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Transportation
OCTOBER 2009 SITELINESLandscape Architecture in British Columbia TransporTaTion Canada Line Opening | Road Rights of Way Receives ASLA Award | Vancouver Green Streets | Multi-modal Pathway Design 2009Ad_Habitat_Evos:Layout 1 9/30/09 4:42 PM Page 1 Inspired Artistic Gyroscopic EvosTM is the unique playsystem where imagination rules and feet never need to touch the ground. Its artistic, Exclusive BC Representative spherical design and play components create a fresh shape in play that’s positively “gyroscopic.” With Evos, kids build agility and confidence as they balance and counterbalance their bodies against the forces of gravity. Exclusively from Landscape Structures; leading the evolution of play. See Evos in action at playlsi.com/go/Evos. 2 SITELINES BC Society Of Landscape Architects Editor’s note By Brett Hitchins 110 - 355 Burrard st. Vancouver, BC V6C 2G8 604.682.5610 604.681.3394 T F Since August 17th, traveling from downtown Vancouver to YVR International Airport W www.bcsla.org E [email protected] www.sitelines.org has been much easier. The $1.9 billion Canada Line SkyTrain project is up and running and critics are clamoring to offer their opinions on the successes and shortcomings of the rapid transit. Canada Line is the poster child of recent transportation projects, but it is one of many projects in progress across the province that are focusing on two objectives: (1) Improving the PresidenT Katherine Dunster PresidenT Elect Mark van der Zalm efficiency and safety of our daily commutes and the transport of goods, and (2) bolstering lo- Past PresidenT David Thompson cal economies through improved access to business and industrial areas. -
Mapping Recreational Trails Withing the Lower Seymour Conservation
Final Project Report Mapping Recreational Trails Within The Lower Seymour Conservation Reserve For: Heidi Walsh April 2001 From: Tony Botica Patrick Kaiser Mark McGough Table of Contents Summary…………………………………………..……………………………………………………..1 Introduction…………………………………………………………..…………………………………..2 Procedure………………………………………………………………………………..……………….4 Results………………………………………………..…………………………………………………..7 Problems………………………………………………………………….……………………………..11 Conclusion…...…………………………………………………………………………………………13 List of Appendices: Appendix 1: Access Road………………………………………………………………………………14 Appendix 2: Baselines 1,2,3……………………………………………………………………………17 Appendix 3: Blair Range………………………………………………………………………………..33 Appendix 4: Bottle Top…………………………………………………………………………………37 Appendix 5: CBC Trail…………………………………………………………………………………43 Appendix 6: Corkscrew Connector…………………………………………………………………..…90 Appendix 7: Corkscrew………………………………………………………………………………...93 Appendix 8: Cut-off Trail……………………………………………………………………………..102 Appendix 9: Dales Trail……………………………………………………………………………….106 Appendix 10: Dales/Blair Range Connector…………………………………………………………..120 Appendix 11: Fork Connector…………………………………………………………………………122 Appendix 12: Incline…………………………………………………………………………………..125 Appendix 13: Lizzie Lake Loop………………………………………………………………………130 Appendix 14: Mystery Creek………………………………………………………………………….134 Appendix 15: Mystery Falls…………………………………………………………………………...155 Appendix 16: Mystery Creek Fork……………………………………………………………………160 Appendix 17: Mushroom Lot………………………………………………………………………….164 Appendix 18: Mushroom Path………………………………………………………………………...167 -
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. -
Downloaded from the Online Library of the International Society for Soil Mechanics and Geotechnical Engineering (ISSMGE)
INTERNATIONAL SOCIETY FOR SOIL MECHANICS AND GEOTECHNICAL ENGINEERING This paper was downloaded from the Online Library of the International Society for Soil Mechanics and Geotechnical Engineering (ISSMGE). The library is available here: https://www.issmge.org/publications/online-library This is an open-access database that archives thousands of papers published under the Auspices of the ISSMGE and maintained by the Innovation and Development Committee of ISSMGE. The paper was published in the proceedings of the 13th International Symposium on Landslides and was edited by Miguel Angel Cabrera, Luis Felipe Prada-Sarmiento and Juan Montero. The conference was originally scheduled to be held in Cartagena, Colombia in June 2020, but due to the SARS-CoV-2 pandemic, it was held online from February 22nd to February 26th 2021. SCG-XIII INTERNATIONAL SYMPOSIUM ON LANDSLIDES. CARTAGENA, COLOMBIA- JUNE 15th-19th-2020 Methods comparison to predict debris avalanche and debris flow susceptibility in the Capilano Watershed, British Columbia, Canada Silvana Castillo* and Matthias Jakob^ *Department of Earth, Ocean and Atmospheric Sciences, The University of British Columbia ^BGC Engineering Inc. [email protected] Abstract Landslide susceptibility can be assessed by statistical and empirical methods. Statistical methods often require landslide conditioning factors and inventories of events to predict the occurrence probability for regional scales. In contrast, empirical methods compute susceptibility values based on theorical concepts and compare them with observations. Both approaches were followed to evaluate debris avalanche and debris flow susceptibility in the Capilano Watershed in southwestern B.C. This was accomplished through Random Forest (RF) and Flow-R models. The RF model resulted in predictive accuracies of 76% and 83% for debris avalanche and debris flow models, respectively, and 45% and 28% of the total watershed area were classified as high susceptibility for these landslide types, respectively. -
Hop-On Hop-Off
HOP-ON Save on Save on TOURS & Tour Attractions SIGHTSEEING HOP-OFF Bundles Packages Bundle #1 Explore the North Shore Hop-On in Vancouver + • Capilano Suspension Bridge Tour Whistler • Grouse Mountain General Admission* • 48H Hop-On, Hop-Off Classic Pass This bundle takes Sea-to-Sky literally! Start by taking in the spectacular ocean You Save views in Vancouver before winding along Adult $137 $30 the Sea-to-Sky Highway and ascending into Child $61 $15 the coastal mountains. 1 DAY #1: 48H Hop-On, Hop-Off Classic Pass 2020 WINTER 19 - OCT 1, 2019 APR 30, Your perfect VanDAY #2: Whistler + Shannon Falls Tour* Sea to Bridge Experience You Save • Capilano Suspension Bridge day on Hop-On, Adult $169 $30 • Vancouver Aquarium Child $89 $15 • 48H Hop-On, Hop-Off Classic Pass You Save Hop-Off Operates: Dec 1, 2019 - Apr 30, 2020 Classic Pass Adult $118 $30 The classic pass is valid for 48 hours and * Whistler + Shannon Falls Tour operates: Child $53 $15 Choose from 26 stops at world-class • Dec 1, 2019 - Jan 6, 2020, Daily includes both Park and City Routes • Apr 1 - 30, 2020, Daily attractions and landmarks at your • Jan 8 - Mar 29, 2020, Wed, Fri, Sat & Sun 2 own pace with our Hop-On, Hop-Off Hop-On, Hop-Off + WINTER 19 - OCT 1, 2019 - APR 30, 2020 WINTER 19 - OCT 1, 2019 APR 30, Sightseeing routes. $49 $25 Lookout Tower Special Adult Child (3-12) Bundle #2 Hop-On in Vancouver + • Vancouver Lookout Highlights Tour Victoria • 48H Hop-On, Hop-Off Classic Pass • 26 stops, including 6 stops in Stanley Park CITY Route PARK Route and 1 stop at Granville Island Take an in-depth look at Vancouver at You Save (Blue line) (Green Line) your own pace before journeying to the Adult $53 $15 • Recorded commentary in English, French, Spanish, includes 9 stops includes 17 stops quaint island city of Victoria on a full day of Child $27 $8 German, Japanese, Korean & Mandarin Fully featuring: featuring: exploration. -
Erasing Indigenous Indigeneity in Vancouver
Erasing Indigenous Indigeneity in Vancouver J EAN BARMAN1 anada has become increasingly urban. More and more people choose to live in cities and towns. Under a fifth did so in 1871, according to the first census to be held after Canada C 1867 1901 was formed in . The proportion surpassed a third by , was over half by 1951, and reached 80 percent by 2001.2 Urbanization has not benefited Canadians in equal measure. The most adversely affected have been indigenous peoples. Two reasons intersect: first, the reserves confining those deemed to be status Indians are scattered across the country, meaning lives are increasingly isolated from a fairly concentrated urban mainstream; and second, the handful of reserves in more densely populated areas early on became coveted by newcomers, who sought to wrest them away by licit or illicit means. The pressure became so great that in 1911 the federal government passed legislation making it possible to do so. This article focuses on the second of these two reasons. The city we know as Vancouver is a relatively late creation, originating in 1886 as the western terminus of the transcontinental rail line. Until then, Burrard Inlet, on whose south shore Vancouver sits, was home to a handful of newcomers alongside Squamish and Musqueam peoples who used the area’s resources for sustenance. A hundred and twenty years later, apart from the hidden-away Musqueam Reserve, that indigenous presence has disappeared. 1 This article originated as a paper presented to the Canadian Historical Association, May 2007. I am grateful to all those who commented on it and to Robert A.J. -
Capilano IR No. 5 Transportation Study I
Squamish Nation Capilano IR No. 5 Transportation Study Squamish Nation - Capilano IR No. 5 Transportation Study i Contents 1 Introduction ............................................................................................................................ 1 2 Transportation Objectives for the Capilano Lands ............................................................ 4 2.1 Create a Safe, Walkable Community ............................................................................. 4 2.2 Provide Access for Members, Residents, and Businesses on the Capilano Lands ....... 8 2.3 Manage the Impact of Regional Traffic on the Local Network ...................................... 14 3 Ideas for the Transportation Network Today .................................................................... 20 3.1 Ideas for Creating a Safe, Walkable Community .......................................................... 20 3.2 Ideas for Providing Access for Members, Residents and Businesses ......................... 29 3.3 Ideas for Managing the Impact of Regional Traffic ....................................................... 34 4 Considerations for the Future Network Improvements ................................................... 37 4.1 Developing New Connections Across the North Shore ................................................ 37 4.2 Transit Services to Connect Capilano Lands ............................................................... 40 5 Summary ............................................................................................................................. -
Vancouver British Columbia
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The Chilcotin Uprising: a Study Of
THE CHILCOTIN UPRISING: A STUDY OF INDIAN-WHITE RELATIONS IN NINETEENTH CENTURY BRITISH COLUMBIA by EDWARD SLEIGH HEWLETT B.A,, University of British Columbia, 1964 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of History We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA March, 1972 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of History The University of British Columbia Vancouver 8, Canada ill ABSTRACT This thesis deals with a disturbance which broke out in April of 1864 when a group of ChJLlcotin Indians massacred seventeen^workmen on a trail being built from Bute Inlet to the interior of British Columbia, The main endeavours of this thesis are three-fold. It seeks to provide an accurate account of the main events: the killings and the para-military expeditions which resulted from them. It attempts to establish as far as possible the causes of the massacres. Finally, it examines the attitudes of whites towards the Indians as revealed in the actions they took and the views they expressed in connection with the uprising and the resulting expeditions to the Chilcotin territory. -
Outcomes in Suicidal Bridge Jumping in the Lower Mainland-JRB
Outcomes in suicidal bridge jumping in the Lower Mainland by DYLAN STEPHANIAN BASc, The University of British Columbia, 2014 Thesis submitted in partial fulfilment of the requirements for the degree of Master of Science in The Faculty of Graduate and Postdoctoral Studies (Experimental Medicine) The University of British ColumbiA (Vancouver) December, 2019 © Dylan Stephanian, 2019 The following individuals certify that they have read, and recommend to the faculty of Graduate and Postdoctoral Studies for acceptance, the thesis entitled: Outcomes in suicidal bridge jumping in the Lower Mainland Submitted by Dylan Stephanian in partial fulfillment of the requirements for the degree of MAster of Science in Experimental Medicine. Examining committee Dr Jeff Brubacher, Emergency Medicine Supervisor Dr Doug Brown, Emergency Medicine Supervisory Committee Member Dr Andrew MacPherson, Emergency Medicine External Examiner ii Abstract On average, one person attempts suicide by jumping from a bridge in the Lower Mainland of British ColumbiA once every 14 days, but the population that jumps and their outcomes following a suicide attempt are poorly understood. A multi-agency retrospective chart review was performed using records from the Canadian Coast Guard, Joint Rescue Coordination Center, police departments, and the British Columbia Coroner’s Service to identify incidents. A complete picture of each incident was then built by identifying corresponding BC Ambulance Service and hospital records, and linking all records for each incident. This methodology successfully identified a comprehensive list of incidents, and may be useful in future prehospital and search and rescue medicine research. Records from the ten agencies involved in these incidents were collected and linked to create a dataset describing all known jumps from a bridge >12m in height in the Lower Mainland of BC from January 1, 2006 to February 28, 2017. -
COUNCIL CORRESPONDENCE UPDATE to DECEMBER 6, 2019 (8:30 A.M.)
COUNCIL CORRESPONDENCE UPDATE TO DECEMBER 6, 2019 (8:30 a.m.) Referred for Action (1) November 29, 2019, regarding “Rodgers Creek Bylaw Changes Questions and Concerns” (Referred to the Director of Planning & Development Services for consideration and response) (2) December 1, 2019, regarding Leaf Blower Noise Complaint (Referred to the Director of Corporate Services for consideration and response) (3) December 4, 2019, regarding “4175 Burkehikk Place, W.V.” (Referred to the Director of Planning & Development Services for consideration and response) Referred for Action from Other Governments and Government Agencies No items. Received for Information (4) Committee and Board Meeting Minutes – Audit Committee meeting May 13, 2019 (5) 73 submissions, November 17 - December 3, 2019 and undated, regarding Proposed: Zoning Bylaw No. 4662, 2010, Amendment Bylaw No. 5044, 2019; Official Community Plan Bylaw No. 4985, 2018, Amendment Bylaw No. 5045, 2019; and Phased Development Agreement Authorization Bylaw No. 5041, 2019 (Areas 5 and 6 of Rodgers Creek) (Received at the December 3, 2019 public hearing) (6) 4 submissions, November 29 - December 1, 2019, regarding Wireless Technologies (7) 6 submissions, November 29 - December 3, 2019, regarding Proposed Zoning Bylaw No. 4662, 2010, Amendment Bylaw No. 4938, 2019 (5776 Marine Drive - Thunderbird Marina) (Received at the December 3, 2019 public hearing) (8) November 30, 2019, regarding “A job well done” (Sidewalk Maintenance) (9) Vancouver Beideng Society, December 3, 2019, regarding “An Invitation -
Appendix 1: Overview of Plaintiff’S Witnesses, Select Tsilhqot’In Genealogies, Trapline Summaries
No. 90 0913 Victoria Registry IN THE SUPREME COURT OF BRITISH COLUMBIA BETWEEN: ROGER WILLIAM, on his own behalf and on behalf of all other members of the Xeni Gwet’in First Nations Government and on behalf of all other members of the Tsilhqot’in Nation PLAINTIFF AND: HER MAJESTY THE QUEEN IN RIGHT OF THE PROVINCE OF BRITISH COLUMBIA, THE REGIONAL MANAGER OF THE CARIBOO FOREST REGION and THE ATTORNEY GENERAL OF CANADA DEFENDANTS ARGUMENT OF THE PLAINTIFF APPENDIX 1: OVERVIEW OF PLAINTIFF’S WITNESSES, SELECT TSILHQOT’IN GENEALOGIES, TRAPLINE SUMMARIES WOODWARD & ATTORNEY GENERAL DEPARTMENT OF COMPANY OF BRITISH COLUMBIA JUSTICE, CANADA Barristers and Solicitors Civil Litigation Section Aboriginal Law Section 844 Courtney Street, 2nd Floor 3RD Floor, 1405 Douglas Street 900 – 840 Howe Street Victoria, BC V8W 1C4 Victoria, BC V8W 9J5 Vancouver, B.C. V6Z 2S9 Solicitors for the Plaintiff Solicitor for the Defendants, Her Solicitor for the Defendant, Majesty the Queen in the Right of The Attorney General of Canada the Province of British Columbia and the Manager of the Cariboo Forest Region ROSENBERG & BORDEN LADNER ROSENBERG GERVAIS LLP Barristers & Solicitors Barristers & Solicitors 671D Market Hill Road 1200 Waterfront Centre, 200 Vancouver, BC V5Z 4B5 Burrard Street Solicitors for the Plaintiff Vancouver, BC V7X 1T2 Solicitor for the Defendants, Her Majesty the Queen in the Right of the Province of British Columbia and the Manager of the Cariboo Forest Region Exhibit 43 Photograph 29 Appendix 1 Overview of Plaintiff's Witnesses, Select Tsilhqot'in Genealogies, Trapline Summaries Tab Summary of the Lay Witness Evidence A Summary of the Expert Witness Evidence B Select Tsilhqot'in Genealogies C Trapline Summaries D Appendix 1A Summary of Lay Witnesses of the Plaintiff SUMMARY OF LAY WITNESSES OF THE PLAINTIFF.........................................................