Our Constitution Is Set in Stone: Looking at The
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Diary of William a Quantz © Lived 1854 – 1945
Diary of William A Quantz © Lived 1854 – 1945 Volume 6 1920 – 1922 Source and Copy Reference Information While copyright and ownership remains with all direct descendants of William A. Quantz, the family welcomes inquiries from readers about additional usage consistent with the spirit and purposes as stated by the author." You can contact us at [email protected]. Note: Starting with volume 5 the page numbers started at 1 again. Volume 6 starts at page 127. Page 127 1920 - Happy New Year - 1920 A bright new year and a sunny track Along and upward way, And a song of praise on looking back Wednesday year has passed away, And golden sheaves, nor small north you, This is my New Year’s wish for you. January 3:. Last Sunday I went up to the First Christian Church on Bathurst Street, and heard Morton preach. Went home with him for dinner and had a good visit. Monday Flo and I went up to cousin Jake Quantz’s at Edgely. Had another good visit and came back to the city on Wednesday in Joe Quantz’s car with them. New Year’s Day was spent with the girls again and yesterday we came home. Brother Ed is down from Alberta and he brought Minnie Ruth from Wellington’s and I expect they will be with us for some time. January 10:. We are enjoying ourselves at home once more. Ed and Minnie are here and we are doing as much visiting as work. The weather has been cold and it seems to be a cozy place in the bay-window over the register. -
Self-Guiding Geology Tour of Stanley Park
Page 1 of 30 Self-guiding geology tour of Stanley Park Points of geological interest along the sea-wall between Ferguson Point & Prospect Point, Stanley Park, a distance of approximately 2km. (Terms in bold are defined in the glossary) David L. Cook P.Eng; FGAC. Introduction:- Geomorphologically Stanley Park is a type of hill called a cuesta (Figure 1), one of many in the Fraser Valley which would have formed islands when the sea level was higher e.g. 7000 years ago. The surfaces of the cuestas in the Fraser valley slope up to the north 10° to 15° but approximately 40 Mya (which is the convention for “million years ago” not to be confused with Ma which is the convention for “million years”) were part of a flat, eroded peneplain now raised on its north side because of uplift of the Coast Range due to plate tectonics (Eisbacher 1977) (Figure 2). Cuestas form because they have some feature which resists erosion such as a bastion of resistant rock (e.g. volcanic rock in the case of Stanley Park, Sentinel Hill, Little Mountain at Queen Elizabeth Park, Silverdale Hill and Grant Hill or a bed of conglomerate such as Burnaby Mountain). Figure 1: Stanley Park showing its cuesta form with Burnaby Mountain, also a cuesta, in the background. Page 2 of 30 Figure 2: About 40 million years ago the Coast Mountains began to rise from a flat plain (peneplain). The peneplain is now elevated, although somewhat eroded, to about 900 metres above sea level. The average annual rate of uplift over the 40 million years has therefore been approximately 0.02 mm. -
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. -
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. -
Occurrence and Genesis of Apline Linears Due To
OCCURRENCE AND GENESIS OF ALPINE LINEARS DUE TO GRAVITATIONAL DEFORMATION IN SOUTH WESTERN, BRITISH COLUMBIA Derek Kinakin BSc, Simon Fraser University 2002 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the Department of Earth Sciences O Kinakin 2004 SIMON FRASER UNIVERSITY Fa11 2004 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: Derek Kinakin Degree: MSc Title of Thesis: Occurrence and genesis of alpine hears due to gravitational deformation in South Western, British Columbia Examining Committee: Chair: Dr. Peter Mustard Associate Professor Department of Earth Sciences, SFU Dr. Doug Stead Senior Supervisor Professor Department of Earth Sciences, SFU Dr. Brent Ward Supervisor Associate Professor Department of Earth Sciences, SFU Bruce Thomson, MSc., PGeo. Supervisor Ministry of Water, Land & Air Protection (Ret.) Tom Stewart, MSc., PEng. External Examiner Civil Engineer B.C. Hydro Date DefendedlApproved: November 15,2004 DECLARATION OF PARTIAL COPYRIGHT LICENCE The author, whose copyright is declared on the title page of this work, has granted to Simon Fraser University the right to lend this thesis, project or extended essay 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. The author has further granted permission to Simon Fraser University to keep or make a digital copy for use in its circulating collection, and, without changing the content, to translate the thesislproject or extended essays, if technically possible, to any medium or format for the purpose of preservation of the digital work. -
Dendrohydrological Reconstruction and Hydroclimatic Variability in Southwestern British Columbia, Canada
Dendrohydrological reconstruction and hydroclimatic variability in southwestern British Columbia, Canada by Bryan J. Mood B.Sc., Mount Allison University, 2013 M.Sc., University of Victoria, 2015 A Dissertation Submitted in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY in the Department of Geography © Bryan Mood, 2019 University of Victoria All rights reserved. This dissertation may not be reproduced in whole or in part, by photocopying or other means, with the permission of the author. Supervisory Committee Dendrohydrological reconstruction and hydroclimatic variability in southwestern British Columbia, Canada by Bryan J. Mood B.Sc., Mount Allison University, 2013 M.Sc., University of Victoria, 2015 Supervisory Committee Dr. Dan J. Smith (Department of Geography) Supervisor Dr. David Atkinson (Department of Geography) Departmental Member Dr. Tobi Gardner (Victoria Capital Regional District) Outside Member ii Abstract Supervisory Committee Dr. Dan J. Smith (Department of Geography) Supervisor Dr. David Atkinson (Department of Geography) Departmental Member Dr. Tobi Gardner (Victoria Capital Regional District) Outside Member The hydrology of southwestern British Columbia is influenced by the region’s mountainous topography and climate oscillations generated from the Pacific Ocean. While much of the region is characterized as a temperate rainforest, recent summers are defined by record-breaking droughts that focus attention on the threat to regional water supply security likely to accompany future climate changes. The limited length and distribution of hydrological records in southwestern British Columbia provide poor context for resource managers tasked with developing policy and water management strategies. The purpose of the dissertation was to describe long-term variability in several key hydroclimatic variables and hydroecological interactions that may be used in updated water resource policy and management strategies. -
Revised Draft Experiences with Inter Basin Water
REVISED DRAFT EXPERIENCES WITH INTER BASIN WATER TRANSFERS FOR IRRIGATION, DRAINAGE AND FLOOD MANAGEMENT ICID TASK FORCE ON INTER BASIN WATER TRANSFERS Edited by Jancy Vijayan and Bart Schultz August 2007 International Commission on Irrigation and Drainage (ICID) 48 Nyaya Marg, Chanakyapuri New Delhi 110 021 INDIA Tel: (91-11) 26116837; 26115679; 24679532; Fax: (91-11) 26115962 E-mail: [email protected] Website: http://www.icid.org 1 Foreword FOREWORD Inter Basin Water Transfers (IBWT) are in operation at a quite substantial scale, especially in several developed and emerging countries. In these countries and to a certain extent in some least developed countries there is a substantial interest to develop new IBWTs. IBWTs are being applied or developed not only for irrigated agriculture and hydropower, but also for municipal and industrial water supply, flood management, flow augmentation (increasing flow within a certain river reach or canal for a certain purpose), and in a few cases for navigation, mining, recreation, drainage, wildlife, pollution control, log transport, or estuary improvement. Debates on the pros and cons of such transfers are on going at National and International level. New ideas and concepts on the viabilities and constraints of IBWTs are being presented and deliberated in various fora. In light of this the Central Office of the International Commission on Irrigation and Drainage (ICID) has attempted a compilation covering the existing and proposed IBWT schemes all over the world, to the extent of data availability. The first version of the compilation was presented on the occasion of the 54th International Executive Council Meeting of ICID in Montpellier, France, 14 - 19 September 2003. -
Building of the Coquitlam River and Port Moody Trails Researched and Written by Ralph Drew, Belcarra, BC, June 2010; Updated Dec 2012 and Dec 2013
Early Trail Building in the New Colony of British Columbia — John Hall’s Building of the Coquitlam River and Port Moody Trails Researched and written by Ralph Drew, Belcarra, BC, June 2010; updated Dec 2012 and Dec 2013. A recent “find” of colonial correspondence in the British Columbia Archives tells a story about the construction of the Coquitlam River and Port Moody Trails between 1862 and 1864 by pioneer settler John Hall. (In 1870 Hall pre-empted 160 acres of Crown Land on Indian Arm and became Belcarra’s first European settler.) The correspondence involves a veritable “who’s who” of people in the administration in the young ‘Colony of British Columbia’. This historic account serves to highlight one of the many challenges faced by our pioneers during the period of colonial settlement in British Columbia. Sir James Douglas When the Fraser River Gold Rush began in the spring of 1858, there were only about 250 to 300 Europeans living in the Fraser Valley. The gold rush brought on the order of 30,000 miners flocking to the area in the quest for riches, many of whom came north from the California gold fields. As a result, the British Colonial office declared a new Crown colony on the mainland called ‘British Columbia’ and appointed Sir James Douglas as the first Governor. (1) The colony was first proclaimed at Fort Langley on 19th November, 1858, but in early 1859 the capital was moved to the planned settlement called ‘New Westminster’, Sir James Douglas strategically located on the northern banks of the Fraser River. -
Points of Interest
16 15 NORTH POINTS OF INTEREST VANCOUVER SCIENCE WORLD SHIPPING CONTAINER DOCK 13 Not-for-profit organization dedicated (PORT METRO VANCOUVER) Canada’s largest and most diversified 14 12 to engaging British Columbians in 5 science and inspiring future science and port, a dynamic gateway for domestic 17 technology leadership. and international trade and tourism, and a major economic force that strengthens BC PLACE STADIUM the Canadian economy. Multi-purpose stadium located at the north side of False Creek. LONSDALE QUAY BURRARD With over 80 specialty shops and INLET YALETOWN services, Lonsdale Quay Market and Trendy and upscale renovated Shops is the premier destination for warehouse district. This fresh urban tourists and locals alike. STANLEY neighbourhood is just an easy walk from 6 the centre of downtown. SEASPAN SHIPYARD PARK Conveniently located to serve the WEST END BEACHES Pacific Northwest's marine industry, The southern edge of the West our full-service shipyards have a solid End neighbourhood has two of the reputation for the design, construction most attractive waterfront urban and maintenance of all types of vessels. environments - English Bay and Sunset LOST Beach. SULPHUR PILE The powder like substance is extracted LAGOON SIWASH ROCK from natural gas and though once A Squamish first nation legend has it, considered a waste product is now that as a reward for putting the needs used readily in fertilizers. Up to 35% of BEACH AVE of his family first, a young swimmer was the world’s trade in sulphur is passed 7 transformed into Siwash Rock. through the Port of Vancouver. COAL VANCOUVER STANLEY PARK 8 9 LIONS GATE BRIDGE HARBOUR 11 HARBOUR 1,001-acre public park that borders the Opened in 1938, officially known as the 4 downtown of Vancouver and is almost First Narrows Bridge, is a suspension W GEORGIA ST entirely surrounded by waters of the bridge that crosses the first narrows 10 Pacific Ocean. -
Cheam Range, Lady Peak, North Face
AAC Publications Cheam Range, Lady Peak, North Face Canada, British Columbia, North Cascades On May 7, Brette Harrington and Marc-André Leclerc climbed the north face of Lady Peak (2,178m) in the Cheam Range, near Chilliwack. This was likely the first ascent of the face, whose steepest section gains about 500m and is comprised of loose but compact volcanic rock. The two spent 13 hours on the climb, which involved thin ice and technical dry tooling on slabs, often with marginal protection (11 long pitces, 5.8 M4 80°). They topped out at sundown and scrambled to the summit before descending easy slopes to the west. In January 2016, the same pair made the probable first ski descent of the northeast couloir on Lady Peak. – Dougald MacDonald, with information from Marc-André Leclerc The following first-person account of this ascent, by Marc-André Leclerc, unfortunately was received too late for publication in the print edition of AAJ 2018: On May 7, Brette Harrington and I climbed a line, right of center, on the imposing north face of Lady Peak in the Cheam Range, the same range of mountains where I essentially began my true mountaineering apprenticeship, with an ascent of Welch Peak, at 11 years old. The area is well known for very loose rock, and the more technical routes are often done in winter or spring as frozen mixed routes. The north face of Lady Peak is the steepest in the range and could be considered the last major face in the range to be climbed, as the unclimbed north face of the Still, while appealing, is quite small in comparison. -
RG 42 - Marine Branch
FINDING AID: 42-21 RECORD GROUP: RG 42 - Marine Branch SERIES: C-3 - Register of Wrecks and Casualties, Inland Waters DESCRIPTION: The finding aid is an incomplete list of Statement of Shipping Casualties Resulting in Total Loss. DATE: April 1998 LIST OF SHIPPING CASUALTIES RESULTING IN TOTAL LOSS IN BRITISH COLUMBIA COASTAL WATERS SINCE 1897 Port of Net Date Name of vessel Registry Register Nature of casualty O.N. Tonnage Place of casualty 18 9 7 Dec. - NAKUSP New Westminster, 831,83 Fire, B.C. Arrow Lake, B.C. 18 9 8 June ISKOOT Victoria, B.C. 356 Stranded, near Alaska July 1 MARQUIS OF DUFFERIN Vancouver, B.C. 629 Went to pieces while being towed, 4 miles off Carmanah Point, Vancouver Island, B.C. Sept.16 BARBARA BOSCOWITZ Victoria, B.C. 239 Stranded, Browning Island, Kitkatlah Inlet, B.C. Sept.27 PIONEER Victoria, B.C. 66 Missing, North Pacific Nov. 29 CITY OF AINSWORTH New Westminster, 193 Sprung a leak, B.C. Kootenay Lake, B.C. Nov. 29 STIRINE CHIEF Vancouver, B.C. Vessel parted her chains while being towed, Alaskan waters, North Pacific 18 9 9 Feb. 1 GREENWOOD Victoria, B.C. 89,77 Fire, laid up July 12 LOUISE Seaback, Wash. 167 Fire, Victoria Harbour, B.C. July 12 KATHLEEN Victoria, B.C. 590 Fire, Victoria Harbour, B.C. Sept.10 BON ACCORD New Westminster, 52 Fire, lying at wharf, B.C. New Westminster, B.C. Sept.10 GLADYS New Westminster, 211 Fire, lying at wharf, B.C. New Westminster, B.C. Sept.10 EDGAR New Westminster, 114 Fire, lying at wharf, B.C. -
Racial Identity and Rights Activism in Vancouver, 1919
“OUTOFMANYKINDREDSANDTONGUES”: RACIALIDENTITYANDRIGHTSACTIVISMINVANCOUVER,1919Ͳ1939 by LiLynnWan Submittedinpartialfulfilmentoftherequirements forthedegreeofDoctorofPhilosophy at DalhousieUniversity Halifax,NovaScotia April2011 ©CopyrightbyLiLynnWan,2011 DALHOUSIEUNIVERSITY DEPARTMENTOFHISTORY TheundersignedherebycertifythattheyhavereadandrecommendtotheFacultyof GraduateStudiesforacceptanceathesisentitled““OUTOFMANYKINDREDSAND TONGUES”:RACIALIDENTITYANDRIGHTSACTIVISMINVANCOUVER,1919Ͳ1939”by LiLynnWaninpartialfulfillmentoftherequirementsforthedegreeofDoctorof Philosophy. Dated: April14,2011 ExternalExaminer: _________________________________ ResearchSupervisor: _________________________________ ExaminingCommittee: _________________________________ _________________________________ DepartmentalRepresentative:_________________________________ ii DALHOUSIEUNIVERSITY DATE: April14,2011 AUTHOR: LiLynnWan TITLE: “OUTOFMANYKINDREDSANDTONGUES”:RACIALIDENTITYANDRIGHTS ACTIVISMINVANCOUVER,1919Ͳ1939 DEPARTMENTORSCHOOL: DepartmentofHistory DEGREE: PhD CONVOCATION: October YEAR: 2011 PermissionisherewithgrantedtoDalhousieUniversitytocirculateandtohavecopied for nonͲcommercial purposes, at its discretion, the above title upon the request of individualsorinstitutions.Iunderstandthatmythesiswillbeelectronicallyavailableto thepublic. The author reserves other publication rights, and neither the thesis nor extensive extractsfromitmaybeprintedorotherwisereproducedwithouttheauthor’swritten permission. The authorattests