C S a S S C C S
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Barriers to Fish Passage in Nova Scotia the Evolution of Water Control Barriers in Nova Scotia’S Watershed
Dalhousie University- Environmental Science Barriers to Fish Passage in Nova Scotia The Evolution of Water Control Barriers in Nova Scotia’s Watershed By: Gillian Fielding Supervisor: Shannon Sterling Submitted for ENVS 4901- Environmental Science Honours Abstract Loss of connectivity throughout river systems is one of the most serious effects dams impose on migrating fish species. I examine the extent and dates of aquatic habitat loss due to dam construction in two key salmon regions in Nova Scotia: Inner Bay of Fundy (IBoF) and the Southern Uplands (SU). This work is possible due to the recent progress in the water control structure inventory for the province of Nova Scotia (NSWCD) by Nova Scotia Environment. Findings indicate that 586 dams have been documented in the NSWCD inventory for the entire province. The most common main purpose of dams built throughout Nova Scotia is for hydropower production (21%) and only 14% of dams in the database contain associated fish passage technology. Findings indicate that the SU is impacted by 279 dams, resulting in an upstream habitat loss of 3,008 km of stream length, equivalent to 9.28% of the total stream length within the SU. The most extensive amount of loss occurred from 1920-1930. The IBoF was found to have 131 dams resulting in an upstream habitat loss of 1, 299 km of stream length, equivalent to 7.1% of total stream length. The most extensive amount of upstream habitat loss occurred from 1930-1940. I also examined if given what I have learned about the locations and dates of dam installations, are existent fish population data sufficient to assess the impacts of dams on the IBoF and SU Atlantic salmon populations in Nova Scotia? Results indicate that dams have caused a widespread upstream loss of freshwater habitat in Nova Scotia howeverfish population data do not exist to examine the direct impact of dam construction on the IBoF and SU Atlantic salmon populations in Nova Scotia. -
Striped Bass Morone Saxatilis
COSEWIC Assessment and Status Report on the Striped Bass Morone saxatilis in Canada Southern Gulf of St. Lawrence Population St. Lawrence Estuary Population Bay of Fundy Population SOUTHERN GULF OF ST. LAWRENCE POPULATION - THREATENED ST. LAWRENCE ESTUARY POPULATION - EXTIRPATED BAY OF FUNDY POPULATION - THREATENED 2004 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2004. COSEWIC assessment and status report on the Striped Bass Morone saxatilis in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vii + 43 pp. (www.sararegistry.gc.ca/status/status_e.cfm) Production note: COSEWIC would like to acknowledge Jean Robitaille for writing the status report on the Striped Bass Morone saxatilis prepared under contract with Environment Canada, overseen and edited by Claude Renaud the COSEWIC Freshwater Fish Species Specialist Subcommittee Co-chair. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Ếgalement disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur la situation de bar rayé (Morone saxatilis) au Canada. Cover illustration: Striped Bass — Drawing from Scott and Crossman, 1973. Her Majesty the Queen in Right of Canada 2004 Catalogue No. CW69-14/421-2005E-PDF ISBN 0-662-39840-8 HTML: CW69-14/421-2005E-HTML 0-662-39841-6 Recycled paper COSEWIC Assessment Summary Assessment Summary – November 2004 Common name Striped Bass (Southern Gulf of St. -
A Review of Ice and Tide Observations in the Bay of Fundy
A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients. -
Isaac Deschamps Fonds (MG 1 Volume 258)
Nova Scotia Archives Finding Aid - Isaac Deschamps fonds (MG 1 volume 258) Generated by Access to Memory (AtoM) 2.5.3 Printed: October 09, 2020 Language of description: English Nova Scotia Archives 6016 University Ave. Halifax Nova Scotia B3H 1W4 Telephone: (902) 424-6060 Fax: (902) 424-0628 Email: [email protected] http://archives.novascotia.ca/ https://memoryns.ca/index.php/isaac-deschamps-fonds Isaac Deschamps fonds Table of contents Summary information ...................................................................................................................................... 3 Administrative history / Biographical sketch .................................................................................................. 3 Scope and content ........................................................................................................................................... 3 Notes ................................................................................................................................................................ 4 Series descriptions ........................................................................................................................................... 4 - Page 2 - MG 1 volume 258 Isaac Deschamps fonds Summary information Repository: Nova Scotia Archives Title: Isaac Deschamps fonds ID: MG 1 volume 258 Date: 1750-1814, predominant 1756-1768 (date of creation) Physical description: 4 cm of textual records Dates of creation, Revised 2017-06-16 Carli LaPierre (items imported -
Labour Day 2011 Returns to the Gaspereau Valley Wolfville, Nova Scotia September 2 to 5, 2011
Labour Day 2011 Returns to the Gaspereau Valley Wolfville, Nova Scotia September 2 to 5, 2011 Long time members of the Maritime Organization of Rover Enthusiasts (MORE) will remember Labour Day in and around Wolfville back in 1999 and 2000. After years of resistance we, Julie and Peter Rosvall, will host Labour Day on our property once again. With the help of fellow Rover owners in our neighbourhood we will invite folks from across the Maritimes, New England, points west and internationally to our home. Kris Lockhart has been scouting and doing trail maintenance for so long already that the local joke is that by Labour Day 2011 he might have them paved if we don't watch out. All trailheads will be within 5 minutes of our property, and will have lots of options for every driving preference. Rosie Browning is taking the lead on food, after the great success of her desserts in Cape Breton. She has dreams of sandwiches made with roast beef and turkey (yes, real roast, really, cooked just prior to making the sandwiches, I'm drooling already). Rosie will be helped by a team of my relatives and our neighbours. All meals from Friday evening to Sunday night are provided on site, and the food will be amazing. I'm sure we'll have the Barr family put to work on this and other logistical details, and the Rudermans as well, and anyone else we can sucker in to volunteering leading up to the event and during. (willing volunteers can contact me using the coordinates below) Camping for the event will be on our property; tents will be setup among the cherry and pear trees, bordered by blackberry bushes. -
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. -
2019 Bay of Fundy Guide
VISITOR AND ACTIVITY GUIDE 2019–2020 BAYNova OF FUNDYScotia’s & ANNAPOLIS VALLEY TIDE TIMES pages 13–16 TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia and New Brunswick. Ferries.ca Find Yourself on the Cliffs of Fundy TWO STUNNING PROVINCES. ONE CONVENIENT CROSSING. Digby, NS – Saint John, NB Isle Haute - Bay of Fundy Experience the phenomenal Bay of Fundy in comfort aboard mv Fundy Rose on a two-hour journey between Nova Scotia Take the scenic route and fi nd yourself surrounded by the and New Brunswick. natural beauty and rugged charm scattered along the Fundy Shore. Find yourself on the “Cliffs of Fundy” Cape D’or - Advocate Harbour Ferries.ca www.fundygeopark.ca www.facebook.com/fundygeopark Table of Contents Near Parrsboro General Information .................................. 7 Top 5 One-of-a-Kind Shopping ........... 33 Internet Access .................................... 7 Top 5 Heritage and Cultural Smoke-free Places ............................... 7 Attractions .................................34–35 Visitor Information Centres ................... 8 Tidally Awesome (Truro to Avondale) ....36–43 Important Numbers ............................. 8 Recommended Scenic Drive ............... 36 Map ............................................... 10–11 Top 5 Photo Opportunities ................. 37 Approximate Touring Distances Top Outdoor Activities ..................38–39 Along Scenic Route .........................10 -
Hydrodynamic Modelling for Flood Management in Bay of Fundy Dykelands”
Hydrodynamic Modelling for Flood Management in Bay of Fundy Dykelands By Michael Fedak A Thesis Submitted to Saint Mary’s University, Halifax, Nova Scotia in Partial Fulfillment of the Requirements for the Degree of Master of Science in Applied Science July 16, 2012, Halifax Nova Scotia © Michael Fedak, 2012 Approved: Dr. Danika van Proosdij Supervisor Department of Geography Approved: Dr. Ryan Mulligan External Examiner Department of Civil Engineering Queen’s University Approved: Dr. Timothy Webster Supervisory Committee Member COGS, NSCC Approved: Dr. Peter Secord Graduate Studies Representative Date: July 16, 2012 Abstract “Hydrodynamic Modelling for Flood Management in Bay of Fundy Dykelands” By Michael Fedak Storm surge in the coastal Bay of Fundy is a serious flood hazard. These lands are low-lying and adapted to farming through the use of coastal defences, namely dykes. Increasing rates of sea level rise due to climate change are expected to increase flood hazard in this area. In this thesis, flood risk to communities in the Avon River estuary of the Upper Bay of Fundy is investigated through computer based modelling and data management techniques. Flood variables from 14 possible storm surge scenarios (based on sea level rise predictions) were modelled using TUFLOW software. A GIS was used to create a database for simulation outputs and for the analysis of outputs. TUFLOW and a geographic information system (GIS) flood algorithm are compared .It was found that obstructions to flow controlled flooding and drainage and these features required the use of a hydrodynamic model to represent flows properly. July 16, 2012 2 Acknowledgements Funding Sources: • Atlantic Canada Adaptation Solutions Association part of the Natural Resources Canada Regional Adaptation Collaboratives (RAC) Project. -
Overview of 2013 Bay of Fundy Striped Bass Biology and General Status
Canadian Science Advisory Secretariat (CSAS) Research Document 2015/024 Maritimes Region Overview of 2013 Bay of Fundy Striped Bass Biology and General Status R.G. Bradford1, E.A. Halfyard1, T. Hayman2, and P. LeBlanc1 Fisheries and Oceans Canada 1Science Branch, Maritimes Region 2Species at Risk Management Division P.O. Box 1006 Dartmouth, Nova Scotia, B2Y 4A2 July 2015 Foreword This series documents the scientific basis for the evaluation of aquatic resources and ecosystems in Canada. As such, it addresses the issues of the day in the time frames required and the documents it contains are not intended as definitive statements on the subjects addressed but rather as progress reports on ongoing investigations. Research documents are produced in the official language in which they are provided to the Secretariat. Published by: Fisheries and Oceans Canada Canadian Science Advisory Secretariat 200 Kent Street Ottawa ON K1A 0E6 http://www.dfo-mpo.gc.ca/csas-sccs/ [email protected] © Her Majesty the Queen in Right of Canada, 2015 ISSN 1919-5044 Correct citation for this publication: Bradford, R.G., Halfyard, E.A., Hayman, T., and LeBlanc, P. 2015. Overview of 2013 Bay of Fundy Striped Bass Biology and General Status. DFO Can. Sci. Advis. Sec. Res. Doc. 2015/024. iv + 36 p. TABLE OF CONTENTS ABSTRACT ................................................................................................................................ iv RÉSUMÉ .................................................................................................................................. -
Fishing the Gaspereau Chris Gertridge
Wolfville Historical Society Summer 2019 Newsletter – Regatta Edition Volume 19 Issue 2 Up Tails All! An Account of the Inaugural Randall House Regatta By Martin Hallett, President Having dodged a meteorological bullet on Canada Day, when it looked as if the WHS hotdog stand in Willow Park would be submerged for the second time in three years, our merry band of BBQers could be forgiven for feeling that the weather gods Just don’t like the Historical Society – the only consolation being that if anyone fell into the pond, they couldn’t get Photo by C. Gertridge any wetter. problem by sending in their renowned team of hotdoggers But wouldn’t you know it -- we to feed the communal tummy; those in need of some dodged another bullet! The rain held off, sweetness in their lives were quick to spot The Real Scoop more or less, and by the time we packed up, Ice-cream stand Just a hop, skip and a Jump away. And a rather steamy sun was making its presence those who wished to offer their faces for artistic purposes felt. were obliged by Mme. Jasmine Renaud, who moonlights We really didn’t know what to as a WHS board-member. expect: the sale of boats had gone well, but Last but not least, the Joys of “messing about in whether that would translate into a host of boats” (or, in our case, “with”) were attested to by young would-be sailors eager to commit Michael Bawtree, who read – as only he can – an their craft to the deeps of Willow Pond appropriate chapter from Kenneth Grahame’s The Wind remained to be seen. -
Sedimentation in the Inner Cornwallis Estuary, Minas Basin, Nova
166 ABSTRACTS Sedimentation in the inner Cornwallis F.stuary, Minas Basin, Nova Scotia: implications for contaminant accumulation G. Yeo, E. Bishop, A. Dickinson Department of Geology, Acadia University, Wolfville, Nova Scotia BOP JXO, Canada and R. Faas Department of Geology, Lafayette College, Easton, Pennsylvania 18042, U.SA. The estuary of the Cornwallis River is a macrotidal system Salmon River estuary. Compared to the latter, it is mud-domi within the Minas Basin, like the better-known Cobequid Bay - nated. Tidal range and flow conditions are highly variable: Atlantic Geology, July 1991, Volume 27, Number 2 Copyright © 2015 Atlantic Geology ATLANTIC GEOLOOY 167 Site: Port New Kent ville plane or rippled, silty beds are interbedded with water-saturated Williams Minas clays deposited at slack water. Overpressure conditions resulting Spring tide range (m): 12.15 4.1 2.15 from the ebb of overlying waters produce numerous fluidization Max. velocity (cm/s): 177 132 83 features. Min. velocity (cm/s}: 58 29 21 Except where the river has cut into Triassic sandstone, the banks are dyked and locally faced with rip-rap. Along most of Except at slack water, when suspended sediment settles out their length they are mud, deposited from suspension, and inten rapidly the water column is well-mixed. Suspended sediment sively gullied. Bank mud deposits are continuously recycled to concentration varies from 50 mg/I near Wolfville to >4.5 g/l at the river by fluidized flow, scouring, or undercutting and slump the turbidity maximum between New Minas and Kentville. ing. Seeps and springs are common along the banks at low water. -
Kelly River Wilderness Area
Barronsfield Eastern Habitat Joint Venture Lands Boss Pt. Maccan n Maccan Woods 242 KELLY RIVER i s 242 a Joggins Fossil Cliffs Strathcona An Overview of A New Candidate B River Hebert East Harrison Maccan River Wilderness Area Hardscrabble Lake Wildlife Management Area d Pt Joggins n River Hebert a 242 l Athol Station Cartography by the Protected Areas Branch of r Nova Scotia Environment, April 2011. e b Ragged Round 302 http://www.gov.ns.ca/nse/protectedareas/ m Reef Pt u Ragged Reef Meadow Bk Lake The information shown here was obtained C Athol courtesy of the NS Geomatics Centre (SNSMR) and the NS Department of Natural Resources. Ragged Pt k C © Crown Copyright, Province of Nova Scotia, n 2011. All rights reserved. o tt Two Rivers a This map is only a geographic representation. Christie Bk P Nova Scotia Environment and does not accept responsibility for any errors or omissions r contained herein. R e k rter B v Po South Athol i Haycock Bk i v y R k B e n e r rr a a r e B F l a t B k r v B k e l B v i i l ill i H h R d h n R L é a n n S o it r b t t Boars Back Ridge l p Lower e a S e 302 B m Pt h a Raven u r k lie Bearden s B th t d R Barrens oo ou o r rw n S Head ga r Shulie a B e Su E t Mitchell Bucktagen v K e l l y i c East c Meadows Barrens c Raven Head R Southampton Southampton e a r Chignecto Game Sanctuary Boundary M n 2 e k lm B g R i v e r E v R k to n iv e Tompkin Plains o S p r i i o o u m y r t h a B h R l k eir B w l h s C i F e r South e n v K Thundering i o 2 Brook R s LEGEND e Hill Bearden Bk n d i i n k Spar a l t ks S A Candidate Wilderness Areas (CWA) ch u B West ran k E B h Franklin Manor Brook Kelly River and Raven Head CWA S Forty Pettigrew I.R.