Fundy Tidal Energy Demonstration Project Volume I: Environmental Assessment
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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. -
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. -
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. -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
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. -
On Cape Breton Island, Nova Scotia, Canada
Canadian Journal of Earth Sciences Remnants of Early Mesozoic basalt of the Central Atlantic Magmatic Province (CAMP) on Cape Breton Island, Nova Scotia, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2016-0181.R1 Manuscript Type: Article Date Submitted by the Author: 07-Nov-2016 Complete List of Authors: White, Chris E.; Nova Scotia Department of Natural Resources Kontak, DanielDraft J.; Department of Earth Sciences, Demont, Garth J.; Nova Scotia Department of Natural Resources Archibald, Douglas; Queens University, Department of Geological Sciences Keyword: CAMP, Mesozoic, Fundy Basin, Ashfield Formation https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 48 Canadian Journal of Earth Sciences 1 Remnants of Early Mesozoic basalt of the Central Atlantic Magmatic Province (CAMP) on Cape Breton Island, Nova Scotia, Canada Chris E. White 1, Daniel J. Kontak 2, Garth J. DeMont 1, and Douglas Archibald 3 1. Nova Scotia Department of Natural Resources, Halifax, Nova Scotia, B3J 3T9, Canada 2. Department of Earth Science, Laurentian University, Sudbury, Ontario, P3E 2C6, Canada 3. Department of Geological Sciences and Geological Engineering, Queens University, Kingston, Ontario, K7L 3N6, Canada Corrected version:Draft for re-submission to CJES November 7, 2016 ABSTRACT Amygdaloidal basaltic flows of the Ashfield Formation were encountered in two drillholes in areas of positive aeromagnetic anomalies in the Carboniferous River Denys Basin in southwestern Cape Breton Island, Nova Scotia. One sample of medium-grained basalt yielded a plateau age of 201.8 ± 2.0 Ma, similar to U-Pb and 40 Ar/ 39 Ar crystallization ages from basaltic flows and dykes in the Newark Supergroup. -
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 -
Identification of Atlantic Mud-Piddock Habitat in Atlantic Canadian Waters
Identification of Atlantic Mud-piddock Habitat in Atlantic Canadian Waters C.M. Clark, A. Hebda, G. Jones, S. Butler, and G. Pardy Population Ecology Division Fisheries and Oceans Canada 1 Challenger Drive Dartmouth, NS B2Y 4A2 2019 Canadian Technical Report of Fisheries and Aquatic Sciences 3295 1 Canadian Technical Report of Fisheries and Aquatic Sciences Technical reports contain scientific and technical information that contributes to existing knowledge but which is not normally appropriate for primary literature. Technical reports are directed primarily toward a worldwide audience and have an international distribution. No restriction is placed on subject matter and the series reflects the broad interests and policies of Fisheries and Oceans Canada, namely, fisheries and aquatic sciences. Technical reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in the data base Aquatic Sciences and Fisheries Abstracts. Technical reports are produced regionally but are numbered nationally. Requests for individual reports will be filled by the issuing establishment listed on the front cover and title page. Numbers 1-456 in this series were issued as Technical Reports of the Fisheries Research Board of Canada. Numbers 457-714 were issued as Department of the Environment, Fisheries and Marine Service, Research and Development Directorate Technical Reports. Numbers 715-924 were issued as Department of Fisheries and Environment, Fisheries and Marine Service Technical Reports. The current series name was changed with report number 925. Rapport technique canadien des sciences halieutiques et aquatiques Les rapports techniques contiennent des renseignements scientifiques et techniques qui constituent une contribution aux connaissances actuelles, mais qui ne sont pas normalement appropriés pour la publication dans un journal scientifique. -
Tourism Asset Inventory
November 2019 Tourism Asset Inventory- Accomodations Product Type Name Address Community Web-Site Lochlomand Tenting and Trailer Park 1 lochlomand drive Upper Nappan www.lochlomondrvpark.com/ Five Islands Ocean Resort & RV Campground 482 Hwy 2, Lower Five Islands, Lower Five Islands www.fiveislands.ca/ Gulf Shore Camping Park 2367 Gulf Shore Rd Pugwash www.gulfshorecampingpark.com/ Glooscap Park Campground 1380 Two Island Rd Parrsboro www.town.parrsboro.ns.ca/accommodations.html Camping Amherst Shore Provincial Park 6596 NS-366 Northport www.parks.novascotia.ca/content/amherst-shore ADDA Fundy Tides Campground 95 Mills Rd Advocate Harbour Old Shipyard Beach Campground 774 Spencer’s Beach Road Spencer's Island D&D Bayview Campground 3323 South Shore Road Malagash Cape Chignecto Provincial Park 1108 West Advocate Road Advocate Harbour www.parks.novascotia.ca/content/cape-chignecto The Loco Yolkel B & B 2330 Western Ave Parrsboro Gillespie House Inn 358 Main Street Parrsboro http://www.gillespiehouseinn.com/ Evangeline's Tower Bed & Breakfast 322 Main St Parrsboro http://www.evangelinestower.com/ Maple Inn 2358 Western Ave Parrsboro http://www.mapleinn.ca/ Spencer's Island Bed & Breakfast 789 Spencer’s Beach Rd Spencer’s Island Advocate Harbour Bed & Breakfast 37 School Lane Advocate Harbour Lightkeepers Kitchen & Guest House 1 Cape d'Or Rd Advocate Harbour Country Stiles Bed & Breakfast 3936 Hwy 302 Nappan Apothic Inn 169 Victoria St East Amherst https://www.apothicinn.ca/ Brown's Guest Home Bed & Breakfast 158 Victoria St East Amherst -
The Annapolis Basin Scallop Fishery: a Historical Perspective and 1993 Stock Assessment
Scientific Excellence • Resource Protection & Conservation • Benefits for Canadians Excellence scientifique • Protection et conservation des ressources • Bénéfices aux Canadiens DFO Library MPO - Bbliothèque III IIIIHIIIIJIIII II I/9-- - 12022666 The Annapolis Basin Scallop Fishery: A Historical Perspective and 1993 Stock Assessment E. L. Kenchington and M. J. Lundy Benthic Fisheries and Aquaculture Division Biological Sciences Branch Department of Fisheries and Oceans P.O. Box 550 Halifax, Nova Scotia B3J 2S7 1994 Canadian Manuscript Report of Fisheries and Aquatic Sciences No. 2230 5-é-/ 23 Fisheries Pêches 1+1 and Oceans et Océans Canada. Canadian Manuscript Report of Fisheries and Aquatic Sciences Manuscript reports contain scientific and technical information that contributes to existing knowledge but which deals with national or regional problems. Distribu- tion is restricted to institutions or individuals located in particular regions of Canada. However, no restriction is placed on subject matter, and the series reflects the broad interests and policies of the Department of Fisheries and Oceans, namely, fisheries and aquatic sciences. Manuscript reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in Aquatic Sciences and Fisherics Abstracts and indexed in the Department's annual index to scientific and technical publications. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports ( Biological Series) of the Fisherics Research Board of Canada. Numbers 901-1425 were issued as Manuscript Reports of the Fisheries Research Board of Canada. -
Annapolis Basin Bay of Fundy Estuary Profile Annapolis Basin
Bay of Fundy Estuary Profiles Annapolis Basin Bay of Fundy Estuary Profile Annapolis Basin The Annapolis Basin is a sub-basin of the Bay of Fundy along the northwestern shore of Nova Scotia and at the western end of the Annapolis Valley. The Annapolis River is the major water source flowing into the estuary. At the NB mouth of the estuary, a narrow channel known as the Digby Gut connects the 44 NS estuary to the Bay of Fundy. Annapolis Royal and Digby are the main communities along the shore of the estuary, and Kingston-Greenwood is within the catchment area. Near Digby, there is a ferry port that connects to Saint John, New Brunswick. The estuary also hosts a tidal power generating station, which is near Annapolis Royal. The economy within the catchment area is largely driven by agriculture. However, Estuary surface area 104.07 km2 there are also several shellfish and finfish aquaculture tenures, and some Width at estuary mouth 1.85 km commercial fisheries near the mouth of the estuary that largely target Shoreline length 200.63 km invertebrates such as crab, lobster, and clams that inhabit tidal mudflats. The Catchment area 2322.05 km2 extensive tidal mudflats within the estuary are important habitat for Shorebird colonies 2 shorebirds. Within the catchment area there is freshwater habitat for wood Protected area 94.81 km2 turtles, and two protected areas that overlap with the landward boundary of Paved roads 1028 km the estuary. Although the upper valley is primarily agricultural land, much of Aquaculture leases 10 the rest of the catchment area is covered by forest. -
Geological Map of the North Mountain Basalt from Cape Split to Brier Island, with Comments on Its Resource Potential
Report of Activities 2005 39 Geological Map of the North Mountain Basalt from Cape Split to Brier Island, with Comments on its Resource Potential D. J. Kontak Introduction preparation and will be published elsewhere (Kontak, in prep.), where it is demonstrated that the sequence corresponds to other continental flood The Jurassic North Mountain Basalt (NMB) forms basalt provinces (e.g. 65 Ma Deccan Traps, 17- a prominent cuesta along the southern coastline of 15 Ma Columbia River Basalt Group) that have the Bay of Fundy, and is contiguous with outliers analogues in the active flows of Hawaii. This along the northern side of the bay (Fig. 1). This correspondence provides a basis for interpreting the prominent topographic feature, roughly 200 km in volcanological features of the NMB (see Kontak, length, is the focus of this paper and the topic of 2002, for discussion). field studies over the past few years (Kontak, 2000, 2002; Kontak et al., 2005). One result of this work is the first geological map of this unit over the Geological Setting length of the North Mountain (Kontak, 2005, 2006), which provides a basis for assessment of the Numerous, early Mesozoic continental tholeiitic area’s resources. Previous work indicated that the basalt flows, dykes and sills formed along the NMB contained three distinct flow units, referred eastern margin of North America, concurrent with to as the Lower, Middle and Upper flow units the infilling of basins with non-marine sedimentary (Kontak, 2002), and the results of this work have rocks during Pangean rupture, as a prelude to the shown that this subdivision can be extended over opening of the present-day Atlantic Ocean.