Analysis of the Efficacy of Lidar Data As a Tool for Archaeological Prospection at the Highland Valley Copper Mine

Total Page:16

File Type:pdf, Size:1020Kb

Analysis of the Efficacy of Lidar Data As a Tool for Archaeological Prospection at the Highland Valley Copper Mine Analysis of the Efficacy of LiDAR Data as a Tool for Archaeological Prospection at the Highland Valley Copper Mine by Sarah K. Smith B.A., University of British Columbia 2005 Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Arts in the Department of Archaeology Faculty of Environment © Sarah K Smith 2021 SIMON FRASER UNIVERSITY Spring 2021 Copyright in this work rests with the author. Please ensure that any reproduction or re-use is done in accordance with the relevant national copyright legislation. Declaration of Committee Name: Sarah K . Smith Degree: Master of Ar ts Title: Analysis of the Efficacy of LiDAR Data as a Tool for Archaeological Prospection at the Highland Valley Copper Mine Committee: Chair: John Welch Professor , Archaeology David Burley Supervisor Professor, Archaeology Kristin Safi Committee Member Senior Archaeologist Wood Environment & Infrastructure Solutions Travis Freeland Examiner Project Manager Kleanza Consulting Ltd. ii Abstract As heritage resource management and Indigenous heritage stewardship moves into the forefront of project design and operational planning in British Columbia, researchers look for innovative ways to foster impact assessment efficiency without sacrificing quality. In this study I explore methods for employing LiDAR-derived digital elevation models as a tool for archaeological prospection within the Highland Valley Copper Mine. A review of contemporary and formative LiDAR-analysis archaeological prospection research was conducted to identify the most appropriate visualization techniques and data management workflow. Specific methods for the identification of microtopographic relief with the potential to contain archaeological resources were developed. The efficacy of LiDAR-based topographic analysis using manual feature extraction is validated through comparison with georeferenced survey and ground-truthing data provided by my research partners at the Nlaka’pamux Nation Tribal Council. The LiDAR analysis method identified a high percentage of recorded archaeological sites and meets provincial requirements for a moderately effective predictive model. Results of LiDAR analysis are presented along with recommendations for improved performance using best practices and an interpolation workflow. An analysis of the cost implications of incorporating LiDAR-survey into the heritage management workflow in the study area identified a significant benefit during survey. These savings would allow for redistribution of resources and potentially a greater focus on mitigative systematic data recovery. The use of remote sensing technologies and methods can have a positive impact on heritage resource management industry in BC by decreasing program costs while maintaining quality. Keywords : LiDAR (Light Detection and Ranging); Highland Valley Copper Mine; Nlaka’pamux Nation Tribal Council; Heritage Resource Management (HRM); Manual Feature Extraction (MFE); Archaeological Prospection iii Acknowledgements I would like to thank the Nlaka’pamux Nation Tribal Council for providing me with the opportunity to conduct research within their traditional territory and Teck Resources for their support of this research and for allowing me to access the Highland Valley Copper Mine study area. I would also like to acknowledge the Mitacs Accelerate Program, which facilitated on-line training and a funded internship providing me with the financial wiggle-room I needed to focus my time on research and data collection. iv Table of Contents Declaration of Committee ................................................................................................ ii Abstract .......................................................................................................................... iii Acknowledgements ........................................................................................................ iv Table of Contents ............................................................................................................ v List of Tables ................................................................................................................. vii List of Figures................................................................................................................ viii List of Acronyms .............................................................................................................. x Glossary ........................................................................................................................ xii Executive Summary ..................................................................................................... xiv Chapter 1. Introduction and Research Context ........................................................ 1 1.1. Introduction ............................................................................................................ 1 1.2. Research Problem and Goals ................................................................................ 1 1.3. Research Questions .............................................................................................. 3 1.4. Research Strategy and Methods ........................................................................... 4 1.5. Research Results .................................................................................................. 5 1.6. Research Context .................................................................................................. 5 1.6.1. Biophysical Setting ........................................................................................ 6 1.6.2. Ancient Environment...................................................................................... 7 1.6.3. Ethnographic Setting ..................................................................................... 8 1.6.4. Historic Setting .............................................................................................. 9 1.6.5. Highland Valley Copper Mine ...................................................................... 10 1.6.6. Regional Cultural Chronology ...................................................................... 10 1.6.7. Previous Archaeological Research in Highland Valley ................................. 13 1.6.8. Recorded Archaeological Sites within the Study Area .................................. 17 1.6.9. Subsurface Test Area Dataset Slope Analysis ............................................. 19 1.6.10. Heritage Protection Standards in British Columbia ................................... 20 1.6.11. Research Context Discussion .................................................................. 22 Chapter 2. LiDAR Research for Archaeological Prospection ................................ 24 2.1. LiDAR & Orthophotograph Imagery ..................................................................... 25 2.2. Formative and Current LiDAR Research ............................................................. 29 2.3. LiDAR Analysis for Archaeological Research in BC ............................................. 32 Chapter 3. Research Methods, Data Acquisition, and Interpretation ................... 35 3.1. Research Methods .............................................................................................. 36 3.1.1. Traditional Survey Methodology at HVC ...................................................... 36 3.1.2. Manual vs Automated Feature Extraction .................................................... 40 3.1.3. LiDAR-Derived DEM Interpolation Best Practice and Workflow ................... 41 3.2. Data Collection .................................................................................................... 43 3.2.1. Background Research (Step 1) .................................................................... 43 3.2.2. Target Feature Landform Attributes, Data Trimming and Zonal Statistics (Step 2) .................................................................................................................... 44 v 3.2.3. LiDAR Data Acquisition ............................................................................... 49 3.3. Data Review and Interpolation ............................................................................. 51 3.3.1. Imagery Visualization Techniques (Step 3) .................................................. 51 3.3.2. Imagery Display Errors ................................................................................ 58 3.3.3. Manual Feature Extraction Review of Test Areas and Iterative Comparison of Results (Step 4) ................................................................................. 58 3.3.4. Interpretive Mapping of Blind Study Areas (Step 5) ..................................... 59 3.3.5. Ground Observation/Field Visit (Step 6)....................................................... 59 3.4. Data Analysis and Interpretation .......................................................................... 60 3.4.1. Interpretation and Contextualization of Results (Step 7) .............................. 60 3.4.2. Analytic Methods ......................................................................................... 61 3.4.3. Evaluation and Contextualization of Results ................................................ 64 Chapter 4. Analysis Results .................................................................................... 65 4.1. Interpretation Bias Analysis ................................................................................. 66 4.2.
Recommended publications
  • Basin Architecture of the North Okanagan Valley Fill, British Columbia
    BASIN ARCHITECTURE OF THE NORTH OKANAGAN VALLEY FILL, BRITISH COLUMBIA sandy Vanderburgh B.Sc., University of Calgary I984 M.Sc., University of Calgary 1987 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in the Department of Geography 0 Sandy Vanderburgh SIMON FRASER UNIVERSITY July 1993 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL ' Name: Sandy Vanderburgh Degree: Doctor of Philosophy Title of Thesis: Basin Architecture Of The North Okanagan Valley Fill, British Columbia Examining Committee: Chair: Alison M. Gill Associate Professor Dr. M.C. Roberts, Protessor Senior Supervisor Idr. H. Hickin, professor Dr. Dirk Tempelman-Kluit, Director Cordilleran Division, Geological Survey of Canada Dr. R.W. Mathewes, Professor, Department of Biological Sciences Internal Examiner Dr. James A. Hunter, Senior scientist & Program Co-ordinator, Terrain Sciences Division Geological Survey of Canada External Examiner Date Approved: Julv 16. 1993 PARTIAL COPYRIGHT LICENSE 8* I hereby grant to Simon Fraser University the right to lend my thesis, projector extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without my written permission.
    [Show full text]
  • North Thompson Official Community Plan
    Schedule “A” to Bylaw 2700 North Thompson Official Community Plan Foreword and Acknowledgements The North Thompson Official Community Plan is the outcome of over two years of research, public participation and planning. The Regional District is grateful to all those residents and groups who provided interest, passion, and support from all corners of the Plan area culminating in the Plan development. In particular, we wish to recognize the following people for the exceptional amount of time and energy they dedicated to the planning process. OCP Advisory Committee Director Carol Schaffer, Electoral Area “A” Director Stephen Quinn, Electoral Area “B” Director Bill Kershaw, Electoral Area “O” Tom Eustache – Simpcw First Nation Rick Dee Harley Wright Willow Macdonald (past member) Meetings, Conversations and Information Providers Anna Kay Eldridge – Simpcw First Nation Ashley Dyck – Planning Services Celia Nord – Little Shuswap Indian Band Chris Ortner Dan Winiski Doris Laner – North Thompson Arts Council James Demens and Brandon Gustafsen – Ministry of Transportation and Infrastructure Jenny Green and Clare Audet – Interior Health Authority Kelly Funk – Kelly Funk Photography Laura Ryser – Research Manager, Rural and Small Town Studies Program, UNBC Leanne Nystoruk Mike Scarff, TNRD GIS Services PIBC and the Planners from the local Interior Chapter Sarah Cooke and Mike Cloet – Ministry of Mines, Energy and Petroleum Resources Staff and students at Clearwater and Barriere Secondary Schools Staff from the Agricultural Land Commission Staff
    [Show full text]
  • Note. to Users
    NOTE.TO USERS This reproduction is the best copy available. TEE FRUIT OF THEIR LABOUR: A PALAEOETHNOBOTANICAL STUDY OF SITE EeRb 140, A MULTI-COMPONENT OPEN-AIR ARCHAEOLOGICAL SITE ON TEIE BiUTISH COLUMBIA PLATEAU Michde M. Wollstonecroft B.A. (Hon.), Simon Fraser University, 1995 A THESIS SUBMïlTED IN PARTIAL FüLFiLLMENT OF THE REQUREMENTS FOR TIIE DEGREE OF MASTER OF ARTS in the Departmat of Arcbaeology O Michéle M. Wollstonecmft, 2000 Simon Fraser University, December 2000 AH dghts reserved. This thesis may not be roproduced in whole or in part, by photocopy or other meanq withoiit the permission of the author. uisiaons and AcquilMcm et "9Bib iographii Senrices seniiEes biMiographiiues The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant & la National Li'brary of Canada to Bibliothéque nationale du Canada de reprodwe, loan, distriiute or seii reproduire, @ter, distriiuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la fime de microfiche/fiim, de reproduction sur papier ou sur format 61ectronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thèse ni des exûaits substantiels may be printed or othhse de celle-ci ne doivent être imprimes reproduced without the author's ou autrement reproduits sans son autorisation. The quality of preservation and richness of the plant assemblage recovered hmsite EeRb 140 demonstrate the great potential for investigating plant-use at archaeological sites on the British Columbia Plateau, EeRb 140 is an open-air multi-component site located on a g~aciolaucusirineterrace on the north side of the South Thompson River.
    [Show full text]
  • Syilx Okanagan Flood and Debris Flow Risk Assessment Report 4 of 4 – Quantitative Study (R4) Appendices
    Syilx Okanagan Flood and Debris Flow Risk Assessment Report 4 of 4 – Quantitative Study (R4) Appendices R4 List of Appendices Appendix A: Data Summary Appendix B: Flood Hazard Assessment Appendix C: Debris Flow Hazard Assessment Syilx Okanagan Flood and Debris Flow Risk Assessment Report 4 of 4 – Quantitative Study Appendix A: Data Summary The following provides a list of data used to support the analyses presented in the Quantitative Study. Legend Hazard Data Topographic Data Exposure Data Risk Data Syilx Okanagan Flood and Debris Flow Risk Assessment, Report 4 of 4 – Quantitative Study A-1 Appendix A: Data Summary Table 1: Summary of data used for Geohazard Risk Assessment DATA DATA CONFIDENCE FILE NAME Data Purpose DATA TYPE SOURCE CATEGORY DESCRIPTION SCORE 136_GFA_FloodProne_HighMagnitude.shp Hazard used Geomorphic as the basis GFA Flood Flood Area 136_GFA_FloodProne_ModerateMagnitude.shp for the flood Shapefile Ebbwater 3 Model (GFA) Model risk 136_GFA_FloodProne_LowMagnitude.shp assessment Debris Flow Model. Hazard used Including the as the basis Debris Flow 136_Palmer_DebrisInitiationandPath debris flow for the debris Shapefile Palmer 4 Hazard Model initiation flow risk zones and assessment flow paths Flood Map Based on Soils Early Flood Geological Layers. Mapping. 136_GSM Complete.shp Shapefile Ebbwater 2 Soils Mapping Approach Flood Map Developed by Calibration AE for RDCO Provincial Flood Provincial 136_FDRP_floodplains_EPSG4617.shp FDRP Flood mapping Shapefile BC Data Catalogue 4 Flood Maps Maps calibration Flood maps produced
    [Show full text]
  • Origins of Lake Okanagan
    ORIGINSORIGINS OFOF LAKELAKE OKANAGANOKANAGAN By Murray A. Roed, PhD, PEng Information provided is primarily from a book entitled “Okanagan Geology, British Columbia” published in 2004 by the Kelowna Geology Committee. 05/12/2005 1 INTRODUCTIONINTRODUCTION z Precambrian Time – Vast granitic Continental Crust, Pangaea z Paleozoic Time – Oceanic shelf environment, major mountain building z Mesozoic Time – Island Arc archipelago, plate tectonic structure, Continental Drift, obduction, Interior Mountain Building, Massive Stream Erosion z Cenozoic Time…the valley begins 05/12/2005 2 TheThe CenozoicCenozoic EraEra (Tertiary(Tertiary andand QuaternaryQuaternary Periods)Periods) z Initiation of the Okanagan Rift System z Eocene Volcanic activity, explosive type – Knox Mountain, Mount Boucherie z Development of White Lake River System z Erosion of Highlands, Deposition onto Alberta Plains z The rise of the Rocky Mountains z Folding and Faulting in the Okanagan z Mission Creek Fault z Peneplanation of the Interior of BC 05/12/2005 3 PlateauPlateau VulcanismVulcanism z Uplift, Rifting, and Erosion, regional near- surface magma chamber. z Widespread fluid basaltic flows erupt along fractures and inundate low relief valley system (200 to 300 metres local relief) including part of the Okanagan Valley (Wrinkly Faced Cliff, Oyama). z Continued Uplift, Cooling of the Earth, High 05/12/2005Precipitation, Erosion 4 PreglacialPreglacial ValleyValley SystemSystem z Massive deep erosion along fractured and fault- bounded rocky terrain in the Canadian Cordillera and Interior Plains. z Development of major valleys; topography highly rugged with sharp bold profiles. z Incision or dissection of the Thompson Plateau and Okanagan Highland 05/12/2005 5 THETHE ICEICE AGEAGE z Ice accumulation from massive snowfall z Development of Cordilleran Ice Sheets -beginning with valley glaciers and ending with ice so thick, it overtopped mountains.
    [Show full text]
  • Eocene Paleo-Physiography and Drainage Directions, Southern Interior Plateau, British Columbia1
    215 Eocene paleo-physiography and drainage directions, southern Interior Plateau, British Columbia1 Selina Tribe Abstract: A map of reconstructed Eocene physiography and drainage directions is presented for the southern Interior Plateau region, British Columbia south of 53°N. Eocene landforms are inferred from the distribution and depositional paleoenvironment of Eocene rocks and from crosscutting relationships between regional-scale geomorphology and bedrock geology of known age. Eocene drainage directions are inferred from physiography, relief, and base level elevations of the sub-Eocene unconformity and the documented distribution, provenance, and paleocurrents of early Cenozoic fluvial sediments. The Eocene landscape of the southern Interior Plateau resembled its modern counterpart, with highlands, plains, and deeply incised drainages, except regional drainage was to the north. An anabranching valley system trending west and northwest from Quesnel and Shuswap Highlands, across the Cariboo Plateau to the Fraser River valley, contained north-flowing streams from Eocene to early Quaternary time. Other valleys dating back at least to Middle Eocene time include the North Thompson valley south of Clearwater, Thompson valley from Kamloops to Spences Bridge, the valley containing Nicola Lake, Bridge River valley, and Okanagan Lake valley. During the early Cenozoic, highlands existed where the Coast Mountains are today. Southward drainage along the modern Fraser, Chilcotin, and Thompson River valleys was established after the Late Miocene. Résumé : Cet article présente une carte reconstituée de la géographie physique et des directions de drainage, à l’Éocène, pour la région du plateau intérieur de la Colombie-Britannique, au sud du 53e parallèle Nord. Les formes de terrain à l’Éocène sont déduites de la distribution et du paléoenvironnement de déposition des roches de l’Éocène et à partir de relations de recoupement entre la géomorphologie à l’échelle régionale et la géologie du socle, d’âge connu.
    [Show full text]
  • NATURESCAPE BRITISH COLUMBIA Caring for Wildlife Habitat at Home
    The Stewardship Series NATURESCAPE BRITISH COLUMBIA Caring for Wildlife Habitat at Home Native Plant and Animal Booklet, Central Interior Naturescape British Columbia IS FUNDED BY For More information, call 1-800-387-9853 Canadian Cataloguing in Publication Data Naturescape British Columbia. Native plant and animal booklet, central interior (Stewardship series) ISBN 0-7726-4333-4 1. Zoology - British Columbia - Cariboo Region. 2. Botany - British Columbia - Cariboo Region. 3. Biotic communities - British Columbia - Cariboo Region. 4. Habitat (Ecology) - British Columbia - Cariboo Region. 5. Nature conservation - British Columbia - Cariboo Region. I. Hemphill, Susan M. II. Naturescape British Columbia. III. Series. QH77.C3H452 2000 578’.09711’7 C00-960275-5 Notice: The information contained in the Naturescape British Columbia Guide and booklets is true and complete to the best of our knowledge. All recommendations are made without any guarantees on the part of the authors and Naturescape British Columbia sponsors. Because the means, materials and procedures followed by home- owners are beyond our control, the authors and Naturescape British Columbia disclaim all liability in connection with the use of this information. Naturescape British Columbia publications are copyright© 1995 by the Government of British Columbia. All rights reserved. Except for use in review, or other means, now known or hereafter invented, including xerography, photocopying, and recording, and in any information storage and retrieval system is forbidden without the written permission of Naturescape British Columbia and Havitat Conservation Trust Foundation Naturescape British Columbia Havitat Conservation Trust Foundation Suite 107 19 Dallas Road Victoria BC V8V 5A6 www.naturescapebc.ca NAT U R E S C A P E BR I T I S H CO L U M B I A Native Plant and Animal Booklet,Central Interi o r W r itten and compiled by Susan M.
    [Show full text]
  • The Penticton Map Area Is Located in the Southeastern Part of British Columbia. It Contains
    MINFILE NTS 082ESW - PENTICTON Original release date: October 1997 Researched and compiled by: K.J. Mountjoy The Penticton map area, located in south-central British Columbia, contains 257 documented mineral occurrences in diverse geological settings. The map area includes the historically important Beaverdell, McKinney, Fairview and Olalla mining camps. These camps and surrounding areas continue to attract exploration interest and activity. The area is roughly divided into an eastern-half physiograpically known as the Okanagan Highland and a western-half known as the Thompson Plateau that coincide respectively, with the Omineca and Intermontane tectonic belts. The two physiographic areas are separated by the Okanagan Valley fault, that trends south-southeast along the Okanagan Valley from Penticton to Osoyoos Lake on the Canada-United States Boundary. The regional structural features in the Penticton map area are the result of post-Laramide extensional tectonism along a probable east-west axis, marked at its peak by Eocene Marron volcanism and coeval Coryell intrusions. Late Pliocene uplift was probably responsible for extensive block faulting and the development of major north-south fault lineaments such as the Okanagan Valley fault. The region is underlain principally by upper Paleozoic to lower Mesozoic rocks of the Quesnel Terrane. From west to east these consist of the Nicola Group, the Old Tom, Shoemaker, Bradshaw and Independence formations, and the Kobau and Anarchist groups. All groups consist of marine sedimentary and volcanic, arc-related rocks. These strata form a broadly folded, east-dipping MINFILE NTS 082ESW - Penticton sequence that has an overall increase in age towards structurally higher rocks in the east, formed at least in part by an ancient subduction complex that formed by progressive eastward-directed underthrusting and accretion of successively younger slices of oceanic sediments and volcanic rocks.
    [Show full text]
  • A Field Guide to Forest Site Identification and Interpretation for the Cariboo Forest Region
    A FIELD GUIDE TO FOREST SITE IDENTIFICATION AND INTERPRETATION FOR THE CARIBOO FOREST REGION O. A. Steen and R. A. Coupé Ministry of Forests Research Program 1997i AUTHORS AND AFFILIATIONS Ordell Steen, Research Ecologist, Cariboo Forest Region, Ministry of Forests, 200 - 640 Borland Street, Williams Lake, B.C. V2G 4T1 Ray Coupé, Research Ecologist, Cariboo Forest Region, Ministry of Forests, 200 - 640 Borland Street, Williams Lake, B.C. V2G 4T1 Canadian Cataloguing in Publications Data Steen, O. A. A field guide to forest site identification and interpretation for the Cariboo Forest Region Includes bibliographical references: p. ISBN 0-7726-3495-5 1. Bioclimatology British Columbia Cariboo Region. 2. Forest site quality British Columbia Cariboo Region. 3. Biogeography British Columbia Cariboo Region. 4. Forest ecology British Columbia Cariboo Region. 5. Forest management British Columbia Cariboo Region. 6. Cariboo Forest Region (B. C.). I. Coupé, R., 1952- . II. British Columbia. Ministry of Forests. Research Branch. QH541.5.F6S73 1998 581.7'37'09711 C989600637 © 1997 Province of British Columbia Published by the Research Branch, Ministry of Forests, 712 Yates Street, Victoria, B. C. V8W 3E7 Citation: Steen, O.A and R.A. Coupé. 1997. A field guide to forest site identification and interpretation for the Cariboo Forest Region. B.C. Min. For., Victoria, B.C. Land Manage. Handb. No. 39. Copies of this and other Ministry of Forests titles are available from Crown Publications Inc., 521 Fort Street, Victoria, B.C. V8W 1E7 ii ACKNOWLEDGEMENTS The classification and interpretations presented in this field guide have evolved over the past 20 years through the collective work of several individuals involved in the many phases of the Cariboo Forest Region ecological classification project.
    [Show full text]
  • Lac Du Bois Grasslands Park
    LAC DU BOIS GRASSLANDS PARK MANAGEMENT PLAN BACKGROUND DOCUMENT Prepared for BC Parks Ministry of Environment, Lands and Parks 1210 McGill Road Kamloops BC V2C 6N6 MARCH, 2000 INTRODUCTION........................................................................................................................................................................... 2 PARK HIGHLIGHTS...................................................................................................................................................................... 2 HISTORY OF PLANNING AND MANAGEMENT .......................................................................................................................... 2 PARK ESTABLISHMENT , LEGISLATION, AND MANAGEMENT DIRECTION. ......................................................................... 5 NATURAL RESOURCES ............................................................................................................................................................. 9 CLIMATE....................................................................................................................................................................................... 9 PHYSIOGRAPHY........................................................................................................................................................................... 9 GEOLOGY...................................................................................................................................................................................
    [Show full text]
  • Appendix 6.8-A
    Appendix 6.8-A Terrestrial Wildlife and Vegetation Baseline Report AJAX PROJECT Environmental Assessment Certificate Application / Environmental Impact Statement for a Comprehensive Study Ajax Mine Terrestrial Wildlife and Vegetation Baseline Report Prepared for KGHM Ajax Mining Inc. Prepared by This image cannot currently be displayed. Keystone Wildlife Research Ltd. #112, 9547 152 St. Surrey, BC V3R 5Y5 July 2015 Ajax Mine Terrestrial Wildlife and Vegetation Baseline Keystone Wildlife Research Ltd. DISCLAIMER This report was prepared exclusively for KGHM Ajax Mining Inc. by Keystone Wildlife Research Ltd. The quality of information, conclusions and estimates contained herein is consistent with the level of effort expended and is based on: i) information available at the time of preparation; ii) data collected by Keystone Wildlife Research Ltd. and/or supplied by outside sources; and iii) the assumptions, conditions and qualifications set forth in this report. This report is intended for use by KGHM Ajax Mining Inc. only, subject to the terms and conditions of its contract with Keystone Wildlife Research Ltd. Any other use, or reliance on this report by any third party, is at that party’s sole risk. 2 Ajax Mine Terrestrial Wildlife and Vegetation Baseline Keystone Wildlife Research Ltd. EXECUTIVE SUMMARY Baseline wildlife and habitat surveys were initiated in 2007 to support a future impact assessment for the redevelopment of two existing, but currently inactive, open pit mines southwest of Kamloops. Detailed Project plans were not available at that time, so the general areas of activity were buffered to define a study area. The two general Project areas at the time were New Afton, an open pit just south of Highway 1, and Ajax, east of Jacko Lake.
    [Show full text]
  • Belted Kingfisher
    Belted King fisher Megaceryle alcyon Laure Wilson Neish lower abundance) occur across the wetland-studded plateaus of Characteristics and Range This spectacular, large kingfisher the Central Interior and Sub-boreal Interior ecoprovinces. with its outrageous "Mohawk" crest and startling staccato rattling call is one of North America's most widespread birds. It Belted Kingfishers prefer clear, fresh or salt water wetlands, breeds across the continent from the Low Arctic south to the especially with rocky shoals and shallower fast-flowing sections, United States Southern Coastal Plains and arid southwest. It is a in close proximity to natural or man-made exposed banks where partial migrant; northern breeders migrate south to winter in they can excavate nest burrows, and with abundant perches from ice-free areas, some moving as far as Central America and the which they can forage for prey, chiefly fish, but also crayfish and Caribbean (Kelly et al. 2009). other larger aquatic invertebrates. Distribution, Abundance, and Habitat The Atlas surveys show Conservation and Recommendations The Breeding Bird Survey the Belted Kingfisher is still widespread throughout the province; shows a long-term decrease in Belted Kingfishers, across Canada comparison with The Birds of British Columbia indicates there and in British Columbia; reasons for the decline are not well has been no appreciable change in distribution, provincially or understood, but declining habitat quality, contaminants, locally, over the past two decades. reduction in available nest sites (especially man-made sites like gravel pits, road cuts and quarry sites), and human disturbance The Probability of Observation model highlights several most are all potential contributors.
    [Show full text]