Fundy Tidal Energy Demonstration Project Volume I: Environmental Assessment
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BLAZING the TRAIL in NOVA SCOTIA in Canada’S Second Ook Up, Way Up, Because Glooscap Is a Giant in Atlantic Canada’S Mi’Kmaq Culture
article and photos by Jan Napier BLAZING THE TRAIL IN NOVA SCOTIA In Canada’s second ook up, way up, because Glooscap is a giant in Atlantic Canada’s Mi’kmaq culture. This almighty being was of such gargantuan proportions that the smallest province, a province of Nova Scotia was his bed and Prince Edward Island his pillow. larger-than-life demigod, Ancient legends of the mythical creator live on, and there’s no better place Lto explore them than the spectacular Glooscap Trail in northwestern Nova Scotia. over-the-top scenery and The trail stretches 227 miles, all told, but our itinerary focuses on a 125-mile the world’s highest tides segment between Truro and Joggins. It’s a laid-back, mostly coastal drive, beloved by those in the know. set the stage for RV The Mi’kmaq (pronounced Meeg-mah), an indigenous people native to travels on a grand scale Canada’s Maritime Provinces and the Gaspé Peninsula of Quebec, once lived freely in this region. Silas Tertius Rand, a Baptist missionary who traveled among the Mi’kmaq in the mid- to late-1800s, documented their stories featuring the heroic Glooscap. He “lived like other men ... but he never died, never was sick, never grew old,” wrote Rand. “He could do anything and everything.” Traveling RVers can learn more about Mi’kmaq myths and culture, and stand — dwarfed — beneath the demigod’s towering bronze likeness, at the Glooscap Heritage Centre, less than 5 miles from Truro in Millbrook. If you’re lucky, Climb Five Islands Lighthouse Program Director Gordon Pictou or a heritage interpreter will be on hand to for panoramic views of the Bay of Fundy, Minas Basin and the share some of the Mi’kmaq creation stories, like the one about Five Islands. -
Preliminary Management Plan May 2009
NovaNova ScotiaScotia ProvincialProvincial ParksParks Preliminary Management Plan May 2009 Cape Split Provincial Park Reserve ...discover our nature 1.0 EXECUTIVE SUMMARY ..................................................1 2.0 INTRODUCTION .........................................................2 3.0 VISION ..................................................................3 Vision .................................................................3 4.0 PARK VALUES ...........................................................3 Natural Heritage .......................................................4 Geology .........................................................4 Marine Environment ..............................................4 Flora ...........................................................4 Fauna ...........................................................5 Cultural Heritage .................................................5 Outdoor Recreation .....................................................6 Outdoor Education .....................................................6 Tourism ...............................................................6 5.0 PARK OBJECTIVES ......................................................7 Protection .............................................................7 Outdoor Recreation .....................................................7 Heritage Appreciation ...................................................7 Tourism ...............................................................8 6.0 PARK CLASSIFICATION ..................................................8 -
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. -
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. -
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. -
R E P O R T S 112 Structure of the Minas Passage, Bay of Fundy: A
Reports 112 Structure of the Minas Passage, Bay of Fundy: A Preliminary Report* DONALD J. P. SWIFT Duke University, Durham, N. C. FRANK L. JAGODITS Huntec Limited, Toronto, Ont. BERNARD L. MANISTRE Lockwood Survey Corporation Limited, Toronto, Ont. NORMAN R. PATERSON Huntec Limited, Toronto, Ont. Introduction From July, 1965 to March, 1966, a joint geological-geophysical study of the Minas Passage, Bay of Fundy, was undertaken by Huntec Limited of Toronto for the Atlantic Development Board of Canada. The purpose of the project was to test the feasibility of a tidal power station in the Passage. This paper presents a portion of the study, namely the structure of the geologically critical Minas Passage area and its bearing on regional structure. The Bay of Fundy is a funnel-shaped body of water lying between Nova Scotia and New Brunswick (Fig. 1). Fundy proper is 144 kilometers long, 100 kilometers wide at the base, and averages 75 meters in depth. The northeast end bifurcates into northeast-trending Chignecto Bay, and the east-trending Minas Basin. Three distinct bodies of water are included within the latter; the Minas Basin proper; the Minas Channel, separated from the basin by the great curved peninsula of Cape Blomidon-Cape Split; and the Minas Passage, connecting the Channel and the Basin (Fig. 2). ^Manuscript received 12 January, 1968. Reports 113 -V. N - ~M ' , , , - I . , I - I Figure 2 - The Minas Passage with Cape Split in the background. Stratigraphy Three well-defined bedrock sequences occur in the Minas Passage area. The Cobequid Complex is a lower Paleozoic metamorphic and igneous complex comprising the upraised Cobequid Fault Block (Fig. -
The Atlantic Geoscience Society (AGS) La Société Géoscientifique De L’Atlantique
The Atlantic Geoscience Society (AGS) La Société Géoscientifique de l’Atlantique 42nd Colloquium and Annual Meeting Special Sessions: Geoscience Education and Outreach: Creating an Awareness Offshore Geology of Eastern Canada Tin-related mineralization and exploration in the Maritimes Dates, Rates, and Durations of Tectonic Processes Advances in Carboniferous Geology in the Atlantic Provinces General Sessions: Current Research in the Atlantic Provinces 5-6 February, 2016 Holiday Inn, Truro, Nova Scotia PROGRAM WITH ABSTRACTS We gratefully acknowledge sponsorship from the following companies and organizations: Department of Energy Department of Natural Resources Welcome to the 42nd Colloquium and Annual Meeting of the Atlantic Geoscience Society in Truro. This is a new venue for us this year, and we hope you will soon find your way around both the hotel and the town. You have contributed a very full program, which we hope you will find stimulating, broadening, and the source of much discussion. AGS members are clearly pushing the boundaries of geoscience in all its branches! Be sure to take in the science on the posters and the displays from sponsors. And don’t miss the after-banquet jam and open mike on Saturday night. For social media types, please consider sharing updates on Facebook. We hope you will be able to use the weekend to renew old acquaintances, make new ones, and further the aims of your Atlantic Geoscience Society. The organizers: Tim Fedak, Bob Grantham, Rob Raeside, Chris White 2 ATLANTIC GEOSCIENCE SOCIETY 42nd COLLOQUIUM AND ANNUAL GENERAL MEETING 5-6 February, 2016, Holiday Inn, Truro, Nova Scotia PROGRAM SUMMARY Locations: see campus plan, inside back cover Friday, 5th February, 2016 9.00 – 4.00 p.m. -
The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus
19 The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus Paul E. Olsen and Emma C. Rainforth nomoepus is an Early Jurassic footprint genus and 19.2). Because skeletons of dinosaur feet were not produced by a relatively small, gracile orni- known at the time, he naturally attributed the foot- A thischian dinosaur. It has a pentadactyl ma- prints to birds. By 1848, however, he recognized that nus and a tetradactyl pes, but only three pedal digits some of the birdlike tracks were associated with im- normally impressed while the animal was walking. The pressions of five-fingered manus, and he gave the name ichnogenus is diagnosed by having the metatarsal- Anomoepus, meaning “unlike foot,” to these birdlike phalangeal pad of digit IV of the pes lying nearly in line with the axis of pedal digit III in walking traces, in combination with a pentadactyl manus. It has a pro- portionally shorter digit III than grallatorid (theropod) tracks, but based on osteometric analysis, Anomoepus, like grallatorids, shows a relatively shorter digit III in larger specimens. Anomoepus is characteristically bi- pedal, but there are quadrupedal trackways and less common sitting traces. The ichnogenus is known from eastern and western North America, Europe, and southern Africa. On the basis of a detailed review of classic and new material, we recognize only the type ichnospecies Anomoepus scambus within eastern North America. Anomoepus is known from many hundreds of specimens, some with remarkable preservation, showing many hitherto unrecognized details of squa- mation and behavior. . Pangea at approximately 200 Ma, showing the In 1836, Edward Hitchcock described the first of what areas producing Anomoepus discussed in this chapter: 1, Newark we now recognize as dinosaur tracks from Early Juras- Supergroup, eastern North America; 2, Karoo basin; 3, Poland; sic Newark Supergroup rift strata of the Connecticut 4, Colorado Plateau. -
They Planted Well: New England Planters in Maritime Canada
They Planted Well: New England Planters in Maritime Canada. PLACES Acadia University, Wolfville, Nova Scotia, 9, 10, 12 Amherst Township, Nova Scotia, 124 Amherst, Nova Scotia, 38, 39, 304, 316 Andover, Maryland 65 Annapolis River, Nova Scotia, 22 Annapolis Township, Nova Scotia, 23, 122-123 Annapolis Valley, Nova Scotia, 10, 14-15, 107, 178 Annapolis County, Nova Scotia, 20, 24-26, 28-29, 155, 258 Annapolis Gut, Nova Scotia, 43 Annapolis Basin, Nova Scotia, 25 Annapolis-Royal (Port Royal-Annapolis), 36, 46, 103, 244, 251, 298 Atwell House, King's County, Nova Scotia, 253, 258-259 Aulac River, New Brunswick, 38 Avon River, Nova Scotia, 21, 27 Baie Verte, Fort, (Fort Lawrence) New Brunswick, 38 Barrington Township, Nova Scotia, 124, 168, 299, 315, Beaubassin, New Brunswick (Cumberland Basin), 36 Beausejour, Fort, (Fort Cumberland) New Brunswick, 17, 22, 36-37, 45, 154, 264, 277, 281 Beaver River, Nova Scotia, 197 Bedford Basin, Nova Scotia, 100 Belleisle, Annapolis County, Nova Scotia, 313 Biggs House, Gaspreau, Nova Scotia, 244-245 Blomidon, Cape, Nova Scotia, 21, 27 Boston, Massachusetts, 18, 30-31, 50, 66, 69, 76, 78, 81-82, 84, 86, 89, 99, 121, 141, 172, 176, 215, 265 Boudreau's Bank, (Starr's Point) Nova Scotia, 27 Bridgetown, Nova Scotia, 196, 316 Buckram (Ship), 48 Bucks Harbor, Maine, 174 Burton, New Brunswick, 33 Calkin House, Kings County, 250, 252, 259 Camphill (Rout), 43-45, 48, 52 Canning, Nova Scotia, 236, 240 Canso, Nova Scotia, 23 Cape Breton, Nova Scotia, 40, 114, 119, 134, 138, 140, 143-144 2 Cape Cod-Style House, 223 -
Wampanoag, Tribespeople “Of the Dawn”
THE WAMPANOAG, TRIBESPEOPLE “OF THE DAWN” “Ye see, Hinnissy, th’ Indyun is bound f’r to give way to th’ onward march iv white civilization. You ’an me, Hinnissy, is th’ white civilization... The’ on’y hope f’r th’ Indyun is to put his house on rollers, an’ keep a team hitched to it, an’, whin he sees a white man, to start f’r th’ settin’ sun.” — Finley Peter Dunne, OBSERVATIONS BY MR. DOOLEY, New York, 1902 HDT WHAT? INDEX WAMPANOAG WAMPANOAG When the English settlements first commenced in New England, that part of its territory, which lies south of New Hampshire, was inhabited by five principal nations of Indians: the Pequots, who lived in Connecticut; the Narragansets, in Rhode Island; the Pawkunnawkuts, or Womponoags, east of the Narragansets and to the north as far as Charles river;1 the Massachusetts, north of Charles river and west of Massachusetts Bay; and the Pawtuckets, north of the Massachusetts. The boundaries and rights of these nations appear not to have been sufficiently definite to be now clearly known. They had within their jurisdiction many subordinate tribes, governed by sachems, or sagamores, subject, in some respects, to the principal sachem. At the commencement of the seventeenth century, they were able to bring into the field more than 18,000 warriors; but about the year 1612, they were visited with a pestilential disease, whose horrible ravages reduced their number to about 1800.2 Some of their villages were entirely depopulated. This great mortality was viewed by the first Pilgrims, as the accomplishment of one of the purposes of Divine Providence, by making room for the settlement of civilized man, and by preparing a peaceful asylum for the persecuted Christians of the old world.