Lower Nooksack River Geomorphic Assessment APPENDIX a Geologic
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The Nooksack River: Floodplains That Work Phase 1
The Nooksack River: Floodplains That Work Phase 1 PROJECT BENEFITS Protect critical infrastructure: 2 water treatment plants 2 wastewater treatment plants 1 elementary school Reduce risk of loss of life & property: Building a resilient floodplain Mitigate debris flows Restore alluvial fan functions A community-driven approach to floodplain management Protect rural communities The Nooksack River: Floodplains That Work project uses an integrated approach to Protect valuable agricultural reduce flood hazards, improve habitat, and increase the resiliency of our rural lands communities and agriculture. The Whatcom County Flood Control Zone District is leading this effort, bringing diverse interests together to find solutions that work for Improve critical habitat: the community and achieve project goals. This project builds on improved relationships and trust built among multiple interests through the Lower Nooksack Restore riparian vegetation River Comprehensive Flood Hazard Management Plan update process. Improve fish passage Project Components: Support salmon &Puget Ferndale Levee Improvement – Preliminary Design: reduce flood hazards Sound recovery for the City of Ferndale water and wastewater treatment plants and the Public Utility District No. 1 of Whatcom County water treatment facility; re-establish PROJECT PARTNERS riparian vegetation; improve recreational opportunities City of Ferndale Lynden Levee Improvement – Final Design and Construction: reduce flood hazards for the City of Lynden wastewater treatment plant, 500 -
Fraser Valley Geotour: Bedrock, Glacial Deposits, Recent Sediments, Geological Hazards and Applied Geology: Sumas Mountain and Abbotsford Area
Fraser Valley Geotour: Bedrock, Glacial Deposits, Recent Sediments, Geological Hazards and Applied Geology: Sumas Mountain and Abbotsford Area A collaboration in support of teachers in and around Abbotsford, B.C. in celebration of National Science and Technology Week October 25, 2013 MineralsEd and Natural Resources Canada, Geological Survey of Canada Led by David Huntley, PhD, GSC and David Thompson, P Geo 1 2 Fraser Valley Geotour Introduction Welcome to the Fraser Valley Geotour! Learning about our Earth, geological processes and features, and the relevance of it all to our lives is really best addressed outside of a classroom. Our entire province is the laboratory for geological studies. The landscape and rocks in the Fraser Valley record many natural Earth processes and reveal a large part of the geologic history of this part of BC – a unique part of the Canadian Cordillera. This professional development field trip for teachers looks at a selection of the bedrock and overlying surficial sediments in the Abbotsford area that evidence these geologic processes over time. The stops highlight key features that are part of the geological story - demonstrating surface processes, recording rock – forming processes, revealing the tectonic history, and evidence of glaciation. The important interplay of these phenomena and later human activity is highlighted along the way. It is designed to build your understanding of Earth Science and its relevance to our lives to support your teaching related topics in your classroom. Acknowledgments We would like to thank our partners, the individuals who led the tour to share their expertise, build interest in the natural history of the area, and inspire your teaching. -
Salmon and Steelhead Limiting Factors in WRIA 1, the Nooksack Basin, 2002
SALMON AND STEELHEAD HABITAT LIMITING FACTORS IN WRIA 1, THE NOOKSACK BASIN July, 2002 Carol J. Smith, Ph.D. Washington State Conservation Commission 300 Desmond Drive Lacey, Washington 98503 Acknowledgements This report was developed by the WRIA 1 Technical Advisory Group for Habitat Limiting Factors. This project would not have been possible without their vast expertise and willingness to contribute. The following participants in this project are gratefully thanked and include: Bruce Barbour, DOE Alan Chapman, Lummi Indian Nation Treva Coe, Nooksack Indian Tribe Wendy Cole, Whatcom Conservation District Ned Currence, Nooksack Indian Tribe Gregg Dunphy, Lummi Indian Nation Clare Fogelsong, City of Bellingham John Gillies, U.S.D.A. Darrell Gray, NSEA Brady Green, U.S. Forest Service Dale Griggs, Nooksack Indian Tribe Milton Holter, Lummi Indian Nation Doug Huddle, WDFW Tim Hyatt, Nooksack Indian Tribe Mike MacKay, Lummi Indian Nation Mike Maudlin, Lummi Indian Nation Shannon Moore, NSEA Roger Nichols, U.S. Forest Service Andrew Phay, Whatcom Conservation District Dr. Carol Smith, WA Conservation Commission Steve Seymour, WDFW John Thompson, Whatcom County Tyson Waldo, NWIFC SSHIAP Bob Warinner, WDFW Barry Wenger, DOE Brian Williams, WDFW Stan Zyskowski, National Park Service A special thanks to Ron McFarlane (NWIFC) for digitizing and producing maps, to Andrew Phay (Whatcom Conservation District) for supplying numerous figures, to Llyn Doremus (Nooksack Indian Tribe) for the review, and to Victor Johnson (Lummi Indian Nation) for supplying the slope instability figure. I also extend appreciation to Devin Smith (NWIFC) and Kurt Fresh (WDFW) for compiling and developing the habitat rating standards, and to Ed Manary for writing the “Habitat Limiting Factors Background”. -
Flood Control and Sediment Transport Study of The
FLOOD CONTROL AND SEDIMENT TRANSPORT STUDY OF THE VEDDER RIVER by DAVID GEORGE McLEAN .A.Sc., University of British Columbia, 1975 \ THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF APPLIED SCIENCE in THE FACULTY OF GRADUATE STUDIES The Department of Civil Engineering We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA April, 1980 (5) David George McLean 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 Cim / moo^i^y The University of British Columbia 2075 Wesbrook Place Vancouver, Canada V6T 1W5 E-6 BP 75-51 1 E ABSTRACT The Chilliwack River flows through the Cascade Mountains until reaching a narrow gorge near Vedder Crossing where it flows onto the Fraser Lowlands and eventually meets the Fraser River. Below Vedder Crossing, the river is actively building an alluvial fan by depos• iting its sediment load of gravel and sand. This deposi• tion has resulted in frequent channel shifts over the fan surface with the most recent migration occurring around 1894 when the river shifted down Vedder Creek. Over the last century the Vedder River has been undergoing very complex changes in response to changes in the incidence of severe floods, changes in sediment supply and interference from river training. -
Swift Creek Consent Decree Final
}: s FILFD COQ N'Y "L-FRK 1 10 k 43 2 3 4 BY ---- 5 6 7 STATE OF WASHINGTON 8 WHATCOM COUNTY SUPERIOR COURT 9 STATE OF WASHINGTON, ° 9 2 0 2 7 DEPARTMENT OF ECOLOGY, NO. 37 10 Plaintiff, 11 CONSENT DECREE V. RE: SUMAS MOUNTAIN 12 LANDSLIDE WHATCOM COUNTY; WHATCOM 13 . COUNTY FLOOD CONTROL ZONE DISTRICT; GREAT WESTERN 14 LUMBER COMPANY; and MILLMAN FAMILY LLC, 15 Defendants. 16 17 18 TABLE OF CONTENTS 19 I. INTRODUCTION ........................................................................................................ 3 20 II. JURISDICTION ........................................................................................................... 5 III. PARTIES BOUND ....................................................................................................... 6 21 IV. DEFINITIONS ............................................................................................................. 6 22 V. FINDINGS OF FACTS ................................................................................................ 7 VI. WORK TO BE PERFORMED ................................................................................... 14 23 VII. DURATION OF DECREE ......................................................................................... 21 VIII. DESIGNATED PROJECT COORDINATORS ......................................................... 22 24 IX. PERFORMANCE .......................................................................................................23 X. ACCESS .................................................................................................................... -
Trans Mountain Pipeline ULC Trans Mountain Expansion Project
TRANS MOUNTAIN PIPELINE ULC TRANS MOUNTAIN EXPANSION PROJECT PRELIMINARY GEOTECHNICAL HDD FEASIBILITY ASSESSMENT SUMAS RIVER AT V10 RK 1114.6 PROJECT NO.: 0095150-04 DISTRIBUTION: DATE: February 20, 2015 TMP ULC: 2 copies DOCUMENT NO.: 0095150-14-SUM BGC: 2 copies OTHER: 1 copy Trans Mountain Pipeline ULC February 20, 2015 Sumas River at V10 RK 1114.6 Project No.: 0095150-04 EXECUTIVE SUMMARY As part of the engineering design and assessment for the Trans Mountain Expansion Project (TMEP), BGC Engineering Inc. (BGC) has been retained to complete geotechnical feasibility assessments for horizontal directional drilling (HDD) at select stream crossings along the proposed pipeline corridor. In September 2014, BGC supervised the drilling of three boreholes adjacent to the proposed HDD alignment at Sumas River east of Abbotsford, BC. WorleyParsons, under subcontract to BGC, completed geophysical surveys at the same site in August 2013 and November 2014. Analysis of historical aerial photographs shows that the banks of Sumas River appear stable with respect to bank erosion and avulsion, and the proposed HDD alignment is not expected to be compromised by these hydrotechnical hazards. Results from the scour analysis estimate a maximum scour depth of approximately 2.0 m below the channel thalweg during a 200-year flood event, corresponding to an elevation of 1.5 m below sea level. Given this result, the depth of cover above the proposed HDD borepath remains adequate for the entire HDD length. The HDD entry and exit points are located beyond the dykes that parallel the Sumas River at an elevation of approximately 3.8 and 11.8 masl, respectively. -
The Stō:Ló Is a River of Knowledge, Halq'eméylem Is a River of Stories
Walking Backwards into the Future with Our Stories: The Stō:ló is a River of Knowledge, Halq’eméylem is a River of Stories by lolehawk Laura Buker M.A. (Education), Simon Fraser University, 1980 B.Ed., University of British Columbia, 1975 Thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in the Curriculum Theory & Implementation Program Faculty of Education © lolehawk Laura Buker Simon Fraser University Summer 2011 All rights reserved. However, in accordance with the Copyright Act of Canada, this work may be reproduced, without authorization, under the conditions for "Fair Dealing." Therefore, limited reproduction of this work for the purposes of private study, research, criticism, review and news reporting is likely to be in accordance with the law, particularly if cited appropriately. APPROVAL Name: Laura Buker Degree: Doctor of Philosophy Title of Thesis: Walking Backwards Into the Future With Our Stories: The St6:lo is a River of Knowledge, Haq'emeylem is a River of Stories Examining Committee: Chair: Robin Brayne, Adjunct Professor Allan MacKinnon, Associate Professor Senior Supervisor Vicki Kelly, Assistant Professor Committee Member Elizabeth Phillips, Elder, St6:lo Nation Committee Member Heesoon Bai, Associate Professor Internal/External Examiner Jan Hare, University of British Columbia External Examiner Date Defended/Approved: ii Partial Copyright Licence Abstract Storytelling is the original form of education for the indigenous families along the Fraser River. These stories have informed ecological, linguistic and cultural knowledge for thousands of years. This story begins in the time of the oldest inhabitants of the Fraser Valley along the St ó:lō where the river and the indigenous peopleevolutionary share changethe same and name: transformation Stó:lō, People that of is the personal River. -
Explore Local History Through Collage: Semá:Th Xόtsa (Sumas Lake) and Sumas Prairie
Explore Local History through Collage: Semá:th Xόtsa (Sumas Lake) and Sumas Prairie Self-guided activity OVERVIEW Try your hand at an art making activity inspired by historical photographs from The Reach Gallery Museum archives1 of Semá:th Xόtsa (Sumas Lake, pronounced seMATH hOTsa) and our permanent museum exhibition Voices of the Valley.2 This Edukit uses Historical Thinking Concepts to encourage participants to use primary resources and to develop historical literacy. Both experiences use Visual Thinking Strategies to encourage participants to construct meaning based on their own observations. Figure 1. Collage example. Through this project participants will: Explore connections to identity, place, culture, and belonging through creative expression. Create works of art, collaboratively or individually using imagination, inquiry, experimentation, and purposeful play. Examine relationships between local history, the arts, and the wider world. Experience, document, and present creative works in a variety of ways. Figure 2 (above left). Semá:th Xόtsa in 1920 prior to the drainage. Catalogue no. P188, The Reach Gallery Museum archive. Figure 3 (above right). Contemporary image of Sumas Prairie. 1 For more information on The Reach Gallery Museum archives, visit https://www.thereach.ca/research-and-collections/ 2 For more information on Voices of the Valley, visit https://www.thereach.ca/exhibitions/voices-of-the-valley/ The Importance of Place and Language The Reach Gallery Museum acknowledges that the City of Abbotsford is located on S’olh Temexw. [pronounced: suh-oll TUMM ook] S’olh Temexw is the unceded, traditional, ancestral shared territory of the Semá:th First Nation and Mathekwi First Nation. These two First Nations are part of the Stό:lō Nation, the People of the River. -
The Lummi Nation -- WRIA 1 (Mountains to the Sea)
The Lummi Nation -- WRIA 1 (Mountains to the Sea) WRIA 1 is 1410 square miles in area: 832 square miles of WRIA 1 is in the Nooksack River watershed, the largest single watershed in the WRIA. Forty-nine square miles of the Nooksack watershed is in Canada. It has three main forks: the North, Middle, and South that Bellingham originate in the steep high-elevation headwaters of the North Cascades and flow westerly descending into flats of the Puget lowlands.The North and Middle Forks are glacial rivers and originate from Mount Baker. The South Fork is a snow/rain fed river and Watersheds of originates from the non-glaciated slope of theTwin Sisters peaks. The WRIA 01 Middle Fork flows into the North Fork upstream of where the North Fork confluences with the South Fork to form the mainstem Nooksack River. The mainstem then flows as a low-gradient, low-elevation river until discharging through the Lummi Nation and into Bellingham Bay. Historically, the Nooksack River alternated between discharging into Bellingham Bay, and flowing through the Lummi River and discharging into Lummi Bay (Collins and Sheikh 2002). The Nooksack River has five anadromous salmon species: pink, chum , Chinook , coho, sockeye; and three anadromous trout: steelhead, cutthroat and bull trout (Williams et al. 1975; Cutler et al. 2003). Drayton Blaine Harbor Whatcom County Lynden Land Zoning Everson Birch Bay Nooksack R. Urban Growth Area 4% of total land use NF Nooksack R. Agriculture Ferndale 8% of total land use Rural Residential Bellingham Deming 12% of total land use Lummi Lummi R. -
Sword Swallowing, Music and More! P.16
Amy Goodman, P.6 * Paper Cuts, P.18 * Free Will, P.29 cascadia REPORTING FROM THE HEART OF CASCADIA WHATCOM SKAGIT ISLAND LOWER B.C. {03.14.12}{#11}{V.07}{FREE} Wicked Games The undeniable attraction of CHRIS ISAAK P.20 Gas Grief: Easy oil’s grim realities, P.8 :: Green Scene: The sounds of St. Patrick’s Day, P.21 Sideshow Alert: Sword swallowing, music and more! P.16 34 34 cascadia FOOD Stevie Coyle, a former member of the Waybacks and 27 a lauded fingerstyle guitarist, B-BOARD performs March 21 at the A glance at what’s happening this week Roeder Home 24 FILM FILM 20 MUSIC 18 ART ART 16 STAGE STAGE 14 GET OUT 12 WORDS 2 ) .4[03.x{.12] !-$4[03.x}.12] “Owls Outback” will be one of the many featured top- 8 ONSTAGE ONSTAGE ics at this year’s 2 *2 Northwest Bird- Lysistrata: 7:30pm, Syre Auditorium, WCC JustinCredible Sideshow: 7pm, 9pm and 11pm, The Fantasticks: 7:30pm, MBT’s Walton Theatre Bellingham Flea Market ing Festival, which takes place both outdoors and in CURRENTS CURRENTS MUSIC Lysistrata: 7:30pm, Syre Auditorium, WCC March 17 throughout Blaine The Fantasticks: 7:30pm, MBT’s Walton Theatre 6 Persa Gitana: 7:30pm, Roeder Home Cabaret: 7:30pm, RiverBelle Theatre, Mount FOOD Vernon VIEWS VIEWS Celebrate your love Beer Week: Through March 17, throughout The Wizard of Oz: 7:30pm, McIntyre Hall, Mount 4 Mount Vernon Vernon of Japanese comics Harold: 8pm, Upfront Theatre MAIL MAIL Games Galore: 10pm, Upfront Theatre and animation at an [03. -
Wetland Action Plan for British Columbia
Wetland Action Plan for British Columbia IAN BARNETT Ducks Unlimited Kamloops, 954 A Laval Crescent, Kamloops, BC, V2C 5P5, Canada, email [email protected] Abstract: In the fall of 2002, the Wetland Stewardship Partnership was formed to address the need for improved conservation of wetland ecosystems (including estuaries) in British Columbia. One of the first exercises undertaken by the Wetland Stewardship Partnership was the creation of a Wetland Action Plan. The Wetland Action Plan illustrates the extent of the province's wetlands, describes their value to British Columbians, assesses threats to wetlands, evaluates current conservation initiatives, and puts forth a set of specific actions and objectives to help mitigate wetland loss or degradation. It was determined that the most significant threats to wetlands usually come from urban expansion, industrial development, and agriculture. The Wetland Stewardship Partnership then examined which actions would most likely have the greatest positive influence on wetland conservation and restoration, and listed nine primary objectives, in order of priority, in a draft ‘Framework for Action’. Next, the partnership determined that meeting the first four of these objectives could be sufficient to provide meaningful and comprehensive wetland protection, and so, committed to working together towards enacting specific recommendations in relation to these objectives. These four priority objectives are as follows: (1) Work effectively with all levels of government to promote improved guidelines and stronger legislative frameworks to support wetlands conservation; (2) Provide practical information and recommendations on methods to reduce impacts to wetlands to urban, rural, and agricultural proponents who wish to undertake a development in a wetland area; (3) Improve the development and delivery of public education and stewardship programs that encourage conservation of wetlands, especially through partnerships; and (4) Conduct a conservation risk assessment to make the most current inventory information on the status of B.C. -
Dionisio Point Excavations
1HE• Publication of the Archaeological Society of Vol. 31 , No. I - 1999 Dionisio Point Excavations ARCHAEOLOGICAL SOCIETY OF &MIDDEN BRITISH COLUMBIA Published four times a year by the Archaeological Society of British Columbia Dedicated to the protection of archaeological resot:Jrces and the spread of archaeological knowledge. Editorial Committee Editor: Heather Myles (274-4294) President Field Editor: Richard Brolly (689-1678) Helmi Braches (462-8942) arcas@istar. ca [email protected] News Editor: Heather Myles Publications Editor: Robbin Chatan (215-1746) Membership [email protected] Sean Nugent (685-9592) Assistant Editors: Erin Strutt [email protected] erins@intergate. be.ca Fred Braches Annual membership includes I year's subscription to [email protected] The Midden and the ASBC newsletter, SocNotes. Production & Subscriptions: Fred Braches ( 462-8942) Membership Fees I SuBSCRIPTION is included with ASBC membership. Individual: $25 Family: $30 . Seniors/Students: $I 8 Non-members: $14.50 per year ($1 7.00 USA and overseas), Send cheque or money order payable to the ASBC to: payable in Canadian funds to the ASBC. Remit to: ASBC Memberships Midden Subscriptions, ASBC P.O. Box 520, Bentall Station P.O. Box 520, Bentall Station Vancouver BC V6C 2N3 Vancouver BC V6C 2N3 SuBMISSIONs: We welcome contributions on subjects germane ASBC on Internet to BC archaeology. Guidelines are available on request. Sub http://home.istar.ca/-glenchan/asbc/asbc.shtml missions and exchange publications should be directed to the appropriate editor at the ASBC address. Affiliated Chapters Copyright Nanaimo Contact: Rachael Sydenham Internet: http://www.geocities.com/rainforest/5433 Contents of The Midden are copyrighted by the ASBC.