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WITHIN and WITHOUT the ARCTIC CIRCLE. by N. E. Odell
Within and Without the Arctic Circle. 27 WITHIN AND WITHOUT THE ARCTIC CIRCLE. BY N. E. ODELL. (The substance of parts of this paper was read before the Alpine Club, February 7, 1933.) URING the past twelve years, often with geological exploration and research as the chief end in view, it bas been my good fortune to visit some of the remoter moun tains that either lie proximate to that romantic parallel of latitude the Arctic Circle, or are situated well N. of it. Many of these mountain ranges differ much one from another on · account of widely varying climate and precipitation, apart from altitude, and their unfrequented if not unexplored character in many cases makes them formidable as well as strenuous propositions. Indeed, without qualm of exaggeration, the writer can say that in his experience the type of mountaineering involved in these expeditions is of an order of exaction usually much in excess of the average biggish Alpine excursion. In spite of the quite moderate altitude, often, of these Arctic and Subarctic ranges, the methods of approach, the long line of camps, and the heavy porterage necessary, apart from climatic conditions, place them more in a Himalayan category, and nowhere is this resemblance borne in on one so forcibly as amongst the giant glaciers of Greenland, or even of Spitsbergen. In the following account it is my purpose to give an outline of impressions and experiences, on two recent summer expeditions to the mountains of North-east Labrador, and those of North east Greenland, including an ascent of Beerenberg in the island of Jan Mayen. -
The Hitch-Hiker Is Intended to Provide Information Which Beginning Adult Readers Can Read and Understand
CONTENTS: Foreword Acknowledgements Chapter 1: The Southwestern Corner Chapter 2: The Great Northern Peninsula Chapter 3: Labrador Chapter 4: Deer Lake to Bishop's Falls Chapter 5: Botwood to Twillingate Chapter 6: Glenwood to Gambo Chapter 7: Glovertown to Bonavista Chapter 8: The South Coast Chapter 9: Goobies to Cape St. Mary's to Whitbourne Chapter 10: Trinity-Conception Chapter 11: St. John's and the Eastern Avalon FOREWORD This book was written to give students a closer look at Newfoundland and Labrador. Learning about our own part of the earth can help us get a better understanding of the world at large. Much of the information now available about our province is aimed at young readers and people with at least a high school education. The Hitch-Hiker is intended to provide information which beginning adult readers can read and understand. This work has a special feature we hope readers will appreciate and enjoy. Many of the places written about in this book are seen through the eyes of an adult learner and other fictional characters. These characters were created to help add a touch of reality to the printed page. We hope the characters and the things they learn and talk about also give the reader a better understanding of our province. Above all, we hope this book challenges your curiosity and encourages you to search for more information about our land. Don McDonald Director of Programs and Services Newfoundland and Labrador Literacy Development Council ACKNOWLEDGMENTS I wish to thank the many people who so kindly and eagerly helped me during the production of this book. -
Environmental Statement for the Bacchus Development
APACHE NORTH SEA LIMITED Bacchus Production Increase Environmental Statement BEIS Project Reference: D/4256/2020 July 2020 Environmental Statement Apache North Sea Limited Bacchus Production Increase July 2020 This page is intentionally blank Environmental Statement Apache North Sea Limited Bacchus Production Increase July 2020 STANDARD INFORMATION SHEET Project name Bacchus Production Increase Project reference D/4256/2020 number Type of project Production increase Undertaker name Apache North Sea Limited Undertaker address Caledonia House Prime Four Business Park Kingswells Causeway, Aberdeen AB15 8PU Short description The assessment of the environmental impacts from an increase in production from the Bacchus Field in excess of 500 tonnes of oil per day over the current consent threshold, and the drilling of a new infill well. Dates Anticipated Q4 2020 commencement of works Date and reference D/4066/2009; December 2009 number of any earlier Statement related to this project Significant None environmental impacts identified Statement prepared Apache North Sea Limited by Hartley Anderson Limited Environmental Statement Apache North Sea Limited Bacchus Production Increase July 2020 This page is intentionally blank Environmental Statement Apache North Sea Limited Bacchus Production Increase July 2020 CONTENTS Glossary and Abbreviations ........................................................................................ i Non-Technical Summary ........................................................................................... -
Offshore Seabed Survey of Turbot Bank Possible MPA
JNCC/Cefas Partnership Report Series Report No. 20 Offshore seabed survey of Turbot Bank possible MPA Eggleton, J., Diesing, M. & Schinaia, S. July 2019 © JNCC, Cefas 2019 ISSN 2051-6711 Offshore seabed survey of Turbot Bank possible MPA Eggleton, J., Diesing, M. & Schinaia, S. Report completed 2013 and published July 2019 © JNCC, Cefas, 2019 ISSN 2051-6711 For further information, please contact: Joint Nature Conservation Committee Monkstone House City Road Peterborough PE1 1JY http://jncc.defra.gov.uk This report is compliant with the JNCC Evidence Quality Assurance Policy http://jncc.defra.gov.uk/default.aspx?page=6675 and has been reviewed by Cefas and JNCC prior to publication. This report should be cited as: Eggleton, J., Diesing, M. & Schinaia, S. 2019. Offshore seabed survey of Turbot Bank possible MPA. JNCC/Cefas Partnership Report No. 20. JNCC, Peterborough, ISSN 2051- 6711. Summary This report presents the findings from analyses of the acoustic data and groundtruth samples gathered during the seabed survey of the Turbot Bank possible Marine Protected Area (pMPA). Turbot Bank lies within a coarse sandy sediment plain to the east of Scotland, approximately 65km east of Peterhead on the Aberdeenshire coast, south of the Fladen Ground, and comprises a shelf bank and mound feature. The report describes the presence, location and extent of broadscale habitats, biotopes and Scottish Marine Protected Area (SMPA) Priority Marine Features within the Turbot Bank pMPA. Full coverage multibeam echosounder data (bathymetry and backscatter) collected under the Civil Hydrography Programme were available for the western half of Turbot Bank pMPA. During a dedicated survey in December 2012, new acoustic data were collected in the eastern part of the bank. -
Connectivity Among Marine Protected Areas, Particularly Valuable and Vulnerable Areas in the Greater North Sea and Celtic Seas Regions 2
Connectivity among marine protected areas, particularly valuable and vulnerable areas in the greater North Sea and Celtic Seas regions 2 Introduction to the connectivity study The NorthSEE project is focusing on transnational coordination between plans and planning processes in the North Sea Region on three main topics: Energy, Shipping and Environment. For the environmental strand the partners have been researching the designation of Marine Protected Areas (MPAs) and other marine conservation measures, as well as the application of the Ecosystem Based Approach (EBA) in the planning processes. This report is part of WP3 environment and deals with the connectivity of MPAs in the North Sea. The reasons for this is that the North Sea ecosystem is interlinked and does not respect land borders. In MSP, it is important to understand the way in which a marine conservation site is relevant to areas elsewhere, and what significance different sites may have for the ecosystem as a whole. Another incentive for analyzing the ecological coherence, is that the OSPAR Recommendation 2003/31, amended by OSPAR Recommendation 2010/2, on a network of Marine Protected Areas (MPAs) sets out the goal of OSPAR Contracting Parties (CPs) to continue the establishment of the OSPAR Network of MPAs in the North-East Atlantic. In the status report of 2016, OSPAR identified the need to using case-studies of connectivity to illustrate how the use of life-history traits information in combination with oceanographic modelling products can improve confidence in MPA network connectivity assessments. This study meets the need described by OSPAR. In order to have a better understanding of ecological relationships and conditions, the connectivity between all marine protected areas (MPAs) and particularly valuable and vulnerable areas (as part of the Norwegian Management Plans), have been analyzed. -
Cirques Have Growth Spurts During Deglacial and Interglacial Periods: Evidence from 10Be and 26Al Nuclide Inventories in the Central and Eastern Pyrenees Y
Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees Y. Crest, M Delmas, Regis Braucher, Y. Gunnell, M Calvet, A.S.T.E.R. Team To cite this version: Y. Crest, M Delmas, Regis Braucher, Y. Gunnell, M Calvet, et al.. Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees. Geomorphology, Elsevier, 2017, 278, pp.60 - 77. 10.1016/j.geomorph.2016.10.035. hal-01420871 HAL Id: hal-01420871 https://hal-amu.archives-ouvertes.fr/hal-01420871 Submitted on 21 Dec 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Geomorphology 278 (2017) 60–77 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees Y. Crest a,⁎,M.Delmasa,R.Braucherb, Y. Gunnell c,M.Calveta, ASTER Team b,1: a Univ Perpignan Via-Domitia, UMR 7194 CNRS Histoire Naturelle de l'Homme Préhistorique, 66860 Perpignan Cedex, France b Aix-Marseille Université, CNRS–IRD–Collège de France, UMR 34 CEREGE, Technopôle de l'Environnement Arbois–Méditerranée, BP80, 13545 Aix-en-Provence, France c Univ Lyon Lumière, Department of Geography, UMR 5600 CNRS Environnement Ville Société, 5 avenue Pierre Mendès-France, F-69676 Bron, France article info abstract Article history: Cirques are emblematic landforms of alpine landscapes. -
Rapid Lake Lodge ……… . Experience an Exceptional Moment with Nature
Rapid Lake Lodge ……… .www.rapidlake.com Experience an exceptional moment with nature Quebec et Labrador AIR SAFARI THROUGH THE HEARTH OF THE TORNGAT MOUNTAINS Departures on July 22, 2011 Small group 5-day/4-night trip From 1526 $ CAD (plus tax) Full board A trip exclusively designed for floatplane and helicopter pilots. Hebron Fjord Trip Description This safari by air incorporates the best of Torngat Mountains National Park into a 5-day tour covering more than 500 nautical miles, mixing exploration of natural wonders with discovery of arctic wildlife, from mountain flights to short exploratory hikes and fishing excursions to a variety of rivers. Just follow your guide and take full advantage of your stay. The ultimate experience of the arctic region! Your Itinerary Day 1: Arrival in Rapid Lake Upon arrival at Rapid Lake, the manager-owner and pilot- guide will welcome you with a cocktail, followed by registration, access permit submission to the Torngat Mountains National Park, and a presentation of your upcoming itinerary. In the afternoon, you are free to fish for brook trout, lake trout, landlocked salmon and Arctic char. Enjoy your catch of the day, smoked, BBQ or sushi style. Dinner and overnight stay at the Lodge. Day 2: Air Safari to the Land’s End (450 n. miles):Rapid Lake - Barnoin Camp - Bell Lake - Odell Lake - Miriam Lake - Kangalaksiorvik Lake - Barnoin Camp - Rapid Lake This air safari to the north-eastern tip of North America immerses you in the great open wilderness of Arctic Quebec and Labrador. Fly over gigantic icebergs and numerous fjords. -
Maps Radio Communication HF Radio Base Satellite Phone
Thank you for your interest in the exciting region of Arctic Quebec & Labrador. VNC Navigation charts Whether your visit takes you to Land's End, Labrador coast, or to the Kaumajet mountains you'll find world famous Radio Communication exhilaration. You'll enjoy an A HF (high frequency) radio or a satellite extraordinary mix of history, wide open phone should be considered as part of spaces, magnificent fjords and your aircraft equipment. Sometimes challenging mountain flying. you'll be more than 200 miles from the Rapid Lake Lodge promotes and nearest flight service station and only this protects the remarkable Torngat long-range communication system will Mountains Scenic Air Routes for air allow you to call for weather or to close travelers. your flight plan. We look forward to helping you to discover the Arctic Natural Wonders. HF Radio Base If you have an HF radio you can reach us Maps on the camp's frequency (3255) between: The Canadian VFR Navigation charts and 7:00 and 21:00 local time. Flight Supplements are available at the VIP store in Montreal 1-800-361-1696 Satellite Phone vippilot.com Let us know if you are planning to use a sat phone. We can schedule some calling hours that suit your needs. Weather Conditions The best weather conditions and mildest temperatures are found in July and August. (15°C / 55°F) -1- Beaching Last Fuel Stops M The recommended beaching spots along Schefferville is your last fuel stop before the Scenic Air Routes are generally made the next 228 –mile leg to Barnoin. -
Fault-Controlled Asymmetric Landscapes and Low-Relief Surfaces on Vestvågøya, Lofoten, North Norway: Inherited Mesozoic Rift-Margin Structures?
NORWEGIAN JOURNAL OF GEOLOGY Vol 98 Nr. 4 https://dx.doi.org/10.17850/njg98-3-06 Fault-controlled asymmetric landscapes and low-relief surfaces on Vestvågøya, Lofoten, North Norway: inherited Mesozoic rift-margin structures? Steffen G. Bergh1, Kristian H. Liland2, Geoffrey D. Corner1, Tormod Henningsen2 & Petter A. Lundekvam1 1Department of Geosciences, University of Tromsø UiT-The Arctic University of Norway, 9037 Tromsø, Norway. 2Equinor ASA, Harstad, Norway E-mail corresponding author (Steffen G. Bergh): [email protected] The Lofoten Ridge is an integral basement horst of the hyperextended continental rift-margin off northern Norway. It is a key area for studying onshore–offshore rift-related faults, and for evaluating tectonic control on landscape development along the North Atlantic margin. This paper combines onshore geomorphological relief/aspect data and fault/fracture analysis with offshore bathymetric and seismic data, to demonstrate linkage of landscapes and Mesozoic rift-margin structures. At Leknes on Vestvågøya, an erosional remnant of a down-faulted Caledonian thrust nappe (Leknes Group) is preserved in a complex surface depression that extends across the entire Lofoten Ridge. This depression is bounded by opposing asymmetric mountains comprising fault-bounded steep scarps and gently dipping, partly incised low- relief surfaces. Similar features and boundary faults of Palaeozoic–Mesozoic age are present on the offshore margin surrounding the Lofoten Ridge. The offshore margin is underlain by a crystalline, Permo–Triassic to Early Jurassic, peneplained basement surface that was successively truncated by normal faults, down-dropped and variably rotated into asymmetric fault blocks and basins in the Mesozoic, and the basins were subsequently filled by Late Jurassic to Early Cretaceous sedimentary strata. -
Grade 3 Social Studies Curriculum Guide (2011)
Social Studies Grade 3 Interim Edition Curriculum Guide 2011 TABLE OF CONTENTS Table of Contents Acknowledgements.......................................................................................................................... i Introduction. Background............................................................................................................................................................. 1 Aims.of.Social.Studies............................................................................................................................................. 1 Purpose.of.Curriculum.Guide.................................................................................................................................. 1 Guiding.Principles.................................................................................................................................................... 2 Program.Design.and.Outcomes. Overview................................................................................................................................................................. 3 Essential.Graduation.Learnings............................................................................................................................... 4 General.Curriculum.Outcomes............................................................................................................................... .6 Processes................................................................................................................................................................ -
Environment Baseline Report Scottish Sustainable Marine Environment Initiative
State of the Clyde Environment Baseline Report Scottish Sustainable Marine Environment Initiative SSMEI Clyde Pilot State of the Clyde Environment Baseline Report March 2009 D Ross K Thompson J E Donnelly Contents 1 INTRODUCTION............................................................................................................1 2 THE PHYSICAL ENVIRONMENT..............................................................................3 2.1 GEOLOGY....................................................................................................................3 2.2 THE SEALOCHS ...........................................................................................................6 2.3 THE ESTUARIES ..........................................................................................................9 2.4 THE INNER FIRTH......................................................................................................12 2.5 THE OUTER FIRTH ....................................................................................................14 2.6 COASTAL FLOODING .................................................................................................18 3 CLEAN AND SAFE SEAS............................................................................................19 3.1 THE CHEMICAL ENVIRONMENT ................................................................................19 3.1.1 Dissolved Oxygen.............................................................................................19 3.1.2 Nutrients...........................................................................................................22 -
The Deglaciation of Labrador-Ungava – an Outline J
Document généré le 2 oct. 2021 07:11 Cahiers de géographie du Québec The deglaciation of Labrador-Ungava – An outline J. D. Ives Mélanges géographiques canadiens offerts à Raoul Blanchard Volume 4, numéro 8, 1960 URI : https://id.erudit.org/iderudit/020222ar DOI : https://doi.org/10.7202/020222ar Aller au sommaire du numéro Éditeur(s) Département de géographie de l'Université Laval ISSN 0007-9766 (imprimé) 1708-8968 (numérique) Découvrir la revue Citer cet article Ives, J. D. (1960). The deglaciation of Labrador-Ungava – An outline. Cahiers de géographie du Québec, 4(8), 323–343. https://doi.org/10.7202/020222ar Tous droits réservés © Cahiers de géographie du Québec, 1960 Ce document est protégé par la loi sur le droit d’auteur. L’utilisation des services d’Érudit (y compris la reproduction) est assujettie à sa politique d’utilisation que vous pouvez consulter en ligne. https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Cet article est diffusé et préservé par Érudit. Érudit est un consortium interuniversitaire sans but lucratif composé de l’Université de Montréal, l’Université Laval et l’Université du Québec à Montréal. Il a pour mission la promotion et la valorisation de la recherche. https://www.erudit.org/fr/ THE DEGLACIATION OF LABRADOR-UNGAVA — AN OUTLINE* W J. D. IVES Field Director, McGill Sub-Arctic Research Laboratory, Schefferville, P.Q. Since the days of the Canadian Government geologrst, A. P. Low, towards the close of the Iast century, the great peninsula of Labrador-Ungava has been recognised as a major centre of ice accumulation and dispersai, and as one of the final centres of wastage.