Nova Scotia Field Guide
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ABCO Industries Limited 1 HANSARD INDEX A ABCO Industries Limited, Machine Shop Division - Occupational Health and Safety Workplace Achievement Award: Employers/Employees - Congratulations (res. 1200), n 3527, app 3527 Aboriginal Affairs - Aboriginal Art Exhibit: Participants - Congratulations (res. 416), n 981, app 982 Aboud, Crystal: Allister MacIntyre Memorial Trophy/Scholarship - Congratulations (res. 1400), n 4017, app 4018 Acadia Park (Westville) - Signs: Western Star Lodge - Members Thank (res. 1389), n 4005 Acadia University, 93 Acadia University: Pioneer Award - Congratulations (res. 79), n 171, app 172 Acadian Affairs - Acadian/Francophone Community: Contribution - Recognize (res. 6), n 38, app 39 Acadian Affairs - Executive Director: Position - Interview Details, qu 2955 Acadian Federation of Nova Scotia - Equipe Acadie: Participants - Congratulations (res. 388), n 892, app 893 Acadian Games (17th Regional): Participants/Volunteers - Congratulations (res. 1287), n 3794, app 3795 Acadians - Economy/Culture: Contribution - Recognize (res. 520), n 1197 Access Awareness Week - Support: Access Efforts - Year-Round Achieve (res. 1416), n 4029, app 4030 Access Awareness Week (27/05-02/06/01): Partnership for Access Awareness/Participants - Congratulations (res. 1478), n 4230, app 4231 ACS Trading, Division of Farocan Incorporated/St. Anne Community Nursing Care Centre - Occupational Health and Safety Workplace Achievement Awards: Employers/Employees - Congratulations (res. 1178), n 3507 Adams, Mrs. Beatrice - Salute: East Preston United Baptist Church Ladies Auxiliary - Commend (res. 1497), n 4311 ADDRESS IN REPLY to Speech from the Throne Carey, Mr. J., 151-155 Clarke, Mr. C., 24-28 Estabrooks, Mr. W., 156-165 Gaudet, Mr. W., 231-239 MacDonald, Mr. Manning, 135-151 MacDonell, Mr. J., 28-31; 69-79 Olive, Mr. -
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. -
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. -
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 -
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 -
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 -
Geology of the West-Central Cape Breton Highlands, Nova Scotia
Geological Survey of Canada Commission géologique du Canada Paper 87-13 GEOLOGY OF THE WEST-CENTRAL CAPE BRETON HIGHLANDS, NOVA SCOTIA R.A. Jamieson P. Tall man J.A. Marcotte H.E. Plint K.A. Connors 1987 Canada Department of Mines and Energy Contribution to Canada-Nova Scotia Mineral Development Agreement 1984-89, a subsidiary agreement under the Economic and Regional Development Agreement. Project funded by the Geological Survey of Canada. Contribution à l'Entente auxiliaire Canada/ Nouvelle Ecosse sur l'Exploitation minérale 1984-89 faisant partie de l'Entente de développement économique et régional. Ce projet a été financé par la Commission géologique du Canada. Energy, Mines and Énergie, Mines et Resources Canada Resso1 Tces Canada Geological Survey of Canada Paper 87-13 GEOLOGY OF THE WEST-CENTRAL CAPE BRETON HIGHLANDS, NOVA SCOTIA R.A. Jamieson P. Tallman J.A. Marcotte H.E. Plint K.A. Connors 1987 GEOLOGY OF THE WEST-CENTRAL CAPE BRETON HIGHLANDS, NOVA SCOTIA Abstract Mapping of metavolcanic, metasedimentary, and metaplutonic rocks in the vicinity of the Northeast Margaree River, west-central Cape Breton Highlands, has been carried out on 1:10 000 and 1:25 000 scales. The Jumping Brook metamorphic suite (redefined) consists of a lower unit of metabasalts and associated pyroclastic and sedimentary rocks (Faribault Brook metavolcanics), overlain by quartz-rich sedimentary rocks with local conglomerate and tuff (Barren Brook schist), and semi-pelitic to psammitic schists (Dauphinee Brook schist), which grade into porphyroblastic schists ranging up to staurolite-kyanite grade (Corney Brook schist). Medium grained amphibolite (George Brook amphibolite) with relict dioritic texture is common in the sequence and probably represents synvolcanic intrusions. -
Canadian Maritimes Nova Scotia | New Brunswick | Prince Edward Island
NO SINGLE SUPPLEMENT SfoMr SAoLloL T GraRvOelUerP s Ma xi mum of LAND 24 Travele rs SMALL GROUP JO URNEY Ma xi mum of 24 Travele rs Canadian Maritimes Nova Scotia | New Brunswick | Prince Edward Island Inspiring Moments > Delight in picture-perfect fishing villages, historic beacons and quiet coves along Nova Scotia’s Lighthouse Route. > Take in sensational ocean vistas on the Cabot Trail, one of Canada’s INCLUDED FEATURES most scenic roads, that hugs Cape Breton Island’s coastline. Accommodations (with baggage handling) Itinerary – 2 nights in Halifax, Nova Scotia, Canada, Day 1 Depart gateway city . Arrive in > Spot whales breaching in the Bay at the Halifax Marriott Harbourfront Hotel, Halifax and transfer to hotel of Fundy, a favorite summer gathering a first-class property. Day 2 Halifax | Lunenburg spot for up to 12 different species. – 2 nights in Saint John, New Brunswick, Day 3 Annapolis Valley | Grand-Pr é > Marvel at the Bay’s mighty tides, the at the first-class Hilton Saint John. National Historic Site | Embark world’s highest, at Hopewell Rocks. – 2 nights in Charlottetown, Prince ferry | Saint John Edward Island, at the first-class Day 4 Saint John | St. Andrews > Immerse yourself in the enchanting Prince Delta Hotels Prince Edward. Day 5 Hopewell Rocks Park | Edward Island settings that inspired the – 2 nights in Baddeck, Nova Scotia, at the Moncton | Charlottetown Anne of Green Gables books. first-class Auberge Gisele’s Inn. Day 6 Prince Edward Island > Delve into the provinces’ enduring bond – 1 night in Halifax at the Halifax Marriott Day 7 Embark ferry | Cape Breton with the sea, from shipbuilding to fishing, Harbourfront Hotel, a first-class property. -
Pre-Carboniferous Tectonostrati Graphic Subdivisions of Cape Breton Island, Nova Scotia Sandra M
Document generated on 09/26/2021 10:55 a.m. Atlantic Geology Pre-CarbonIferous TectonostratI graphIc Subdivisions of Cape Breton Island, Nova Scotia Sandra M. Barr and Robert P. Raeside Volume 22, Number 3, December 1986 Article abstract Cape Breton Island can be divided Into four zones on the basis of contrasting URI: https://id.erudit.org/iderudit/ageo22_3art03 stratigraphy, metamorphism, and plutonlsm. A Southeastern zone Is characterized by late Precambrian volcanism and plutonlsm, followed by See table of contents Cambro-Ordovlclan rlft-baslu sedimentation and minor volcanlsm. The Bras d'Qr zone to the northwest Is underlain by gnelsslc basement and overlying platforms! (carbonate and clastic) sedimentary rocks. Intruded by mainly late Publisher(s) Precambrian and Grdovician(?) granitoid rocks. The fflghlands zone has a gnelsslc core flanked by typically lower grade sedimentary and volcanic rocks Atlantic Geoscience Society of probable Precambrian age intruded by diverse and abundant dioritlc to granitic plutons ranging In age from Precambrlfln to Carboniferous. The ISSN Northwestern m^tmA» zone has gnelsslc basement Intruded by varied plutonlc rocks Including anorthosite and syenite, the latter of GrenvUUan age. The 0843-5561 (print) nature and significance of the boundaries between these zones are as yet 1718-7885 (digital) uncertain, but only the Southeastern and Bras d'Qr zones are considered to be part of the Avalon Terrane. Explore this journal Cite this article Barr, S. M. & Raeside, R. P. (1986). Pre-CarbonIferous TectonostratI graphIc Subdivisions of Cape Breton Island, Nova Scotia. Atlantic Geology, 22(3), 252–263. All rights reserved © Atlantic Geology, 1986 This document is protected by copyright law. -
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. -
Nova Scotia Inland Water Boundaries Item River, Stream Or Brook
SCHEDULE II 1. (Subsection 2(1)) Nova Scotia inland water boundaries Item River, Stream or Brook Boundary or Reference Point Annapolis County 1. Annapolis River The highway bridge on Queen Street in Bridgetown. 2. Moose River The Highway 1 bridge. Antigonish County 3. Monastery Brook The Highway 104 bridge. 4. Pomquet River The CN Railway bridge. 5. Rights River The CN Railway bridge east of Antigonish. 6. South River The Highway 104 bridge. 7. Tracadie River The Highway 104 bridge. 8. West River The CN Railway bridge east of Antigonish. Cape Breton County 9. Catalone River The highway bridge at Catalone. 10. Fifes Brook (Aconi Brook) The highway bridge at Mill Pond. 11. Gerratt Brook (Gerards Brook) The highway bridge at Victoria Bridge. 12. Mira River The Highway 1 bridge. 13. Six Mile Brook (Lorraine The first bridge upstream from Big Lorraine Harbour. Brook) 14. Sydney River The Sysco Dam at Sydney River. Colchester County 15. Bass River The highway bridge at Bass River. 16. Chiganois River The Highway 2 bridge. 17. Debert River The confluence of the Folly and Debert Rivers. 18. Economy River The highway bridge at Economy. 19. Folly River The confluence of the Debert and Folly Rivers. 20. French River The Highway 6 bridge. 21. Great Village River The aboiteau at the dyke. 22. North River The confluence of the Salmon and North Rivers. 23. Portapique River The highway bridge at Portapique. 24. Salmon River The confluence of the North and Salmon Rivers. 25. Stewiacke River The highway bridge at Stewiacke. 26. Waughs River The Highway 6 bridge.