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Canada 21: Shepody Bay, New Brunswick
CANADA 21: SHEPODY BAY, NEW BRUNSWICK Information Sheet on Ramsar Wetlands Effective Date of Information: The information provided is taken from text supplied at the time of designation to the List of Wetlands of International Importance, May 1987 and updated by the Canadian Wildlife Service - Atlantic Region in October 2001. Reference: 21st Ramsar site designated in Canada. Name and Address of Compiler: Canadian Wildlife Service, Environment Canada, Box 6227, 17 Waterfowl Lane, Sackville, N.B, E4L 1G6. Date of Ramsar Designation: 27 May 1987. Geographical Coordinates: 45°47'N., 64°35'W. General Location: Shepody Bay is situated at the head of the Bay of Fundy, 50 km south of the City of Moncton, New Brunswick. Area: 12 200 ha. Wetland Type (Ramsar Classification System): Marine and coastal wetlands: Type A - marine waters; Type D - rocky marine shores and offshore islands; Type F - estuarine waters; Type G -intertidal mud, sand, and salt flats; Type H - intertidal marshes. Altitude: Range is from - 6 to 6 m. Overview (Principle Characteristics): The area consists of 7700 ha of open water, 4000 ha of mud flats, 800 ha of salt marsh and 100 ha of beach. Physical Features (Geology, Geomorphology, Hydrology, Soils, Water, Climate): The area is situated at the head of the Bay of Fundy, an area with the largest tidal range in the world (up to 14 m in Shepody Bay). Shepody Bay is a large tidal embayment surrounded by low, rolling upland. A narrow band of salt marsh occurs along the western shore, whereas the eastern side is characterised by a rocky, eroding coastline with sand- gravel beaches. -
An Organization of the Scientific Investigation of the Indian Place«Nomenclatiire of the Maritime Provinces of Canada by W
FROM THE TRANSACTIONS OF THE ROYAL SOCIETY OF CANADA THIRD SERIES—1914 VOLUME vin An Organization of the Scientific Investigation of the Indian Place«nomenclatiire of the Maritime Provinces of Canada by W. F. GANONG. M.AHBb.E OTTAWA PRINTED FOR THE ROYAL SOCIETY OF CANADA 19 14 Transactions of The Royal Society of Canada SECTION II SERIES III DECEMBER 1914 VOL. VIII An Organization of the Scientific Investigation of the Indian Place- nomenclature of the Maritime Provinces of Canada, (Fourth Paper). By W. F. GANONG, M.A., Ph.D. (Read by Title May 27, 1914.) This paper is identical in aim and method with its three pre decessors, which were published in the immediately foregoing volumes of these Transactions. In a word, I am trying to apply the principles of scientific analysis to a very interesting subject especially prone to doubt and error. The comparative method which I use, explained in the introduction to the first paper, is proving wonderfully successful in solving the problems, as this paper will further illustrate. For convenience of reference I may add that the former papers made analysis of the names Oromocto, Magaguadavic, Upsalquitch, Manan, Nepisiguit, Kouchibouguac, Anagance, Wagan, Pokiok, Penniac, Bocabec, Pentagoet-Penobscot, Pohenegamook, and Cobs- cook, and used the roots thus made available in the analysis of a good many other words, both existent and extinct, of lesser importance. Of these extinct Indian names,—indigenous to the country, ap propriate to the places, and often reducible to a highly pleasing form, —the greater number may be revived to obvious advantage when additional place-names become needed in future; and I have tried to suggest simplified and softened forms for such purpose. -
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A LATE MARITIME WOODLAND PESKOTOMUHKATI FISHERY FROM THE MAINLAND QUODDY REGION, SOUTHWESTERN NEW BRUNSWICK, CANADA by W. Jesse Webb B.A. (Hons.), Anthropology, 2009 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts in the Graduate Academic Unit of Anthropology Supervisors: Susan E. Blair, Ph.D, Anthropology, Chair Matthew W. Betts, Ph.D, Anthropology Examining Board: Darcy J. Dignam, M.A., Anthropology Richard A. Cunjak, Ph.D., Biology This thesis is accepted by the Dean of Graduate Studies THE UNIVERSITY OF NEW BRUNSWICK April 2018 © William Jesse Webb, 2018 ABSTRACT The nature of precontact Indigenous fisheries and their significance to subsistence economies, seasonal mobility, and diachronic cultural change remain underdeveloped in the archaeology of the Maritime Peninsula, northeastern North America. This thesis presents an analysis of a precontact fishery from BgDs-15, a small shell-bearing site located on the northern mainland of Passamaquoddy Bay, southwestern New Brunswick, Canada. Several hundred bones recovered during the 2004 field excavations and over 3,000 fish remains from midden column and bulk feature samples were examined. Most of these fish bones are attributable to Atlantic tomcod (Microgadus tomcod Walbaum, 1792) and unidentified, tomcod-sized gadids, with some herring (Clupeidae) present. Multiple lines of complementary evidence, including taxonomic composition, relative abundances, skeletal element frequency, seasonality, and the ethnohistoric record were examined to produce a high-resolution analysis of the BgDs-15 fishery and provide insight into ancestral Peskotomuhkati settlement-subsistence strategies during the Late Maritime Woodland period (ca. 1350–550 BP). ii ACKNOWLEDGMENTS The process of developing this thesis has, on the one hand, been the ideal of curiosity-driven academic research and, on the other, a Sisyphean personal struggle. -
EIA Final Report (PDF)
YB299A ENVIRONMENTAL IMPACT ASSESSMENT REPORT FOR MODIFICATIONS TO THE PETITCODIAC RIVER CAUSEWAY Submitted to: New Brunswick Department of Supply and Services Fredericton, New Brunswick Submitted by: AMEC Earth & Environmental, A Division of AMEC Americas Limited Fredericton, New Brunswick September 30, 2005 TE23520.4 NB Department of Supply and Services EIA Report Modifications to the Petitcodiac River Causeway September 2005 EXECUTIVE SUMMARY Background This document is the Environmental Impact Assessment (EIA) Report for the Modifications to the Petitcodiac River Causeway Project. The Petitcodiac River causeway (“causeway”) is a gated dam structure with an installed vertical slot fishway that was built across the Petitcodiac River between the City of Moncton and the Town of Riverview. Figure 1 shows the location of the Petitcodiac River and Figure 2 shows an aerial view of the causeway. Completed in 1968, the causeway was intended to create a second transportation link between the two communities, offer flood protection for farmland between the causeway and the head of tide at Salisbury, and create a freshwater headpond with potential for recreation and as an industrial water source. A bridge would have achieved the transportation objective, but not the other benefits. As early as 1961, it was recognized by Fisheries and Oceans Canada (“DFO”) that fish passage would be an issue if a causeway was built across the Petitcodiac River. Consequently, DFO required that a fishway be included in the structure. However, the construction of the causeway with the fishway resulted in fish passage issues from the outset. The fishway proved ineffective for all fish species that require passage for life cycle purposes, including the Inner Bay of Fundy Atlantic salmon that is now also protected under the Species at Risk Act because of declining numbers. -
East Bay Hills Wind Project Mi'kmaq Ecological Knowledge Study
East Bay Hills Wind Project Mi’kmaq Ecological Knowledge Study Prepared for: Cape Breton Hydro Inc. December 2012 – Version 1 M.E.K.S. Project Team Jason Googoo, Project Manager Dave Moore, Author and Research Craig Hodder, Author and GIS Technician Mary Ellen Googoo, MEKS Interviewer John Sylliboy, MEKS Traditionalist Prepared by: Reviewed by: ___________________ ____________________ Craig Hodder, Author Jason Googoo, Manager Executive Summary This Mi’kmaq Ecological Knowledge Study, also commonly referred to as an MEKS or a Traditional Ecological Knowledge Study (TEKS), was developed by Membertou Geomatics Solutions (MGS) on behalf of Cape Breton Hydro Inc. (CBHI) for the proposed East Bay Hills Wind Power Project. This MEKS mandate is to consider land and water areas which the proposed project will utilize, and to identify what Mi’kmaq traditional use activities have occurred, or are currently occurring within, and what Mi’kmaq ecological knowledge presently exists in regards to the area. In order to ensure accountability and ethic responsibility of this MEKS, the MEKS development has adhered to the “Mi’kmaq Ecological Knowledge Protocol”. This protocol is a document that has been established by the Assembly of Nova Scotia Mi’kmaq Chiefs, which speaks to the process, procedures and results that are expected of a MEKS. The Mi’kmaq Ecological Knowledge Study consisted of two major components: • Mi’kmaq Traditional Land and Resource Use Activities , both past and present, • A Mi’kmaq Significance Species Analysis , considering the resources that are important to Mi’kmaq use. The Mi’kmaq Traditional Land and Resource Use Activities component utilized interviews as the key source of information regarding Mi’kmaq use in the Project Site and Study Area. -
MCP No 02-E.Cdr
Silica Natural Resources Lands, Minerals and Petroleum Division Mineral Commodity Profile No. 2 ilicon (Si) is the second most common element on Earth after World Production and Reserves Soxygen. Si does not occur naturally in its pure state but instead is found chiefly in mineral form as either silica (SiO2) or silicates. Silica Silica deposits occur, and are mined, in most and/or silicate minerals are a constituent of nearly every rock type in countries. Global silica output is estimated at Earth's crust. roughly 120 Mt to 150 Mt per year (Dumont 2006). The most familiar silica mineral is quartz. In commodity terms, silica About 5.9 Mt of ferrosilicon were produced also refers to geological deposits enriched in quartz and/or other silica worldwide in 2006. The major contributors were minerals. Silica resources include 1) poorly consolidated quartzose China, Russia, United States, Brazil and South sand and gravel, 2) quartz sand/pebbles in consolidated rock (e.g. Africa (U.S. Geological Survey [USGS] 2006). quartzose sandstone), 3) quartzite , and 4) quartz veins. Global production of silicon metal reportedly Uses approached 1.2 Mt in 2006, almost half of which came from China (USGS 2006). Other important Silica is hard, chemically inert, has a high melting point, and functions producers are the United States, Brazil, Norway, as a semiconductor—characteristics that give it many industrial France, Russia, South Africa and Australia. applications. Silica deposits generally must be processed to remove iron, clay and other impurities. The most valuable resources contain Silica Consumption in Canada (Total = 2.57 Mt) >98% SiO2 and can be readily crushed into different sizes for the various end products. -
Broken Brooks Improving Acccess to Aquatic Habitat Through Diverse Partnership
2019–2020 BROKEN BROOKS IMPROVING ACCCESS TO AQUATIC HABITAT THROUGH DIVERSE PARTNERSHIP Prepared by Shane Boyd PETITCODIAC WATERSHED ALLIANCE 0 This page was intentionally left blank. i DISCLAIMER The Petitcodiac Watershed Alliance (PWA) is a non-profit environmental charity who works to protect and improve the ecological systems within the Petitcodiac River Watershed. We use local science to educate community members within the watershed about the ecology within the Petitcodiac River’s watershed boundary, and the importance of protecting this unique river system. Photographic Credits Unless otherwise indicated, photographs, charts, and maps in this publication are courtesy of the Petitcodiac Watershed Alliance. All other photograph or map credits appear following the image caption. General Disclaimer While every effort has been made to present accurate maps and data, the Petitcodiac Watershed Alliance does not guarantee that the maps and data are correct. Users of facts presented in this report, as well as the data herein must take care to ensure that applications envisaged for these data are appropriate uses. The opinions expressed in this document are solely those of the author, and do not necessarily represent the opinion of the employees and board members of the organisation, or of the Petitcodiac Watershed Alliance. The Petitcodiac Watershed Alliance 236 St. George St., Suite 405 Moncton, NB E1C 1W1 (506) 384-3369 ii We gratefully acknowledge the support of the Atlantic Salmon Conservation Foundation, New Brunswick’s Environmental Trust Fund, Government of Canada’s Recreational Fisheries Conservation Partnerships Program, New Brunswick’s Student Employment Experience Development and Government of Canada Summer Jobs. iii Table of Contents Executive Summary ............................................................................................................. -
Support for Delineation of Inner Bay of Fundy Salmon Marine Critical Habitat Boundaries in Minas Basin and Chignecto
Canadian Science Advisory Secretariat Maritimes Region Science Response 2015/035 SUPPORT FOR DELINEATION OF INNER BAY OF FUNDY SALMON MARINE CRITICAL HABITAT BOUNDARIES IN MINAS BASIN AND CHIGNECTO BAY Context In April 2014, the Fisheries and Oceans Canada (DFO) Species at Risk Management Division (SARMD) in the Maritimes Region requested information from DFO Science to assist with the delineation of boundaries for critical habitat (CH) being considered for Inner Bay of Fundy (IBOF) Atlantic Salmon within Chignecto Bay and Minas Basin, specifically: to assist with the delineation of the boundary between estuarine and marine habitat for several large, tidal estuaries (i.e., Petitcodiac River, Avon River, Salmon River Colchester, Shubenacadie River estuary and Cumberland Basin). DFO Science had previously provided advice on the characteristics and general location of important marine and estuarine habitat for IBOF salmon (DFO 2008; DFO 2013); however, additional information was requested to assist in delineating the precise boundaries of important marine habitat within Chignecto Bay and Minas Basin in order to subsequently propose, describe and map these as CH within an amended Recovery Strategy for IBOF salmon. Once identified in the Recovery Strategy, measures will be taken to protect this marine CH under the Species at Risk Act (SARA). This Science Response Report results from the Science Response Process of 11 July 2014 on Support for Delineation of Inner Bay of Fundy Salmon Marine Critical Habitat Boundaries. Background The inner Bay of Fundy populations of Atlantic salmon (Salmo salar) are listed as Endangered under the Species at Risk Act, and SARA requires the identification of CH for endangered species within a Recovery Strategy (or Action Plan). -
Nova Scotia New Brunswick U.S
Moncton • • Dieppe World’s Highest Tides Ecozone Fredericton Hillsborough • Sea Cliffs and Fossils Ecozone • Sackville Hopewell Cape • • • Amherst Dorchester NEW BRUNSWICK Cape • Sussex • Marys Point Harvey • Joggins New Horton • Fundy National • 7 Waterside Park of Canada • • Alma • Cape Enrage • Hampton Chignecto Bay • Apple River Five Islands Bass River Port Greville • • • Parrsboro • Economy Cape Chignecto Five Islands • Provincial Park Provincial Park Truro St. Martins • • • Advocate Harbour Cape Split • Oak Bay Cape d’Or Minas Basin Burntcoat Head • • Provincial Park • Maitland Blomidon • • St. Stephen Saint John Noel 1 Provincial Park New River Beach • South Maitland • Provincial Park Walton Halls Harbour • St. George • Medford Urbania• • Harbourville • St. Andrews • Dipper Harbour • • Stewiacke • Blacks Harbour Grand Pré Bay of Fundy Kentville • • • Margaretsville Wolfville Deer • • Hantsport Shubenacadie • U.S. Island • Avondale • Middleton • Windsor • Brooklyn • Eastport Campobello Island Herring Cove Valleyview Lubec • Provincial Park Provincial Park Port Royal Grand • Manan • Annapolis Royal Island Anchorage UNITED STATES Provincial Park CANADA Digby • Bear River • Halifax NOVA SCOTIA DIGBY NECK • Weymouth Tiverton • East Ferry • Long Island Legend Fundy Aquarium Ecozone Areas where whales are commonly seen Westport • Freeport • Seacliffs and Fossils Ecozone Northern Right whale conservation area Brier Island World’s Highest Tides Ecozone Fundy Coastal Drive Meteghan • Whale Watching Tour Glooscap Trail (Fundy Shore & Annapolis Valley) Geology Exhibit Evangeline Trail (Fundy Shore & Annapolis Valley) Coastal Hiking Trail Multi-lane Highway/Trans Canada Highway Atlantic Ocean Horizontal Tidal Effect Controlled Access Highway Vertical Tidal Effect Secondary road N Tidal Bore Ferry Yarmouth Tidal Rapids Elevation 0-500’ 500-1000’ 1000’+ Fundy Aquarium Ecozone • National or Provincial Park Scale 0 10 20 30 40 km bayoffundytourism.com . -
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The Dispossession of the Míkmaq Indians from Chignecto to Elsipogtog1: A Case Study Analysis of the Health Determinants of the Physical Environment by Patrick J. Augustine A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Indigenous and Canadian Studies Carleton University Ottawa, Ontario © 2021, Patrick J. Augustine 1 The community uses the Pacifique orthography, while the Francis-Smith system spells it L’sipuktuk (Sable & Francis, 2012). Abstract Traditionally, the Míkmaq enjoyed an interconnected relationship with the land, harvesting what they needed from the earth and the ocean, guided by the concept of Netukulimk, the practice of sustainability. Upon the arrival of European settlers, new trade practices were introduced, and what was once plentiful was quickly depleted. Although the original inhabitants were assured that their lands would be protected by agreements and treaties, these assurances proved to be false, and the traditional relationship with the land was threatened, as the Míkmaq—presaging the fate of most Indigenous Peoples in Canada—were dispossessed of their historical lands and forced to live on reserves; many of them far away from the environments to which they had had biological and spiritual ties. Land is central to our understanding of current Indigenous health issues; centering around how the Míkmaq traditionally employed land and resources, what changes in that relationship were brought about by colonization, and how their removal to reserves influenced their relationship vis-à-vis their environment. In addressing the ways that land policies, post-first contact, were developed and implemented over time, it is possible and necessary to juxtapose that history with the story of the forced mobilization of the Míkmaq and examine the effects that the dispossession of land had upon their livelihood and economic activity. -
11Th Workshop Proceedings
Fundy in Flux: Challenges for Science, Policy and Society Proceedings of the 11th BoFEP Bay of Fundy Science Workshop, Fredericton, New Brunswick, 9–11 June 2016 Editors Marianne Janowicz, Blythe Chang, Sarah Chamberlain, Susan J. Rolston, and Peter G. Wells BoFEP Technical Report No. 10 March 2017 This publication should be cited as: M. Janowicz, B. Chang, S. Chamberlain, S.J. Rolston and P.G. Wells (eds.). 2017. Fundy in Flux: Challenges for Science, Policy and Society. Proceedings of the 11th BoFEP Bay of Fundy Science Workshop, Fredericton, New Brunswick, 9–11 June 2016. Bay of Fundy Ecosystem Partnership Technical Report No. 10. Bay of Fundy Ecosystem Partnership, Tantallon, NS. 52 p. Photographs: Sarah Chamberlain, Jack Fife, Fundy Ocean Research Center for Energy (FORCE), Marianne Janowicz, Kimberly Robichaud-Leblanc, Susan Rolston, Peter G. Wells For further information, contact: Bay of Fundy Ecosystem Partnership Secretariat PO Box 3062 Tantallon, Nova Scotia, Canada B3Z 4G9 E-mail: [email protected] www.bofep.org © Bay of Fundy Ecosystem Partnership, 2017 ISBN 978-0-9783120-7-7 2 Table of Contents Preface ........................................................................................................................................................... 4 Acknowledgements ........................................................................................................................................ 5 Workshop Organizers .................................................................................................................................... -
Seasonal Variability of Total Suspended Matter in Minas Basin, Bay of Fundy
SEASONAL VARIABILITY OF TOTAL SUSPENDED MATTER IN MINAS BASIN, BAY OF FUNDY by Jing Tao Submitted in partial fulfilment of the requirements for the degree of Master of Science at Dalhousie University Halifax, Nova Scotia July 2013 © Copyright by Jing Tao, 2013 For my parents, who encouraged me all the way long. I love them forever. ii TABLE OF CONTENTS LIST OF TABLES .............................................................................................................. v LIST OF FIGURES ........................................................................................................... vi ABSTRACT ................................................................................................................ viii LIST OF ABBREVIATIONS AND SYMBOLS USED ................................................... ix ACKNOWLEDGEMENTS ............................................................................................... xi CHAPTER 1 INTRODUCTION ..................................................................................... 1 1.1 Background ........................................................................................................... 1 1.2 Geology of Minas Basin ....................................................................................... 2 1.3 Literature Review .................................................................................................. 4 1.3.1 Point Measurements ....................................................................................... 4 1.3.2 Satellite Measurements