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Gwa'sala"Nakwaxda'xw Statement of Intent
Statement of Intent Gwa'Sala - 'Nakwaxda'xw 1. What is the First Nation Called? Gwa'Sala - 'Nakwaxda'xw Nation 2. How is the First Nation established? Please Describe: The Gwa'Sala - 'Nakwaxda'xw First Nation is an Indian Band formally recognized under legislation of Canada (Indian Act, R.S.C. 1985 c. 1-5, as amended, and regulations made thereunder). Is there an attachment? No 3. Who are the aboriginal people represented by the First Nation? The Gwa'Sala - 'Nakwaxda'xw First Nation represents all members of the First Nation as shown on the Official Band List maintained by the Gwa'Sala - 'Nakwaxda'xw First Nation. 4. How many aboriginal people are represented by the First Nation? 547 members Is there any other First Nation that claims to represent the aboriginal people described in questions 3 and 4? If so, please list. Through a March 14, 1997 accord with the British Columbia Treaty Commission there are other First Nations who may collectiVely enter into negotiations on common issues with both Canada and British Columbia which may be considered to be representative of the Gwa'Sala - 'Nakwaxda'xw First Nation membership. The other First Nations are as follows: Kwakiutl First Nation Namgis First Nation Tanakteuk First Nation Tlatlasikwala First Nation Quatsino First Nation 5. Please list any First Nations with whom the First Nation may have overlapping or shared territory. 1.Oweekeno First Nation 2. Tsawataineuk First Nation 3. Kwicksutaineuk First Nation 4. Kwa-wa-aineuk First Nation 5. Kwakiutl First Nation 6. Tlatlasikwala First Nation 6. What is the First Nation's traditional territory in BC? Refer to the attached map showing the traditional territory of the Gwa'Sala- 'Nakwaxda'xw First Nation. -
KWAKIUTL BAND COUNCIL PO Box 1440 Port Hardy BC Phone (250) 949-6012 Fax (250) 949-6066
1 KWAKIUTL BAND COUNCIL PO Box 1440 Port Hardy BC Phone (250) 949-6012 Fax (250) 949-6066 February 5, 2007 Att: Mr. Rich Coleman, RE: GOVERNMENT APPROVAL FOR WESTERN FOREST PRODUCTS LAND TRANSFER AND INFRINGEMENT OF THE KWAKIUTL FIRST NATION DOUGLAS TREATIES AND TRADITIONAL TERRITORY We learned of the BC Government’s approval of Western Forest Product’s application to remove private lands from its Tree Farm License via news broadcasts. Our relationship, or lack of it, with Western Forest Products and the Ministry of Forests and Range is indicative of the refusal to openly discuss the application and especially when the Kwakiutl First Nation Council met with them on October 4th and 18th of 2006 (contrary to what we stated at these two meetings that this was not consultation nor accommodation). Western Forest Products historically has been blatantly allowed to disregard their obligations by your “watchdogs” to notify First Nation communities of their harvesting plans. These plans have, and always will have, the end result of infringement on our Treaty and Aboriginal rights and title as it exists for our traditional territory. This situation is further exacerbated by non-notification from your office of the recommendation to approve Western Forest Product’s application. It should be obvious to your ministry that there is the obligation to meaningfully consult and accommodate with First Nations and that message should have been strongly stressed to Western Forest Products. Western Forest Products has touted that it has good relationships with First Nations communities on its website but when we look at our relationship with them, the Kwakiutl First Nation must protest that Western Forest Products and Ministry of Forests and Range do not entirely follow legislated protocol. -
British Columbia Regional Guide Cat
National Marine Weather Guide British Columbia Regional Guide Cat. No. En56-240/3-2015E-PDF 978-1-100-25953-6 Terms of Usage Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: • Exercise due diligence in ensuring the accuracy of the materials reproduced; • Indicate both the complete title of the materials reproduced, as well as the author organization; and • Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1-800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Disclaimer: Her Majesty is not responsible for the accuracy or completeness of the information contained in the reproduced material. Her Majesty shall at all times be indemnified and held harmless against any and all claims whatsoever arising out of negligence or other fault in the use of the information contained in this publication or product. Photo credits Cover Left: Chris Gibbons Cover Center: Chris Gibbons Cover Right: Ed Goski Page I: Ed Goski Page II: top left - Chris Gibbons, top right - Matt MacDonald, bottom - André Besson Page VI: Chris Gibbons Page 1: Chris Gibbons Page 5: Lisa West Page 8: Matt MacDonald Page 13: André Besson Page 15: Chris Gibbons Page 42: Lisa West Page 49: Chris Gibbons Page 119: Lisa West Page 138: Matt MacDonald Page 142: Matt MacDonald Acknowledgments Without the works of Owen Lange, this chapter would not have been possible. -
3LMANUSCRIPT REPORT SERIES No. 36
DFO - L bra y MPOBibio heque II 1 111111 11 11 11 V I 1 120235441 3LMANUSCRIPT REPORT SERIES No. 36 Some If:eat/viz& 3,5,unamia, Olt the Yacific ettadt of South and ✓ cuith anwitica, T. S. Murty, S. 0. Wigen and R. Chawla Marine Sciences Directorate 975 Department of the Environment, Ottawa Marine Sciences Directorate Manuscript. Report Series No. 36 SOME FEATURES OF TSUNAMIS ON THE PACIFIC COAST OF SOUTH AND NORTH AM ERICA . 5 . Molly S . O. Wigen and R. Chawla 1975 Published by Publie par Environment Environnement Canada Canada I' Fisheries and Service des !Aches Marine Service et des sciences de la mer Office of the Editor Bureau du fiedacteur 116 Lisgar, Ottawa K1 A Of13 1 Preface This paper is to be published in Spanish in the Proceedings of the Tsunami Committee XVII Meeting, Lima, Peru 20-31 Aug. 1973, under the International Association of Seismology and Physics of the Earth Interior. 2 Table of Contents Page Abstract - Resume 5 1. Introduction 7 2. Resonance characteristics of sonic inlets on the Pacific Coast of Soulh and North America 13 3. Secondary undulations 25 4. Tsunami forerunner 33 5. Initial withdrawal of water 33 6. Conclusions 35 7. References 37 3 4 i Abstract In order to investigate the response of inlets to tsunamis, the resonance characteristics of some inlets on the coast of Chile have been deduced through simple analytical considerations. A comparison is made with the inlets of southeast Alaska, the mainland coast of British Columbia and Vancouver Island. It is shown that the general level of intensif yy of secondary undulations is highest for Vancouver Island inlets, and least for those of Chile and Alaska. -
First Nations of the North Island – Central Coast Forest District
First Nations of the North Island – Central Coast Resource District Link to Current Version: http://www.for.gov.bc.ca/ftp/DNI/external/!publish/Aboriginal%20Affairs/FN_NICC_CONTACTS.pdf Revised 10 August 2021 Hereditary Administration Main Village First Nation Chief or Chief Office Mailing Referrals Office Contact Location Councillor Address 1650 Old Spit Road Chief Councillor Campbell River, BC ENGAGE AS PER NANWAKOLAS SEA WITH Campbell River (Wei Wai Campbell Christopher V9W 3E8 NANWAKOLAS REFERRALS OFFICE Kum) First Nation River Roberts Ph: (250) 286-6949 Email: [email protected] Fax: (250) 287-8838 Box 220 Send referrals to: Quathiaski Cove, BC Cape Mudge (We Wai Chief Councillor Quathiaski Merci Brown: [email protected] V0P 1N0 Kai) First Nation Ronnie Chickite Cove 690 Head Start Crescent Ph: (250) 285-3316 Campbell River, BC Fax: (250) 285-2400 V9H 1P9 Hereditary Chief Box 521 ENGAGE AS PER NANWAKOLAS SEA WITH New William Alert Bay, BC NANWAKOLAS REFERRALS OFFICE Vancouver Glendale V0N 1A0 Email: [email protected] Hereditary Da’naxda’xw-Awaetlala Box 330 Chiefs Council Also send referrals to: First Nation Alert Bay, BC (Robert Duncan, New Hereditary Chiefs Council V0N 1A0 Norman Vancouver c/o Ruby Mannila, Band Administrator Ph: (250) 974-2703 Email: [email protected] Glendale, and Fax: (866) 450-3707 Ph: (250) 974-3718 Billy Peters) General Delivery Kingcome Inlet, BC Email referral and shapefiles to: Dzawada’enuxw First Council Chair Kingcome V0N 2B0 Referrals Office: [email protected] Nation Willie -
Jennifer Galloway's 2010 Paper
Marine Micropaleontology 75 (2010) 62–78 Contents lists available at ScienceDirect Marine Micropaleontology journal homepage: www.elsevier.com/locate/marmicro Research paper A high-resolution marine palynological record from the central mainland coast of British Columbia, Canada: Evidence for a mid-late Holocene dry climate interval Jennifer M. Galloway a,⁎, Lameed O. Babalola a, R. Timothy Patterson a, Helen M. Roe b a Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, Canada KIS 5B6 b School of Geography, Archaeology & Palaeoecology, Queen's University Belfast, Belfast, BT7 1NN, United Kingdom article info abstract Article history: Sediments collected in a 12-m long core (VEC02A04) obtained from Frederick Sound in the Seymour–Belize Received 24 December 2009 Inlet Complex of British Columbia were deposited between ca. 4540 cal. yr BP and ca. 1090 cal. yr BP in Received in revised form 6 March 2010 primarily dysoxic conditions. The sediments are characterized by alternating intervals of fine grained Accepted 8 March 2010 massive and laminated units. Laminated sediments consist of light-coloured diatom-rich layers deposited during summer and dark-coloured mineral-rich layers deposited during winter. Laminated sediments are Keywords: most common in portions of the core deposited between ca. 2840 cal. yr BP and ca. 1820 cal. yr BP, and Climate change correspond to a decline in the relative abundance and pollen accumulation rate of Cupressaceae pollen Late Holocene Coastal Western Hemlock biogeoclimatic between ca. 3190 cal. yr BP and ca. 2250 cal. yr BP. The preservation of laminated units and decline of zone Cupressaceae pollen at this time suggest that a drier and possibly cooler climate punctuated otherwise wet Marine palynology and temperate late Holocene conditions in the Seymour–Belize Inlet Complex. -
Tlatlasikwala
Statement of Intent Tlatlasikwala 1. What is the First Nation Called? Tlatlasikwala Nation 2. How is the First Nation established? Please Describe: Custom band with a Hereditary Chief and appointed Council. Is there an attachment? No 3. Who are the aboriginal people represented by the First Nation? Tlatlasikwala and the Nakumgalisala Peoples 4. How many aboriginal people are represented by the First Nation? Approx. 39 Is there any other First Nation that claims to represent the aboriginal people described in questions 3 and 4? If so, please list. 5. Please list any First Nations with whom the First Nation may have overlapping or shared territory. Quatsino First Nation and Kwakiutl First Nation 6. What is the First Nation's traditional territory in BC? Traditional Territories from the west coast of Vancouver Island from Sea Otter Cove and its adjacent waters to and including Triangle Island to a south-easterly direction, to Pine Island, down to a south-easterly course to the Gordon Islands and back across to Sea Otter Cove; inclusive of the rivers, head-waters and lakes across this stretch of land east to west as earlier identified. The Tlatlasikwala Traditional Territory Map may be updated in the future. Attach a map or other document, if available or describe. Map Available? Yes 7. Is the First Nation mandated by its constituents to submit a Statement of Intent to negotiate a treaty with Canada and British Columbia under the treaty process? Yes How did you receive your Mandate? (Please provide documentation) The Tlatlasikwala Council received its mandate to enter treaty negotiations by personally contacting its members living in Vancouver, Port Coquitlam, Kamloops, Kelowna, Whe-La-La-u (Alert Bay) Quatsino and Bella Bella for their approval. -
Kwicksutaineuk/Ah-Kwa-Mish Decision (2010)
Editor’s Note: Corrigendum released on December 20, 2010. Original judgment has been corrected with text of corrigendum appended. IN THE SUPREME COURT OF BRITISH COLUMBIA Citation: Kwicksutaineuk/Ah-Kwa-Mish First Nation v. British Columbia (Agriculture and Lands), 2010 BCSC 1699 Date: 20101201 Docket: S090848 Registry: Vancouver Between: 2010 BCSC 1699 (CanLII) Chief Robert Chamberlin, Chief of the Kwicksutaineuk/Ah-Kwa-Mish First Nation, on his own behalf and on behalf of all members of the Kwicksutaineuk/Ah-Kwa-Mish First Nation Plaintiff And Her Majesty the Queen in Right of the Province of British Columbia as represented by the Minister of Agriculture and Lands and Attorney General of Canada Defendants Corrected Judgment: The text of the judgment was corrected on the front page and at paragraphs 19, 22, 23, 27, and 94 on December 20, 2010. Before: The Honourable Mr. Justice Slade Reasons for Judgment In Chambers Counsel for the Plaintiff: J.J. Camp, Q.C. R. Mogerman K. Robertson Counsel for the Defendant, J. Sullivan Province of British Columbia: S. Knowles J. Oliphant Counsel for the Defendant, H. Wruck, Q.C. Attorney General of Canada: S. Postman A. Semple Place and Date of Hearing: Vancouver, B.C. April 13-16 & 19-21, 2010 Kwicksutaineuk/Ah-Kwa-Mish First Nation v. British Columbia (Agriculture and Lands) Page 2 Further Written Submissions: July 7 - 8, 2010 November 18, 22-24, 2010 Place and Date of Judgment: Vancouver, B.C. December 1, 2010 TABLE OF CONTENTS I. INTRODUCTION ................................................................................................ 4 II. COMMON ISSUES............................................................................................. 5 III. THE PROPOSED CLASS: SECTION 4(1)(b) - IS THERE AN IDENTIFIABLE CLASS OF TWO OR MORE PERSONS? ................................................................ -
CHS Index Chart
Fisheries and Oceans Pi'lches et Oceans Canada Canada Canada ••• 137 ° 136 " 134" 133 ° 131° 129 ° ,.. 126 ° 125 " 124 " 123° 122° 119° 124 ° 118 ° GENERAL CHARTS CARTES GENERALES SMALL-CRAFT CHARTS REV ILLAG IGEDO LARGER SCALE CHARTS ISLAND CARTES POUR EMBARCATIONS CARTES A PLUS GRANDE ECHELLE 3050 Kootenay Lake and Rovet 75 000 3311 Sunshtno Coast- Vancouver Ha rbour lo/A 3052 Okanagan Lako so 000 Desolatoon Sound 40 000 3053 Shuswap Lake so 000 331:2 JerviS Intel ond/et Do•o latoon Sound 0 305S Waneta to /~ Hugh Keen leyside Dam 20 000 Vo,ous Scolo•JEche tle• vo"h• > z 3056 Hugh Koon loySido Dam to/A Burlon 40 000 3313 Gull Islands and Ad jacent Watotways/el les Vo1es Navigables Ad1acentes ~ ' 3057 Button IO/~ 1\rrowhood 40 000 Variou• Scale•/Echel le• vo"~"' 3058 Arrowhead lo/6 Rovo lotoko Go «m• 20 000 3488 Fro5er River/F I&uve Fraser, Cre•<ent l5land 3061 " "'"'on Lake and/ol Hamson R1ver '""'' to/~ Hon loon Mills 20 000 Harrison Lake 40 000 3469 Fraser Rovor/Fiouve Fr8set, Pattullo B"dgo Harrison R1ver 30 000 to/a Crescent Is land 20 000 Pitt River and/ot Poll l ak e 25 000 Stuaot L a~e (Not•howniP••rnd•qu o!) 50 000 54 " ~f--- ' ~ 0 "" I < ''"0' 't)Go iUn "?1- Cocoov• 3053 Foo ..o<o o l 0 "' GJ ,. Shu wap .•. Lake CANAOA !'; "'""""'' •·o~ d 130" 125° 120 " •5"omouo .,cocho Cceo> ,... ,. ' GJ ... ' <om l oops ~ DIXON E'N TRANCE' LEGENO/LEGENDE • •• • Scales smaller ttlan 1"40 000 Ectlellas plus petites qua 1:40 000 '' GJ Scales 1:40 000 and larger Ectlelles 1: 40 000 et plus grande& CHART SCALE Chart soale os the rat10 of one umt of d1stance 011 the cha" to the actual d.stance on the Earth's surface expressed on tho same unots. -
Climate Change and Decadal to Centennial-Scale Periodicities Recorded in a Late Holocene NE Pacific Marine Record: Examining the Role of Solar Forcing
Palaeogeography, Palaeoclimatology, Palaeoecology 386 (2013) 669–689 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Climate change and decadal to centennial-scale periodicities recorded in a late Holocene NE Pacific marine record: Examining the role of solar forcing J.M. Galloway a,⁎, A. Wigston a, R.T. Patterson a, G.T. Swindles b, E. Reinhardt c, H.M. Roe d a Department of Earth Sciences and Ottawa Geoscience Centre, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario K1S 5B6, Canada b School of Geography, University of Leeds, Leeds LS2 9JT, United Kingdom c School of Geography and Earth Sciences, McMaster University, Hamilton, ON L8S 4K1, Canada d School of Geography, Archaeology and Palaeoecology, Queen's University Belfast, Belfast BT7 1NN, United Kingdom article info abstract Article history: We present a decadal-scale late Holocene climate record based on diatoms, biogenic silica, and grain size Received 29 November 2012 from a 12-m sediment core (VEC02A04) obtained from Frederick Sound in the Seymour-Belize Inlet Complex Received in revised form 21 June 2013 of British Columbia, Canada. Sediments are characterized by graded, massive, and laminated intervals. Accepted 22 June 2013 Laminated intervals are most common between c. 2948–2708 cal. yr BP and c. 1992–1727 cal. yr BP. Available online 4 July 2013 Increased preservation of laminated sediments and diatom assemblage changes at this time suggest that cli- mate became moderately drier and cooler relative to the preceding and succeeding intervals. Spectral and Keywords: fi Late Holocene wavelet analyses are used to test for statistically signi cant periodicities in time series of proxies of primary Climate change production (total diatom abundance, biogenic silica) and hydrology (grain size) preserved in the Frederick Diatoms Sound record. -
REC-EWED by APR 1 1,2009 J
PROSPECTING ASSESSMENT REPORT ON THE SEYMOUR INLET PROJECT (WIGWAM CLAIMS, Tenure # 572620 & 572621) (Pt/Os/Rh/lr ALASKAN TYPE INTRUSION) Seymour Inlet, Vancouver Mining Division NTS 92 M/2 (92M.017) Latitude 51°08'19", Longitude: 126°43'48" REC-EWED By APR 1 1,2009 J. T. ~Ihearer, M.Sc., P.Geo. Gold Commissioner's MfM5' - 2330 Tyner Street VANCOUVER, B.C. Port Coquitlam, BC !fJ r V3C 221 ;;e; ~~ • Phone:604-970-6402 ~ 1:1 I, ,j E-mail: [email protected] ~ [,! ,1 ~ri' " ("-I For § [~, l;j /2,. , i &-1' ...; ~,. "< ", Homegold Resources ltd /O-'"iI! c.":'/ v c' Unit 5 - 2330 Tyner Street t: £; ~ c«( Port Coquitlam, BC v c .. ~';.".;;- "'" V3C 221 ~J September 15, 2008 Fieldwork completed between August 1, 2008 and August 30, 2008 r- • TABLE of CONTENTS PAGE INTRODUCTION 1 PROPERTy 2 LOCATION, ACCESS and TOPOGRAPHY : 3 HISTORY and DEVELOPMENT 4 REGIONAL GEOLOGY 5 LOCAL GEOLOGy 6 ROCK DESCRIPTIONS 7 2008 PROSPECTING and GEOLOGY 9 CONCLUSIONS and RECOMMENDATIONS 10 ESTIMATE of COSTS for FUTURE WORK 11 STATEMENT of QUALIFICATIONS 12 REFERENCES 13 APPENDICES Appendix I Statement of Costs 14 Appendix II List of Specimens 15 Appendix III Titaniferous Zoned Pt-OZ-Rh/lr Vadadium Deposit Model And Magmatic Oxide Deposit Model 17 Prospecting Report on the Seymour Inlet Project (Wigwam Claims) September 15, 2008 Page ii • LIST of ILLUSTRATIONS and TABLES Following Page FIGURE 1 Property Location, 1":190km ii FIGURE 2 Detail Property Location 1 FIGURE 3 Claim Location Map, 1:51,000 2 FIGURE 4 Regional Geology Map, 1:147,869 4 FIGURE 5 Local Geology, 1:50,000 5 FIGURE 6 Local Prospecting Map, 1:10,000, Rainbow Creek Area 8 FIGURE 7 Local Prospecting Map, 1:10,000, Haig Bay Area 9 TABLES Page TABLE I List of Claims ! •••••••••••• 2 Prospecting Report on the Seymour Inlet Project (Wigwam Claims) September 15, 2008 Page iii ----------------~-------- pW INTRODUCTION The Wigwam Project is located near the head of Seymour Inlet, BC, a narrow coastal mainland fjord 85km east of the north tip of Vancouver Island in the Vancouver Mining Division. -
Postglacial Vegetation and Climate Dynamics in the Seymour-Belize Inlet Complex, Central Coastal British Columbia, Canada: Palynological Evidence from Tiny Lake
Postglacial vegetation and climate dynamics in the Seymour-Belize Inlet Complex, central coastal British Columbia, Canada: palynological evidence from Tiny Lake. Galloway, J. M., Doherty, C. T., Patterson, R. T., & Roe, H. (2009). Postglacial vegetation and climate dynamics in the Seymour-Belize Inlet Complex, central coastal British Columbia, Canada: palynological evidence from Tiny Lake. Journal of Quaternary Science, 24(4), 322-335. https://doi.org/10.1002/jqs.1232 Published in: Journal of Quaternary Science Document Version: Early version, also known as pre-print Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:23. Sep. 2021 JOURNAL OF QUATERNARY SCIENCE (2009) 24(4) 322–335 Copyright ß 2008 John Wiley & Sons, Ltd. Published online 23 October 2008 in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/jqs.1232 Postglacial vegetation and climate dynamics in the Seymour-Belize Inlet Complex, central coastal British Columbia, Canada: palynological evidence from Tiny Lake JENNIFER M.