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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. -
Tusket River & Basin
Tusket River & Basin Introduction The Tusket River presents an area of 3000 square kilometres (1158 square miles) on the southwestern tip of Nova Scotia. The area consists of a coastal basin with an inland watershed associated with the great Tusket River. This name is derived from a Mi'kmaq word "Neketaouksit" meaning "Great Forked Tidal River". This unique and diverse environment has offered natural resources to the Mi'kmaq First Nation's people for 7000 years and to the French Acadian settlers since the early 17th century. In the context of sustainable development, the present-day Acadians can offer a bilingual ecotourism package of nature-adventure and discovery blended with local history and heritage. The following natural history of the area will be presented in two segments. The first section will describe the natural environment of the Tusket Basin and its interrelationships with the Acadian people. The second segment will describe the natural history of the Tusket River in a similar manner to present the Acadian in his natural environment. Basin description 1. Physical features The Tusket Basin has a width of 32 kilometres (20 miles) between headlands at Chebogue Point and Lower East Pubnico. The mainland coastline between these two boundaries is highly indented and irregular with a measure of 500 kilometres (310 miles). Elongated points, peninsulas, ridges, drumlins (low hills) and eskers are oriented North-South and are separated by many tidal channels, inlets, estuaries and bays. High tide in the estuary of the "great forked tidal river" (Tusket) carries salt water inland for 24 kilometres (15 miles). -
Lady Crabs, Ovalipes Ocellatus, in the Gulf of Maine
18_04049_CRABnotes.qxd 6/5/07 8:16 PM Page 106 Notes Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine J. C. A. BURCHSTED1 and FRED BURCHSTED2 1 Department of Biology, Salem State College, Salem, Massachusetts 01970 USA 2 Research Services, Widener Library, Harvard University, Cambridge, Massachusetts 02138 USA Burchsted, J. C. A., and Fred Burchsted. 2006. Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine. Canadian Field-Naturalist 120(1): 106-108. The Lady Crab (Ovalipes ocellatus), mainly found south of Cape Cod and in the southern Gulf of St. Lawrence, is reported from an ocean beach on the north shore of Massachusetts Bay (42°28'60"N, 70°46'20"W) in the Gulf of Maine. All previ- ously known Gulf of Maine populations north of Cape Cod Bay are estuarine and thought to be relicts of a continuous range during the Hypsithermal. The population reported here is likely a recent local habitat expansion. Key Words: Lady Crab, Ovalipes ocellatus, Gulf of Maine, distribution. The Lady Crab (Ovalipes ocellatus) is a common flats (Larsen and Doggett 1991). Lady Crabs were member of the sand beach fauna south of Cape Cod. not found in intensive local studies of western Cape Like many other members of the Virginian faunal Cod Bay (Davis and McGrath 1984) or Ipswich Bay province (between Cape Cod and Cape Hatteras), it (Dexter 1944). has a disjunct population in the southern Gulf of St. Berrick (1986) reports Lady Crabs as common on Lawrence (Ganong 1890). The Lady Crab is of consid- Cape Cod Bay sand flats (which commonly reach 20°C erable ecological importance as a consumer of mac- in summer). -
Minas Basin, N.S
An examination of the population characteristics, movement patterns, and recreational fishing of striped bass (Morone saxatilis) in Minas Basin, N.S. during summer 2008 Report prepared for Minas Basin Pulp and Power Co. Ltd. Contributors: Jeremy E. Broome, Anna M. Redden, Michael J. Dadswell, Don Stewart and Karen Vaudry Acadia Center for Estuarine Research Acadia University Wolfville, NS B4P 2R6 June 2009 2 Executive Summary This striped bass study was initiated because of the known presence of both Shubenacadie River origin and migrant USA striped bass in the Minas Basin, the “threatened” species COSEWIC designation, the existence of a strong recreational fishery, and the potential for impacts on the population due to the operation of in- stream tidal energy technology in the area. Striped bass were sampled from Minas Basin through angling creel census during summer 2008. In total, 574 striped bass were sampled for length, weight, scales, and tissue. In addition, 529 were tagged with individually numbered spaghetti tags. Striped bass ranged in length from 20.7-90.6cm FL, with a mean fork length of 40.5cm. Data from FL(cm) and Wt(Kg) measurements determined a weight-length relationship: LOG(Wt) = 3.30LOG(FL)-5.58. Age frequency showed a range from 1-11 years. The mean age was 4.3 years, with 75% of bass sampled being within the Age 2-4 year class. Total mortality (Z) was estimated to be 0.60. Angling effort totalling 1732 rod hours was recorded from June to October, 2008, with an average 7 anglers fishing per tide. Catch per unit effort (Fish/Rod Hour) was determined to be 0.35, with peak landing periods indicating a relationship with the lunar cycle. -
Modelling the Sea Level in the Upper Bay of Fundy
Modelling the sea level in the upper Bay of Fundy Fred´ eric´ Dupont, Charles G. Hannah, David Greenberg Fisheries and Oceans Canada, Bedford Institude of Oceanography, P.O. Box 1006, Dartmouth, N.S. Canada B2Y 4A2 December 9, 2003 Abstract A high resolution model of the upper Bay of Fundy was developed to simulate the tides and sea level. The model includes the wetting and drying (inundation) of the extensive tidal flats in Minas Basin. The model reproduces the dominant M2 tidal harmonic with an error of order 0.30 m, and the total water level in Minas Basin with an RMS error of 0.30-0.50 m. Overall the system is capable of simulation with sea level error of 8-11%. The motivation for the model development was the simulation of the land/water interface (instantaneous coastline) to aid in the validation of coastline retrieval algorithms from remotely sensed observations. Qualitative comparison of observed and simulated coastlines showed that the misfit was dominated by errors in the details of the local topography/bathymetry. For example, long narrow features such as dykes are difficult to resolve in a dynamical model but are important for inundation of low lying areas. 1 1 Introduction This paper reports on the development of a sea level prediction system for the upper Bay of Fundy (Fig. 1). The motivation is the simulation of the land-water boundary (instanta- neous coastline) in the Bay as part of the validation of the land-water boundary extracted from remotely sensed observations (e.g. RADARSAT-1, polarimetric SAR, CASI, Land- sat and Ikonos imagery) as described by Deneau (2002) and Milne (2003). -
South Western Nova Scotia
Netukulimk of Aquatic Natural Life “The N.C.N.S. Netukulimkewe’l Commission is the Natural Life Management Authority for the Large Community of Mi’kmaq /Aboriginal Peoples who continue to reside on Traditional Mi’Kmaq Territory in Nova Scotia undisplaced to Indian Act Reserves” P.O. Box 1320, Truro, N.S., B2N 5N2 Tel: 902-895-7050 Toll Free: 1-877-565-1752 2 Netukulimk of Aquatic Natural Life N.C.N.S. Netukulimkewe’l Commission Table of Contents: Page(s) The 1986 Proclamation by our late Mi’kmaq Grand Chief 4 The 1994 Commendation to all A.T.R.A. Netukli’tite’wk (Harvesters) 5 A Message From the N.C.N.S. Netukulimkewe’l Commission 6 Our Collective Rights Proclamation 7 A.T.R.A. Netukli’tite’wk (Harvester) Duties and Responsibilities 8-12 SCHEDULE I Responsible Netukulimkewe’l (Harvesting) Methods and Equipment 16 Dangers of Illegal Harvesting- Enjoy Safe Shellfish 17-19 Anglers Guide to Fishes Of Nova Scotia 20-21 SCHEDULE II Specific Species Exceptions 22 Mntmu’k, Saqskale’s, E’s and Nkata’laq (Oysters, Scallops, Clams and Mussels) 22 Maqtewe’kji’ka’w (Small Mouth Black Bass) 23 Elapaqnte’mat Ji’ka’w (Striped Bass) 24 Atoqwa’su (Trout), all types 25 Landlocked Plamu (Landlocked Salmon) 26 WenjiWape’k Mime’j (Atlantic Whitefish) 26 Lake Whitefish 26 Jakej (Lobster) 27 Other Species 33 Atlantic Plamu (Salmon) 34 Atlantic Plamu (Salmon) Netukulimk (Harvest) Zones, Seasons and Recommended Netukulimk (Harvest) Amounts: 55 SCHEDULE III Winter Lake Netukulimkewe’l (Harvesting) 56-62 Fishing and Water Safety 63 Protecting Our Community’s Aboriginal and Treaty Rights-Community 66-70 Dispositions and Appeals Regional Netukulimkewe’l Advisory Councils (R.N.A.C.’s) 74-75 Description of the 2018 N.C.N.S. -
Atlantic Maritime Ecozone+: Evidence for Key Findings
Atlantic Maritime Ecozone+ evidence for key findings summary Canadian Biodiversity: Ecosystem Status and Trends 2010 Evidence for Key Findings Summary Report No. 3 Published by the Canadian Councils of Resource Ministers Library and Archives Canada Cataloguing in Publication Atlantic Maritime Ecozone+ evidence for key findings summary. Issued also in French under title: Sommaire des éléments probants relativement aux constatations clés pour l’écozone+ maritime de l’Atlantique. Electronic monograph in PDF format. En14-43/0-3-2015E-PDF 978-1-100-23826-5 Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: Exercise due diligence in ensuring the accuracy of the materials reproduced; Indicate both the complete title of the materials reproduced, as well as the author organization; and Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1- 800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Cover photos: Margaree Valley, Cape Breton Island, Nova Scotia, © iStock.com / cworthy; Hopewell Rocks, Bay of Fundy, New Brunswick, © iStock.com / MorganLeFaye This report should be cited as: ESTR Secretariat. 2014. -
Geographic Names
GEOGRAPHIC NAMES CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES ? REVISED TO JANUARY, 1911 WASHINGTON GOVERNMENT PRINTING OFFICE 1911 PREPARED FOR USE IN THE GOVERNMENT PRINTING OFFICE BY THE UNITED STATES GEOGRAPHIC BOARD WASHINGTON, D. C, JANUARY, 1911 ) CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES. The following list of geographic names includes all decisions on spelling rendered by the United States Geographic Board to and including December 7, 1910. Adopted forms are shown by bold-face type, rejected forms by italic, and revisions of previous decisions by an asterisk (*). Aalplaus ; see Alplaus. Acoma; township, McLeod County, Minn. Abagadasset; point, Kennebec River, Saga- (Not Aconia.) dahoc County, Me. (Not Abagadusset. AQores ; see Azores. Abatan; river, southwest part of Bohol, Acquasco; see Aquaseo. discharging into Maribojoc Bay. (Not Acquia; see Aquia. Abalan nor Abalon.) Acworth; railroad station and town, Cobb Aberjona; river, IVIiddlesex County, Mass. County, Ga. (Not Ackworth.) (Not Abbajona.) Adam; island, Chesapeake Bay, Dorchester Abino; point, in Canada, near east end of County, Md. (Not Adam's nor Adams.) Lake Erie. (Not Abineau nor Albino.) Adams; creek, Chatham County, Ga. (Not Aboite; railroad station, Allen County, Adams's.) Ind. (Not Aboit.) Adams; township. Warren County, Ind. AJjoo-shehr ; see Bushire. (Not J. Q. Adams.) Abookeer; AhouJcir; see Abukir. Adam's Creek; see Cunningham. Ahou Hamad; see Abu Hamed. Adams Fall; ledge in New Haven Harbor, Fall.) Abram ; creek in Grant and Mineral Coun- Conn. (Not Adam's ties, W. Va. (Not Abraham.) Adel; see Somali. Abram; see Shimmo. Adelina; town, Calvert County, Md. (Not Abruad ; see Riad. Adalina.) Absaroka; range of mountains in and near Aderhold; ferry over Chattahoochee River, Yellowstone National Park. -
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 . -
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 -
The Management Of, and Fishery For, American Eel Elvers in the Maritime Provinces, Canada
Bull. Fr. Pêche Piscic. (1998) 349:103-116 — 103 — THE MANAGEMENT OF, AND FISHERY FOR, AMERICAN EEL ELVERS IN THE MARITIME PROVINCES, CANADA. B.M. JESSOP Biological Sciences Branch, Department of Fisheries and Oceans, P.O. Box 550, Halifax, Nova Scotia, B3J 2S7, Canada. ABSTRACT The fishery for American eel, Anguilla rostrata, elvers in the Scotia-Fundy area of Atlantic Canada has, since inception in 1989, increased catches from 26 kg to about 3 000 kg in 1996. Development of the fishery has been tightly controlled with nine licenses presently (1996) issued, three of which are restricted to aquaculture use. No elver fishery is permitted in rivers in which an active fishery for larger eels exists, each license has a quota of up to 1 ton, with a limit of 300 kg from any given river, and records of daily catch and fishing effort, by gear type, are now required for each river fished. Elver catches and CPUE vary geographically, being highest along the south shore and lower Bay of Fundy areas of Nova Scotia, moderately high along the lower Bay of Fundy, New Brunswick, and lowest along the eastern shore of Nova Scotia and upper Bay of Fundy areas (Minas Basin and Chignecto Bay). In all areas but the eastern shore of Nova Scotia, commercial quantities of elvers first arrive in April. Elver catch peaks during May, then declines through June with small (less than 1% of total) catches occurring in some areas during early July. Geographic differences in elver catches and run timing may be linked to océanographie current patterns, particularly the southwestward flow of the Nova Scotia Current along the Atlantic coast and the counter-clockwise flow around the Bay of Fundy, and differences in the timing of rising river water temperatures during spring.