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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”. -
Occurrence and Genesis of Apline Linears Due To
OCCURRENCE AND GENESIS OF ALPINE LINEARS DUE TO GRAVITATIONAL DEFORMATION IN SOUTH WESTERN, BRITISH COLUMBIA Derek Kinakin BSc, Simon Fraser University 2002 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the Department of Earth Sciences O Kinakin 2004 SIMON FRASER UNIVERSITY Fa11 2004 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: Derek Kinakin Degree: MSc Title of Thesis: Occurrence and genesis of alpine hears due to gravitational deformation in South Western, British Columbia Examining Committee: Chair: Dr. Peter Mustard Associate Professor Department of Earth Sciences, SFU Dr. Doug Stead Senior Supervisor Professor Department of Earth Sciences, SFU Dr. Brent Ward Supervisor Associate Professor Department of Earth Sciences, SFU Bruce Thomson, MSc., PGeo. Supervisor Ministry of Water, Land & Air Protection (Ret.) Tom Stewart, MSc., PEng. External Examiner Civil Engineer B.C. Hydro Date DefendedlApproved: November 15,2004 DECLARATION OF PARTIAL COPYRIGHT LICENCE The author, whose copyright is declared on the title page of this work, has granted to Simon Fraser University the right to lend this thesis, project or extended essay 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. The author has further granted permission to Simon Fraser University to keep or make a digital copy for use in its circulating collection, and, without changing the content, to translate the thesislproject or extended essays, if technically possible, to any medium or format for the purpose of preservation of the digital work. -
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. -
Dendrohydrological Reconstruction and Hydroclimatic Variability in Southwestern British Columbia, Canada
Dendrohydrological reconstruction and hydroclimatic variability in southwestern British Columbia, Canada by Bryan J. Mood B.Sc., Mount Allison University, 2013 M.Sc., University of Victoria, 2015 A Dissertation Submitted in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY in the Department of Geography © Bryan Mood, 2019 University of Victoria All rights reserved. This dissertation may not be reproduced in whole or in part, by photocopying or other means, with the permission of the author. Supervisory Committee Dendrohydrological reconstruction and hydroclimatic variability in southwestern British Columbia, Canada by Bryan J. Mood B.Sc., Mount Allison University, 2013 M.Sc., University of Victoria, 2015 Supervisory Committee Dr. Dan J. Smith (Department of Geography) Supervisor Dr. David Atkinson (Department of Geography) Departmental Member Dr. Tobi Gardner (Victoria Capital Regional District) Outside Member ii Abstract Supervisory Committee Dr. Dan J. Smith (Department of Geography) Supervisor Dr. David Atkinson (Department of Geography) Departmental Member Dr. Tobi Gardner (Victoria Capital Regional District) Outside Member The hydrology of southwestern British Columbia is influenced by the region’s mountainous topography and climate oscillations generated from the Pacific Ocean. While much of the region is characterized as a temperate rainforest, recent summers are defined by record-breaking droughts that focus attention on the threat to regional water supply security likely to accompany future climate changes. The limited length and distribution of hydrological records in southwestern British Columbia provide poor context for resource managers tasked with developing policy and water management strategies. The purpose of the dissertation was to describe long-term variability in several key hydroclimatic variables and hydroecological interactions that may be used in updated water resource policy and management strategies. -
Cheam Range, Lady Peak, North Face
AAC Publications Cheam Range, Lady Peak, North Face Canada, British Columbia, North Cascades On May 7, Brette Harrington and Marc-André Leclerc climbed the north face of Lady Peak (2,178m) in the Cheam Range, near Chilliwack. This was likely the first ascent of the face, whose steepest section gains about 500m and is comprised of loose but compact volcanic rock. The two spent 13 hours on the climb, which involved thin ice and technical dry tooling on slabs, often with marginal protection (11 long pitces, 5.8 M4 80°). They topped out at sundown and scrambled to the summit before descending easy slopes to the west. In January 2016, the same pair made the probable first ski descent of the northeast couloir on Lady Peak. – Dougald MacDonald, with information from Marc-André Leclerc The following first-person account of this ascent, by Marc-André Leclerc, unfortunately was received too late for publication in the print edition of AAJ 2018: On May 7, Brette Harrington and I climbed a line, right of center, on the imposing north face of Lady Peak in the Cheam Range, the same range of mountains where I essentially began my true mountaineering apprenticeship, with an ascent of Welch Peak, at 11 years old. The area is well known for very loose rock, and the more technical routes are often done in winter or spring as frozen mixed routes. The north face of Lady Peak is the steepest in the range and could be considered the last major face in the range to be climbed, as the unclimbed north face of the Still, while appealing, is quite small in comparison. -
SXTA Land Selection, Protection, and Governance Frameworks: Developing Intra- and Inter-Governmental Relations
SXTA Land Selection, Protection, and Governance Frameworks: Developing Intra- and Inter-Governmental Relations A Treaty Related Measures Project funded by Canada prepared and submitted on behalf of the Stó:lō Xwexwilmexw Treaty Association October 31, 2013 ACKNOWLEDGEMENTS Yálh yexw kwás hó:y to all those who participated in, informed and otherwise contributed to this project...in an effort to advance understanding of Stó:lō principles, teachings and relationships with and within S’ólh Téméxw. ‘We have to learn to live together in a good way.’ – T’xwelátse (Time Immemorial) i CREDITS Project Direction and Authorship Project Director / Co-Author ............................... David Schaepe, Ph.D. Researcher / Co-Author ....................................... Sue Formosa, Msc., Cert. Geom., Adv. Dip. GIS Researcher / Co-Author ....................................... Sheila Schmidt Researcher / Co-Author ....................................... Karen Brady, Ph.D. Researcher .................................................... Naxaxalhts’i (Albert ‘Sonny’ McHalsie), Hon. Ph.D. Analysts................................................................ Mehaffey Consulting Inc. Research Assistant ............................................... Cathy Hall Research Assistant ............................................... Lisa Davidson Research Assistant & Copy Editor ...................... Carly Teillet SXTA Lands Working Group - Project Steering Committee .............................................................................. Angie Bailey, -
Cliff Paintbrush (Castilleja Rupicola) in Canada
PROPOSED Species at Risk Act Recovery Strategy Series Adopted under Section 44 of SARA Recovery Strategy for the Cliff Paintbrush (Castilleja rupicola) in Canada Cliff Paintbrush 2016 Recommended citation: Environment Canada. 2016. Recovery Strategy for the Cliff Paintbrush (Castilleja rupicola) in Canada [Proposed]. Species at Risk Act Recovery Strategy Series. Environment Canada, Ottawa. 20 pp. + Annex. For copies of the recovery strategy, or for additional information on species at risk, including the Committee on the Status of Endangered Wildlife in Canada (COSEWIC) Status Reports, residence descriptions, action plans, and other related recovery documents, please visit the Species at Risk (SAR) Public Registry1. Cover illustration: © Ross Vennesland Également disponible en français sous le titre « Programme de rétablissement de la castilléjie des rochers (Castilleja rupicola) au Canada [Proposition] » © Her Majesty the Queen in Right of Canada, represented by the Minister of the Environment, 2016. All rights reserved. ISBN Catalogue no. Content (excluding the illustrations) may be used without permission, with appropriate credit to the source. 1 http://sararegistry.gc.ca/default.asp?lang=En&n=24F7211B-1 RECOVERY STRATEGY FOR THE CLIFF PAINTBRUSH (Castilleja rupicola) IN CANADA 2016 Under the Accord for the Protection of Species at Risk (1996), the federal, provincial, and territorial governments agreed to work together on legislation, programs, and policies to protect wildlife species at risk throughout Canada. In the spirit of cooperation of the Accord, the Government of British Columbia has given permission to the Government of Canada to adopt the Recovery Strategy for Cliff Paintbrush (Castilleja rupicola) in British Columbia (Part 2) under Section 44 of the Species at Risk Act (SARA). -
The Persistence of Oxbow Lakes As Aquatic Habitats: an Assessment of Rates of Change and Patterns of Alluviation
The Persistence of Oxbow Lakes as Aquatic Habitats: an Assessment of Rates of Change and Patterns of Alluviation Pauline L. Dieras 2013 Thesis submitted for the degree of Doctorate of Philosophy Declaration This work has not been submitted in substance for any other degree or award at this or any other university or place of learning, nor is being submitted concurrently in candidature for any degree or other award. Signed Pauline Dieras Date: 05/03/2013 This thesis is being submitted in partial fulfilment of the requirements for the degree of PhD Signed Pauline Dieras Date: 05/03/2013 This thesis is the result of my own independent work/investigation, except where otherwise stated. Other sources are acknowledged by explicit references. The views expressed are my own. Signed Pauline Dieras Date: 05/03/2013 I hereby give consent for my thesis, if accepted, to be available for photocopying and for inter-library loan, and for the title and summary to be made available to outside organisations. Signed Pauline Dieras Date: 05/03/2013 i Abstract Oxbow lakes are of high ecological importance due to the number and the diversity of habitats they provide. They are created after the abandonment of meanders and subsequent sediment infilling leads to their progressive terrestrialisation, taking from a few months up to several centuries. Nonetheless, little is known about oxbow lake terrestrialisation processes, sediment composition, or why such a disparity exists in lakes’ longevity. To understand the controls on oxbow lakes alluviation, field observations, remotely sensed data and GIS analyses were combined. Sediment transfers in oxbow lakes were documented by topographic and sampling surveys of sites in France and Wales. -
E Ofo - Library I MPO Bibliothequo EX LIBRIS - Ian D
qH 0 ;;; e oFO - Library I MPO Bibliothequo EX LIBRIS - Ian D. Thomson fl1 t_f <J 1111 llil Ill II m Ill\ 120099451\1 1\1 ~\11 1 1 PERCEPTIONS ON RECREATION AND SPORT FISHERIES OF THE CHILLIWACK/ VEDDER RIVER by Philip A. Meyer Chief Social Science Unit Southern Operations Branch Fisheries & Marine Service JOINTLY FUNDED BY: Southern Operations Branch Fish and Wildlife Branch Fisheries and Marine Service Department of Recreation Environment Canada and Conservation Province of British Columbia SH 572 . BS M48 c . 2 JANUARY, 1976 '273D) THE LIBRARY BEDFORD INSTITUTE OF O CEA O GRAPHY PREFACE B.;X l 006 DARTMO UTH, N.S. B2Y 4A2 This study is the second of two funded jointly by the Fish and Wildlife Branch; Department of Recreation and Conservation , Province of British Columbia , and the Fisheries and Marine Service, Environment Canada , and focussing on recreational management of river systems. Wh i l e the analysis of results , and the writing of the report have fallen to t he .under signed, many persons contributed to the final product. Study design was a joint undertaking by Richard C. Bryan and Gerard J. Mos , both then with my unit, Christopher Dodd, of the Province of British Columbia, and the author. Field work was conducted by William Cotter and Victor Willms, under the supervision of Mr. Bryan. Data was arranged for computor analysis by Katherine J. Racey, and Mary C. Harrison. Finally, the study is particu larly indebted to Mr. Dodd for forceful and effective criticism during the write-up stage. Despite this substantial assistance t he author, nevertheless, retains claim to any and a ll errors. -
REGION 2 - Lower Mainland
REGION 2 - Lower Mainland CONTACT INFORMATION Fish and Wildlife Regional Office Salmon Information: (604) 586-4400 200-10428 153 St Fisheries and Oceans Canada Surrey BC V3R 1E1 District Offices (DFO) Conservation Officer Service Chilliwack: (604) 824-3300 Please call 1-877-952-7277 for recorded Delta: (604) 666-8266 information or to make an appointment at Langley: (604) 607-4150 any of the following Field Offices: Mission: (604) 814-1055 Mission, North Vancouver, Powell River, Squamish: (604) 892-3230 Sechelt, and Squamish Steveston: (604) 664-9250 Vancouver: (604) 666-0384 RAPP Shellfish Information line: (604) 666-2828 Report All Poachers Rand Polluters Mahood L i C in hilco Conservation Officerl 24 Hour Hotline tin k na STAY UP TO DATE: li R R 1-877-952-RAPPK (7277) iver ko Canim il Check website for in-season changes or h L Please refer to page 78 for more informationC closure dates for the 2021-2023 season rapp.bc.ca g at: www.gov.bc.ca/FishingRegulations r T o Cr a D C s y e 100 Mile House 5-6 e Tatlayoko k l o s o Lake M R r C 5-5 r 5-3 C CHILKO ig B Bonaparte n LAKE r L u R R h Taseko C te o ar hk Lakes ap at 5-4 3-31 on m FR B R Ho A S Y E a R n a R la k m o d m a R e Bish rd 3-32 D op o 2-15 L R R So Carpenter uthg ate ge Lake R Brid Gold ive Cache Creek Kamloops r Bridge R Lake 1-15 2-14 Seton BUTE L INLET 3-33 Anderson Lillooet 3-17 KAMLOOPS Phillips 2-13 L G R u i a R N Arm b r c o I O T C V h L h S o ILL s E OO o R P n E T o M y a O C C H r 2-11 3-16 T Sonora N TOBA ic Island R o INLET Pemberton la n E i e R l n a t e -
Nooksack River Overflow Flood Mitigation Plan
COUNCIL REPORT Executive Committee Report No. ENG 050-2020 Date: December 09, 2020 File No: 5225-03/Nooksack To: Mayor and Council From: Stella Chiu, Senior Engineer, Drainage and Wastewater Subject: Nooksack River Overflow Flood Mitigation Plan RECOMMENDATION THAT staff continue to work with the Province to encourage the United States to complete the cost-benefit analysis and fulfill the purpose and mandate of the International Task Force. REPORT CONCURRENCE General Manager City Manager The General Manager concurs with the The City Manager concurs with the recommendation of this report. recommendation of this report. SUMMARY OF THE ISSUE Major flooding of West Sumas Prairie and the Washington State cities of Everson, Sumas and the unincorporated areas of Whatcom, occurred in November 1990 when the overflow from the Nooksack River flooded into the Sumas River basin. The Nooksack River Overflow Flood Mitigation Plan (“Study”) is one of the next steps to address the international and transboundary issue from the United States (“US”) into Canada. The work was recently completed with funding from the National Disaster Mitigation Program; the Province supported the work in a technical advising role. This report provides a high-level summary of the findings and recommends next steps. BACKGROUND Major flooding of West Sumas Prairie and the Washington State cities of Everson, Sumas and the unincorporated areas of Whatcom, occurred in November 1990 when the overflow from the Nooksack River flooded into the Sumas River basin. A Nooksack River International Task Force (NRITF) was established in response to the flooding. The Task Force comprises members from both Canada and the US. -
A Comparison of the November 1990 and November 1995 Floods Along the Main Stem Nooksack River, Whatcom County, Washington Ryan T
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Winter 1997 A Comparison of the November 1990 and November 1995 Floods along the Main Stem Nooksack River, Whatcom County, Washington Ryan T. (Ryan Travis) Houser Western Washington University Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Houser, Ryan T. (Ryan Travis), "A Comparison of the November 1990 and November 1995 Floods along the Main Stem Nooksack River, Whatcom County, Washington" (1997). WWU Graduate School Collection. 828. https://cedar.wwu.edu/wwuet/828 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. WWU LIBRARIES A Comparison of the N ovember 1990 and N ovember 1995 Floods^ along the main stem N ooksack R iver, Whatcom County, Washington. by Ryan T. Houser Accepted in Partial Completion of the Requirements for the Degree Master of Science Dr. Moheb A. Ghali, Dean of Graduate School ADVISORY COMMITTEE Master’s Thf.sts In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Western Washington University, I agree that the Library shall make its copies freely available for inspection. I further agree that extensive copying of this thesis is allowable