lowest is the Luchtbal Sands Member, estimated to have been deposited between 3.71 and 3.21 Ma, under cooler conditions but with an open-water influence. The Oorderen Sands, Kruisschans Sands and Merksem Sands members of the Lillo Formation are considered a single depositional sequence, and biostratigraphically dated between 3.71 and c. 2.6 Ma, with the Oorderen Sands Member no younger than 2.72–2.74 Ma. Warm-temperate conditions had returned, but a cooling event is noted within the Oorderen Sands Member. Shoaling of the depositional environment is also evidenced, with the transgressive Oorderen Sands Member passing upwards into (near-)coastal high- stand deposits of the Kruisschans Sands and Merksem Sands members, as accommodation space decreased. -
English Nature Research Report
Yatural Area: 23. Lincolnshire Marsh and Geological Significance: Notable Coast (provisional) General geological character: The solid geology of the Lincolnshire Marsh and Coast Natural Area is bminated by Cretaceous chalk (approximately 97-83 Ma) although the later Quaternary deposits (the last 2 Ma) give thc area its overall. charactcr. 'The chalk is only well exposed on thc south bank of the Humber, where quarries and cuttings providc exposures of the Upper Cretaceous Chalk. 'me chalk is a very pure limestone deposited on the floor of a tropical sea. During Quaternary timcs, the area was glaciated on several occasions and as a result the area is covered by a variety of glacial deposits, representing an unknown number of glacial ('lcc Age') and interglacial phases. rhe glacial deposits consist mainly of sands, gravels and clays in variable thicknesses. These are derived primarily from the erosion of surrounding bedrock and therefore tend to have similar lithological characteristics, usually with a high chalk content. The glacial deposits are particularly important because of the controversy surrounding their correlation with the timing and sequence in other parts of England, especially East Anglia. The Quaternary deposits are well exposed in coastal cliffs of the area. Key geological features: Coastal cliffs consisting of glacial sands, gravels and clays Exposures of Cretaceous chalk Number of GCR sites: Oxfordian: 1 Kimmeridgian: I Aptian-Rlbian: i Quaternary of Eastern England: 1 ~ ~ ~ ~ ~ ~~~ ~ ~ ~~ GeologicaVgeomorphological SSSI coverage: 'here are 2 (P)SSSIs in the Natural Area covering 4 GCR SlLs which represent 4 different GCR networks. The site coverage includes South Ferriby Chalk Pit SSSI which contains an important Upper Jurassic succession, overlain by Cretaceous deposits. -
Íítefuid*/;Or. Ríe %Urna,Mrn'
No. 28605-A Gaceta Oficial Digital, miércoles 05 de septiembre de 2018 1 ÍÍtefuid*/;or. rÍe %urna,mrn'. Ministerio de Economia y Finanzas Dirección General de lngresos Despacho del Director RESOLUC¡Ótrl trlo. 201 -5734 De 29 de agosto de 2018 "Por la cual se publica la lista de personas jurídicas con una morosidad de tres (3) años consecutivos del tributo de Tasa Unica, en cumplimiento de los parágrafos 2, 3 y 4 del ar1ículo 318-A del Código Fiscal, reformado por Ia Ley No.6 de 2 de febrero de 2005, Ley 49 de 17 de septiembre de 2009 y Ley 52 de 27 de octubre de 2016" EL D¡RECTOR GENERAL DE INGRESOS, ENCARGADO CONSIDERANDO: Que el Decreto de Gabinete No. 109 de 7 de mayo de 1970 y sus modificaciones establece en sus aftículos 5 y 6, que el Director Generalde lngresos es responsable por la permanente adecuación y perfeccionamiento de los procedimientos administrativos y lo facultan para regular las relaciones formales de los contribuyentes con el Fisco, en aras de mejorar el servicio y facilitar a los contribuyentes el cumplimiento de las obligaciones tributarias. Que el artículo 318-A del Código Fiscal, modificado por la Ley No. 6 de 2 de febrero de 2005, Ley No. 49 de 17 de septiembre de 2009 y Ley No. 52 de 27 de octubre de 2016, establece el pago del tributo denominado tasa única por las sociedades anónimas, sociedades de responsabilidad limitada y cualesquiera otras personas jurídicas al momento de su insóripción y en los años subsiguientes para mantener plena vigencia.