DOCSLIB.ORG

LILLOOET RIVER CORRIDOR Submission of Final Report Our File713.002

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
LILLOOET RIVER CORRIDOR Submission of Final Report Our File713.002 EngineeringStudyfor LillooetRiverCorridor FinalReport December2002 PembertonValleyDykingDistrict MountCurrieBand December 23, 2002 Mr. John Pattle, P.Eng. B.C. Ministry of Water, Land and Air Protection 10470 - 152nd Street Surrey, B.C. V3R 0Y3 Dear Mr. Pattle: RE: ENGINEERING STUDY FOR LILLOOET RIVER CORRIDOR Submission of Final Report Our File713.002 We are pleased to submit 3 copies of the Engineering Study for Lillooet River Corridor Final Report. This report presents current conditions and up-to-date hydraulic modelling results, with a backdrop of historical data and analysis of long-term geomorphological changes within the Pemberton Valley. This report will assist the Steering Group, and communities at large, in understanding and documenting the problem areas. Further, this report will form the foundation of a flood mitigation and management plan for the Pemberton Valley. We have very much enjoyed working on this project with you, and hope we can be of service to you again. We trust this is satisfactory. Yours truly, KERR WOOD LEIDAL ASSOCIATES LTD. Jonathon Ng, P.Eng., PMP Project Manager JN/am Encl. (3) P:\0700-0799\713-002\Report\TransLETTER.doc Engineering Study for Lillooet River Corridor Final Report December 2002 KWL File No. 713.002 ENGINEERING STUDY FOR LILLOOET RIVER CORRIDOR FINAL REPORT PEMBERTON VALLEY DYKING DISTRICT DECEMBER 2002 MOUNT CURRIE BAND STATEMENT OF LIMITATIONS This document has been prepared by Kerr Wood Leidal Associates Ltd. (KWL) for the exclusive use and benefit of the Mount Currie Band, the Pemberton Valley Dyking District, B.C. Ministry of Water, Land and Air Protection, Public Works and Government Services Canada, and Indian and Northern Affairs Canada. No other party is entitled to rely on any of the conclusions, data, opinions, or any other information contained in this document. This document represents KWL’s best professional judgement based on the information available at the time of its completion and as appropriate for the project scope of work. Services performed in developing the content of this document have been conducted in a manner consistent with that level and skill ordinarily exercised by members of the engineering profession currently practising under similar conditions. No warranty, expressed or implied, is made. COPYRIGHT NOTICE These materials (text, tables, figures and drawings included herein) are copyright of Kerr Wood Leidal Associates Limited (KWL). These materials may be reproduced for archiving and for distribution to third parties only as required to conduct business specifically relating river management activities on the Lillooet River. Any other use of these materials without the written permission of KWL is prohibited. KERR WOOD LEIDAL ASSOCIATES LTD. Consulting Engineers 713.002 ENGINEERING STUDY FOR LILLOOET RIVER CORRIDOR PEMBERTON VALLEY DYKING DISTRICT FINAL REPORT MOUNT CURRIE BAND DECEMBER 2002 CONTENTS EXECUTIVE SUMMARY ............................................................................i 1. INTRODUCTION.....................................................................................1-1 1.1 BACKGROUND....................................................................................................................1-1 STAKEHOLDERS .................................................................................................................1-1 NEED FOR STUDY...............................................................................................................1-1 1.2 STUDY OBJECTIVES ...........................................................................................................1-2 1.3 ENGINEERING WORK PROGRAM AND PROJECT DELIVERABLES ...........................................1-3 1.4 ENVIRONMENTAL ISSUES....................................................................................................1-3 1.5 PROJECT TEAM..................................................................................................................1-4 1.6 DEFINITIONS ......................................................................................................................1-4 DESIGN FLOOD ..................................................................................................................1-4 DESIGN FLOOD ELEVATION.................................................................................................1-4 FREEBOARD.......................................................................................................................1-5 DYKE DESIGN ELEVATION...................................................................................................1-5 2. STUDY AREA.........................................................................................2-1 2.1 LILLOOET RIVER WATERSHED ............................................................................................2-1 2.2 SETTLEMENT HISTORY OF THE PEMBERTON VALLEY ...........................................................2-1 2.3 BEDROCK GEOLOGY ..........................................................................................................2-3 2.4 GEOMORPHOLOGY AND SURFICIAL GEOLOGY .....................................................................2-4 3. PREVIOUS WORK .................................................................................3-1 3.1 ENGINEERING STUDIES AND WORKS ...................................................................................3-1 1946 TO 1952 ...................................................................................................................3-1 1953 TO 1978 ...................................................................................................................3-2 1979 TO 1985 ...................................................................................................................3-3 1985 TO 1990 ...................................................................................................................3-5 1988 HEC2 MODELS.........................................................................................................3-5 1990 TO PRESENT .............................................................................................................3-6 3.2 SCIENTIFIC STUDIES...........................................................................................................3-9 LILLOOET RIVER DELTA FORMATION....................................................................................3-9 SEDIMENT BUDGET FROM DELTA DEPOSITS ......................................................................3-10 MASS MOVEMENTS AND THEIR HYDROLOGIC LINK .............................................................3-11 4. WORK PROGRAM IMPLEMENTATION................................................4-1 4.1 FIELD WORK......................................................................................................................4-1 4.2 ANALYSIS ..........................................................................................................................4-4 4.3 STUDY PROCESS................................................................................................................4-5 5. FLUVIAL GEOMORPHOLOGY..............................................................5-1 5.1 MORPHOLOGICAL CHARACTERIZATION ...............................................................................5-2 5.2 CHANNEL CHANGES AND SEDIMENT TRANSPORT IN UPPER REACHES OF LILLOOET RIVER ...5-4 MORPHOLOGIC APPROACH TO SEDIMENT TRANSPORT.........................................................5-6 RESULTS ...........................................................................................................................5-9 CONCLUSIONS .................................................................................................................5-14 5.3 CHANNEL CHANGES AND SEDIMENT TRANSPORT IN LOWER REACHES OF LILLOOET RIVER 5-14 CHANNEL ADJUSTMENTS TO 1946-1953 ENGINEERING WORKS .........................................5-15 CROSS SECTIONAL CHANGES ...........................................................................................5-21 SEDIMENT TRANSPORT.....................................................................................................5-22 KERR WOOD LEIDAL ASSOCIATES LTD. i Consulting Engineers 713.002 ENGINEERING STUDY FOR LILLOOET RIVER CORRIDOR PEMBERTON VALLEY DYKING DISTRICT FINAL REPORT MOUNT CURRIE BAND DECEMBER 2002 CONCLUSIONS .................................................................................................................5-26 5.4 BANK EROSION................................................................................................................5-27 LILLOOET RIVER...............................................................................................................5-27 GREEN RIVER ..................................................................................................................5-32 BIRKENHEAD RIVER..........................................................................................................5-33 RYAN RIVER AND MILLER CREEK ......................................................................................5-34 5.5 DELTA FORMATION ..........................................................................................................5-34 6. CLIMATE AND HYDROLOGY ...............................................................6-1 6.1 BACKGROUND AND HISTORICAL ANALYSIS .........................................................................6-1 6.2
Load more

Recommended publications
  • British Columbia Geological Survey Geological Fieldwork 1989
    GEOLOGY AND MINERAL OCCURRENCES OF THE YALAKOM RIVER AREA* (920/1, 2, 92J/15, 16) By P. Schiarizza and R.G. Gaba, M. Coleman, Carleton University J.I. Garver, University of Washington and J.K. Glover, Consulting Geologist KEYWORDS:Regional mapping, Shulaps ophiolite, Bridge REGIONAL GEOLOGY River complex, Cadwallader Group Yalakom fault, Mission Ridge fault, Marshall Creek fault. The regional geologic setting of the Taseko-Bridge River projectarea is described by Glover et al. (1988a) and Schiarizza et al. (1989a). The distributicn and relatio~uhips of themajor tectonostratigraphic assemblages are !;urn- INTRODUCTION marized in Figures 1-6-1 ;and 1-6-2. The Yalakom River area covers about 700 square kilo- The Yalakom River area, comprisinl: the southwertem metres of mountainous terrain along the northeastern margin segment of the project area, encompasses the whole OF the of the Coast Mountains. It is centred 200 kilometres north of Shubdps ultramafic complex which is interpreted by hagel Vancouver and 35 kilometresnorthwest of Lillooet.Our (1979), Potter and Calon et a1.(19901 as a 1989 mapping provides more detailed coverageof the north- (1983, 1986) dismembered ophiolite. 'The areasouth and west (of the em and western ShulapsRange, partly mapped in 1987 Shulaps complex is underlain mainly by Cjceanic rocks cf the (Glover et al., 1988a, 1988b) and 1988 (Schiarizza et al., Permian(?)to Jurassic €!ridge Rivercomplex, and arc- 1989d, 1989b). and extends the mapping eastward to include derived volcanic and sedimentary rocksof the UpperTri %sic the eastem part of the ShulapsRange, the Yalakom and Cadwallader Group. These two assemhkgesare struclurally Bridge River valleys and the adjacent Camelsfoot Range.
    [Show full text]
  • Community Risk Assessment
    COMMUNITY RISK ASSESSMENT Squamish-Lillooet Regional District Abstract This Community Risk Assessment is a component of the SLRD Comprehensive Emergency Management Plan. A Community Risk Assessment is the foundation for any local authority emergency management program. It informs risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflects their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. SLRD Emergency Program [email protected] Version: 1.0 Published: January, 2021 SLRD Community Risk Assessment SLRD Emergency Management Program Executive Summary This Community Risk Assessment (CRA) is a component of the Squamish-Lillooet Regional District (SLRD) Comprehensive Emergency Management Plan and presents a survey and analysis of known hazards, risks and related community vulnerabilities in the SLRD. The purpose of a CRA is to: • Consider all known hazards that may trigger a risk event and impact communities of the SLRD; • Identify what would trigger a risk event to occur; and • Determine what the potential impact would be if the risk event did occur. The results of the CRA inform risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflect their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property.
    [Show full text]
  • Dynamics of Aboriginal Land Use Institutions: the Rise and Fall of Community Control Over Reserve Systems in the Lil'wat Nation, Canada
    DYNAMICS OF ABORIGINAL LAND USE INSTITUTIONS: THE RISE AND FALL OF COMMUNITY CONTROL OVER RESERVE SYSTEMS IN THE LIL'WAT NATION, CANADA Akihiko Nemoto Forest Economics Research Institute #301 Mansion Yoneda, 2-13-12 Hakusan, Bunkyo-Ku, Tokyo, Japan zip 112-0001 E-mail: [email protected] Abstract I Resume Through a combination of the participant-observer method and archival data collection, this descriptive study deals with the changing dynam­ ics of land use institutions in an Aboriginal community of British Columbia, Canada, namely the LiI'wat Nation. En alliant la methode du participant-observateur et la collecte de donnees d'archives, I'etude descriptive se penche sur la dynamique en evolution des institutions responsables de I'utilisation du sol dans une collectivite autochtone de la Colombie-Britannique (Canada), soit la Nation Lil'wat. The Canadian Journal of Native Studies XXII, 2(2002}:207-237. 208 Akihiko Nemoto 1. Research Objectives and Methodology In the context of "sustainable development," traditional resource use systems around the world have been gaining attention as practical ways to conserve natural resources today.1 With respect to Aboriginal peoples in Canada, some scholars have advocated that there is a strong hope for contemporary resource management practices to incorporate the Aboriginal knowledge that has sustained the living resource base over extended periods of time.2 However, these arguments tend to fol­ low only philosophical lines, ignoring the reality of Aboriginal people who have been subjected to the politics of assimilation and economic modernization. As a way to explore Aboriginal relationship to land against the reality of their life, it is worthwhile investigating de facto land use institutions evolving in an Aboriginal community.
    [Show full text]
  • Volcanic Landslide Risk Management, Lillooet River Valley, BC: Start of North and South Fsrs to Meager Confluence, Meager Creek and Upper Lillooet River
    Volcanic Landslide Risk Management, Lillooet River Valley, BC: Start of north and south FSRs to Meager Confluence, Meager Creek and Upper Lillooet River. Submitted to: Malcolm Schulz, RPF Engineering Officer Metro Vancouver Squamish District Ministry of Forests, Lands and Natural Resource Operations Submitted by: Pierre Friele, P. Geo. Cordilleran Geoscience, PO Box 612, 1021 Raven Drive, Squamish, BC V8B 0A5 March 10, 2012 Table of Contents Introduction ......................................................................................................................... 1 Scope ................................................................................................................................... 1 Hazard & Risk Assessment ................................................................................................. 1 Volcanic Landslide Hazard ................................................................................................. 2 Hazard Frequency and Magnitude .................................................................................. 2 Affected Areas ................................................................................................................ 3 Proximal Zones ........................................................................................................... 3 Distal Zone .................................................................................................................. 4 Consequences of Volcanic Landslide Impacts ..............................................................
    [Show full text]
  • Electoral Area Directors Committee Agenda September 7, 2016; 10:30 AM SLRD Boardroom 1350 Aster Street, Pemberton, BC
    Electoral Area Directors Committee Agenda September 7, 2016; 10:30 AM SLRD Boardroom 1350 Aster Street, Pemberton, BC Item Item of Business and Page Number Page 1. Call to Order We would like to recognize that this meeting is being held on the Traditional Territory of the Líl’wat Nation. 2. Approval of Agenda 3. Electoral Area Directors Closed Meeting THAT the Committee close the meeting to the public under the authority of Section 90(1)(i) of the Community Charter. 4. Rise & Report from the Closed Meeting 5. Consent Agenda (Voting rule on each item may vary; unanimous vote required) Items appearing on the consent agenda which present a conflict of interest for Committee Members must be removed from the Consent Agenda and considered separately. Any items to be debated or voted against must be removed from the Consent Agenda and considered separately. THAT the resolutions set out in the Consent Agenda be approved, and those Consent Agenda items which do not have resolutions related thereto be received. 5.1 Confirmation and Receipt of Minutes 5.1.1. Electoral Area Directors Committee Meeting Draft 4 - 9 Minutes of July 13, 2016 THAT the Electoral Area Directors Committee Meeting Minutes of July 13, 2016 be approved as circulated. 5.2 Staff Reports & Other Business 5.2.1. July and August 2016 Select Funds Report 10 - 14 For Information 5.2.2. July and August 2016 Monthly Building Report 15 - 27 For Information Item Item of Business and Page Number Page 5.3 Correspondence for Information 5.3.1. Correspondence for Information - Completion of Fuel 28 Management Prescription (Gates Lake) 6.
    [Show full text]
  • Fee Creek Salmon Spawning Channel Riparian Restoration Project
    Fee Creek Spawning and Rearing Channel Re-Vegetation Project Fee Creek Salmon Spawning Channel Riparian Restoration Project Prepared for: University of Victoria Restoration of Natural Systems Diploma Program ER- 390 Selected Project Prepared by: Kathy Jenkins Student # - 0135005 February, 2008 Fee Creek Spawning and Rearing Channel Re-Vegetation Project ABSTRACT In 1991, the Department of Fisheries and Oceans created a spawning and rearing system beside the Birkenhead River to enhance habitat for Coho (Oncorhynchus kisutch) and Chinook (Oncorhynchus tshawytscha) salmon primarily. The stocks of salmon from the Fraser River salmon runs had been declining since the 1970’s and there were efforts undertaken around the province to change this pattern of decline. A fish hatchery was built near the Fee Creek spawning channel before this development. The channel was designed to help enhance the salmon population more naturally; through increasing important habitat and to use the area in coordination with the hatchery for increased hatchery success... The DFO created a series of ponds and riffles to provide both spawning and rearing habitat for salmon and the area has been maintained since and has provided a healthy habitat for salmon. Fee Creek is currently used not only for important reproduction habitat but also for educational purposes. As part of the Department of Fisheries Salmonids in the Classroom program children are brought to the area to learn about the life cycle of salmon and their importance in our ecosystems. The Fee Creek re- vegetation project was developed to restore an area of the system that had been destroyed by BC Hydro clearing during their routine power line protection.
    [Show full text]
  • Impact of a Quaternary Volcano on Holocene Sedimentation in Lillooet River Valley, British Columbia
    Sedimentary Geology 176 (2005) 305–322 www.elsevier.com/locate/sedgeo Impact of a Quaternary volcano on Holocene sedimentation in Lillooet River valley, British Columbia P.A. Frielea,T, J.J. Clagueb, K. Simpsonc, M. Stasiukc aCordilleran Geoscience, 1021, Raven Drive, P.O. Box 612, Squamish, BC, Canada V0N 3G0 bDepartment of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada V5A 1S6; Emeritus Scientist, Geological Survey of Canada, 101-605 Robson Street, Vancouver, BC, Canada V6B 5J3 cGeological Survey of Canada, 101-605 Robson Street, Vancouver, BC, Canada V6B 5J3 Received 3 May 2004; received in revised form 15 December 2004; accepted 19 January 2005 Abstract Lillooet River drains 3850 km2 of the rugged Coast Mountains in southwestern British Columbia, including the slopes of a dormant Quaternary volcano at Mount Meager. A drilling program was conducted 32–65 km downstream from the volcano to search for evidence of anomalous sedimentation caused by volcanism or large landslides at Mount Meager. Drilling revealed an alluvial sequence consisting of river channel, bar, and overbank sediments interlayered with volcaniclastic units deposited by debris flows and hyperconcentrated flows. The sediments constitute the upper part of a prograded delta that filled a late Pleistocene lake. Calibrated radiocarbon ages obtained from drill core at 13 sites show that the average long-term floodplain aggradation rate is 4.4 mm aÀ1 and the average delta progradation rate is 6.0 m aÀ1. Aggradation and progradation rates, however, varied markedly over time. Large volumes of sediment were deposited in the valley following edifice collapse events and the eruption of Mount Meager volcano about 2360 years ago, causing pulses in delta progradation, with estimated rates to 150 m aÀ1 over 50-yr intervals.
    [Show full text]
  • Lands and Resources Department Newsletter July 2019
    LANDS AND RESOURCES DEPARTMENT NEWSLETTER JULY 2019 Welcome to our first edition of the Lands & Resources Department Newsletter! We are introducing this quarterly newsletter to provide regular updates about the work carried out by the Lands and Resources Department. News and updates will also be posted on the Lílwat̓ Nation website. www.lilwat.ca The Land is central to Lílwat̓ culture and identity as expressed in the Ucwalmicwts phrase “Pal7míntwal i ucwalmícwa múta7 ti tmicw” The land and people are together as one. This core belief is the cornerstone of the Land’s and Resources Department’s work – it’s goal being to maximize the Lil’wat Nation’s control over its land and resources. 1 | P a g e Lands and Resources Department Newsletter – July 2019 Lands and Resources Department New Logo We are very excited to be using this drawing created by Johnny Jones as the logo for our department. The image can be found in pictographs throughout Lílwat̓ Territory. It symbolizes the traveler. Look for it on our vehicles and field worker uniforms. Skél7awlh ~ STEWARD To honour and recognize the important stewardship role our field workers take on throughout Lílwat̓ Territory they will now be wearing uniforms with the words “Skél7awlh” and “STEWARD”. The Ucwalmicwts word Skél7awlh was described by Charlie Mack as meaning a “resources or game steward” and used to describe a person with the responsibility to manage and protect the land and resources and pass this knowledge on to their kin. 2 | P a g e Lands and Resources Department Newsletter – July 2019 Lands and Resources Department Staff The Lands and Resources Department has nine (9) full time staff and many more seasonal and on-call workers.
    [Show full text]
  • Health Society Set to Disappear
    ;::bortion access lacking Highway turns 50 Dynamic duo A provincial study finds there isn't The Second' World War spurred The Gibsons turned on the power equal access to abortion Terrace's road connections to the to give locals lots to cheer at services/NEWS A7 outside/COMMUNITY B1 Grass Blast '94/SPORTS Cl WEDNESDAY 75¢ PLUS 5¢ GST SEPTEMBER 71 1994 TANDARD VOL. 7 NO. 21 Health society set to disappear WHAT COULD very well be the Terrace Regional Health Care municipal, regional district and "The community health council That's because the society itself the Terrace Regional Health Cam last ever annual general meeting Society is to cease to exist be- school board elections. will have control and will have was formed in 1988 when the Society takes place Sept. 15 at8 of the Terrace Regional Health tween this fall and the fail of Another one-third of the board the mandate to do what they boards of Mills Memorial Hospi- p.m. in the cafeteria of Mills Care Society takes place next 1996," society chief executive will be appointed by the provin- want. Each community is being tal and Terraceview Lodge amal- Memorial Hospital. week. officer Michael Leisinger said cial government and the remain- allowed to develop their own gamated. Coming open are the positions Responsible for the operations last week. ing one-third appointed by exist- model," Leisinger added. "Ours was one of the first to now held by board members Ray of Mills Memorial Hospital and ing local governments. At $15 million, the budgets of look at what was possible," said Jones, Wilton Costain and Sandy That new health council is in its the Terraceview Lodge extended Leisinger said it's too early to Mills Memorial and Terraceview Leisinger.
    [Show full text]
  • Black Tusk Area
    ., Johnny Jones 7"'-.li, ,, .l•"'~ 7N-"':jiii:r ::f4~ U Q'ELQAMTENSA TI SKENKNAPA- BLACK TUSK AREA We are pleased to present these The name,Q 'elqamtensa n Skenknapa, refers to Black Tusk, the mountaintop drawings ofLil'watlandscapes by Johnny on which the thunderbird rests. Jones. Each represents a certain portion of their traditional territory, and Johnny ~ ~ ~ Sunulhkaz is the name of the serpent-like water mon­ Jones has done this in a manner that con­ ~ ster that flowed between Alta Lake and Green Lake. nects it with the artistic rock-art styles of their ancestors: these are pictographic A shaman, scwena7em, in a canoe on Green Lake, once saw a falling star. representations ofthei r landscape. He picked it up and kept it in his medicine bag, thereafter giving him greater In the drawings are images from power and luck. the rock art of their territory as well as pictographic markings ofother ancestral A- A woman once led a war party across the ice of Green Lake in winter. She archaeological sites, such as villages, ( said, "1 am hungry," and stopped to sit down and wash her hands in the camps, hunting areas, and gathering * snow. Then, she pointed to geese flying overhead-one dropped straight to sites. He includes spiritual areas and the ice, dead. transformer sites to show how the stories inform the shapes of the landscapes and A Wolf Clan village was located at the base of Tsiqten, or Fitzsimmons their meaning. Creek, which flows between Tsiqten (Blackcomb Mountain) and Kacwitma Some of these drawings eventually (Whistler Mountain).
    [Show full text]
  • Publication of the Archaeological Society of British Columbia INSIDE
    Publication of the Archaeological Society of British Columbia ISSN 0047-7222 Vol.23, No.3 June 1991 INSIDE: Archaeology gets its feet wet ... page 1. Debitage ... page 5. Victoria ASBC chapter digs in ... page 6. Letter to the editor ... page 8. Volunteer opportunities ... page 8. Heritage legislation news ... page 9. Book reviews ... page 10. Permits ... page 12. What to see this summer ... page 13. The Midden Publication of the Archaeological Society of British Columbia Editor: Kathryn Bernick Subscriptions and Mailing: Helmi Braches Submissions and exchange publications should be directed Subscription is by membership in the A.S.B.C. (see below), or to the Editor. Contributions on subjects germane to B.C. non-member rates of $12.00 a year (5 issues). U.S.A. and overseas archaeology are welcomed: maximum length 1,500 words, $14.00 a year. Check or postal money order in Canadian funds no footnotes, and only a brief bibliography (if necessary at payable to the A.S.B.C. Address to: Midden Subcriptions, P.O. Box 520, Station A, Vancouver, B.C. V6C 2N3. all). Guidelines available. The contents of The Midden are copyrighted by the A.S.B.C. It is The next issue of The Midden will appear unlawful to reproduce all or part by any means whatsoever, without mid-October 1991. permission of the Society, which is usually gladly given. Publication of The Midden is made possible in part by financial Contributors this issue: Brian Apland, Kathryn assistance from the Ministry of Municipal Affairs, Recreation and Bernick, Norm Easton, Grant Keddie, Phyllis Mason, Culture through the British Columbia Heritage Trust and B.C.
    [Show full text]
  • Download Download
    Ames, Kenneth M. and Herbert D.G. Maschner 1999 Peoples of BIBLIOGRAPHY the Northwest Coast: Their Archaeology and Prehistory. Thames and Hudson, London. Abbas, Rizwaan 2014 Monitoring of Bell-hole Tests at Amoss, Pamela T. 1993 Hair of the Dog: Unravelling Pre-contact Archaeological Site DhRs-1 (Marpole Midden), Vancouver, BC. Coast Salish Social Stratification. In American Indian Linguistics Report on file, British Columbia Archaeology Branch, Victoria. and Ethnography in Honor of Lawrence C. Thompson, edited by Acheson, Steven 2009 Marpole Archaeological Site (DhRs-1) Anthony Mattina and Timothy Montler, pp. 3-35. University of Management Plan—A Proposal. Report on file, British Columbia Montana Occasional Papers No. 10, Missoula. Archaeology Branch, Victoria. Andrefsky, William, Jr. 2005 Lithics: Macroscopic Approaches to Acheson, S. and S. Riley 1976 Gulf of Georgia Archaeological Analysis (2nd edition). Cambridge University Press, New York. Survey: Powell River and Sechelt Regional Districts. Report on Angelbeck, Bill 2015 Survey and Excavation of Kwoiek Creek, file, British Columbia Archaeology Branch, Victoria. British Columbia. Report in preparation by Arrowstone Acheson, S. and S. Riley 1977 An Archaeological Resource Archaeology for Kanaka Bar Indian Band, and Innergex Inventory of the Northeast Gulf of Georgia Region. Report on file, Renewable Energy, Longueuil, Québec. British Columbia Archaeology Branch, Victoria. Angelbeck, Bill and Colin Grier 2012 Anarchism and the Adachi, Ken 1976 The Enemy That Never Was. McClelland & Archaeology of Anarchic Societies: Resistance to Centralization in Stewart, Toronto, Ontario. the Coast Salish Region of the Pacific Northwest Coast. Current Anthropology 53(5):547-587. Adams, Amanda 2003 Visions Cast on Stone: A Stylistic Analysis of the Petroglyphs of Gabriola Island, B.C.
    [Show full text]