List of Lights, Buoys and Fog Signals for Pacific Coast
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Gary's Charts
Gary’s Garage Sale - Chart List Chart Number Chart Name Area Scale Condition Price 3410 Sooke Inlet West Coast Vancouver Island 1:20 000 Good $ 10.00 3415 Victoria Harbour East Coast Vancouver Island 1:6 000 Poor Free 3441 Haro Strait, Boundary Pass and Sattelite Channel East Vancouver Island 1:40 000 Fair/Poor $ 2.50 3441 Haro Strait, Boundary Pass and Sattelite Channel East Vancouver Island 1:40 000 Fair $ 5.00 3441 Haro Strait, Boundary Pass and Sattelite Channel East Coast Vancouver Island 1:40 000 Poor Free 3442 North Pender Island to Thetis Island East Vancouver Island 1:40 000 Fair/Poor $ 2.50 3442 North Pender Island to Thetis Island East Vancouver Island 1:40 000 Fair $ 5.00 3443 Thetis Island to Nanaimo East Vancouver Island 1:40 000 Fair $ 5.00 3459 Nanoose Harbour East Vancouver Island 1:15 000 Fair $ 5.00 3463 Strait of Georgia East Coast Vancouver Island 1:40 000 Fair/Poor $ 7.50 3537 Okisollo Channel East Coast Vancouver Island 1:20 000 Good $ 10.00 3537 Okisollo Channel East Coast Vancouver Island 1:20 000 Fair $ 5.00 3538 Desolation Sound & Sutil Channel East Vancouver Island 1:40 000 Fair/Poor $ 2.50 3539 Discovery Passage East Coast Vancouver Island 1:40 000 Poor Free 3541 Approaches to Toba Inlet East Vancouver Island 1:40 000 Fair $ 5.00 3545 Johnstone Strait - Port Neville to Robson Bight East Coast Vancouver Island 1:40 000 Good $ 10.00 3546 Broughton Strait East Coast Vancouver Island 1:40 000 Fair $ 5.00 3549 Queen Charlotte Strait East Vancouver Island 1:40 000 Excellent $ 15.00 3549 Queen Charlotte Strait East -
Babine Lake Region and Covers the Central Part of the Babine Porphyry Belt
T L a a k ke la M o r r is o n L a k e H a La u k te e te Hearne Hill East Hautete Lake H a tc h e r y A r m Natowite B a Old Fort Lake L b a in Mountain ke e Smithers Landing Nizik McKendrick Lake Island Ba b in e L H a a g a k n e A r m Ministry of Employment and Investment Energy and Minerals Division Geological Survey Branch TILL GEOCHEMISTRY OF THE OLD FORT MOUNTAIN MAP AREA, CENTRAL BRITISH COLUMBIA (NTS 93Ml1) By Victor M. Levson, Stephen J. Cook, Jennifer Hobday, Dave H. Huntley, Erin K. O'Brien, Andrew J. Stumpf and Gordon Weary OPEN FILE 1997- 1Oa INTRODUCTION - - - - This paper describes selected results of a till in low-lying drift-covered regions of the northern Interior geochemical sampling program conducted in the Old Fort Plateau. For example, prior till and lake sediment Mountain map area (NTS 93 M/1) by the British geochemistry surveys in the Nechako River map ania Columbia Geological Survey as part of a comprehensive (NTS 93F) to the south were successful in delineating survey of the entire Babine copper porphyry belt. The several areas of known mineralization (Cook et al., 1995; results of complimentary lake sediment geochemistry ad Levson and Giles, 1997) and in revealing locations of new bedrock geology mapping progms are presented by Cook mineralized zones. For this reason, till geochemical et al. (1997%b) and MacIntyre et al. (1997%b in pocket), studies in the Babine porphyry belt have been conducted in respectively. -
KR/KL Burbot Conservation Strategy
January 2005 Citation: KVRI Burbot Committee. 2005. Kootenai River/Kootenay Lake Conservation Strategy. Prepared by the Kootenai Tribe of Idaho with assistance from S. P. Cramer and Associates. 77 pp. plus appendices. Conservation strategies delineate reasonable actions that are believed necessary to protect, rehabilitate, and maintain species and populations that have been recognized as imperiled, but not federally listed as threatened or endangered under the US Endangered Species Act. This Strategy resulted from cooperative efforts of U.S. and Canadian Federal, Provincial, and State agencies, Native American Tribes, First Nations, local Elected Officials, Congressional and Governor’s staff, and other important resource stakeholders, including members of the Kootenai Valley Resource Initiative. This Conservation Strategy does not necessarily represent the views or the official positions or approval of all individuals or agencies involved with its formulation. This Conservation Strategy is subject to modification as dictated by new findings, changes in species status, and the completion of conservation tasks. 2 ACKNOWLEDGEMENTS The Kootenai Tribe of Idaho would like to thank the Kootenai Valley Resource Initiative (KVRI) and the KVRI Burbot Committee for their contributions to this Burbot Conservation Strategy. The Tribe also thanks the Boundary County Historical Society and the residents of Boundary County for providing local historical information provided in Appendix 2. The Tribe also thanks Ray Beamesderfer and Paul Anders of S.P. Cramer and Associates for their assistance in preparing this document. Funding was provided by the Bonneville Power Administration through the Northwest Power and Conservation Council’s Fish and Wildlife Program, and by the Idaho Congressional Delegation through a congressional appropriation administered to the Kootenai Tribe by the Department of Interior. -
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. -
Ethnohistory of the Kootenai Indians
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1983 Ethnohistory of the Kootenai Indians Cynthia J. Manning The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Manning, Cynthia J., "Ethnohistory of the Kootenai Indians" (1983). Graduate Student Theses, Dissertations, & Professional Papers. 5855. https://scholarworks.umt.edu/etd/5855 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1976 Th is is an unpublished m a n u s c r ip t in w h ic h c o p y r ig h t su b s i s t s . Any further r e p r in t in g of it s c o n ten ts must be a ppro ved BY THE AUTHOR. MANSFIELD L ib r a r y Un iv e r s it y of Montana D a te : 1 9 8 3 AN ETHNOHISTORY OF THE KOOTENAI INDIANS By Cynthia J. Manning B.A., University of Pittsburgh, 1978 Presented in partial fu lfillm en t of the requirements for the degree of Master of Arts UNIVERSITY OF MONTANA 1983 Approved by: Chair, Board of Examiners Fan, Graduate Sch __________^ ^ c Z 3 ^ ^ 3 Date UMI Number: EP36656 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. -
Rock Art Studies: a Bibliographic Database Page 1 800 Citations: Compiled by Leigh Marymor 04/12/17
Rock Art Studies: A Bibliographic Database Page 1 800 Citations: Compiled by Leigh Marymor 04/12/17 Keywords: Peterborough, Canada. North America. Cultural Adams, Amanda Shea resource management. Conservation and preservation. 2003 Reprinted from "Measurement in Physical Geography", Visions Cast on Stone: A Stylistic Analysis of the Occasional Paper No. 3, Dept. of Geography, Trent Petroglyphs of Gabriola Island, BCMaster/s Thesis :79 pgs, University, 1974. Weathering. University of British Columbia. Cited from: LMRAA, WELLM, BCSRA. Keywords: Gabriola Island, British Columbia, Canada. North America. Stylistic analysis. Marpole Culture. Vision. Alberta Recreation and Parks Abstract: "This study explores the stylistic variability and n.d. underlying cohesion of the petroglyphs sites located on Writing-On-Stone Provincial ParkTourist Brochure, Alberta Gabriola Island, British Columbia, a southern Gulf Island in Recreation and Parks. the Gulf of Georgia region of the Northwest Coast (North America). I view the petroglyphs as an inter-related body of Keywords: WRITING-ON-STONE PROVINCIAL PARK, ancient imagery and deliberately move away from (historical ALBERTA, CANADA. North America. "THE BATTLE and widespread) attempts at large regional syntheses of 'rock SCENE" PETROGLYPH SITE INSERT INCLUDED WITH art' and towards a study of smaller and more precise PAMPHLET. proportion. In this thesis, I propose that the majority of petroglyphs located on Gabriola Island were made in a short Cited from: RCSL. period of time, perhaps over the course of a single life (if a single, prolific specialist were responsible for most of the Allen, W.A. imagery) or, at most, over the course of a few generations 2007 (maybe a family of trained carvers). -
Link to Full Text
~ .......... ~ ~ - - -- .. ~~ -- .... ..... .., - .. - ... ...., .... IX. ADYNAMIC HESEHV01H SIMULATION MODEL-DYHESM:5 i\ 311 c. transverse and longitUdinal direction playa secondary role and only the variations) ." I in the vertical enter lhe first order balances of mass, momentum and energy. 1/ I Departures from this Stilte of horizontalisopyc'nalsare possible, but these \ tI l A DYNAMIC RESERVOIR SIl\olULATION MODEL enter only as isolated events or as \I/eak pe.!lurbatiQ.D.S. In both cases the.•net eJJ;cJ,J CI DYRESM: 5 is e~plured wi(h a parame!efizalion of their inp,ut (0 the vertical s(rUelure"iiild , ) I comparison of the model prediction and field data must thus be confined to ~ ~ .....of.............,.calm when the structure is truly one-dimensional. lorg 1mberger and John C.. Pattetsun .. ~ ,. The constraints imposed by ~uch a one-dimer.:Jional model may best be University of Western Australia quantified by defining a series of non-dimensional llUmbers. The value of the Nedlands, Western Australia Wedderburn number :) LV =.i.!!.. h (.J" I I '( 14.2 • L- '7 y(l .. n, (I) , \ ..,' I / 1. INTRODUCTION where g' is an effective reoufed gravity across the thermocline, h the depth of the mixed layer, L the basin scale, and u· the surface shear velocity, is a measure of """·".',j<}·,t-·;~·'",,,"~~,'ti The dynamic reservoir simulation model, DYRESM, is a one-dimensional the activity within the mixed layer. Spigel and Imberger (I980) have shown thah, numerical model for the prediction of temperature and salinity in small to medium for W > 00) the departure fmm one-dimensionality is minimal and for I ':I sized reservoirs and Jakes. -
The Toxicological Effects of the Mount Polley Tailings Impoundment Breach on Freshwater Amphipods
THE TOXICOLOGICAL EFFECTS OF THE MOUNT POLLEY TAILINGS IMPOUNDMENT BREACH ON FRESHWATER AMPHIPODS RAEGAN D. PLOMP Bachelor of Science, University of Lethbridge, 2017 A thesis submitted in partial fulfilment of the requirements for the degree of MASTER OF SCIENCE in BIOLOGICAL SCIENCES Department of Biological Sciences University of Lethbridge LETHBRIDGE, ALBERTA, CANADA © Raegan Plomp, 2019 THE TOXICOLOGICAL EFFECTS OF THE MOUNT POLLEY TAILINGS IMPOUNDMENT BREACH ON FRESHWATER AMPHIPODS RAEGAN D. PLOMP Date of Defence: September 6, 2019 Dr. G. Pyle Professor Ph.D. Supervisor Dr. S. Wiseman Associate Professor Ph.D. Thesis Examination Committee Member Dr. R. Laird Associate Professor Ph.D. Thesis Examination Committee Member Dr. Laura Chasmer Assistant Professor Ph.D. Internal External Examiner Department of Geography Dr. T. Russell Associate Professor Ph.D. Chair, Thesis Examination Committee ii Abstract The bioavailability and toxicity of metals to amphipods is influenced by exposure route and co-toxic mechanisms. Metal bioavailability was studied in amphipods at sites affected by the 2014 Mount Polley Mining Corporation tailings impoundment breach. The area around the lake was also subjected to wildfire in 2017. Bioavailability was more correlated with sediment than waterborne metal concentrations with Cu correlating well with distance from the breach. Copper-sediment bioavailability to amphipods in combination with wildfire runoff was studied resulting in non-additive toxicity. Hyalella azteca exposed to Cu-enriched sediment with fire extract (FE) experienced a more-than- additive effect on survival and amphipod whole-body Cu concentration but no significant reduction in growth or acetylcholinesterase activity compared to the Cu-contaminated sediment or FE alone, respectively. -
British Columbia Vegetation and Climate History with Focus on 6 Ka BP
Document generated on 10/01/2021 4:51 p.m. Géographie physique et Quaternaire British Columbia Vegetation and Climate History with Focus on 6 ka BP Histoire du climat et de la végétation de la Colombie-Britannique, notamment de la période de 6 ka BP Geschichte der Vegetation und des Klimas in British Columbia während des Holozäns, besonders um 6 ka v.u.Z. Richard J. Hebda La paléogéographie et la paléoécologie d’il y a 6000 ans BP au Canada Article abstract Paleogeography and Paleoecology of 6000 yr BP in Canada British Columbia Holocene vegetation and climate is reconstructed from pollen Volume 49, Number 1, 1995 records. A coastal Pinus contorta paleobiome developed after glacier retreat under cool and probably dry climate. Cool moist forests involving Picea, Abies, URI: https://id.erudit.org/iderudit/033030ar Tsuga spp., and Pinus followed until the early Holocene. Pseudotsuga menziesii DOI: https://doi.org/10.7202/033030ar arrived and spread in the south 10 000-9000 BP, and Picea sitchensis - Tsuga heterophylla forests developed in the north. T. heterophylla increased 7500-7000 BP, and Cupressaceae expanded 5000-4000 BP. Bogs began to See table of contents develop and expland. Modern vegetation arose 4000-2000 BP. There were early Holocene grass and Artemisia communities at mid-elevations and pine stands at high elevations in southern interior B.C. Forests expanded downslope and Publisher(s) lakes formed 8500-7000 BP. Modern forests arose 4500-4000 BP while lower and upper tree lines declined. In northern B.C. non-arboreal communities Les Presses de l'Université de Montréal preceded middle Holocene Picea forests. -
Seton Ridge Trail
Code: GC3QN9X Rails & Trails Written and Researched by Wayne Robinson Seton Ridge Trail Site Identification Nearest Community: Lillooet, B.C. Geocache Location: N 50°38.913' W 122°07.020' Ownership: Crown Land Accuracy: Photo: Wayne Robinson 5 meters Overall Difficulty: 3 Overall Terrain: 4.5 Access Information and Seton Ridge follows the height of the land with dizzyingly Restrictions: steep drops of nearly 1600 meters to either side. Seton From the Mile 0 cairn on Main Street follow Hwy 99 South on the Duffey Ridge is the eastern terminus of the Cayoosh Ranges of the Lake Road for 19.5 km and turn right Coast Mountains of British Columbia. To the north of the on Seton Ridge Forstery Service Road. trail is Seton Lake and to the south, the Cayoosh Creek Cross the bridge over Cayoosh Creek, valley. Cayoosh Creek originates just west of Duffy Lake and continue on about 6 km to flat area on the left. Trail is adequately marked in Cayoosh Pass, close to Lillooet Lake. Seton Lake is with flagging tape. 4x4 with high classified as a freshwater fjord that drains to the east into clearance. Cayoosh Creek which is referred to as the Seton River in the BC Freshwater Fishing Regulations. Seton Lake’s Parking Advice: actual depth is not entirely known but is known to exceed Park in pull out. Trail starts to your left. 500 meters. Although it is called a lake, Seton is a reservoir; the eastern end was dammed as a part of the Bridge River Power complex that was completed in 1960. -
Carrier Sekani Tribal Council Aboriginal Interests & Use Study On
Carrier Sekani Tribal Council Aboriginal Interests & Use Study on the Enbridge Gateway Pipeline An Assessment of the Impacts of the Proposed Enbridge Gateway Pipeline on the Carrier Sekani First Nations May 2006 Carrier Sekani Tribal Council i Aboriginal Interests & Use Study on the Proposed Gateway Pipeline ACKNOWLEDGEMENTS The Carrier Sekani Tribal Council Aboriginal Interests & Use Study was carried out under the direction of, and by many members of the Carrier Sekani First Nations. This work was possible because of the many people who have over the years established the written records of the history, territories, and governance of the Carrier Sekani. Without this foundation, this study would have been difficult if not impossible. This study involved many community members in various capacities including: Community Coordinators/Liaisons Ryan Tibbetts, Burns Lake Band Bev Ketlo, Nadleh Whut’en First Nation Sara Sam, Nak’azdli First Nation Rosa McIntosh, Saik’uz First Nation Bev Bird & Ron Winser, Tl’azt’en Nation Michael Teegee & Terry Teegee, Takla Lake First Nation Viola Turner, Wet’suwet’en First Nation Elders, Trapline & Keyoh Holders Interviewed Dick A’huille, Nak’azdli First Nation Moise and Mary Antwoine, Saik’uz First Nation George George, Sr. Nadleh Whut’en First Nation Rita George, Wet’suwet’en First Nation Patrick Isaac, Wet’suwet’en First Nation Peter John, Burns Lake Band Alma Larson, Wet’suwet’en First Nation Betsy and Carl Leon, Nak’azdli First Nation Bernadette McQuarry, Nadleh Whut’en First Nation Aileen Prince, Nak’azdli First Nation Donald Prince, Nak’azdli First Nation Guy Prince, Nak’azdli First Nation Vince Prince, Nak’azdli First Nation Kenny Sam, Burns Lake Band Lillian Sam, Nak’azdli First Nation Ruth Tibbetts, Burns Lake Band Ryan Tibbetts, Burns Lake Band Joseph Tom, Wet’suwet’en First Nation Translation services provided by Lillian Morris, Wet’suwet’en First Nation. -
FANR Booklet November 2020
LAKE BABINE NATION Foundation Agreement & Natural Resources Team Update November 2020 Team Updates… Lake Babine Nation Natural Resources Portfolio Verna Power Foundation Agreement Implementation Project Manager Verna Power & Betty Patrick Referral Officer Georgina West Natural Resource Sector Liaison Officer Murphy Patrick Sr. Lake Babine Nation Forestry Services Ltd. Operations Manager Duane Crouse Labour Market Strategy Project Evelyn George Governance Research Team Darcy Dennis, Marvin Williams, Barbara Adam-Williams & Dr. Alan Hanna Indigenous Skills Training Development (ISTD) BC Ministry of Advanced Education Deanna Brown-Nolan Verna Power Natural Resources Portfolio Exploration and Mining in Lake Babine Nation Territory Greetings and Blessings to the community and citizens of Old Fort who I represent at the Council table. First of all I would like to send prayers to those that have lost a loved one, those that may be dealing with health issues and ask the Lord to bless the entire Nation. It has been a full and busy year even with the pandemic, which is priority for Lake Babine as the safety and wellness of all member is important to us. You will notice the Foundation update that was submitted as a team providing information on the recently signed Foundation Agreement, in addition to the Foundation work LBN has continued to work on other Natural Resource developments. I am happy to report that LBN has finally recruited a Director for Natural Resources and will be introduced at the AGA. There is also a briefing that gives a summary of the mining and exploration development that is happening within the territory. Major resource development projects require approval from BC through an environmental assessment (“EA”) in order to happen.