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Newsletter Varnish
The Cover The outlook's bleak for the future of passenger trains in Newfoundland, as our report on page 78 indicates. In a matter of months, buses will appear on the St. John's- Port aux Basques run, phasing out CN's narrow gauge newsletter varnish. Here's the easthound Caribou waiting for its westbound counterpart at Cooke siding in June, 1967. — Tom Henry Number 270 Published monthly by the Upper Canada Railway Society, Inc., Box 122, Terminal A, Toronto, Ont. James A. Brown, Editor Coming Events :.:.:.;-:.:.;.:.:.:.:.:.:.;.;.:.:.x-:.;'X-:':':-;-:-:'X-:w^^^^^ Regular meetings of the Society are held on the third Friday of Authorized as Second Class Matter by the Post Office Department, each month (except July and August) at 589 Mt. Pleasant Road, Ottawa, Ont. and for payment of postage in cash. Toronto, Ontario. 8.00 p.m. Members are asked to give the Society at least five weeks notice of address changes. Aug 16: Summer meeting and social night at 589 Mt. (Fri) Pleasant Road, featuring refreshments and pro• fessional films of rail interest. Sept 20: Regular Meeting. Please address NEWSLETTER contributions to the Editor at (Fri) 3 Bromley Crescent, Bramalea, Ontario. No responsibility is assumed for loss or nonreturn of material. All other Society business, including membership inquiries, should be addressed to UCRS, Box 122, Terminal A, Toronto, Ontario. Contributors: John Bromley, Reg Button, Tom Henry, Bill Hood, George Horner, Omer Lavallee, Boh McMann, Ernie Modler, Steve Munro, John Thompson, Ted Wickson. Production: John Bromley, Tom Henry, Omer Lavallee. Distribution: Chas. Bridges, George Meek, Bill Miller, Steve Munro, John Thompson, Ted Wickson. -
Regional Geology of the Scotian Basin
REGIONAL GEOLOGY OF THE SCOTIAN BASIN David E. Brown, CNSOPB, 2008 INTRODUCTION The Scotian Basin is a classic passive, mostly non-volcanic, conjugate margin. It represents over 250 million years of continuous sedimentation recording the region's dynamic geological history from the initial opening of the Atlantic Ocean to the recent post-glacial deposition. The basin is located on the northeastern flank of the Appalachian Orogen and covers an area of approximately 300,000 km2 with an estimated maximum sediment thickness of about 24 kilometers. The continental-size drainage system of the paleo-St. Lawrence River provided a continuous supply of sediments that accumulated in a number of complex, interconnected subbasins. The basin's stratigraphic succession contains early synrift continental, postrift carbonate margin, fluvial-deltaic-lacustrine, shallow marine and deepwater depositional systems. PRERIFT The Scotian Basin is located offshore Nova Scotia where it extends for 1200 km from the Yarmouth Arch / United States border in the southwest to the Avalon Uplift on the Grand Banks of Newfoundland in the northeast (Figure 1). With an average breadth of 250 km, the total area of the basin is approximately 300,000 km2. Half of the basin lies on the present-day continental shelf in water depths less than 200 m with the other half on the continental slope in water depths from 200 to >4000 m. The Scotian Basin formed on a passive continental margin that developed after North America rifted and separated from the African continent during the breakup of Pangea (Figure 2). Its tectonic elements consist of a series of platforms and depocentres separated by basement ridges and/or major basement faults. -
Canadian Rail No162 1965
<:;an..adi J~mnn Number 162 / Janua r y 1965 Cereal box coupons and soap package enclosures do not general ly excite much enthusiasm from the editor of 'Canadian Rail', but we must admit we are looking forward with some eagerness to comp leting our collection of RAILWAY MUGS currently being distribut e d by the Quaker Oats Company, in their specially-marked packages of Quaker Oats. This series of twelve hot chocolate mugs depicts the develop - ment of the steam locomotive in Canada from the 0-6-0 "Samson", to the CPR 2-10-4 #8000. The mugs are being offered by the Quaker Oats Company of Cana da to salute Canada's Centennial, and the part played by the rail ways and their steam locomotives in furthering the pro ~ ress of the nation. Each cup pictures an authentic locomotive design -- one shows a Canadian Northern 2-8-0, a type of locomotive that made a major contribution to the country's prairie economy by moving grain from the Western provinces to the Lakehead -- another shows one of the Canadian Pacific's ubiquitous D-10 engines. There are 12 different locomotives in the series - each a col lector's item. The reproductions are precisely etched in decora tive colours and trimmed with 22k gold. Canadian Rail Par,e 3 &eee_eIPIrWB __waBS} -- E.L.Modler. Once a Ga in this year, the Canadian National Railways has leased a number of road switcher type diesels from the Duluth, Missabe and Iron Range Railroad. :,ihile last year all the uni ts leased from the D.I.L& I.R. -
Atlantic Geoscience Society Abstracts: 37Th Annual Colloquium & Annual General Meeting 2011
Document generated on 09/28/2021 10:41 a.m. Atlantic Geology Atlantic Geoscience Society Abstracts 37th Annual Colloquium & Annual General Meeting 2011 Volume 47, 2011 URI: https://id.erudit.org/iderudit/ageo47abs01 See table of contents Publisher(s) Atlantic Geoscience Society ISSN 0843-5561 (print) 1718-7885 (digital) Explore this journal Cite this document (2011). Atlantic Geoscience Society Abstracts: 37th Annual Colloquium & Annual General Meeting 2011. Atlantic Geology, 47, 9–53. All rights reserved © Atlantic Geology, 2011 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal. Its mission is to promote and disseminate research. https://www.erudit.org/en/ atlantic geology . volume 47 . 2011 9 Atlantic Geoscience Society ABSTRACTS 37th Annual Colloquium & Annual General Meeting 2011 Fredericton, new Brunswick The 2011 Colloquium & Annual General Meeting was held at the Fredericton Inn, Fredericton, New Brunswick, on February 11 and 12, 2011. On behalf of the society, we thank Colloquium Chairman Dave Keighley and his organizing committee (Kay Thorne, Dave Lentz, Joe MacIntosh, Chris McFarlane, Susan Johnson, Mike Parkhill, Elisabeth Kosters, Sherry McCoy, Grant Ferguson, Pierre Jutras, Rob Raeside, Brian Roulston, Cliff Shaw, and the student volunteers from the Department of Geology, University of New Bruns- wick) for providing an excellent meeting. We also wish to acknowledge support of the corporate sponsors: Potash Corp.(Potash Company of Saskatchewan); SWN Resources; Agilent Technologies; Resonetics; Asso- ciation of Professional Engineers and Geoscientists of New Brunswick; Geodex Minerals; Apache; Natural Resources Canada, Geological Survey of Canada (Atlantic); Cache Exploration; C.I.M. -
Country Note on Fisheries Management Systems -- Canada
COUNTRY NOTE ON FISHERIES MANAGEMENT SYSTEMS -- CANADA 1. Overview of Canadian Fisheries 1. Canada has traditionally benefited from the abundant fisheries resources in some of the world’s most productive marine and freshwater systems. These rich fisheries resources have maintained an important fishing industry that provides employment and supports the livelihood of hundreds of small communities in coastal areas. 2. In addition, there is a large recreational fisheries sector comprised of some 3.6 million anglers with annual expenditures of close to CAD 4.7 billion exclusively on sport fishing activities and investments. Furthermore, fishing has been entrenched in the daily life of Canadian aboriginal people in more than 300 First Nations who participate in fisheries for food, social and ceremonial purposes. 3. Aside from capture fisheries, aquaculture has been growing rapidly in Canada. In 1986, the total farm gate value of aquaculture was CAD 35 million. By 2000, production had increased to CAD 600 million, of which 81% was salmon. Trout, mussels and oysters are also major aquaculture species. 4. Canada’s commercial fisheries operate in three broad regions - along the Atlantic and Pacific coasts and inland (mainly near the Great Lakes and Lake Winnipeg). The last decade has seen major changes in the Canadian commercial fisheries on both coasts. The collapse of the Atlantic groundfishery in the early 1990s and the subsequent failure of Pacific salmon fishery in the mid-1990s -- the two traditional staple species in the Atlantic and Pacific fisheries respectively -- have completely changed the landscape of the Canadian fishing industry. 5. The rapid expansion of shrimp and crab fisheries along with continuing strong price performance for shellfish in general, have not only made shellfish the most dominant sector on the Atlantic coast but also brought the overall landed value past the historical record prior to the groundfish moratoria. -
New Orleans, LA USA
July 28-August 1, 2014 | New Orleans, LA USA CEER 2014 Conference on Ecological and Ecosystem Restoration ELEVATING THE SCIENCE AND PRACTICE OF RESTORATION A Collaborative Effort of NCER and SER July 28-August 1, 2014 New Orleans, Louisiana, USA www.conference.ifas.ufl.edu/CEER2014 Welcome to the UF/IFAS OCI App! The University of Florida IFAS Office of Conferences & Institutes is happy to present a mobile app for the Conference on Ecological and Ecosystem Restoration. To access the conference app, scan the QR Code or search “IFAS OCI” in the App Store or Google Play on your Apple or Android device. Log in with the email address you used to register, a social media account, or as a guest. You will be prompted to select an event – choose CEER 2014. The event password is eco14. The app allows you to build a personal conference agenda, stay updated with conference announcements, and connect with sponsors, exhibitors, and fellow attendees. Should you have any questions about the app, please stop by our registration desk for assistance. Stay connected! #CEER2014 July 28-August 1, 2014 | New Orleans, LA USA Table of Contents Welcome Letter ...................................................................................................... 3 In Honor of David Allen Vigh ................................................................................... 4 About CEER ............................................................................................................. 6 About the Society for Ecological Restoration ........................................................ -
Community Management in the Inshore Groundfish Fishery on the Canadian Scotian Shelf
101 Community management in the inshore groundfish fishery on the Canadian Scotian Shelf F.G. Peacock Fisheries and Oceans Canada, Maritimes Region PO Box 1035, Dartmouth Nova Scotia, B2Y 4T3 Canada [email protected] Christina Annand Fisheries and Oceans Canada, Maritimes Region PO Box 1035, Dartmouth Nova Scotia, B2Y 4T3 Canada [email protected] 1. HISTORY LEADING TO COMMUNITY MANAGEMENT The groundfish fishery in Atlantic Canada is arguably the most complex fishery in Canada. Groundfish is the generalized term for a number of species of fish, mostly gadoid that are harvested separately or collectively by many fleets involving thousands of fishermen throughout Atlantic Canada. This chapter will focus on the inshore, fixed-gear sector of relatively small, inshore vessels 10–14 metres in length. This sector uses handline, longline and gillnet gear to harvest groundfish along the Scotian Shelf, in the Bay of Fundy and on Georges Bank (see Figure 1). Groundfish fishing by this sector involves seven separate and distinct fleets harvesting mostly cod, haddock, pollock, flatfish, halibut, redfish and a variety of bycatch species. Following establishment of the 200-mile limit in 1977, Canada began to develop an extensive domestic groundfish fishery that utilized both inshore and offshore fixed and mobile gear. Harvest expansion in the 1980s was followed by significant declines in species populations and associated harvest levels. Harvest moratoria were implemented for several cod resources in Atlantic Canada FIGURE 1 during the early 1990s and several of these Scotian Shelf, Bay of Fundy, and Georges Bank fishing areas moratoria continue today. On the Scotian Shelf, these included haddock stocks and cods stocks in areas 4V and 4W. -
Whole-Rock Chemical and Nd Isotopic Composition of a Late Proterozoic
Document generated on 09/30/2021 5:59 a.m. Atlantic Geology Journal of the Atlantic Geoscience Society Revue de la Société Géoscientifique de l'Atlantique Whole-rock chemical and Nd isotopic composition of a Late Proterozoic metasedimentary sequence in Ganderia: Kellys Mountain, Bras d’Or terrane, Nova Scotia, Canada Sandra M. Barr, Christian Pin, David McMullin and Chris E White Volume 49, 2013 Article abstract The relationship between low-grade metasedimentary and high-grade URI: https://id.erudit.org/iderudit/1062307ar paragneissic Precambrian rock units in the Bras d’Or terrane of central Cape DOI: https://doi.org/10.4138/atlgeol.2013.002 Breton Island is a long-standing geological problem. Whole-rock geochemical and Nd isotopic data from representative components of these units in the See table of contents Kellys Mountain area, the Glen Tosh formation and Kellys Mountain Gneiss, show strong similarity. Major and trace element characteristics suggest that protolith sediments for both units were wackes derived from felsic igneous Publisher(s) sources and deposited at an active continental margin. Neodymium isotopic data in combination with previously published detrital zircon ages show that Atlantic Geoscience Society the sediments contained an ancient (ca. 2 Ga) end-member of recycled continental crust mixed with a juvenile component of Late Neoproterozoic age. ISSN The similarities suggest that the rocks represent the same sedimentary unit at different grades of metamorphism. 0843-5561 (print) 1718-7885 (digital) Explore this journal Cite this article Barr, S., Pin, C., McMullin, D. & White, C. (2013). Whole-rock chemical and Nd isotopic composition of a Late Proterozoic metasedimentary sequence in Ganderia: Kellys Mountain, Bras d’Or terrane, Nova Scotia, Canada. -
Acknowledgements
Acknowledgements I have been blessed by having such St. Peter’s Coastal Trail, and others, I wonderful assistance, cooperation, encountered people who recognized and encouragement on this book pro- me and my task. Every one of them ject from so many people. Whenever thanked me for my work; everyone I asked anyone for information, they encouraged me to continue. To all were prompt in their response. Any those I met, and to those whom I have time I had a question or concern, not but who have used my books, I someone provided an answer. I thank you. Knowing that my work spoke to dozens of people over vari- helps enable you to discover trails ous aspects of the trails; I hope you and more wonderful locations to hike will forgive that I do not list all your is what keeps me writing. names, for I fear that I would forget Finally, I would be remiss if I did someone. Thank you for helping me not acknowledge the debt I owe to make Hiking Trails of Cape Breton the the publisher, Goose Lane Editions. book it is. We have worked together now since Two individuals, however, deserve 1994, and although the process of special mention. Elaine Wallace at publishing a book, like any creative Cape Breton Highlands National Park process, can be tempestuous, we have chatted with me more than everyone done so together seven times now. I else combined and was a wealth of think they do a good job of it. I hope information. Tom Wilson, Director they think the same of me. -
Scotian Basin Exploration Drilling Project Environmental Assessment Report
Scotian Basin Exploration Drilling Project Environmental Assessment Report February 2018 Cover image courtesy of BP Canada Energy Group ULC. © Her Majesty the Queen in Right of Canada, represented by the Minister of the Environment (2017). Catalogue No: En106-203/2018E-PDF ISBN: 978-0-660-24432-7 This publication may be reproduced in whole or in part for non-commercial purposes, and in any format, without charge or further permission. Unless otherwise specified, you may not reproduce materials, in whole or in part, for the purpose of commercial redistribution without prior written permission from the Canadian Environmental Assessment Agency, Ottawa, Ontario K1A 0H3 or [email protected]. This document has been issued in French under the title: Rapport d'évaluation environnementale: Projet de forage exploratoire dans le bassin Scotian. Acknowledgement: This document includes figures, tables and excerpts from the Scotian Basin Exploration Drilling Project Environmental Impact Statement, prepared by Stantec Limited for BP Canada Energy Group ULC. These have been reproduced with the permission of both companies. Executive Summary BP Canada Energy Group ULC (the proponent) proposes to conduct an offshore exploration drilling program within its offshore Exploration Licences located in the Atlantic Ocean between 230 and 370 kilometres southeast of Halifax, Nova Scotia. The Scotian Basin Exploration Drilling Project (the Project) would consist of up to seven exploration wells drilled in the period from 2018 to 2022. The Project would occur over one or more drilling campaigns. The first phase, consisting of one or two wells, would be based on the results of BP Exploration (Canada) Limited’s Tangier 3D Seismic Survey conducted in 2014. -
Atlantic Geoscience Society Abstracts: 39Th Annual Colloquium & Annual General Meeting 2013
Document généré le 30 sept. 2021 14:51 Atlantic Geology Journal of the Atlantic Geoscience Society Revue de la Société Géoscientifique de l'Atlantique Atlantic Geoscience Society Abstracts: 39th Annual Colloquium & Annual General Meeting 2013 Volume 49, 2013 URI : https://id.erudit.org/iderudit/1062316ar DOI : https://doi.org/10.4138/20165 Aller au sommaire du numéro Éditeur(s) Atlantic Geoscience Society ISSN 0843-5561 (imprimé) 1718-7885 (numérique) Découvrir la revue Citer ce document (2013). Atlantic Geoscience Society Abstracts: 39th Annual Colloquium & Annual General Meeting 2013. Atlantic Geology, 49, 15–56. https://doi.org/10.4138/20165 All Rights Reserved ©, 2013 Atlantic Geology 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/ Atlantic Geoscience Society ABSTRACTS 39th Annual Colloquium & Annual General Meeting 2013 Dartmouth-Halifax, Nova Scotia The 2013 Colloquium & Annual General Meeting was held at the Holiday Inn, Dartmouth, Nova Scotia, on February 1 and 2, 2013. On behalf of the society, we thank Colloquium General Chair Bob Ryan, Technical Co- Chairs Elisabeth Kosters and Grant Wach, Nelly Koziel, and the numerous student volunteers for facilitating an excellent meeting. -
Maritime Sediments and Atlantic Geology
Maritime Sediments and Atlantic Geology V o l . 22 December, 1986 No. 3 Pre-Carbon Iferous TectonostratI graphic Subdivisions of Cape Breton Island, Nova Scotia Sandra M. Barr and Robert P. Raeslde Department of Geology, Acadia University Wolfvllle, Nova Scotia BOP 1X0 Cape Breton Island can be divided into four zones on the basis of contrasting stratigraphy, metamorphism, and plutonism. A Southeastern zone is characterized by late Precambrian volcanism and plutonism, followed by Cambro-Ordovician rift-basin sedimentation and minor volcanism. The Bras d'Or zone to the northwest is underlain by gneissic basement and overlying platformal (carbonate and clastic) sedimentary rocks, intruded by mainly late Precambrian and Qrdovician(?) granitoid rocks. The Highlands zone has a gneissic core flanked by typically lower grade sedimentary and volcanic rocks of probable Precambrian age intruded by diverse and abundant dioritic to granitic plutons ranging in age from Precambrian to Carboniferous. The Northwestern Highlands zone has gneissic basement intruded by varied plutonic rocks including anorthosite and syenite, the latter of Grenvillian age. The nature and significance of the boundaries between these zones are as yet uncertain, but only the Southeastern and Bras d'Or zones are considered to be part of the Avalon Terrane. Des contrastes de stratigraphie. mdtamorphisme et plutonisme permettent de diviser l'ile du Cap-Breton en quatre zones. Dn zone sud-est se distinque par un volcanisme et un plutonisme tardi-prAeambriens auxquels succAdent, au Cambro-Grdovicien, une sAdimentation bassinale de type rift et un faible volcanisme. Au Nord-Ouest, la zone de Bras d ’Or comporte un socle gneissique sur lequel s'est effectuAe une sAdimentation nAritique (terrigAne et A carbonates), le tout injectA de granitoides principalement tardi-prAcambriens et ordoviciens(?).