Saanich Peninsula LHA Profile 2019
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City of Parksville 250 248-6144 100 Jensen Avenue East PO Box 1390 Parksville, BC V9P 2H3
City of Parksville 250 248-6144 100 Jensen Avenue East http://parksville.ca PO Box 1390 Parksville, BC V9P 2H3 The 2017 Community Profile serves as a guide to companies, organizations and individuals who require information about the City of Parksville. We have used our best efforts to ensure that the information is correct and current. The City distributes the Community Profile under the strict condition that the City of Parksville will not be liable or responsible for the accuracy of the information in this document. For more information, please contact: Deb Tardiff, Manager of Communications City of Parksville 250 954-3073 [email protected] TABLE OF CONTENTS VANCOUVER ISLAND OVERVIEW ............................................................................................3 LOCATION .................................................................................................................................... 3 GEOGRAPHY ................................................................................................................................. 4 CLIMATE ....................................................................................................................................... 4 HISTORY ....................................................................................................................................... 4 COMMUNITY SERVICES ..........................................................................................................5 EMERGENCY SERVICES ................................................................................................................ -
Concussion in Island Health December 2015.Pdf
Photo: Eric Cote/Shutterstock CONCUSSION AMONG ISLAND CHILDRENHEALTH AUTHORITY & YOUTH: The British Columbia Injury Research and Prevention Unit (BCIRPU) was established by the Ministry of Health and the Minister’s Injury Prevention Advisory Committee in August 1997. BCIRPU is housed in the Evidence to Innovation theme within the Child and Family Research Institute (CFRI) and supported by the Provincial Health Services Authority (PHSA) and the University of British Columbia (UBC). BCIRPU’s vision is “to be a leader in the production and transfer of injury prevention knowledge and the integration of evidence-based injury prevention practices into the daily lives of those at risk, those who care for them, and those with a mandate for public health and safety in British Columbia”. Acknowledgements: The BC Injury Research and Prevention Unit (BCIRPU) would like to acknowledge the contributions of Child Health BC in the development of this report, in particular, BCIRPU would like to acknowledge Jennifer Scarr, Provincial Lead, Health Promotion, Prevention and Primary Care, Child Health BC, who assisted in obtaining the National Ambulatory Care Reporting System data and provided the maps. Child Health BC is a network of BC health authorities, BC government ministries, health professionals, and provincial partners dedicated to improve the health status and health outcomes of BC’s children and youth by working collaboratively to build an integrated and accessible system of health services. One of the focus areas of Child Health BC is Injury Prevention. Authors: Fahra Rajabali, Rachel Ramsden, Marina Wada, Kate Turcotte, Shelina Babul Reproduction, in its original form, is permitted for background use for private study, education instruction and research, provided appropriate credit is given to the BC Injury Research and Prevention Unit. -
Mapping Report
Aquifer Classification Worksheet for Wark-Colquitz Aquifer (680) Aquifer number: 680 Proposed name of aquifer: Wark-Colquitz Aquifer (680). Aquifer Classification: IB (14) Aquifer Priority Ranking for Observation Wells: 68.33 Descriptive location of aquifer: The aquifer is found on south-eastern Vancouver Island, covering a land area that includes much of the municipalities of Colwood, Langford, and all of Esquimalt, Victoria, Oak Bay, Saanich, View Royal and District of Highlands. Date: June 2004. (New well information from 092B053 was included and overall statistics were updated on March 13, 2012 by Margaret Scott) NTS mapsheet: 092B/05, 092B/06, 092B/11, 092B/12. TRIM mapsheets: 092B.043, 092B.044, 092B.053, 092B.054. What geological formation does the aquifer belong to? Four bedrock types are included within this single aquifer: Colquitz gneiss, Wark gneiss, Karmutsen volcanics, and Leech River metavolcanic and metasedimentary bedrock. The majority of the aquifer is made up of Paleozoic crystalline igneous and meta-igneous rocks of the West Coast Crystalline Complex, which includes the Wark-Colquitz Complex. This metamorphic complex has been described by Massey (1994), and includes quartz diorite, tonalite, hornblende-plagioclase gneiss, quartz-feldspar gneiss, amphibolite, diorite, agmatite, gabbro, marble and metasediments. On the eastern area of the aquifer, the rock is mainly the Colquitz gneiss, a quartz-rich, layered, dark to light coloured unit that is thought to have formed from sedimentary protolith1. On the mid- to west area of the aquifer is found the Wark gneiss, a darker, more massive, hornblende-rich meta-igneous to meta-volcanic rock formed from an igneous diorite and volcanic protolith, which is interbedded with the lighter Colquitz gneiss. -
Together in Wellness
Together in Wellness Tripartite Committee on First Nations 2011/2012 Health Interim Annual Report A report on the progress of the integration and the improvement of health services for First Nations in British Columbia. Tripartite First Nations Health Plan Contents Message from Partners 1 Purpose / Context 2 STRUCTURE: NEW HEALTH GOVERNANCE 3 Tripartite Committee on First Nations Health 3 First Nations Health Council 4 First Nations Health Directors Association 4 First Nations Health Authority 4 Federal and Provincial Roles and Responsibilities 5 EVOLVING RELATIONS AND PRACTICES: BUILDING A RELEVANT AND RESPONSIVE HEALTH SYSTEM FOR FIRST NATIOns 7 Transition and Transformation 7 Health Actions 9 Together in Wellness in Every Region 13 Measuring Health Outcomes 19 MOVING FORWARD 20 TOGETHER IN WELLNESS Message from Partners One year ago, the B.C. Tripartite Framework Agreement on First Nation Health Governance was signed as part of a sacred ceremony at the Capilano Longhouse on the traditional territory of the Coast Salish People in West Vancouver. It marked a critical moment of time when each of our respective parties reaffirmed our commit- ment to work together in wellness, and to a shared vision for improved health outcomes of all First Nations in British Columbia. The Framework Agreement was grounded in the Transformative Change Accord: First Nations Health Plan (2006), the First Nations Health Plan Memorandum of Understanding (2006), the Tripartite First Nations Health Plan (2007), and the Basis for a Framework Agreement on First Nation Health Governance (2010). As we continue down this innovative path, we need to work collaboratively to maintain our focus and maximize investments in our programs, services, and innovations to promote wellness, disease prevention, enhanced primary care, and traditional health wisdom. -
Exploring 10000 Years of Human History on Ebey's Prairie, Whidbey
EXPLORING 10,000 YEARS OF HUMAN HISTORY ON EBEY’S PRAIRIE, WHIDBEY ISLAND, WASHINGTON by Andrea L. Weiser B.A., Fort Lewis College, 1992 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS In the Department of Archaeology © Andrea L. Weiser 2006 SIMON FRASER UNIVERSITY Fall 2006 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. SIMON FRASER UNIVERSITY PARTIAL COPYRIGHT LICENCE I hereby grant to Simon Fraser University the right to lend my thesis, project or extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further grant permission to Simon Fraser University to keep or make a digital copy for use in its circulating collection. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying, publication or public performance of this work for financial gain shall not be allowed without my written permission. Public performance permitted: Multimedia materials that form part of this work are hereby licenced to Simon Fraser University for educational, non-theatrical public performance use only. This licence permits single copies to be made for libraries as for print material with this same limitation of use. -
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Index (Italic page numbers indicate major references) Abalone Cove landslide, California, Badger Spring, Nevada, 92, 94 Black Dyke Formation, Nevada, 69, 179, 180, 181, 183 Badwater turtleback, California, 128, 70, 71 abatement districts, California, 180 132 Black Mountain Basalt, California, Abrigo Limestone, Arizona, 34 Bailey ash, California, 221, 223 135 Acropora, 7 Baked Mountain, Alaska, 430 Black Mountains, California, 121, Adams Argillite, Alaska, 459, 462 Baker’s Beach, California, 267, 268 122, 127, 128, 129 Adobe Range, Nevada, 91 Bald Peter, Oregon, 311 Black Point, California, 165 Adobe Valley, California, 163 Balloon thrust fault, Nevada, 71, 72 Black Prince Limestone, Arizona, 33 Airport Lake, California, 143 Banning fault, California, 191 Black Rapids Glacier, Alaska, 451, Alabama Hills, California, 152, 154 Barrett Canyon, California, 202 454, 455 Alaska Range, Alaska, 442, 444, 445, Barrier, The, British Columbia, 403, Blackhawk Canyon, California, 109, 449, 451 405 111 Aldwell Formation, Washington, 380 Basin and Range Province, 29, 43, Blackhawk landslide, California, 109 algae 48, 51, 53, 73, 75, 77, 83, 121, Blackrock Point, Oregon, 295 Oahu, 6, 7, 8, 10 163 block slide, California, 201 Owens Lake, California, 150 Basin Range fault, California, 236 Blue Lake, Oregon, 329 Searles Valley, California, 142 Beacon Rock, Oregon, 324 Blue Mountains, Oregon, 318 Tatonduk River, Alaska, 459 Bear Meadow, Washington, 336 Blue Mountain unit, Washington, 380 Algodones dunes, California, 101 Bear Mountain fault zone, California, -
Aquifers of the Capital Regional District
Aquifers of the Capital Regional District by Sylvia Kenny University of Victoria, School of Earth & Ocean Sciences Co-op British Columbia Ministry of Water, Land and Air Protection Prepared for the Capital Regional District, Victoria, B.C. December 2004 Library and Archives Canada Cataloguing in Publication Data Kenny, Sylvia. Aquifers of the Capital Regional District. Cover title. Also available on the Internet. Includes bibliographical references: p. ISBN 0-7726-52651 1. Aquifers - British Columbia - Capital. 2. Groundwater - British Columbia - Capital. I. British Columbia. Ministry of Water, Land and Air Protection. II. University of Victoria (B.C.). School of Earth and Ocean Sciences. III. Capital (B.C.) IV. Title. TD227.B7K46 2004 333.91’04’0971128 C2004-960175-X Executive summary This project focussed on the delineation and classification of developed aquifers within the Capital Regional District of British Columbia (CRD). The goal was to identify and map water-bearing unconsolidated and bedrock aquifers in the region, and to classify the mapped aquifers according to the methodology outlined in the B.C. Aquifer Classification System (Kreye and Wei, 1994). The project began in summer 2003 with the mapping and classification of aquifers in Sooke, and on the Saanich Peninsula. Aquifers in the remaining portion of the CRD including Victoria, Oak Bay, Esquimalt, View Royal, District of Highlands, the Western Communities, Metchosin and Port Renfrew were mapped and classified in summer 2004. The presence of unconsolidated deposits within the CRD is attributed to glacial activity within the region over the last 20,000 years. Glacial and glaciofluvial modification of the landscape has resulted in the presence of significant water bearing deposits, formed from the sands and gravels of Capilano Sediments, Quadra and Cowichan Head Formations. -
Data Requests a GP for Me Evaluation Contact
Data Requests A GP for Me Evaluation Contact Doctors of BC Petra Lolic: [email protected] Outline The Basics: What do we know for sure? Key Metrics: Advice for obtaining key metrics Guidance: Tips from the Ministry and Health Authorities Resources: Who should we talk to? The Basics What do we know for sure? EASIER TO ACQUIRE INFORMATION Aggregate information that uses pre-defined parameters or measures for example: • Standard geographic health boundaries (LHA, HSDA, HA); • Standard age groupings with or without gender; • Patient cohorts (pre-defined) • Physician cohorts (pre-defined) EASIER TO ACQUIRE INFORMATION Ministry of Health Sourced Information on DivIT Year(s) Region Community Profiles 2010 or 2011 43 communities (using LHA), 5 HAs, and BC Attachment Algorithm 2007/2008 to 2011/2012 LHA, HSDA, HA, BC 2008/2009 to 2012/2013 LHA, HSDA, HA, BC 2009/2010 to 2013/2014 LHA, HSDA, HA, BC Attachment Algorithm 2011/2012 LHA, HSDA, HA, BC by Gender and Age 2012/2013 LHA, HSDA, HA, BC Attachment Algorithm 2010/2011 and 2011/2012 LHA, HSDA, HA, BC by RUB 2011/2012 and 2012/2013 LHA, HSDA, HA, BC CCHS, and Estimates of 2009&2010 HSDA, HA, BC Looking for using CCHS data MSOC 50GPs 2009/2010 to 2011/2012 LHA, HA, BC 2009/2010 to 2012/2013 LHA, HA, BC 2008/2009 to 2013/2014 LHA, HA A GP for Me Incentive 2013 and 2014 Division Fee Items 2013, 2014 and 2015 (Jan. 1-Mar. 31) Division 2013, 2014 and 2015 (Jan. 1-Jun. 30) Division EASIER TO ACQUIRE INFORMATION Ministry of Health Attachment Algorithm • Using MSP billing data, the Algorithm is a measure to estimate an ongoing health care relationship with a family physician practice based on their GP service utilization. -
Bedrock Geology of the North Saanich-Cobble Hill Area, British Columbia, Canada
AN ABSTRACT OF THE THESIS OF John Michael Kachelmeyer for the degree ofMaster of Science in Geology presented on May 30, 1978 Title: BEDROCK GEOLOGY OF THE NORTHSAANICH-COBBLE HILL AREAS, BRITISH COLUMBIA, CANADA Abstract approved: Redacted for Privacy Keith F./Oles The bedrock of the North Saanich-Cobble Hill areas consists of igneous and sedimentary rocks of Early Jurassic through Late Cretaceous age.Early Jurassic andesitic Bonanza Volcanics are intruded by Middle Jurassic Saanich Granodiorite plutonic rocksand dikes.Late Cretaceous Nanaimo Group clastic rocksnonconformably overlie these Jurassic units.The four oldest formations of the group (Comox, Has lam, Extension-Protection, and Cedar District) are exposed within the study area. The Nanaimo Group formations were deposited within a subsid- ing marine basin (the Nanaimo Basin) located to the east ofsouthern Vancouver Island.Uplift of pre-Late Cretaceous basement rocks on Vancouver Island to the west and on mainland British Columbia tothe east of the basin created rugged, high-relief source areasthat were chemically weathered in a warm tropical climate and mechanically eroded by high-energy braided stream systems. The Comox and Has lam sediments were deposited in response to a continual transgression of a Late Cretaceous seaway overthis rugged terrain.Braided stream systems trending north-northwest into the basin deposited Comox (Benson Member) gravelsand sands onto a high-energy, cliffed shoreline.Erosion of the highlands and transgression of the marine seaway resulted in subduedtopographic relief and the deposition of sediments by low-energymeandering streams within a river traversed coastal plain, followedby silt and clay deposition in tidal flat and lagoonal environments,and finally by sand deposition in a higher energy barrier bar environment.Contin- ued marine transgression resulted in the depositionof massive marine mudstones and cyclic sandstone to mudstone sequencesof the Has lam Formation. -
Oceanside Physician WELCOME PACKAGE
:::: Oceanside Physician WELCOME PACKAGE :: LIVE :: WORK :: PLAY :: Orientation Information for New Physicians to the Oceanside Area LIVE Acknowledgement: :::::: The orientation package concept, design and layout was developed by the Comox Valley Division of Family Practice. WELCOME TO OCEANSIDE! www.divisionsbc.ca/oceanside The following is information you may find useful as a new Family Physician (FP) in the Oceanside area. This information in this guide BENEFITS OF MEMBERSHIP is divided into three sections: Live, Work, Play. Information in this handout was compliled with the help of local GPs, for GPs. Being a member of a division offers a number of potential bene- fits, including: A little bit about the Oceanside area... • Greater impact on the organization of local and regional Parksville-Qualicum Beach is thoroughly equipped with modern emer- health services around a division practice area gency service infrastructures. The RCMP, the BC Ambulance Service • Enhanced professional collegiality and access to physician and local fire departments are on call 24 hours. The area has a full com- health and wellness programs plement of physicians, chiropractic, physiotherapy, acupuncture, x-ray • Shared efforts for recruitment, retention and locums. ultrasound clinic, and holistic naturopathic specialists. Urgent care • Support from colleagues in caring for complex or unat- is provided by Island Health at the new Oceanside Health Centre in tached patients Parksville. The Nanaimo Regional General Hospital is a half-hour south • Practice support for information of Parksville.In the community, as of 2019, there are 29 office-based technology programs and pilot projects. physicians and 4 Nurse Practitioners in 9 family practice clinics in the • Free Up-To-Date subscription Oceanside area. -
Visit and Study in Saanich Peninsula, British Columbia
SAANICH Peninsula BRITISH COLUMBIA > VANCOUVER ISLAND • www.sidney.ca / www.centralsaanich.ca • Located at the southern tip of Vancouver Island • 20-30 km North of Victoria • Population: Sidney: 11,600, Central Saanich region: 15,950 Small Town/Suburb Notable features: • Many residents work in nearby Victoria, establishing the Saanich GATEWAY TO Peninsula as a “bedroom community” of the capital • Minutes from Victoria International Airport (located near Sidney) VICTORIA • Less than 30 minute drive to Victoria • Close proximity to Swartz Bay Ferry Terminal (to mainland Vancouver) The Saanich Peninsula is known as one of the most • Long shoreline with many sandy beaches desirable areas in Canada to live or visit, as it offers a • Year-round tourist destination high quality lifestyle and mild climate. It is home to the • One of the most mild climates in Canada District of Central Saanich, the District of North Saanich, • Ideal placement for students who would enjoy hiking or mountain and the Town of Sidney, as well as Victoria International biking on local trails, or sea kayaking/sailing in the local waters Airport. As a bedroom community serving the Greater Victoria Area, Saanich enjoys both Main Attractions: urban amenities as well as rural and • Buchart Gardens: www.butchartgardens.com agricultural traditions, including • Butterfly Gardens: www.butterflygardens.com may still existing vinyards. With • Brentwood Bay Festival (June): www.brentwoodbay.info/Festival.html numerous recreational facilities • Diving: http://www.hellobc.com/sidney/things-to-do/water-activities/diving.aspx and golf courses, parks and trails, • Island View Beach: www.crd.bc.ca/parks/islandview family-oriented programs and • Shaw Ocean Discovery Centre: www.oceandiscovery.ca services most residents agree that • Sidney Street Market the Saanich Peninsula is a wonderful • Whale watching and kayaking: www.sidneywhalewatching.com place to live, to work and to play. -
WSANEC Emerging Land Or Emerging People Jack Horne
The Arbutus Review Vol. 3, No. 2 (2012) Horne WSANEC Emerging Land or Emerging People Jack Horne Abstract: The WSANEC Nation has been located on what is now known as the Saanich Peninsula on southern Vancouver Island since time immemorial. Remarkably little has been written about this Nation, which was divided by the Oregon Treaty in 1846 into Canadian/American sides of the border. In Canada the WSANEC Nation was then further divided into 4 separate reserves. This article examines the WSANEC Nation’s relationship with its traditional territories, the effects of colonization on this relationship, and ongoing resistance to continued colonization from both internal and external forces. WSANEC history is examined through the documentation in the Nation’s oral traditions, using the Douglas Treaties, the landmark Saanich Bay Marina Case, and James Island development as examples. Key Terms: WSANEC; Douglas Treaty; Coast Salish Introduction The WSANEC Nation is located on what is now known as the Saanich Peninsula on the southern part of Vancouver Island. WSANEC territories once encompassed the entire Saanich Peninsula, many of the surrounding Islands, and extended south onto the mainland of Washington State. With the signing of the Oregon treaty in 1846, WSANEC territories and people were divided into Canadian or American sides (Sage, 1946). As a result, family ties were disrupted and families on each side of the border were left to face different government policies. The WSANEC Nation in Canada is currently divided into four separate reserves located in the areas known today as: Tsawout, Tsartlip, Puaquachin, and Tseycum. While a great deal of scholarship has been written about the Indigenous peoples of British Columbia there has been remarkably little written about the WSANEC Nation.