George Black — Early Pioneer Settler on the Coquitlam River
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Plan Employers
Plan Employers 18th Street Community Care Society 211 British Columbia Services Society 28th Avenue Homes Ltd 4347 Investments Ltd. dba Point Grey Private Hospital 484017 BC Ltd (dba Kimbelee Place) 577681 BC Ltd. dba Lakeshore Care Centre A Abilities Community Services Acacia Ty Mawr Holdings Ltd Access Human Resources Inc Active Care Youth and Adult Services Ltd Active Support Against Poverty Housing Society Active Support Against Poverty Society Age Care Investment (BC) Ltd AIDS Vancouver Society AiMHi—Prince George Association for Community Living Alberni Community and Women’s Services Society Alberni-Clayoquot Continuing Care Society Alberni-Clayoquot Regional District Alouette Addiction Services Society Amata Transition House Society Ambulance Paramedics of British Columbia CUPE Local 873 Ann Davis Transition Society Archway Community Services Society Archway Society for Domestic Peace Arcus Community Resources Ltd Updated September 30, 2021 Plan Employers Argyll Lodge Ltd Armstrong/ Spallumcheen Parks & Recreation Arrow and Slocan Lakes Community Services Arrowsmith Health Care 2011 Society Art Gallery of Greater Victoria Arvand Investment Corporation (Britannia Lodge) ASK Wellness Society Association of Neighbourhood Houses of British Columbia AVI Health & Community Services Society Avonlea Care Centre Ltd AWAC—An Association Advocating for Women and Children AXIS Family Resources Ltd AXR Operating (BC) LP Azimuth Health Program Management Ltd (Barberry Lodge) B BC Council for Families BC Family Hearing Resource Society BC Institute -
Ecosystem Status and Trends Report for the Strait of Georgia Ecozone
C S A S S C C S Canadian Science Advisory Secretariat Secrétariat canadien de consultation scientifique Research Document 2010/010 Document de recherche 2010/010 Ecosystem Status and Trends Report Rapport de l’état des écosystèmes et for the Strait of Georgia Ecozone des tendances pour l’écozone du détroit de Georgie Sophia C. Johannessen and Bruce McCarter Fisheries and Oceans Canada, Institute of Ocean Sciences 9860 W. Saanich Rd. P.O. Box 6000, Sidney, B.C. V8L 4B2 This series documents the scientific basis for the La présente série documente les fondements evaluation of aquatic resources and ecosystems scientifiques des évaluations des ressources et in Canada. As such, it addresses the issues of des écosystèmes aquatiques du Canada. Elle the day in the time frames required and the traite des problèmes courants selon les documents it contains are not intended as échéanciers dictés. Les documents qu’elle definitive statements on the subjects addressed contient ne doivent pas être considérés comme but rather as progress reports on ongoing des énoncés définitifs sur les sujets traités, mais investigations. plutôt comme des rapports d’étape sur les études en cours. Research documents are produced in the official Les documents de recherche sont publiés dans language in which they are provided to the la langue officielle utilisée dans le manuscrit Secretariat. envoyé au Secrétariat. This document is available on the Internet at: Ce document est disponible sur l’Internet à: http://www.dfo-mpo.gc.ca/csas/ ISSN 1499-3848 (Printed / Imprimé) ISSN 1919-5044 (Online / En ligne) © Her Majesty the Queen in Right of Canada, 2010 © Sa Majesté la Reine du Chef du Canada, 2010 TABLE OF CONTENTS Highlights 1 Drivers of change 2 Status and trends indicators 2 1. -
The Story of the Coquitlam River Watershed Past, Present and Future
Fraser Salmon and Watersheds Program – Living Rivers Project Coquitlam River Stakeholder Engagement Phase I The Story of the Coquitlam River Watershed Past, Present and Future Prepared for: The City of Coquitlam and Kwikwetlem First Nation Funding provided by: The Pacific Salmon Foundation Additional funding provided by Fisheries and Oceans Canada Prepared by: Jahlie Houghton, JR Environmental – April 2008 Updated by: Coquitlam River Watershed Work Group – October 2008 Final Report: October 24, 2008 2 File #: 13-6410-01/000/2008-1 Doc #: 692852.v1B Acknowledgements I would like to offer a special thanks to individuals of the community who took the time to meet with me, who not only helped to educate me on historical issues and events in the watershed, but also provided suggestions to their vision of what a successful watershed coordinator could contribute in the future. These people include Elaine Golds, Niall Williams, Don Gillespie, Dianne Ramage, Tony Matahlija, Tim Tyler, John Jakse, Vance Reach, Sherry Carroll, Fin Donnelly, Maurice Coulter-Boisvert, Matt Foy, Derek Bonin, Charlotte Bemister, Dave Hunter, Jim Allard, Tom Vanichuk, and George Turi. I would also like to thank members of the City of Coquitlam, Kwikwetlem First Nation, the Department of Fisheries and Oceans, and Watershed Watch Salmon Society (representative for Kwikwetlem) who made this initiative possible and from whom advice was sought throughout this process. These include Jennifer Wilkie, Dave Palidwor, Mike Carver, Margaret Birch, Hagen Hohndorf, Melony Burton, Tom Cadieux, Dr. Craig Orr, George Chaffee, and Glen Joe. Thank you to the City of Coquitlam also for their printing and computer support services. -
List of Persons Entitled to Vote
40 Vic. Voters' List—New Westminster District. 35 LIST OF PERSONS ENTITLED TO VOTE IN THE ELECTORAL DISTRICT OF NEW WESTMINSTER. Residence of Claimant, with full descrip Christian name and surname of Claimant tion of house, if in a town, with num Profession, trade, or calling. at full length. ber, if any, and name of street. Ashwell, George Randall., Chilliwhack ..... Farmer Arthur, James... Centreville Farmer Arthur, James Henry Centreville Farmer Anderson, Peter Lonzo ... Sumass Farmer Anderson, Jacob Langley Prairie Farmer Aitkins, James Langley Farmer Barker, Henry Sumass , Farmer Barker, William Henry Sumass Farmer 9 Barker, John Chilliwhack Farmer 10 Blanchard, John Albert ... Chilliwhack Farmer 11 Banford, George Chilliwhack Farmer 12 Bell, William Chilliwhack Farmer 13 Bell, John Chilliwhack Farmer 14 Bakeson, Henry Harrison River Farmer 15 Beary, John Chilliwhack Farmer 16 Bicknell, Charles Chilliwhack Parmer 17 Burr, Joseph Jr New Westminster District. Carpenter 18 Bremridge, William New Westminster District. Farmer 19 Brough, John Keatzie Farmer 20 Brewer, William John , Mud Bay Farmer 21 Brown, George Pitt River Farmer 22 Boyd, Hugh North Arm Farmer 23 Betts, Elijah John , North Arm Farmer 24 Browne, Edward Sloone.., North Arm Farmer 25 Booth, James William South Arm Farmer 26 Benton, Henry Dean South Arm Farmer 27 Byron, George South Arm Farmer 28 Bales, Henry Pennington, Farmer 29 Barnes, John Matsqui ; Farmer 30 Burton, Ralph Matsqui Farmer 31 Baker, Peter Langley Farmer 32 Boake, Benjamin , Langley Faimer 33 Burr, William Henry Langley Farmer - 34 Boake, Wellington E , Langley Farmer 35 Barnes, Merton Philip , Boundary Bay Farmer 36 Barnes, Samuel William.. Boundary Bay Farmer 37 Bell, James New Westminster District , Stonemason 38 Craswell, John Chilliwhack Farmer 39 Cotton, James W Chilliwhack Farmer 40 Chadsey, George Washington. -
Prehistoric Mobile Art from the Mid-Fraser and Thompson River Areas ARNOUDSTRYD
CHAPTER9 Prehistoric Mobile Art from the Mid-Fraser and Thompson River Areas ARNOUDSTRYD he study of ethnographic and archaeological art the majority of archaeological work in the Plateau but from interior British Columbia has never received also appear to be the "heartland" of Plateau art develop Tthe attention which has been lavished on the art of ment as predicted by Duff (1956). Special attention will be the British Columbia coast. This was inevitable given the focused on the previously undescribed carvings recovered impressive nature of coastal art and the relative paucity in recent excavations by the author along the Fraser River of its counterpart. Nevertheless, some understanding of near the town of Lillooet. the scope and significance of this art has been attained, Reports and collections from seventy-one archaeologi largely due to the turn of the century work by members cal sites were checked for mobile art. They represent all of the Jesup North Pacific Expedition (Teit 1900, 1906, the prehistoric sites excavated and reported as of Spring 1909; Boas, 1900; Smith, 1899, 1900) and the more recent 1976, although some unintentional omissions may have studies by Duff (1956, 1975). Further, archaeological occurred. The historic components of continually oc excavations over the last fifteen years (e.g., Sanger 1968a, cupied sites were deleted and sites with assemblages of 1968b, 1970; Stryd 1972, 1973) have shown that prehistoric less than ten artifacts were also omitted. The most notable Plateau art was more extensive than previously thought, exclusions from this study are most of Smith's (1899) and that ethnographic carving represented a degeneration Lytton excavation data which are not quantified or listed from a late prehistoric developmental climax. -
Spring Bloom in the Central Strait of Georgia: Interactions of River Discharge, Winds and Grazing
MARINE ECOLOGY PROGRESS SERIES Vol. 138: 255-263, 1996 Published July 25 Mar Ecol Prog Ser I l Spring bloom in the central Strait of Georgia: interactions of river discharge, winds and grazing Kedong yinl,*,Paul J. Harrisonl, Robert H. Goldblattl, Richard J. Beamish2 'Department of Oceanography, University of British Columbia, Vancouver, British Columbia, Canada V6T 124 'pacific Biological Station, Department of Fisheries and Oceans, Nanaimo, British Columbia, Canada V9R 5K6 ABSTRACT: A 3 wk cruise was conducted to investigate how the dynamics of nutrients and plankton biomass and production are coupled with the Fraser River discharge and a wind event in the Strait of Georgia estuary (B.C.,Canada). The spring bloom was underway in late March and early Apnl, 1991. in the Strait of Georgia estuary. The magnitude of the bloom was greater near the river mouth, indicat- ing an earher onset of the spring bloom there. A week-long wind event (wind speed >4 m S-') occurred during April 3-10 The spring bloom was interrupted, with phytoplankton biomass and production being reduced and No3 in the surface mixing layer increasing at the end of the wind event. Five days after the lvind event (on April 15),NO3 concentrations were lower than they had been at the end of the wind event, Indicating a utilization of NO3 during April 10-14. However, the utilized NO3 did not show up in phytoplankton blomass and production, which were lower than they had been at the end (April 9) of the wind event. During the next 4 d, April 15-18, phytoplankton biomass and production gradu- ally increased, and No3 concentrations in the water column decreased slowly, indicating a slow re- covery of the spring bloom Zooplankton data indicated that grazing pressure had prevented rapid accumulation of phytoplankton biomass and rapid utilization of NO3 after the wind event and during these 4 d. -
Examining Controls on Peak Annual Streamflow And
Hydrol. Earth Syst. Sci., 22, 2285–2309, 2018 https://doi.org/10.5194/hess-22-2285-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Examining controls on peak annual streamflow and floods in the Fraser River Basin of British Columbia Charles L. Curry1,2 and Francis W. Zwiers1 1Pacific Climate Impacts Consortium, University of Victoria, Victoria, V8N 5L3, Canada 2School of Earth and Ocean Sciences, University of Victoria, Victoria, V8N 5L3, Canada Correspondence: Charles L. Curry ([email protected]) Received: 26 August 2017 – Discussion started: 8 September 2017 Revised: 19 February 2018 – Accepted: 14 March 2018 – Published: 16 April 2018 Abstract. The Fraser River Basin (FRB) of British Columbia with APF of ρO D 0.64; 0.70 (observations; VIC simulation)), is one of the largest and most important watersheds in west- the snowmelt rate (ρO D 0.43 in VIC), the ENSO and PDO ern North America, and home to a rich diversity of biologi- indices (ρO D −0.40; −0.41) and (ρO D −0.35; −0.38), respec- cal species and economic assets that depend implicitly upon tively, and rate of warming subsequent to the date of SWEmax its extensive riverine habitats. The hydrology of the FRB is (ρO D 0.26; 0.38), are the most influential predictors of APF dominated by snow accumulation and melt processes, lead- magnitude in the FRB and its subbasins. The identification ing to a prominent annual peak streamflow invariably oc- of these controls on annual peak flows in the region may be curring in May–July. -
British Columbia Regional Guide Cat
National Marine Weather Guide British Columbia Regional Guide Cat. No. En56-240/3-2015E-PDF 978-1-100-25953-6 Terms of Usage Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: • Exercise due diligence in ensuring the accuracy of the materials reproduced; • Indicate both the complete title of the materials reproduced, as well as the author organization; and • Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1-800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Disclaimer: Her Majesty is not responsible for the accuracy or completeness of the information contained in the reproduced material. Her Majesty shall at all times be indemnified and held harmless against any and all claims whatsoever arising out of negligence or other fault in the use of the information contained in this publication or product. Photo credits Cover Left: Chris Gibbons Cover Center: Chris Gibbons Cover Right: Ed Goski Page I: Ed Goski Page II: top left - Chris Gibbons, top right - Matt MacDonald, bottom - André Besson Page VI: Chris Gibbons Page 1: Chris Gibbons Page 5: Lisa West Page 8: Matt MacDonald Page 13: André Besson Page 15: Chris Gibbons Page 42: Lisa West Page 49: Chris Gibbons Page 119: Lisa West Page 138: Matt MacDonald Page 142: Matt MacDonald Acknowledgments Without the works of Owen Lange, this chapter would not have been possible. -
We Returned. Now He Mouth. Our Older Relatives Are Gone Mouths. Now a Rocket of Words Bursts Dress, Our Dress of More Shape
returned. We went: we returned. Now he mouth. Our older relatives are gone mouths. Now a rocket of words bursts dress, our dress of more shape. Now eople who donate faces and tongues. ow we run our fingers over their fingers uins we’ve burst too from the terrestri- rstand cloth, home, anything. Are we ister? We can’t yet participate in lost g. Now we were born complex, messy, ards and mats. Our faces now model ves. Now we have or own a shelf. We ches out in a continual thin plane. Our ns dirty water, plants, coins, unraveled e necessary. We’re speaking for the air e black branches, the objects covered the metal fence, some spatial confu- ve gently as the prepositions. What is s better than this. Deep in our doubt a in one place yet move like blackbirds. Occasional Work and Seven Walks from the Office for Soft Architecture Lisa Robertson clear cut press Astoria © 2003 Clear Cut Press and Lisa Robertson All rights reserved. Designed by Tae Won Yu Production and layout by Robin Mitchell Copyedited by Viola Funk and Allison Dubinsky Color Separations by Scan Lab Printed and Bound by Toppan Printing Company America OCCASIONAL WORK AND SEVEN WALKS FROM THE OFFICE OF SOFT ARCHITECTURE / Lisa Robertson ISBN 0-9723234-3-0 Library of Congress Control Number: 2003111519 Photographs not otherwise cited in the text are reproduced with permis- sion from the following sources: pp. 6-11: © Andreas Pauly. Photos of Petra Blaisse’s curtains for the Mick Jagger Centre, Dartford Grammar School for Boys, Kent, England. -
Appendix B: Hydrotechnical Assessment
Sheep Paddocks Trail Alignment Analysis APPENDIX B: HYDROTECHNICAL ASSESSMENT LEES+Associates -112- 30 Gostick Place | North Vancouver, BC V7M 3G3 | 604.980.6011 | www.nhcweb.com 300217 15 August 2013 Lees + Associates Landscape Architects #509 – 318 Homer Street Vancouver, BC V6B 2V2 Attention: Nalon Smith Dear Mr. Smith: Subject: Sheep Paddocks Trail Alignment – Phase 1 Hydrotechnical Assessment Preliminary Report 1 INTRODUCTION Metro Vancouver wishes to upgrade the Sheep Paddocks Trail between Pitt River Road and Mundy Creek in Colony Farm Regional Park on the west side of the Coquitlam River. The trail is to accommodate pedestrian and bicycle traffic and be built to withstand at least a 1 in 10 year flood. The project will be completed in three phases: 1. Phase 1 – Route Selection 2. Phase 2 – Detailed Design 3. Phase 3 – Construction and Post-Construction This letter report provides hydrotechnical input for Phase 1 – Route Selection. Currently, a narrow footpath runs along the top of a berm on the right bank of the river. The trail suffered erosion damage in 2007 and was subsequently closed to the public but is still unofficially in use. Potential future routes include both an inland and river option, as well as combinations of the two. To investigate the feasibility of the different options and help identify the most appropriate trail alignment from a hydrotechnical perspective, NHC was retained to undertake the following Phase I scope of work: • Participate in three meetings. • Attend a site visit. • Estimate different return period river flows and comment on local drainage requirements. • Simulate flood levels and velocities corresponding to the different flows. -
Fraser Valley Geotour: Bedrock, Glacial Deposits, Recent Sediments, Geological Hazards and Applied Geology: Sumas Mountain and Abbotsford Area
Fraser Valley Geotour: Bedrock, Glacial Deposits, Recent Sediments, Geological Hazards and Applied Geology: Sumas Mountain and Abbotsford Area A collaboration in support of teachers in and around Abbotsford, B.C. in celebration of National Science and Technology Week October 25, 2013 MineralsEd and Natural Resources Canada, Geological Survey of Canada Led by David Huntley, PhD, GSC and David Thompson, P Geo 1 2 Fraser Valley Geotour Introduction Welcome to the Fraser Valley Geotour! Learning about our Earth, geological processes and features, and the relevance of it all to our lives is really best addressed outside of a classroom. Our entire province is the laboratory for geological studies. The landscape and rocks in the Fraser Valley record many natural Earth processes and reveal a large part of the geologic history of this part of BC – a unique part of the Canadian Cordillera. This professional development field trip for teachers looks at a selection of the bedrock and overlying surficial sediments in the Abbotsford area that evidence these geologic processes over time. The stops highlight key features that are part of the geological story - demonstrating surface processes, recording rock – forming processes, revealing the tectonic history, and evidence of glaciation. The important interplay of these phenomena and later human activity is highlighted along the way. It is designed to build your understanding of Earth Science and its relevance to our lives to support your teaching related topics in your classroom. Acknowledgments We would like to thank our partners, the individuals who led the tour to share their expertise, build interest in the natural history of the area, and inspire your teaching. -
Port Coquitlam Flood Mapping Update
Port Coquitlam Flood Mapping Update RECOMMENDATION: None. PREVIOUS COUNCIL/COMMITTEE ACTION On September 17, 2019 Council carried the following motion: That staff prepare flood maps showing current flood risk to Port Coquitlam from the Fraser Basin and provide a report in the fall 2019 with information about the risks facing the community from rising sea levels that align with projections in the most recent Intergovernmental Panel on Climate Change report. REPORT SUMMARY Port Coquitlam has participated in the Fraser Basin Council’s Lower Mainland Flood Management Strategy (“the Strategy”) since its development in 2014. Participants in the strategy have responsibilities or interests related to flood management and include the Government of Canada, the Province of British Columbia, Lower Mainland local governments, First Nations and non- governmental and private sector entities in the region. This report summarizes the flood projections for Port Coquitlam, the regional work completed to date and presents the Strategy’s next phase. BACKGROUND The Lower Fraser Watershed is fed by 12 major watersheds. 1. The Upper / Middle Fraser 7. Chilcotin 2. Stuart 8. North Thompson 3. McGregor 9. South Thompson 4. Nechako 10. Thompson 5. Quesnel 11. Lillooet 6. West Road-Blackwater 12. Harrison These watersheds are illustrated on Figure 1. Report To: Committee of Council Department: Engineering & Public Works Approved by: F. Smith Meeting Date: November 19, 2019 Port Coquitlam Flood Mapping Update Figure 1 – Fraser Basin Watersheds https://www.fraserbasin.bc.ca/basin_watersheds.html In addition, the Lower Fraser watershed incorporates a number of smaller watersheds: Stave Lake and River drain into the Fraser between Maple Ridge and Mission; Alouette Lake and River flow into the Pitt River; the Pitt River drains south from Garibaldi Provincial Park through Pitt Lake, emptying into the Fraser River between Pitt Meadows and Port Coquitlam.