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Electoral Area Directors Committee Agenda October 9, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood Street, Pemberton, BC
Electoral Area Directors Committee Agenda October 9, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood 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 Committee Closed Meeting THAT the Committee close the meeting to the public under the authority of Section 90(1)() of the Community Charter. 4. Rise & Report from the Closed Electoral Area Directors Committee 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 Approval and Receipt of Minutes 5.1.1. Electoral Area Directors Committee Meeting Draft 5 - 11 Minutes of September 5, 2019 THAT the Electoral Area Directors Committee Meeting Minutes of September 5, 2019 be approved as circulated. 5.2 Staff Reports & Other Business 5.2.1. September 2019 Select Funds Report 12 - 16 THAT the following resolution of the September 5, 2019 Electoral Area Directors Committee meeting with respect Item Item of Business and Page Number Page -
Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996
Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996 CONSOLIDATED COPY May 2016 IMPORTANT NOTICE THIS IS AN UNOFFICIAL CONSOLIDATION OF BYLAW NO. 608 WHICH HAS BEEN PREPARED FOR CONVENIENCE ONLY. Although the Squamish-Lillooet Regional District is careful to assure the accuracy of all information presented in this consolidation, you should confirm all information before making any decisions based on it. Information can be confirmed through the SLRD Planning Department. Bylaw 608 ( Consolidated for Convenience Only) May 2016 SUMMARY OF AMENDMENTS CONSOLIDATED FOR CONVENIENCE ONLY Consolidated bylaws are consolidated for convenience only and are merely representative. Each consolidated bylaw consists of the original bylaw text and maps, together with current amendments which have been made to the original version. Copies of all bylaws (original and amendments) may be obtained from the SLRD Planning and Development Department. BY-LAW NO. DATE OF ADOPTION 1022 – 2006 Major Review of Upper Bridge River Valley OCP January 28, 2008 Rezoning a parcel of unsurveyed Crown land from Resource 1094 – 2008 October 26, 2009 Management to Industrial Tyax Real Estate Ltd. text and map amendments plus 1305 - 2014 housekeeping amendment July 28, 2014 PID 024-877-638 (Lot 5, DL 4931, Plan KAP67637, LLD) Creating a Medical Marihuana Production Facility 1309 - 2014 February 25, 2015 Development Permit Area 1440 - 2016 OCP amendments to the Tyax Staff Housing May 25, 2016 Official Community Plan Bylaw No. 608 Page 2 Bylaw 608 ( Consolidated for Convenience Only) May 2016 SQUAMISH LILLOOET REGIONAL DISTRICT BYLAW NO. 1022, 2006 A bylaw of the Squamish Lillooet Regional District to amend the Upper Bridge River Valley Official Community Plan Bylaw No. -
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. -
Preliminary Calibration of a Numerical Runout Model for Debris Flows in Southwestern British Columbia
7th International Conference on Debris-Flow Hazards Mitigation Preliminary calibration of a numerical runout model for debris flows in Southwestern British Columbia Sophia Zubryckya,*, Andrew Mitchella, Jordan Aaronb, Scott McDougalla a Department of Earth, Ocean and Atmospheric Sciences – University of British Columbia, Vancouver, British Columbia, Canada bDepartment of Engineering Geology – ETH Zürich, Zürich, Switzerland Abstract Debris-flow hazard and risk assessments require reliable estimates of inundation area, velocity and flow depth to evaluate spatial impact and impact intensity. Semi-empirical numerical runout models that simulate bulk flow behavior with simple rheological models are useful in forecasting these parameters, however, they require calibration by back-analyzing past events. This paper presents the back-analysis of six debris flows in southwestern British Columbia using a novel automated calibration approach that systematically optimizes the Dan3D runout model to fit field observations. The calibration method yielded good simulations of runout length, but under-predicted flow depths in some cases, and over-predicted velocities in all cases. The best-fit Voellmy rheology parameters for the studied cases ranged from 46 to 531 m/s2 for the turbulence coefficient and 0.08 to 0.18 for the friction coefficient. There is a potential inverse correlation between friction coefficient and event volume. Calibrated parameters were compared to morphometric parameters for the study sites, which may be useful for guiding parameter selection once a larger dataset is calibrated. Ongoing work is focused on refining the calibration technique, including standardization of input parameters more relevant to debris flows. The long-term goal is to apply the technique to a larger dataset of debris-flow cases and provide practitioners with better guidance on the selection of model input parameters for forecasting purposes. -
Brief on Mining and “Backcasting from Principles of Sustainability”
Creating Resilience in the SLRD The Report of the SLRD Energy Resilience Task Force FINAL REPORT February, 2011 © 2011, Squamish-Lillooet Regional District. All Rights Reserved. The preparation of this sustainable community plan was carried out with assistance from the Green Municipal Fund, a Fund financed by the Government of Canada and administered by the Federation of Canadian Municipalities. Notwithstanding this support, the views expressed are the personal views of the authors, and the Federation of Canadian Municipalities and the Government of Canada accept no responsibility for them. FINAL REPORT February, 2011 A partial list of things made from Oil… Solvents Diesel fuel Motor Oil Bearing Grease Ink Floor Wax Ballpoint Pens Football Cleats Upholstery Sweaters Boats Insecticides Bicycle Tires Sports Car Bodies Nail Polish Fishing lures Dresses Tires Golf Bags Perfumes Cassettes Dishwasher parts Tool Boxes Shoe Polish Motorcycle Helmets Caulking Petroleum Jelly Transparent Tape CD Player Faucet Washers Antiseptics Clothesline Curtains Food Preservatives Basketballs Soap Vitamin Capsules Antihistamines Purses Shoes Dashboards Cortisone Deodorant Footballs Putty Dyes Panty Hose Refrigerant Diapers Life Jackets Rubbing Alcohol Linings Skis TV Cabinets Shag Rugs Electrician's Tape Tool Racks Car Battery Cases Epoxy Paint Mops Slacks Insect Repellent Oil Filters Umbrellas Yarn Fertilizers Hair Colouring Roofing Toilet Seats Fishing Rods Lipstick Denture Adhesive Linoleum Ice Cube Trays Synthetic Rubber Speakers Plastic Wood Electric Blankets -
Gold Bridge Properties
Gold Bridge Properties ASSESSMENT REPORT ON THE GEOCHEMICAL, AND PROSPECTING THE GOLD BRIDGE MINERAL CLAIMS Tenures 696374, 704730, 704734, 704752, 708922 Lillooet Mining Division Property Location Southern British Columbia BCGS 82L.008 Longitude and Latitude 50°8773 N 122°756 W By David A. Wallach For DW Exploration Ltd July 18, 2012 Page 1 of 28 Table of Content 1.0 Introduction........................................................... 3 2.0 Summery............................................................... 3 3.0 List of Mineral Tenures and Status........................ 4 4.0 Access and Location............................................. 5 5.0 Regional Geology.................................................. 5 6.0 Physiography, Vegetation and Climate.................. 5 7.0 Location Map.......................................................... 6 8.0 Claim Map.............................................................. 7 9.0 Rock Sample locations Map.................................. 8 10.0 Sample Analysis Map............................................ 9 11.0 Certificates of Analysis.......................................... 10 12.0 Conclusion.............................................................. 25 13.0 Statement of Costs................................................. 25 14.0 References............................................................. 26 15.0 Qualifications.......................................................... 27 Page 2 of 28 1:0 INTRODUCTION This report has been prepared David A Wallach of DW Exploration -
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. -
Aesthetic Impact Informational Services, LLC Remote Viewing
Aesthetic Impact Informational Services, LLC Remote Viewing Educational Example Remote Viewing Target 130703 Long Freight Train – Canadian Pacific Railway, Seton Lake, British Columbia Coordinates: 130703 Blind Tasking: The target is a location. Describe the location. Online Discussion: https://www.youtube.com/watch?v=pHplxCMHmJc CRV Session Sketches, Summary & Topology Information contributed by Ronald Kuhn, Ohio, USA ----------- Seton Lake is a freshwater fjord draining east via the Seton River into the Fraser River at the town of Lillooet, British Columbia, about 22 km long and 243 m in elevation and 26.2 square kilometres in area.[1] Its depth is 1500 feet. The lake is natural in origin but was raised slightly as part of the Bridge River Power Project, the two main powerhouses of which are on the north shore of the upper end of the lake near Shalalth. At the uppermost end of the lake is the community of Seton Portage and the 1 mouth of the short Seton Portage River, which connects Anderson Lake on the farther side of the Portage to Seton Lake. Retrieved Mar. 1, 2015. http://en.wikipedia.org/wiki/Seton_Lake Image courtesy of Larry Bourne Sketch courtesy of Ronald Kuhn, CRV Intermediate Level Student The Bridge River hydroelectric complex consists of three dams and stores water for four generating stations. The system uses Bridge River water three times in succession to generate 492 megawatts, or 6 to 8 per cent of British Columbia's electrical supply. Hydroelectric development of the system began in 1927 and was completed in 1960. Its waters (Downton Reservoir) initially pass through the Lajoie Dam and powerhouse and are then diverted through tunnels and penstocks from Carpenter Reservoir to the two powerhouses on Seton Lake Reservoir. -
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 .............................................................. -
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. -
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. -
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).