Hiking Routes of the Long Range

Total Page:16

File Type:pdf, Size:1020Kb

Hiking Routes of the Long Range 436000 437000 438000 439000 440000 441000 442000 443000 444000 445000 446000 447000 448000 449000 450000 451000 452000 453000 454000 455000 456000 457000 458000 459000 460000 461000 462000 463000 464000 0 0 0 0 0 0 6 6 1 1 5 5 5 5 Hiking Routes of the Western Brook Pond Trailhead NR-1 Long Range Mountains 0 0 0 0 0 0 5 5 1 1 5 5 5 5 Gros Morne National Park, Newfoundland and Labrador 0 0 0 0 0 0 4 4 1 1 5 5 5 5 NR-3 NR-2 Campsite NR-4 See Inset: Tuckamore Tangle 0 0 0 0 Viewpoint 0 0 3 3 1 1 5 5 5 NR-5 5 Waypoint NT-8 NT-6 Hiking Trails (Maintained) NT-11 NT-7 0 NR-6 0 0 0 0 Triangle Pond 0 2 2 1 1 Long Range Traverse 5 5 5 NT-10 5 NT-12 NT-9 Northern Traverse NT-5 0 0 Snug Harbour to North Rim 0 0 0 0 1 1 1 1 5 5 5 5 Contour Lines (10m) NT-4 0 0 0 0 0 0 0 0 1 1 5 5 5 5 1 0 1 km 0 0 0 0 0 0 9 9 Projection: UTM (Zone U21) 0 0 5 5 5 5 Datum: NAD83 Map produced on February 15, 2016 by Gros Morne National Park. 0 0 0 0 0 0 Map Source: Toporama map series, to downloaded from the Natural Resources Canada website 8 NT-3 8 0 0 5 5 January 25, 2016. For detailed informatin regarding the map series, or to download the most 5 5 Gilley Pond current topographic (1:50,000 scale) maps, visit http://GeoGratis.gc.ca. This map is not for navigation purposes. Please obtain the most current topographic map sheets 12H/13 St Pauls and 12H/12 Gros Morne. LR-1 0 0 0 0 For further information about hiking in the Long Range Mountains, including detailed route descriptions, 0 0 7 7 GPS trackfiles and waypoints, visit Gros Morne National Park website at www.pc.gc.ca/grosmorne. 0 0 5 5 5 NT-2a NT-2 5 Waypoints: Note: The waypoints below are key navigational reference points only. Safe navigation between waypoints requires wilderness route finding skills and experience using maps, compass, and GPS. Detailed route 0 0 NT-1 0 0 descriptions and GPS trackfiles are available on the Gros Morne National Park website at 0 0 6 6 0 0 LR-2 www.pc.gc.ca/grosmorne. 5 5 5 5 LR-3 LR-4 Long Range Traverse Distance Waypoint Location Description UTM (Zone 21U) 4.0 km LR-1 Campsite: Western Brook Pond 452380m E / 5507076m N LR-2 waterfall 454800m E / 5506121m N 0 0 0 0 0 0 LR-3 start of rock slab 455059m E / 5506050m N 5 5 0 0 5 5 LR-4 top of gorge 455782m E / 5506005m N 5 5 2.5 km LR-5 Campsite: Little Island Pond 455426m E / 5503813m N 3.5 km LR-6 Campsite: Marks Pond 454721m E / 5501255m N 4.5 km LR-7 notch 454722m E / 5499601m N LR-8 Campsite: Hardings Pond 453863m E / 5497462m N 0 0 7.0 km LR-9 ridge 452723m E / 5496465m N 0 0 0 0 4 4 LR-10 narrows between two ponds 451291m E / 5496460m N 0 LR-5 0 5 5 5 5 LR-11 Campsite: lower Green Island Pond 449043m E / 5494708m N LR-12 Campsite: upper Green Island Pond 448869m E / 5494669m N 5.5 km LR-13 Bakeapple Pond View Point 446937m E / 5494497m N LR-14a descent into Ferry Gulch 445122m E / 5493862m N LR-14b 444992m E / 5494026m N 0 0 LR 15 Gros Morne Mountain Trail 444483m E / 5493956m N 0 0 0 0 3 3 LR-16 Campsite: Ferry Gulch 444338m E / 5493808m N 0 0 5 5 5 5 7.5 km LR-17 Parking Lot: Gros Morne Mountain trail 439821m E / 5490687m N Northern Traverse Distance Waypoint Location Description UTM (Zone 21U) 4.0 km LR-1 Campsite: Western Brook Pond 452380m E / 5507076m N 0 0 0 0 0 0 LR-2 waterfall 454800m E / 5506121m N 2 2 0 0 5 5 LR-3 bottom of rock slab 455059m E / 5506050m N 5 5 NT-1 top of rock slab 455550m E / 5506083m N LR-6 2.0 km NT-2 saddle 455545m E / 5506764m N NT-2a Viewpoint: Western Brook Pond 454906m E / 5506665m N (optional) NT-3 Campsite: Gilley Pond 454729m E / 5507890m N 0 0 0 0 0 0 7.5 km NT-4 ridge 452772m E / 5510353m N 1 1 0 0 5 5 5 5 NT-5 lead in tuckamore 450846m E / 5511330m N NT-6 Campsite: Triangle Pond 449777m E / 5512197m N 9.0 km NT-7 small river bed 447802m E / 5512153m N NT-8 bog 447436m E / 5512301m N NT-9 rock outcrop 447263m E / 5512014m N 0 0 NT-10 game path 446025m E / 5512046m N 0 0 0 0 0 0 NT-11 narrow bog 445799m E / 5512147m N 0 0 5 5 5 5 NT-12 game path 445665m E / 5511957m N LR-7 NR-5 plateau 444699m E / 5512866m N NR-4 boulder: start of North Rim access trail 444783m E / 5513271m N 5.0 km NR-3 Western Brook Pond: end of North Rim 442726m E / 5513801m N access trail 0 0 NR-2 Campsite: Snug Harbour 442364m E / 5513790m N 0 0 0 0 9 9 NR-1 Western Brook 439644m E / 5512421m N 9 9 4 4 5 5 3.0 km Parking Lot: Western Brook Pond trail 437068m E / 5515346m N Snug Harbour to North Rim Distance Waypoint Location Description UTM (Zone 21U) 3.0 km Parking Lot: Western Brook Pond trail 437068m E / 5515346m N 0 0 0 0 0 0 5.0 km NR-1 Western Brook 439644m E / 5512421m N 8 8 9 9 4 4 NR-2 Campsite: Snug Harbour 442364m E / 5513790m N 5 5 2.5 km NR-3 Start of North Rim access trail 442726m E / 5513801m N L-8 Harding Pond NR-4 boulder: end of North Rim access trail 444783m E / 5513271m N 1.5 km NR-5 plateau 444699m E / 5512866m N NR-6 North Rim viewpoint 444525m E / 5512029m N 0 0 0 0 0 0 7 7 9 9 Ferry Gulch to Bakeapple Pond 4 4 5 5 Distance Waypoint Location Description UTM (Zone 21U) 7.5 km Parking Lot: Gros Morne Mountain trail 439821m E / 5490687m N LR-10 LR-9 2.5 km LR-16 Campsite: Ferry Gulch 444338m E / 5493808m N LR-15 Depart Gros Morne Mountain trail 444483m E / 5493956m N LR-14b ascent out of Ferry Gulch 444992m E / 5494026m N 0 0 0 0 LR- 14a 445122m E / 5493862m N 0 0 6 6 9 9 LR-13 Bakeapple Pond viewpoint 446937m E / 5494497m N 4 4 5 5 0 0 0 0 0 0 5 5 9 9 4 4 5 LR-12 5 Cow Head LR-13 LR-11 0 0 0 LR-15 LR-14b 0 0 Bakeapple Pond 0 4 4 9 9 4 LR-16 4 5 5 LR-14a Sally's Cove 0 0 0 0 0 0 3 3 9 9 4 Inset: Tuckamore Tangle 4 5 5 0 0 0 444500 445000 445500 446000 446500 447000 447500 448000 448500 449000 449500 450000 0 0 0 3 3 1 1 5 NR-5 5 5 5 0 0 0 0 0 0 2 2 9 9 Rocky Harbour 4 4 5 5 0 0 0 0 5 5 2 2 1 1 5 5 5 5 NT-8 Trout 0 0 0 0 0 NT-6 0 River 1 1 9 9 4 NT-11 NT-7 4 5 5 0 0 0 NR-6 NT-10 0 NT-9 Triangle Pond WARNING: This map contains information on hiking routes in Gros Morne National Park of Canada. This 0 0 Gros Morne Mountain 2 NT-12 2 Trailhead map was prepared by Parks Canada using its best judgment in light of the information available to it at the 1 1 5 5 time of preparation. Any use you make of this map and any reliance on or decisions made based 5 5 0 on this map are your own responsibility absolutely. Parks Canada, its employees and its agents accept no 0 0 0 0 0 Wiltondale 0 responsibility for damages, if any, suffered by you or any third party as a result of decisions made or actions 0 9 9 4 4 5 based on these maps. For greater certainty, under no circumstances whatsoever will Parks Canada, its 5 employees, or its agents be held liable for any loss or damage that may occur to you and any person or persons or property by reason of your or their reliance upon these maps. 444500 445000 445500 446000 446500 447000 447500 448000 448500 449000 449500 450000 436000 437000 438000 439000 440000 441000 442000 443000 444000 445000 446000 447000 448000 449000 450000 451000 452000 453000 454000 455000 456000 457000 458000 459000 460000 461000 462000 463000 464000.
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Quaternary Studies in Newfoundland: a Short Review C
    Document generated on 09/29/2021 12:22 a.m. Atlantic Geology Quaternary Studies in Newfoundland: A Short Review C. M. Tucker Volume 12, Number 2, August 1976 URI: https://id.erudit.org/iderudit/ageo12_2rep02 See table of contents Publisher(s) Maritime Sediments Editorial Board ISSN 0843-5561 (print) 1718-7885 (digital) Explore this journal Cite this article Tucker, C. M. (1976). Quaternary Studies in Newfoundland: A Short Review. Atlantic Geology, 12(2), 61–13. All rights reserved © Maritime Sediments, 1976 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal. Its mission is to promote and disseminate research. https://www.erudit.org/en/ 61 QUATERNARY STUDIES IN NEWFOUNDLAND: A SHORT REVIEW C.M. TUCKER Department of Geography, McMaster University, Hamilton, Ontario, L8S 4K1 INTRODUCTION portion of the remaining marine drift and left the island with its present contours. During the past century and a half, a consider- After the raising of the great North-East able body of knowledge has been amassed on the and South-East ranges, first coast-ice Quaternary epoch of Newfoundland. Until recently, flowed East and. West and afterwards the studies were of a reconnaissance nature, generally glaciers followed in a similar deviation, incidental to bedrock mapping projects or regional and thus perhaps the origin of the boulders, prospecting.
    [Show full text]
  • 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................................................................................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • Silica Assessment of the Hawke Bay Formation, Highlands of St. John Area, Great Northern Peninsula, Newfoundland
    Current Research (2002) Newfoundland Department of Mines and Energy Geological Survey, Report 02-1, pages 319-325 SILICA ASSESSMENT OF THE HAWKE BAY FORMATION, HIGHLANDS OF ST. JOHN AREA, GREAT NORTHERN PENINSULA, NEWFOUNDLAND W.L. Dickson, P.Geo. Mineral Deposits Section ABSTRACT The quartz arenite, of the Early Cambrian Hawke Bay Formation, Labrador Group, was sampled on the Highlands of St. John's to determine its potential as a source of silica. The Highlands are located about 10 km northeast of the community of Hawkes Bay and form plateaux that have an area of over 250 km2. The formation, which is estimated to be between 100 and 250 m thick, has reserves of billions of tonnes of silica. The quartz arenites are thick bedded and contain minor amounts of siltstone and conglomerate. Obvious impurities in some of the lower beds include hematite cement and grains, and heavy-min- eral laminae. Overall, the formation is clean and well sorted. INTRODUCTION The Highlands of St. John (the Highlands) are located along the western side of the Great Northern Peninsula (Fig- ure 1), 13 km northeast of Hawkes Bay (Figure 2). The Highlands are capped by a thick sequence of quartz arenite of the Early to Middle Cambrian Hawke Bay Formation, which is the upper most formation of the Labrador Group. A rock geochemical sampling program was conducted to determine the potential of the formation as a source of silica. LOCATION AND ACCESS The silica-assessment project was conducted on the Highlands of St. John and on a newly accessible ridge to the southeast of (Big) East River, which runs along the southern margin of the Highlands (Figure 2).
    [Show full text]