Quaternary Studies in Newfoundland: a Short Review C
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The Hitch-Hiker Is Intended to Provide Information Which Beginning Adult Readers Can Read and Understand
CONTENTS: Foreword Acknowledgements Chapter 1: The Southwestern Corner Chapter 2: The Great Northern Peninsula Chapter 3: Labrador Chapter 4: Deer Lake to Bishop's Falls Chapter 5: Botwood to Twillingate Chapter 6: Glenwood to Gambo Chapter 7: Glovertown to Bonavista Chapter 8: The South Coast Chapter 9: Goobies to Cape St. Mary's to Whitbourne Chapter 10: Trinity-Conception Chapter 11: St. John's and the Eastern Avalon FOREWORD This book was written to give students a closer look at Newfoundland and Labrador. Learning about our own part of the earth can help us get a better understanding of the world at large. Much of the information now available about our province is aimed at young readers and people with at least a high school education. The Hitch-Hiker is intended to provide information which beginning adult readers can read and understand. This work has a special feature we hope readers will appreciate and enjoy. Many of the places written about in this book are seen through the eyes of an adult learner and other fictional characters. These characters were created to help add a touch of reality to the printed page. We hope the characters and the things they learn and talk about also give the reader a better understanding of our province. Above all, we hope this book challenges your curiosity and encourages you to search for more information about our land. Don McDonald Director of Programs and Services Newfoundland and Labrador Literacy Development Council ACKNOWLEDGMENTS I wish to thank the many people who so kindly and eagerly helped me during the production of this book. -
Gros Morne National Park of Canada Management Plan, 2019
Management Plan Gros Morne 2019 National Park of Canada 2019 Gros Morne National Park of Canada A UNESCO World Heritage Site Management Plan ii © Her Majesty the Queen in Right of Canada, represented by the Chief Executive Officer of Parks Canada, 2019. Gros Morne National Park of Canada Management Plan, 2019. Paper: R64-105/67-2019E 978-0-660-30733-6 PDF: R64-105/67-2019E-PDF 978-0-660-30732-9 Cette publication est aussi disponible en français. For more information about the management plan or about GROS MORNE NATIONAL PARK: GROS MORNE NATIONAL PARK PO Box 130 Rocky Harbour, NL A0K 4N0 Tel: 709-458-2417 Email: [email protected] www.pc.gc.ca/en/pn-np/nl/grosmorne Front cover image credits top from left to right: G. Paquette-Jetten/Parks Canada, D. Kennedy, S. Stone/Parks Canada, bottom: G. Paquette-Jetten/Parks Canada Gros Morne National Park iii Management Plan Foreword Canada’s national parks, national historic sites and national marine conservation areas belong to all Canadians and offer truly Canadian experiences. These special places make up one of the finest and most extensive systems of protected natural and cultural heritage areas in the world. The Government is committed to preserving our natural and cultural heritage, expanding the system of protected places and contributing to the recovery of species-at-risk. At the same time, we must continue to offer new and innovative visitor and outreach programs and activities so that more Canadians can experience Parks Canada places and learn about our environment, history and culture. -
Gros Morne National Park
Gros Morne National Park Tuckamore, a Visitor's Guide 1 Cow Head Trail: S.Stone Trail: Cow Head Contact Information Table of Contents Gros Morne National Park of Canada 2 World Heritage P.O. Box 130, Rocky Harbour, NL 4 Great Experiences A0K 4N0 6 Scenic Drives [email protected] 8 Take a Walk www.pc.gc.ca/grosmorne (709) 458-2417 10 Great Small Adventures Campground 12 Boat Tours and Marine Reservations Encounters 1-877-737-3783 / (TTY 1-866-787-6221) 14 Interpretation: Explore with a park interpreter Swimming Pool 16 Trail Guide/Map (709) 458-2350 18 Camping Boat Tours Trout River Pond 20 Wildlife (709) 636-6727 22 Conservation Western Brook Pond 24 History and Heritage (709) 458-2016 / 1-888-458-2016 26 Cultural Crossroads Ferry Information/ 28 Friends Reservations 29 North of the Park Marine Atlantic 1-800-341-7981 30 Port Au Choix Strait of Belle Isle 31 L’Anse Aux Meadows (St. Barbe) 32 Red Bay 1-866-535-2567 33 Distance Chart Bus and Taxi Services Welcome to Gros Morne National Park Viking 430 Shuttle and Tours In 2011, Parks Canada is celebrating its 100th birthday! When the Dominion While here, why not take the Explorer Quotient Quiz™ that is available from a (709) 458-8186 / 3016 Parks Branch was created in 1911, it was the first parks service in the world. number of convenient locations throughout the park area? It’s a fun tool that What's in a name? Martin’s Transportation Gros Morne is proud to join Parks Canada’s family of national parks and will profile what kind of explorer you are according to your unique interests (709) 453-7269 / 2207 The name Gros Morne national historic sites to mark the centennial. -
Portage Pond Subregion NF 1 H E C E N T R a L Named After Portage Pond, Which Lies at the Heart 2 T Newfoundland Forest of the Subregion
ECOREGION Forest Barren Tundra Central Newfoundland Forest Bog Portage Pond subregion NF 1 h e C e n t r a l named after Portage Pond, which lies at the heart 2 T Newfoundland Forest of the subregion. 2 ecoregion covers about Although summer temperatures are higher c 28,000 km2 of the central in this ecoregion than elsewhere on the Island, and northeastern third of they are not as high in the Portage Pond subregion 3 the island of Newfoundland. The Central as in the North-central subregion. Warm summer Newfoundland Forest has the most typically temperatures, and its location east of the Long boreal forests of all the Island's ecoregions, and Range Mountains, make this subregion — and all 4 its climate is the most continental. On of the ecoregion — one of the driest on the average, the highest summer and lowest Island. Not surprisingly, this leads to a large 5 winter temperatures on the Island occur number of forest fires. Only the North-central in this ecoregion, which also has the subregion experiences more fires. least amount of wind and fog. Bogs are common in the Portage 6 The mountain forests and P o n d s u b r e g i o n , a n d a r e bogs that make up the 1,493.2 distinguished from those of the km² Portage Pond subregion n e i g h b o u r i n g W e s t e r n 7 extend over a small south- Portage Pond Newfoundland Forest by the western portion of the subregion absence of some plants — in Central Newfoundland particular, dwarf huckleberry and 8 Forest. -
Grade 3 Social Studies Curriculum Guide (2011)
Social Studies Grade 3 Interim Edition Curriculum Guide 2011 TABLE OF CONTENTS Table of Contents Acknowledgements.......................................................................................................................... i Introduction. Background............................................................................................................................................................. 1 Aims.of.Social.Studies............................................................................................................................................. 1 Purpose.of.Curriculum.Guide.................................................................................................................................. 1 Guiding.Principles.................................................................................................................................................... 2 Program.Design.and.Outcomes. Overview................................................................................................................................................................. 3 Essential.Graduation.Learnings............................................................................................................................... 4 General.Curriculum.Outcomes............................................................................................................................... .6 Processes................................................................................................................................................................ -
Geological Guide to the Bird Cove Region, Great Northern Peninsula
Author’s Address I. Knight W.D. Boyce Department of Natural Resources Department of Natural Resources Geological Survey Geological Survey P.O. Box 8700 P.O. Box 8700 St. John’s, NL, A1E 2H7 St. John’s, NL, A1E 2H7 Tel. 709-729-4119 Tel. 709-729-2163 E-mail: [email protected] E-mail: [email protected] NOTE Open File reports and maps issued by the Geological Survey Division of the Newfoundland and Labrador Department of Natural Resources are made available for public use. They have not been formally edited or peer reviewed, and are based upon preliminary data and evaluation. The purchaser agrees not to provide a digital reproduction or copy of this product to a third party. Derivative products should acknowledge the source of the data. DISCLAIMER The Geological Survey, a division of the Department of Natural Resources (the “authors and publish- ers”), retains the sole right to the original data and information found in any product produced. The authors and publishers assume no legal liability or responsibility for any alterations, changes or misrep- resentations made by third parties with respect to these products or the original data. Furthermore, the Geological Survey assumes no liability with respect to digital reproductions or copies of original prod- ucts or for derivative products made by third parties. Please consult with the Geological Survey in order to ensure originality and correctness of data and/or products. SAFETY CAUTION Many of the localities discussed in this guide can be visited along roadsides, in quarries and along the shore. In each case, care should be exercised to avoid injury by moving vehicles, falling rocks (use hard hats if possible in quarries) and rough seas. -
The Late Proterozoic to Palaeozoic Tectonic Evolution of the Long Range Mountains in Southwestern Newfoundland
The Late Proterozoic to Palaeozoic Tectonic Evolution of the Long Range Mountains in southwestern Newfoundland by Arjan Gerben Brem A thesis presented to the University of Waterloo in fulfillment of the thesis requirement for the degree of Doctor of Philosophy in Earth Sciences Waterloo, Ontario, Canada, 2007 © Arjan G. Brem, 2007 Author’s declaration I hereby declare that I am the sole author of this thesis. This is a true copy of the thesis, including any required final revisions, as accepted by my examiners. I understand that my thesis may be made electronically available to the public. ii Abstract Ever since the first plate-tectonic model for the Appalachians was proposed, the Laurentian margin has been interpreted as having experienced a collision-related dynamo-thermal event during the Middle Ordovician Taconic orogeny. In the western Newfoundland Appalachians, evidence for this collision is well-preserved in the Dashwoods subzone. Nevertheless, rocks of the neighbouring Corner Brook Lake block (CBLB), which is located in the heart of the Laurentian realm, did not show evidence for such an event. Instead, it was affected by Early Silurian Salinic deformation and associated peak metamorphism. Even though this difference in Early Palaeozoic tectonic history between the Dashwoods and the CBLB is widely known, it has not been satisfactorily explained. To better understand the Early Palaeozoic history of the region, in particular to test and better explain the lack of a Taconic dynamo-thermal event in the CBLB, field mapping, microscopic work, and U-Pb and 40Ar/39Ar geochronological studies were undertaken in the western and northern part of the Dashwoods subzone, and in the southern part of the CBLB. -
Arctic Hare (Lepus Arcticus Bangsii)
The Status of Arctic Hare (Lepus arcticus bangsii) in Insular Newfoundland © Steve Sayles THE SPECIES STATUS ADVISORY COMMITTEE REPORT NO. 26 February 20, 2012 RECOMMENDED STATUS Recommended status: Current designation: DATA DEFICIENT None Criteria met: Data Deficient Reasons for designation: Uncertain taxonomic distinction Unknown area of occupancy Uncertain number of extant locations Unknown trend in number of locations Unknown habitat trend Uncertain population size Unknown population size trend Unknown if extreme population size fluctuations (>1 order of magnitude) This report was originally prepared by Brian Hearn and subsequently edited by the Species Status Advisory Committee. 2 STATUS REPORT Lepus arcticus bangsii (Rhoads, 1896) Arctic hare (Newfoundland population) lièvre arctique, Ukaliq Family: Leporidae (Hares and Rabbits) Life Form: Mammal Systematic/Taxonomic Clarifications This report examines the arctic hare population on the island of Newfoundland, a population within the subspecies Lepus arcticus bangsii, as a discrete and evolutionarily significant designatable unit because of its geographic and presumed reproductive isolation and its distinction as the southernmost population of arctic hare in North America. The taxonomy of the arctic or northern hare group(s) is disputed. Presently, three species of arctic (northern) hare are recognized: the Arctic hare (Lepus arcticus) occupying the tundra regions of Canada and along the coastal regions of Greenland; the Alaskan hare (Lepus othus) which is restricted to the western and northwestern regions of Alaska; and the Mountain hare (Lepus timidus) which is found throughout most of the Palaearctic region from Great Britain and Fennoscandia to eastern Siberia (Figure 1). Not surprisingly, the taxonomic status of these three species has been a long-standing controversy (Hall 1951, Best and Henry 1994). -
Grade 3 Social Studies That Have Been Organized According and Perspectives to the Six Conceptual Strands and the Three Processes
2012 Prince Edward Island Department of Education and Early Childhood Development 250 Water Street, Suite 101 Summerside, Prince Edward Island Canada, C1N 1B6 Tel: (902) 438-4130 Fax: (902) 438-4062 www.gov.pe.ca/eecd/ CONTENTS Acknowledgments The Prince Edward Island Department of Education and Early Childhood Development acknowledges the work of the social studies consultants and other educators who served on the regional social studies committee. New Brunswick Newfoundland and Labrador John Hildebrand Darryl Fillier Barbara Hillman Nova Scotia Prince Edward Island Mary Fedorchuk Bethany Doiron Bruce Fisher Laura Ann Noye Rick McDonald Jennifer Burke The Prince Edward Island Department of Education and Early Childhood Development also acknowledges the contribution of all the educators who served on provincial writing teams and curriculum committees, and who reviewed or piloted the curriculum. The Prince Edward Island Department of Education and Early Childhood Development recognizes the contribution made by Tammy MacDonald, Consultation/Negotiation Coordinator/Research Director of the Mi’kmaq Confederacy of Prince Edward Island, for her contribution to the development of this curriculum. ATLANTIC CANADA SOCIAL STUDIES CURRICULUM GUIDE: GRADE 3 i CONTENTS ii ATLANTIC CANADA SOCIAL STUDIES CURRICULUM GUIDE: GRADE 3 CONTENTS Contents Introduction Background ..................................................................................1 Aims of Social Studies ..................................................................1 Purpose -
U-Pb Detrital Zircon Geochronology of the South Portuguese Zone
12 ATLANTIC GEOSCIENCE SOCIETY 37th COLLOQUIUM & ANNUAL GENERAL MEETING February 11-12, 2011, The Fredericton Inn, Fredericton, New Brunswick PROGRAM Meetings, technical sessions, luncheon, and banquet are all at the The Fredericton Inn, Fredericton, New Brunswick (Phone 1-800-561-8777 or http://www.frederictoninn.nb.ca for reservations). For Colloquium registration information contact Kay Thorne @ (506) 453-2206; email: [email protected] or check the AGS website http://ags.earthsciences.dal.ca/ags.php. Friday, February 11, 2011 8:30-5:00pm Workshop: Applications of Laser Ablation to Problems in Mineral Exploration and Ore Petrogenesis. (Quartermain Centre, Room 104, UNB Geology) 1:00-4:30pm Tour: Potash Corporation of Saskatchewan mine and mill, Sussex, NB. (Participants are responsible for their own transportation to and from Sussex) 3:00-4:30pm Tour: UNB's EM facilities (UNB Geology) 3:00-4:30pm Tour: Research and Productivity Council of New Brunswick Mineral Process Development and Testing (921 College Hill Road, Fredericton) 3:30-10:00pm Registration (Foyer) 4:00-5:30pm Poster set-up (Salon A). Friday evening talk set-up (All Friday presenters should load their PowerPoint presentations at this time) 4:15-5:00pm Atlantic Geology Editors Meeting (Salon B) 5:00-7.00 pm AGS Council Meeting (Salon B) 5:30-7:00pm Poster Session I (Salon A). Cash bar. Sandwiches sponsored by Geodex Minerals. 7:00-8:20pm Special Session: New Developments in the Appalachian Orogen: a Symposium in Honour of Hank Williams I - Royal Stewart Room 7:00-8:20pm -
SURFICIAL GEOLOGY of the ST. FINTAN's, LITTLE FRIARS COVE and FLAT BAY MAP AREAS (NTS 12B/2, 12B/3 and 12B/7)
Current Research (1999) Newfoundland Department of Mines and Energy Geological Survey, Report 99-1, pages 139-147 SURFICIAL GEOLOGY OF THE ST. FINTAN'S, LITTLE FRIARS COVE AND FLAT BAY MAP AREAS (NTS 12B/2, 12B/3 and 12B/7) D.G.E. Liverman, K. Sheppard1 and D. Taylor Geophysics, Geochemistry and Terrain Sciences Section ABSTRACT The surficial geology of southern St. George's Bay consists of a broad coastal plain covered by till inland and gravel clos- er to the coast. In the highland areas, a mix of bedrock, till veneers and patches of thicker till is found. Ice-flow mapping was through a combination of till fabric analysis and striation mapping. An early, coast parallel flow, possibly originating from outflow from the Stephenville area, deflected by ice in the Gulf of St. Lawrence, is identified. As ice retreated, ice-flow direc- tions changed to be dominantly westward, from an ice cap centred over the adjacent Long Range Mountains. Although there is no conclusive evidence, erratics and striae found in the Anguille Mountains suggest that their summits were over-topped by ice. Further retreat led to topographic control of ice flow, with diversion of ice along the valley containing Codroy Pond. Deglaciation resulted in complex sedimentary sequences, now exposed at the coast, as the ice sheet grounded in the sea. Thick marine clays pose a geotechnical problem in construction. Such clays are highly susceptible to slope failure, as shown by large rotational slumps along the coast. The coast is eroding rapidly, and construction close to the current cliff edge should be avoided. -
Climate Change and Renewable Resources in Labrador: Looking Toward 2050 Workshop Report
Climate Change and Renewable Resources in Labrador: Looking toward 2050 Workshop Report Hosted by Labrador Highlands Research Group and Labrador Institute of Memorial University North West River, Labrador, March 11–13, 2008 © 2008, Labrador Highlands Research Group Recommended citation: Bell, T., Jacobs, J.D., Munier, A., Leblanc, P., and Trant, A. 2008. Climate Change and Renewable Resources in Labrador: Looking toward 2050. Proceedings and Report of a Conference held in North West River, Labrador, 11–13 March. St. John’s: Labrador Highlands Research Group, Memorial University of Newfoundland, 95 p and CD‐Rom. 2 Climate Change and Renewable Resources in Labrador: Looking toward 2050 TABLE OF CONTENTS Executive Summary.....................................................................................................................................................5 Acknowledgements and Sponsors ..............................................................................................................................8 Conference Rationale and Overview..........................................................................................................................9 Conference Structure ................................................................................................................................................10 Conference Hosts .......................................................................................................................................................11 Labrador Highlands Research