On the Submission of Nominal Catch Statistics by Member States Fishing in the North-West Atlantic
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CABOT's LANDFALL by C
_J_ CABOT'S LANDFALL By C. B. FERGUSSON HILE the profound importance and the far-reaching consequences of the discovery of N ortb America by John Cabot in 1497 have long been realized, and in W some measure recognized, his landfall in the New World still remains unmarked. T hat is actually so. But it in dicates neither a lack of interest in doing honour to a distin guished navigator for his outstanding services, nor a paucity of those who have urged the marking of his landfall or advanced claims with respect to its site. His name and his fame are per petuated by Cabot Strait, which separates Cape Breton I sland :..... r- from Newfoundland, by the Cabot Trail, with its unsurt>assed :., , scenic splendour, in Cape Breton Island, and by Cabot 'l'ower on Signal Hill, at St. John's in Newfoundland. It is very fitting that Cabot's a.ctivities should be so com memorated in both Cape Breton Island and Newfoundland, for his voyages had great significance for each. Yet these me morials, through their different locations, may also indicate the crux of the Cabotian controversy: there is still a lack of un animity with respect to the site of Cabot's landfall in 1497. There are some who would claim it for Cape Breton Island, as well as others who would attribute it to Newfoundland or Labra dor. And now that Newfoundland is a part of the Canadian nation, these rival claims have been revived, the evidence has been re-considered and re-sifted, and, if it is now possible, a decision should be reached on this matter. -
An Eastern Micmac Domain of Islands
An Eastern Micmac Domain of Islands CHARLES A. MARTIJN Ministere des Affaires cullurelles, Quebec Introduction The Micmac Indians of Eastern Canada inhabit a region that borders the lower half of the Gulf of St. Lawrence.1 Their homeland includes portions of the Gaspe Peninsula and New Brunswick, all of Prince Edward Island and mainland Nova Scotia, as well as Cape Breton and parts of southern Newfoundland. Although the boundaries of this traditional territory cannot be determined with any precision because of fluctuations through time, it may have covered as much as 121,760 square kilometres, or about the size of Tunisia. An overview of Micmac culture and society is provided by Hoffman (1955), Nietfeld (1981), Passchier (1985) and Wallis and Wallis (1955). An extensive coastline permitted easy access to aquatic fauna — sea- mammals, fish, waterfowl and invertebrates — which are abundant in the gulf of St. Lawrence area. As a result, the Micmac were probably the most maritime-adapted of all Algonquian groups. Nevertheless, for survival dur ing the winter months they had to depend to a much greater extent on land animals such as moose, caribou, deer and beaver. Some scholars have depicted them as spending up to 10 months of the year obtaining 90% of their food requirements from coastal zones and the sea (Hoffman 1955:230- 236; Nietfeld 1981:360-363). Recent reviews of archaeological and ethno historical data, however, indicate a greater use of terrestrial fauna than has hitherto been acknowledged, and point to the need for a more intensive consideration of regional variation in available resources and subsistence strategies (Nash and Miller 1987; see also Burley 1981 and Clermont 1986). -
Geophysical Modeling in the Cabot Strait - St
GEOPHYSICAL MODELING IN THE CABOT STRAIT - ST. GEORGE’S BAY AREA BETWEEN CAPE BRETON ISLAND AND SOUTHWESTERN NEWFOUNDLAND, CANADA By Louis Zsámboki Honours B. Sc. (Earth Sciences), McMaster University Hamilton, Ontario 2009 Thesis submitted in partial fulfillment of the requirements for the Degree of Master of Science (Geology) Acadia University Fall Graduation 2012 © by Louis Zsámboki, 2012 This thesis by Louis Zsámboki was defended successfully in an oral examination on September 6th, 2012. The examining committee for the thesis was: __________________________________ Dr. Kirk Hillier, Chair __________________________________ Dr. Fraser Keppie, External Reader __________________________________ Dr. Robert P. Raeside, Internal Reader __________________________________ Dr. Sandra M. Barr, Supervisor __________________________________ Dr. Sonya A. Dehler, Supervisor __________________________________ Dr. Ian S. Spooner, (Acting) Head of Department This thesis is accepted in its present form by the Division of Research and Graduate Studies as satisfying the thesis requirements for the degree of Master of Science (Geology). ……………......................…………………. iii I, Louis Zsámboki, grant permission to the University Librarian at Acadia University to reproduce, loan or distribute copies of my thesis in microform, paper or electronic formats on a non-profit basis. I, however, retain the copyright in my thesis. ______________________________________ Author ______________________________________ Supervisor ______________________________________ -
Historical and Descriptive Account of the Island Of
: EISTORICAL AND DES< l.'l I Tl \ K \MHI M (II Mil ISLAND OK CAPE BRETON AND OF ITS MEMORIALS OF THE FRENCH REGIME: WITH BIBLIOGRAPHU HISTORICAL, \NI» CRITICAL NOTES By J. C MOUUINOT, C.M.G., LL.D., D.C.L., PRESIDENT OF THE ROYAL 80C1ETJ OF CANADA, MEMBER OF THE COUNCIL OF THE AMERICAN HISTOl ASSOCIATION, ETC.; AUTHOB OF " PARLIAMENTARY PBOCEDDRE in CANADA," " MANUAL OF THE CONSTITUTIONAL HIBTOR1 OF CANADA," "FEDERAL GOVERNMENT IN CANADA," (JOHNS HOPKINS UNrVBRSITi si 8), ETC MONTEEAL W. FOSTEE BROWX & CO., ST. JAMES STEEET 1892 3 CAPE BRETON AND ITS MEiMORfAL PREFATORY NOTE. Since the beginning of the present centnry Cape Breton, once known as He Royale, h been to the world ai large very little more than a mere raphical expression, and the importance which it possessed in the times when England and Prance were struggling for the supremacy in North America has been long since forgotten ox. :ep1 by the Btndei of history. In the present work it is the object of the writer, a native of I Breton, to record briefly the main facts in its history from the days of its discovery by European voyagers in the remote past down to the present time, when a stream of travel is already beginning to find its way to an island abounding with so many features of natural and historic interest. In the narrative of the days of the French regime, especially from 17 1" to IT'S, stress has been naturally laid on the important position lie Koyale once held with relation to New Prance and the old Thirteen Colonies. -
Although It Relegates Geography to a Secondary Status, Nova Scotia
I 16 CHAPTER ill GEOGRAPHY I I. Introduction I I 42. Although it relegatesgeographyto a secondary status,Nova Scotia neverthelessrelieson a I particularview of geographyto support its argument.However,that view isnotonethat can be justified either as a matter offact or law. I 43. In its Memorial,NewfoundlandandLabrador identifiedthe geographicalconfigurationofthe I area interms of, first, a portion ofthe eastern Gulfof St. Lawrence, second, outsidethe Gulf I in terms of an innerconcavityframedbythe south coast ofNewfoundlandfrom CapeRayto I the Burin Peninsula,and the coast ofN ova ScotiafromMoneyPoint to ScatarieIslandand, third, an outer open area of which the south coast of Newfoundland from the Burin I Peninsula to Cape Race and the Nova Scotia coast from Scatarie Island to Cape Canso, I formed the wings.45Figure 1. I 44. The inner concavityand the outer area constitute essentiallythe delimitationarea beforethe I Court of Arbitration in Canada v. France. The Court of Arbitration describedthe area in general terms as "south of the Canadian island of Newfoundland and east of the Canadian I islandof Cape Breton andthe coast of mainlandNova Scotia.,,46Ingivingmore precisionto I the coasts withinthat area, it identifiedthe relevantNewfoundlandcoasts as lyingbetween Cape Race to the east and Cape Ray to the west. It definedthe relevantNova Scotia coasts I as extending from the "north-eastern point of Cape Breton Island" to a PQintalong the I mainland coast of Nova Scotia 70 nm southwest of Scatarie Island. These coasts were measured according to lines of general direction based on the geographical framework I developed and presented by Canada. The Court of Arbitrationthen went on to describethe I I I 45Memorial of Newfoundland and Labrador, Phase Two, pp. -
Connecting Cape Breton Island and Newfoundland, Canada Geophysical Modeling of Pre-Carboniferous ‘Basement’ Rocks in the Cabot Strait Area Sandra M
Document generated on 09/24/2021 5:32 p.m. Geoscience Canada Journal of the Geological Association of Canada Journal de l’Association Géologique du Canada Connecting Cape Breton Island and Newfoundland, Canada Geophysical Modeling of pre-Carboniferous ‘Basement’ Rocks in the Cabot Strait Area Sandra M. Barr, Sonya A. Dehler and Louis Zsámboki Volume 41, Number 2, 2014 Article abstract Magnetic and gravity data from northeastern Cape Breton Island, URI: https://id.erudit.org/iderudit/1025341ar southwestern Newfoundland, and the intervening Cabot Strait area were compiled and used to generate a series of maps displaying magnetic (filtered See table of contents total field, first and second derivative) and gravity (Bouguer anomaly onshore, free-air anomaly offshore) information to enhance the anomaly pattern associated with regional geology. With further constraints from previously Publisher(s) published seismic reflection interpretations and detailed maps of onshore geology, five two-dimensional subsurface models were generated. Potential The Geological Association of Canada field anomalies in the offshore can be correlated with onshore faults, rock units, and pre-Carboniferous terranes. In Newfoundland, the Cabot – Long ISSN Range Fault separates Grenvillian basement to the northwest from peri-Gondwanan Port aux Basques subzone basement in the southeast and can 0315-0941 (print) be traced to the Wilkie Brook Fault on Cape Breton Island. The Cape Ray 1911-4850 (digital) Fault/Red Indian Line merges offshore with the Cabot – Long Range Fault so that Notre Dame subzone rocks do not extend across the Cabot Strait area. The Explore this journal Port aux Basques – Exploits subzone boundary crosses the strait but is likely buried by younger rocks onshore in Cape Breton Island. -
Fisheries Research Board of Canada
FISHERIES RESEARCH BOARD OF CANADA 614 Incidence of Ice and Icebergs in the Entrances to the Gulf of St. Lawrence and along the South Coast of ewfound1and W. B. Bailey a d L. M. Lauder INCIDENCE OF ICE AND ICEBERGS IN THE ENTRANCES TO THE GULF OF ST. LAWRENqE AND ALONG THE SOUTH COAST OF NEWFOUNDLAND by W. B. Bailey and L. M. Lauzier Map of the Eastern Gulf of St. Lawrence and approaches. Incidence of Ice and Icebergs in the Entrances to the Gulf of St. Lawrence and along the South by W. B. Bailey and L. M. Lauzier The presence of drift ice in shipping lanes creates a very serious navigational hazard. This is particularly true in narrow straits where the ice tends to be jammed by strong Because of this jarnmin~ in the straits, navigation is usually restricted for some time after the inner waters have Observations of the ice distribution have been made along the coasts by lighthouse keepers, and offshore by aerial reconnaissance and shipboard observations in an attempt to keep navigators suitably informed of the ice hazards. attempt is made herein to bring together information available for the Strait of Belle Isle, Cabot Strait and the south coast of Newfoundland. '!he descriptive information is in many in- stances quoted from the work cited whereas reports of sightings have been summarized or presented in tabular form. The informa- tion pertaining to currents or general circulation, average ice conditions, and in some cases, ice condi tions in recent years, is grouped under such headings. STRAIT OF BELLE ISLE I. -
Geophysical Modeling in the Cabot Strait - St
Atlantic Geology . Volume 48 . 2012 53 maps of the study area were generated using UNIX-based GMT software. The magnetic and gravity data were further enhanced using 1st and 2nd vertical derivatives, high pass – low pass filters, and horizontal and vertical gradients. The best results are produced by the 1st and 2nd vertical derivatives of magnetic data, as the first vertical derivative allows for sharper resolution of near-surface features, and the 2nd vertical derivative enhances local anomalies otherwise obscured by regional trends and helps with edge detection of source bodies. Based on the compiled maps and further constrained by seismic interpretations, 2D subsurface modeling is in progress with GM-SYS 4.2 2D modeling software; three models extend across the Cabot Strait, two models cover an enigmatic circular magnetic anomaly located 25 km offshore from Ingonish in eastern Cape Breton Island, and one model is in St. George’s Bay in Newfoundland. The 1st vertical derivative of the magnetic data show a linear magnetic high associated with Ordovician to Silurian Geophysical modeling in the Cabot Strait - St. Georges metasedimentary and metavolcanic rocks of the Money Bay area between Cape Breton Island and western Point and Cape North groups extending offshore to St. Paul Newfoundland, Canada Island. The Money Point Group also extends across the L. Zsamboki1, S.M. Barr1, and S.A. Dehler2 Cabot Strait to the Port aux Basques area of southwestern Newfoundland. The 2nd vertical derivative map reveals 1. Department of Earth and Environmental Science, Acadia that the offshore Ingonish magnetic anomaly is composite University, Wolfville, Nova Scotia B4P 2R6, Canada <108581z@ and some components may link to units inshore. -
Basement and Cover Rocks at Cape North, Cape Breton Island, Nova Scotia E
Document generated on 09/24/2021 2:02 p.m. Atlantic Geology Basement and Cover Rocks at Cape North, Cape Breton Island, Nova Scotia E. R. W. Neale and M. J. Kennedy Volume 11, Number 1, April 1975 URI: https://id.erudit.org/iderudit/ageo11_1rep01 See table of contents Publisher(s) Maritime Sediments Editorial Board ISSN 0843-5561 (print) 1718-7885 (digital) Explore this journal Cite this article Neale, E. R. W. & Kennedy, M. J. (1975). Basement and Cover Rocks at Cape North, Cape Breton Island, Nova Scotia. Atlantic Geology, 11(1), 1–4. All rights reserved © Maritime Sediments, 1975 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/ Reports Basement and Cover Rocks at Cape North, Cape Breton Island, Nova Scotia E.R.W. NEALE Department of Geology, Memorial University of Newfoundland, St. John's, Newfoundland M.J. KENNEDY Department of Geology, Memorial University of Newfoundland, St. John's, Newfoundland Introduction Geological Setting Recent field studies by Wiebe (1972) and iso- Wiebe's (1972) study of the pre-Carboniferous topic dating by Cormier (19 72) suggests that the pre- rocks, particularly in the Ingonish and Black Brook Mississipian history of northern Cape Breton Island regions (Fig. -
Map of Mi'kma'ki
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/322197301 VISIT VINLAND - Developing a New and Innovative Tourism Product in Atlantic Canada by Deciphering Ancient Icelandic Sagas Thesis · July 2016 DOI: 10.13140/RG.2.2.20383.87203 CITATIONS READS 0 878 1 author: Sveinn Traustason Høgskulen på Vestlandet 1 PUBLICATION 0 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Visit Vinland - Tourism Development in Atlantic Canada View project Visit Vinland - Tourism Development in Atlantic Canada View project All content following this page was uploaded by Sveinn Traustason on 02 January 2018. The user has requested enhancement of the downloaded file. Visit Vinland Developing a New and Innovative Tourism Product in Atlantic Canada by Deciphering Ancient Icelandic Sagas Master Thesis submitted in fulfillment of the Degree Master of Business Administration in Tourism and Hotel Development Submitted to Dr. Helmut Zolles Sveinn Rúnar Traustason 1302003 Sogndal, Norway May 29, 2017 1 AFFIDAVIT I hereby affirm that this Master’s Thesis represents my own written work and that I have used no sources and aids other than those indicated. All passages quoted from publications or paraphrased from these sources are properly cited and attributed. The thesis was not submitted in the same or in a substantially similar version, not even partially, to another examination board and was not published elsewhere. Date Signature ABSTRACT Visit Vinland is a name invented for the purpose of this thesis for a new proposed association aimed at developing and marketing Atlantic Canada to Nordic people, people of Nordic descent and anyone interested in Viking explorations and the Vinland Sagas. -
Section 4.0 To
EMERA NEWFOUNDLAND AND LABRADOR MARITIME LINK ENVIRONMENTAL ASSESSMENT REPORT 4.0 ENVIRONMENTAL SETTING This section describes the environmental setting for the Project in each of the jurisdictions – the island of Newfoundland, the Cabot Strait, and Nova Scotia. 4.1 ISLAND OF NEWFOUNDLAND Project components on the island of Newfoundland include an estimated 293 km of transmission line along new and existing transmission corridors between Granite Canal and Cape Ray. Associated infrastructure includes one switchyard; one converter station; one transition compound; one anchor site; up to an estimated 28 km of grounding line; and approximately 2 km of underground cable (refer also to Figure 1.2.2 and Section 2). 4.1.1 ATMOSPHERIC ENVIRONMENT This description of the atmospheric environment considers climate, ambient air quality, and ambient noise in the region of the Project components on the island of Newfoundland. 4.1.1.1 Climate The Study Area on the island of Newfoundland is entirely within the Boreal Shield Ecozone. In general, climate is characterized by long winters and short warm summers, modified by maritime conditions along the coast, thereby resulting in higher mean annual precipitation (900- 1600 mm) (Bell 2002a). The Project components are located within four ecoregions: Maritime Barrens, Central Newfoundland, Long Range Barrens, and Western Newfoundland (Figure 4.1.1). Climate in the Maritime Barrens Ecoregion is highly influenced by the Atlantic Ocean, characterized by foggy, cool summers with an average temperature of 11.5 °C, and moderate winters with an average temperature of -1 °C. Mean annual precipitation ranges from 1200 to >1600 mm. The Western Newfoundland Ecoregion also has a marine-influenced climate, experiencing cool summers with mean annual temperature of 12 °C and short, cold winters with mean annual temperature of -3.5 °C.