Squamish River Watershed Status Report
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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 -
Washington Division of Geology and Earth Resources Open File Report
l 122 EARTHQUAKES AND SEISMOLOGY - LEGAL ASPECTS OPEN FILE REPORT 92-2 EARTHQUAKES AND Ludwin, R. S.; Malone, S. D.; Crosson, R. EARTHQUAKES AND SEISMOLOGY - LEGAL S.; Qamar, A. I., 1991, Washington SEISMOLOGY - 1946 EVENT ASPECTS eanhquak:es, 1985. Clague, J. J., 1989, Research on eanh- Ludwin, R. S.; Qamar, A. I., 1991, Reeval Perkins, J. B.; Moy, Kenneth, 1989, Llabil quak:e-induced ground failures in south uation of the 19th century Washington ity of local government for earthquake western British Columbia [abstract). and Oregon eanhquake catalog using hazards and losses-A guide to the law Evans, S. G., 1989, The 1946 Mount Colo original accounts-The moderate sized and its impacts in the States of Califor nel Foster rock avalanches and auoci earthquake of May l, 1882 [abstract). nia, Alaska, Utah, and Washington; ated displacement wave, Vancouver Is Final repon. Maley, Richard, 1986, Strong motion accel land, British Columbia. erograph stations in Oregon and Wash Hasegawa, H. S.; Rogers, G. C., 1978, EARTHQUAKES AND ington (April 1986). Appendix C Quantification of the magnitude 7.3, SEISMOLOGY - NETWORKS Malone, S. D., 1991, The HAWK seismic British Columbia earthquake of June 23, AND CATALOGS data acquisition and analysis system 1946. [abstract). Berg, J. W., Jr.; Baker, C. D., 1963, Oregon Hodgson, E. A., 1946, British Columbia eanhquak:es, 1841 through 1958 [ab Milne, W. G., 1953, Seismological investi earthquake, June 23, 1946. gations in British Columbia (abstract). stract). Hodgson, J. H.; Milne, W. G., 1951, Direc Chan, W.W., 1988, Network and array anal Munro, P. S.; Halliday, R. J.; Shannon, W. -
Squamish Estuary
OCEAN WATCH | Howe Sound Edition SPECIES AND HABITATS Squamish Estuary AUTHOR Edith B. Tobe, Registered Professional What is happening in Biologist, Squamish River Watershed Society REVIEWER the Squamish Estuary? Gary Williams, M.Sc., R.P.Bio, Professional Wetland Scientist, GL Williams and Associates Ltd. The Squamish Estuary is situated at the head of Howe Sound, one of the southernmost fjords in British Columbia, where the Squamish River drains over 3,650 square kilometers of coastal rainforest into the ocean. An estuary is formed when fresh water mixes with marine waters to create a brackish tidally influenced zone. Estuaries are one of the most productive ecosystems on the planet, providing habitat for fisheries, waterfowl, and wildlife. There have been many anthropomorphic impacts to the Squamish Estuary since it was settled first by First Nations and later by Europeans and other cultures. The impacts have included urbanization, diking and logging and resulted in loss of habitat, changes to hydrology, and introduction of con- tamination. Figure 1. The brownfield site, a former log sort in the central Estuary, is the location of current restoration efforts. (Photo: Colin Bates, June 2015) Squamish Estuary | Page 123 OCEAN WATCH | Howe Sound Edition SPECIES AND HABITATS Organizations such as the Squamish River Water- lish tidal channels, mud flats and sedge marshes on shed Society (SRWS) have been working for close to the site. In 2015, efforts included removal of a large 20 years on re-establishing the estuary to its origin- amount of wood waste, grading the site, and trans- al function by reconnecting tidal channels, installing planting Lyngbye’s sedge (Carex lyngbyei), the dom- culverts, planting aquatic and terrestrial vegetation, inant grassy plant in the estuary and in many Pacific and creating wildlife habitat for aquatic and terrestrial coastal marshes. -
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. -
Teaching Activities
S QUAMISH RIVERS & ESTUARY Squamish Streams Around the Corner Grades: 4-7 Subject, Science, Language Arts Time required:30 –60 minutes Key Concepts: Everyday actions make a difference in watershed and estuary health.. Objectives: To identify local streams and protected areas Background: To use research, mapping and Materials interviewing skills; In British Columbia, there are many different use a variety of ways to types of protected areas. They include public Maps collect and record data; lands in networks of national, provincial and regional parks, wildlife management areas, (community & school) recreation areas, wilderness areas, ecological reserves, nature sanctuaries, greenways and Student Journals municipal parks, cultural heritage sites, heri- Pencil or pen Key Words: tage buildings and more. They also include water areas that are protected but not owned by the Streams, protected areas public but are protected by a range of fed- eral, provincial or local regulations. These types of protected areas include local areas such as water-courses (rivers, streams, lakes, Skills: ponds, wetlands) and their riparian Analysis, discussion, listing, writing/ (streamside) areas, environmentally sensitive drawing areas, and other areas of noted local impor- tance. 1 Squamish Streams Around the Corner Protected areas range in size from vast expanses of wilderness areas to tiny pockets memorabilia. of nature covering a few hectares or less. 4. Ask each group to brainstorm a list of Together, protected areas on public and places and people in their community private lands provide ways to protect natural that might be able to help them answer ecosystems such as streams as well as to the following questions about their enhance and restore local natural areas. -
Where the Rivers Meet The
Natural Hazards in Squamish 1 District of Squamish Where the Rivers Meet the Sea Lessons from the Past HIGHWAY 99 Official Community Plan Adopted 2010 SQUAMISH RIVER The District of Squamish is located at the head of Howe Several conclusions can be drawn from the flood history in VER Schedule D1 YE RI CHEEKE Sound where 5 rivers converge. These mountain rivers, Squamish: FLOOD AND DEBRIS FLOW fed by glaciers, snowmelt and precipitation, descend HAZARD AREAS from their steep mountain tops carrying water, sediment, 1. All the rivers in Squamish pose a risk of flooding. All have Levette Legend Lake and on occasion, rocks and other debris. When these fast Evans Cr B Debris Flow Hazard Area r Brohm Lake o h caused multiple and damaging floods in the past. m Riv Flood Hazard Area !!! e r Dykes flowing rivers reach the gently sloping valley, they tend to Parks and Ecological Reserves Paradise Valley Rd 2. Damaging floods have also occurred as a result of coastal Indian Reserves Boundaries slow down and spread out, and leave sediment behind. Evans hazard zones Lake The terms alluvial fan and floodplain are used to describe inundation. Source: Cheekye River Terrain Hazard and Land Use Study, March 1993 HAZARD ZONES 1. Alluvial fan hazard zone - level 1 (high) the riparian areas along these lower river reaches. 4 2. Alluvial fan hazard zone - level 2 (intermediate) 3. The flood risk in Squamish has strong seasonal variations. Most C 6 H 3 Cat E 3 3. Alluvial fan hazard zone - level 3 (moderate) ER E Lake s Cr IV K Evan R E 5 Y 4. -
Flow Hydraulics, Bedforms and Macroturbulence of Squamish River Estuary, British Columbia
FLOW HYDRAULICS, BEDFORMS AND MACROTURBULENCE OF SQUAMISH RIVER ESTUARY, BRITISH COLUMBIA C. Scott Babakaiff B.Sc. University of British Columbia 1991 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in the Department of Geography OC. Scott Babakaiff Simon Fraser University December 1993 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: Scott Curtis Babakaiff Degree: Master of Science Title of Thesis: Row Hydraulics, Bedforms And Macroturbulence Of Squamish River Estuary, British Columbia Examining Committee: Chair: A.C.B. Roberts, Associate Professor L. Lesack Assistant Professor Mr. K.' Re,HydroloBst Northwest Hydraulics Dr. M.A. Church, Professor Department of Geography University of British Columbia External Examiner Date Approved: December 6.1993 i i PARTIAL COPYRIGHT LICENSE 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 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 or publication of this work for financial gain shall not be allowed without my written permission. Title of Thesis/Project/Extended Essay Flow Hydraulics, Bedforms And Macroturbulence Of Sauamish River Estuary. -
Squamish/ Mamquam River Survey
DISTRICT OF SQUAMISH REPORT TO: Council FOR: Regular Meeting of Council PRESENTED: September 18, 2007 FILE: COMDEV SUBJECT: Award of Squamish and Mamquam River Studies Recommendation: THAT Council award the Research and Survey components of the Squamish & Mamquam River Studies to Kerr Wood Leidal and Associates at a price not to exceed $64,872 plus GST; AND FURTHER THAT Council implore the Province to recognize the urgent need for the remainder of the work to be completed, the historical role of the Province in performing this work and request funding for the remainder of the study from Province. CAO Recommendation: THAT the report from Community Development be approved. K. Anema, CAO 1. Purpose: This report is intended to authorize the award the Squamish and Mamquam River Studies. 2. Time Critical: Flood hazard protection is one of Council’s highest priorities. This assignment is intended to undertake the river surveys that are needed to assess the current level of protection afforded by the existing dykes and then determine what, if any, measures are needed to achieve the 200 year standard of protection. 3. Background: The flood of record for the Squamish River occurred in October of 2003. The subsequent analysis of that flood suggested that the existing dykes on the Squamish and Mamquam Rivers may not be providing protection from the provincially accepted, 200 year design storm. Of further concern is aggradation or sediment build-up of the river bed. This may have the effect of further reducing the level of protection afforded by the dykes. In order to determine the current level of protection and thereby establish what, if any, upgrading is necessary a survey of the floodplain must first be undertaken. -
Electoral Area Directors Committee Agenda June 14, 2017; 10:30 AM SLRD Boardroom 1350 Aster Street, Pemberton, BC
UPDATED Electoral Area Directors Committee Agenda June 14, 2017; 10:30 AM SLRD Boardroom 1350 Aster 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 Electoral Area Directors Committee Closed 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 6 - 16 Minutes of May 10, 2017 THAT the Electoral Area Directors Committee Meeting Minutes of May 10, 2017 be approved as circulated. 5.2 Staff Reports & Other Business 5.2.1. May 2017 Select Funds Report 17 - 21 5.2.2. May 2017 Monthly Building Report 22 - 28 5.3 Correspondence for Information Item Item of Business and Page Number Page 5.3.1. Letter from Lillooet Naturalist Society - Thank You 29 - 33 6. -
An Archaeological Examination of House Architecture and Territoriality in the Salish Sea Region Over Five Millennia
Territory, Tenure, and Territoriality Among the Ancestral Coast Salish of SW British Columbia and NW Washington State by Chris Springer M.A., Simon Fraser University, 2009 B.A., Simon Fraser University, 2006 Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in the Department of Archaeology Faculty of Environment © Chris Springer 2018 SIMON FRASER UNIVERSITY Fall 2018 Copyright in this work rests with the author. Please ensure that any reproduction or re-use is done in accordance with the relevant national copyright legislation. Approval Name: Chris Springer Degree: Doctor of Philosophy (Archaeology) Territory, Tenure, and Territoriality Among the Title: Ancestral Coast Salish of SW British Columbia and NW Washington State Examining Committee: Chair: Jon Driver Professor Dana Lepofsky Senior Supervisor Professor Michael Blake Supervisor Professor Department of Anthropology University of British Columbia Ross Jamieson Supervisor Associate Professor Christina Giovas Internal Examiner Assistant Professor Elizabeth A. Sobel External Examiner Professor Department of Sociology and Anthropology Missouri State University Date Defended/Approved: September 26, 2018 ii Abstract Archaeological studies of territory, tenure, and territoriality seek to understand how past claims and access to land and resources were expressed across landscapes and through time. The foci of such studies include the spatial and temporal patterning of settlements, dwellings, conspicuous burials, monumental constructions, rock art, defensive features, and resources. In line with this research, this dissertation integrates ethnohistoric and archaeological data in three case studies that investigate the roles of house forms, the distribution of local and nonlocal obsidian, and the positioning of defensive networks in communicating territorial and tenurial interests among the ancestral Coast Salish of southwestern British Columbia and northwestern Washington state. -
Geology and Geothermal Potential of the AWA Claim Group, Squamish
Geology and Geothermal Potential- of the AWA Claim$koup, JAN t-l 5 2004 I Squamish, British Columbia Gold COmIniSSioner’S Office I VANCOUVER,B.C. I Prepared for Lisa Rummel & AWA Spa Glenn J. Woodsworth, P. Geo. April 2003 3 SUMMARY A geologicalstudy was done on the AWA group of 6 mineral claims with a view to assessingthe geothermalpotential. The claims are almost entirely underlain by granitic rocks of the latest JurassicCloudburst pluton and, south of the Stawamus River, by the mid-CretaceousSquamish pluton. Fracture and joint analysisshows a , weak north-northeast trend, but fractures tend to be widely spaced.No signsof faulting or of igneousactivity related to Garibaldi volcanism were seenon the .zproperty. Faults, if they exist, are likely to be narrow, making them difficult drilling targets. The low regional heat flow-. and the lack of a “plumbing system”in the granitic, rocks on the property indicate that the geothermalpotential is very low. No further work is warranted. INTRODUCTION The AWA claim group consistsof 6 mineral claims,AWA #l to 6, stakedOctober 8, 2002,and owned by Lisa Rummel. The claims are situated in and just eastof the District of Squamishmunicipality, northeast of the subdivision of Valleycliffe (Figure 1). On the southwest,the claim group abuts StawamusChief Provincial Park and private property of the Valleycliffesubdivision and Squamishwaterworks. I was contracted by the owner to make a geologicalappraisal of the geothermal potential of the claim group and to make suggestionsfor further work. Field work was done in two long days;this work was supplementedwith an air photo study and review of the recent geologicalliterature on the region. -
Investigating Cottid Recolonization in the Cheakamus River, Bc: Implications for Management
INVESTIGATING COTTID RECOLONIZATION IN THE CHEAKAMUS RIVER, BC: IMPLICATIONS FOR MANAGEMENT By CAROLINE KOHAR ARMOUR B.Sc., University of Ottawa, 2001 A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in ENVIRONMENT AND MANAGEMENT We accept this thesis as conforming to the required standard .......................................................... Dr. Lenore Newman, MEM Program Head School of Environment and Sustainability .......................................................... Dr. Tom A. Watson, R.P. Bio., P. Biol., Senior Environmental Scientist Triton Environmental Consultants Ltd. .......................................................... Dr. Tony Boydell, Director School of Environment and Sustainability ROYAL ROADS UNIVERSITY February 2010 © Caroline Kohar Armour, 2010 Investigating Cottid Recolonization ii ABSTRACT An estimated 90% of resident sculpin (Cottus asper and C. aleuticus) were impacted by a spill of 45,000 litres of sodium hydroxide, which occurred on the Cheakamus River, British Columbia on August 5, 2005. This study examined sculpin biology, life history, how sculpins are recovering from the impact, and whether they are re-entering the Cheakamus River from the adjacent Squamish and Mamquam Rivers. Sculpins were sampled in the three river systems via minnow trapping and electrofishing. Morphometric data were recorded and fin clips were taken as deoxyribonucleic acid vouchers to validate field species identification and to determine population distinctiveness among the three systems. Populations were not distinct, suggesting recolonization from other rivers is occurring. The data show sculpins will undergo seasonal downstream spawning migrations and also suggest sculpins are opportunistic habitat colonizers. This research bears useful implications for the adaptive management, recovery, and sustainability of sculpins in the Cheakamus River. Investigating Cottid Recolonization iii ACKNOWLEDGEMENTS First and foremost, I would like to thank my thesis advisor Dr.