DOCSLIB.ORG

N Tbcresearchcorporatio N

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
N Tbcresearchcorporatio N Talc Creek Project New Westminster Mining Division NTS 092H12 Project Area Location: UTM NAD 83: Zone 10, 594000 East, 5486000 North Registered Owner: Doug Warkentin Operator: Crucible Resources Ltd. Talc Creek North Area - Geochemical Sampling Report Project Tenure Numbers: 951349, 1017635, 1017637, 1019961 SOW Event Numbers: 5506605, 5523073 September 18, 2014 Prepared By: Doug Warkentin, P.Eng Page 2 TABLE OF CONTENTS Introduction ……..………….3 Location and Access ……….………..3 Tenure Information ……….………..3 Regional Geology ….……..………6 Local Geology …………..…….8 Property History ……………...…8 Summary of Work …………..….…9 Work Program ………………...9 Sampling and Data Collection ……….……......9 Interpretation of Results ……….……….11 References …………….….11 Author’s Qualifications …………….….12 Statement of Costs …………….….13 FIGURES 1 Talc Creek Project Location Map ……..………….4 2 Project Tenure Outline ………..……….5 3 Regional Geology, Talc and Cogburn Creek Area ………..……….7 TABLES 1 Talc Creek Project Mineral Tenures ……..………….6 2 Rock Sample Analytical Results ……………..…10 Appendix 1 – Sample Location Map Appendix 2 – Assay Reports Page 3 Introduction Location and Access The Talc Creek property lies in the Southern Lillooet Ranges of the Coast Mountains, approximately 25 km north northeast of the community of Harrison Hot Springs, on the east side of Harrison Lake. The general project location is shown in Figure 1. Access to the property is via forestry roads from Harrison Hot Springs. From the town, located at the south end of Harrison Lake, the East Harrison Forest Service Road (FSR) provides two wheel drive access north along the lake to the Bear Creek logging camp at the mouth of Cogburn Creek. In the Cogburn Creek area, secondary logging roads connect with the East Harrison FSR. Two of these roads access the Talc Creek property, on the north and south sides of the creek. Both roads originate from the East Harrison road just to the south of the Cogburn Creek crossing. Both of these roads are gated and the south road is currently in active use, with good four wheel drive conditions to the property area and beyond. The north Talc Creek road is also in active use and in good condition in its lower sections, but deteriorates to rough high-clearance four-wheel drive condition before reaching the property area. The boundaries of the Talc Creek property lie almost entirely within the steep-sloped Talc Creek Valley, with the exception of a small eastern extension that crosses the ridge into the neighbouring Settler Creek watershed. Old logging roads traverse the hillside almost to the crest in the southeast, but these roads are not active and the current condition is unknown. Outside of recent logging cuts, the property is heavily forested with second growth timber. Tenure Information The Talc Creek project area is part of the larger Talc-Zacta Project, which consists of three separate small claim blocks in the area of Talc and Cogburn Creeks. The Talc Creek block is the largest and consists of four MTO claims with a total area of 524 hectares. The four Talc Creek claims form a contiguous block stretching across the Talc Creek Valley, beginning about 2 km upstream from the confluence with Cogburn Creek. The claims are all owned by the author, and Crucible Resources Ltd. has an option to acquire 100% ownership of these claims. Details of the Talc Creek claims are shown in Table 1. Expiry dates shown in this table reflect the application of the work described in this report. There are no known underlying crown grants in the area and the closest legacy claims lie a short distance to the south and west. Figure 2 outlines the tenures of the Talc Creek project area. Page 4 TalcTalc CreekCreek ProjectProject MapMapMap Center:Center:Center: 54.4781N54.4781N54.4781N 124.7082W124.7082W124.7082W Map Center: 54.4781N 124.7082W Figure 1 – Talc Creek Project Location Map Page 5 AL PAL JASON HARRISON LAKE ASBESTOS 10176351017635 10176371017637 092H.052 951349951349 10199611019961 OX HOPE EMORY ZONE COGBURN 092H.042 MapMapMap Center:Center:Center: 49.5260N49.5260N49.5260N 121.7097W121.7097W121.7097W Figure 2 – Project Tenure Outline Page 6 Table 1: Talc Creek Project Mineral Tenures Tenure Number Claim Name Owner Issue Date Good To Date Area (ha) 951349 TALC CREEK 145582 (100%) 2012/feb/21 2015/feb/03 377.4 1017635 TALC N 145582 (100%) 2013/mar/08 2015/feb/03 62.9 1017637 TALC N1 145582 (100%) 2013/mar/08 2015/feb/03 21.0 1019961 TALC NE 145582 (100%) 2013/jun/01 2015/feb/03 62.9 Total Area 524.2 Regional Geology The Talc Creek Property lies near what is interpreted as the eastern margin of the Wrangellia Terrane, near its contact with the Bridge River Terrane. The area also occupies the eastern margins of the Coast Plutonic Complex. The property lies entirely to the west of the Fraser River fault system. In this area large bodies of metamorphic rocks are intruded by plutonic quartz diorites and granodiorites. Trending in a northwest – southeast direction is a broad assemblage of older rocks including mafic to ultramafic intrusive, schists and diorites (Figure 3). These rocks, and particularly the ultramafic units, are sometimes referred to as the Hope Nickel Belt. The Hope Nickel Belt is host to both massive and disseminated nickel or copper-nickel, mineralization associated with ultramafic rocks. Known nickel occurrences include the Giant Mascot Mine, which historically was the largest nickel producer in BC, along with less developed prospects such as Star of Emory, Cogburn, Jason and Big Nic. The ultramafic rocks can include significant bodies of peridotite, serpentinite and other ultramafic rocks carrying high levels of magnesium, such as the Emory Zone in the southwest part of the belt. To the southeast the belt is more altered and affected by the large scale quartz diorite intrusions of the Spuzzum Pluton. The main ultramafic body at the southeast end of the Hope Nickel Belt, which hosts the Giant Mascot nickel mine is referred to as the Pacific Nickel Complex and is the most well defined portion of the belt. The rocks of the Pacific Nickel Complex form an irregular stock-like mass up to 3 kilometres across. The body includes areas of gabbro and hornblendite along with smaller sections of peridotite and dunite that hosted ore bodies of both massive and semi-disseminated sulphide mineralization. Sulphide mineralization consisted mainly of chalcopyrite and pentlandite with pyrrhotite. The northeastern half of the stock consists of barren pyroxenites and peridotites with little hornblende, while the southwestern half of the stock is a highly variable, hornblende-rich assemblage of mineralized peridotites and pyroxenites that contains seventeen orebodies of various sizes associated with the mine. These orebodies occur along a line trending about 285 degrees and many do not outcrop, being discovered through underground exploration and development. Smaller mineralized bodies of hornblende- pyroxenite and peridotite have also been discovered further to the west, including the Star of Emory, an ore body with zones of massive pyrrhotite, chalcopyrite and pentlandite. The northwestern portion of the Hope Nickel Belt trends in a northwest-southeast direction and is bounded on both sides mainly by younger metamorphic rocks, including the Slollicum Schist package to the southwest. To the north and east there are also substantial areas underlain by intrusives of the Coast Plutonic Complex. There are also some more recent smaller granodiorite intrusives to the north and in the central part of the mafic belt. Within the belt, in addition to the large ultramafic bodies, the Cogburn Schist occupies a Central position. To the north of Page 7 Cogburn Creek, and near the Zacta claim block, this unit is known to contain VMS style massive sulphide mineralization at the North Fork prospect. On the northeast side of the Cogburn Schist, intrusive rocks grade from diorite to Gabbro, with the bodies of ultramafic rocks tending to occur along the outside flanks of the belt, although smaller fingers and lenses of ultramafic rocks also occur within the schist. Mineralization associated with smaller mafic and ultramafic bodies has also been identified within the younger plutonic rocks on the northeast side of the belt. KTmm – Cretaceous to Tertiary – mid amphibolite/andalusite grade metamorphic rocks KTSl – Cretaceous to Tertiary Slollicum Schist – greenstone, greenschist metamorphic rocks MKgd – Mid-Cretaceous – granodioritic intrusive rocks MKqd – Mid-Cretaceous – quartz dioritic intrusive rocks OlMigd – Oligocene to Miocene – granodioritic intrusive rocks PrPzY – Proterozoic to Paleozoic Yellow Aster Complex – dioritic intrusive rocks PzMzCS – Paleozoic to Mesozoic Cogburn Schist – greenstone, greenschist metamorphic rocks PzMzum – Paleozoic to Mesozoic - ultramafic rocks Figure 3 – Regional Geology, Talc Creek and Cogburn Creek Area Page 8 Local Geology The Talc Creek claim block occupies the mid part of the Talc Creek Valley, entirely within a wide section of the Hope Nickel Belt, mainly incorporating areas mapped as being underlain by Cogburn Schist, but also covering small parts of one of the main ultramafic bodies as well as some of the adjacent mafic intrusives. Smaller zones of ultramafic rocks are known to occur within the schists on the property. Airborne magnetic data is a good indicator for ultramafic rocks in this area and available data indicate a wider extent of this type of rock than that shown in regional mapping. In the Talc Creek area there are major bodies of ultramafic rock on either side of the valley separated by schists and other mafic intrusives, including gabbro and diorite. Ultramafic units include serpentinite, pyroxenite and peridotite. Ultramafic exposures commonly contain disseminated sulphide mineralization consisting mainly of fine pyrrhotite. Work on the ultramafic body to the south of the property has also shown extensive zones of high grade magnesium, and geochemical sampling has shown areas with a unique combination of high nickel and high arsenic, together with areas of unusually high cobalt.
Load more

Recommended publications
  • Fire 2 and Fire 3 Claims, Pemberton Bc
    REPORT ON THE EXPLORATION OF THE FIRE 1- FIRE 2 AND FIRE 3 CLAIMS, PEMBERTON BC 5/3/2011 Exploration Report During April 8th to 14th a short exploration program was carried out in the Fire 1, 2 and 3 claims in order to identify the access roads, determine a basic geology and rock sampling and facilities existing in the area for future investigation. L rsuReport on the Exploration of the Fire 1- Fire 2 and Fire 3 claims, PEMBERTON BC REPORT ON THE EXPLORATION OF THE FIRE 1, FIRE 2 AND FIRE 3 CLAIMS PEMBERTON, BC, CANADA Map Center: 553.850 E, 5.515.030 N Zone 10 U Map sheet: NTS 092G16 CLAIMS NUMBER: 510817, 510819, 510820 NEW WESTMINSTER MINING DIVISION Date: April 30, 2011 For: Agnico-Eagle Mines Ltd. 400-543 Granville Street Vancouver BC V6C 1X8 By: Jose Barquet, P.Geo. , License # 34361, APEG BC Page 1 Report on the Exploration of the Fire 1- Fire 2 and Fire 3 claims, PEMBERTON BC Report on the Exploration of the Fire 1- Fire 2 and Fire 3 claims, PEMBERTON BC TABLE OF CONTENTS Summary …………………………………………………………………….. page 3 Introduction ………………………………………………………………….. 3 Location and access …………………………………………………………. 3 Mineral claims ……………………………………………………………….. 7 Regional geology ……………………………………………………………. 8 Structures …………………………………………………………………….. 13 Local Geology ……………………………………………………………….. 13 Alterations …………………………………………………………………..... 14 Mineralization ……………………………………………………………….... 15 Previous works ……………………………………………………………….... 15 Rock sampling …………………………………………………………………. 19 Conclusions …………………………………………………………………….. 20 Bibliography ………………………………………………………………….
    [Show full text]
  • Inside: Small Things Considered
    branchlines Volume 27#1 Spring 2016 Inside: Small things considered ...................10 Soil productivity in the Fraser River Delta (cover) ...............................12 The Pacific Salmon Ecology and Conservation Lab ........................14 Unseen connections ..........................18 dean’smessage forest sector, and our Forest Resources employers of the benefits of co-op is Management and Wood Products very welcome. Processing programs continue to We have just wrapped up our grow, as does demand for graduates recent campaign, which was aimed I have previously commented from these programs. With the end of at both raising funds and increasing on the diversity of research interests the school year fast approaching, I am alumni engagement. This does not within the Faculty. These cover all reminded that each year provides a mean that we can now sit back and aspects of forests and their products fresh crop of graduates who will, over relax. We particularly want to ensure and are increasingly extending beyond time, make their mark in the industry. that we can maintain, and even into other aspects of the landscape. However, today, our graduates have a increase, our alumni engagement. We are not just restricted to rural greater choice in front of them than We offer many opportunities for landscapes, and more and more work ever before, and they will not automat- engagement and are always seeking is being done on urban landscapes, ically apply for an entry-level position if out new ideas. If you feel that there is a trend that is likely to increase as it is not accompanied by a clear career something that you think we should our urban forestry program gathers path or some other form of incentive.
    [Show full text]
  • Is Diatom Richness Responding to Catchment Glaciation? a Case Study from Canadian Headwater Streams
    J. Limnol., 2012; 71(1): 72-83 DOI: 10.4081/jlimnol.2012.e7 Is diatom richness responding to catchment glaciation? A case study from Canadian headwater streams Doris GESIERICH*, and Eugen ROTT Institute of Botany, University of Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria *Corresponding author: [email protected] ABSTRACT Due to global change affecting glaciers worldwide, glacial streams are seen as threatened environments deserving specific scientific interest. Glacial streams from the Coast Range and Rocky Mountains in British Columbia and at the border to Alberta were investigated. In particular glacial streams and downstream sites in the Joffré Lakes Provincial Park, a near by mountain river and two large glacial streams in the Rocky Mountains (Kootenay Range, Jasper National Park) were studied. Regardless of a high variability of catchment glaciation (1 to 99%) thin organic biofilms with firmly attached diatom frustules of the genera Achnanthidium, Psammothidium, En- cyonema, Gomphonema and fragilaroid taxa were found in all cases. In spite of fundamentally different geological conditions between the Coast Range sites and the Rocky Mountain sites, the pioneer taxon Achnanthidium minutissimum (with a slimy long ecomorph) was dominating quantitatively in most of the glacier stream samples together with the rheobiontic Hannaea arcus. Individual glacier stream samples were characterized by the dominance of Achnanthidium petersenii and Gomphonema calcifugum/Encyonema latens. The diatom community analysis (cluster analysis) revealed the expected separation of glacier stream sites and sites of the lower segments of the river continuum (e.g., dominance of Diatoma ehrenbergii in the mountain river). In the Joffré area, the total species richness of turbid glacial streams close to the glacier mouth was significantly lower than in the more distant sites.
    [Show full text]
  • Cayoosh Goat Survey Report 2008
    Cayoosh Range Mountain goat survey in the Cayoosh area, management unit 3-16, Thompson region, British Columbia, July 2008 Prepared for: Doug Jury British Columbia Ministry of Environment Thompson Region 1259 Dalhousie Drive Kamloops, BC V2C 5Z5 Prepared by: Kim G. Poole Aurora Wildlife Research 2305 Annable Road, Nelson BC V1L 6K4 Tele. (250) 825-4063; e-mail: [email protected] September 2008 Cayoosh mountain goat survey, July 2008 ii ABSTRACT Mountain goats (Oreamnos americanus) are managed as a big game species in British Columbia, and as such aerial surveys are conducted periodically to document population trend and productivity, and to establish hunting quotas. As a result of suspected declines in the population and a 10-year gap since the last survey, a survey was conducted to determine the numbers and distribution of goats in subzones 3- 16B, C, D, E and F in the Pacific and Lillooet ranges of the Coast Mountains southwest of Lillooet, southeastern British Columbia, in July 2008. Standard survey techniques were followed using a Bell 206B helicopter. We used 18.4 hrs of helicopter time, including 15.7 hrs on survey, and surveyed a 675-km2 census zone of potential goat habitat under good survey conditions. Overall survey effort averaged 1.4 min/km2. We observed 210 goats (150 adults, 60 kids) in 56 groups. Kids comprised 29% of total goats (40 kids:100 adults [non-kids]). Groups were distributed from 5,400 to 8,100 feet (1,650–2,470 m) elevation. I applied a sightability correction factor of 60% to derive an estimate of 350 goats for the census zone within the 5 subzones (density of 0.52 goats/km2).
    [Show full text]
  • Prepared For
    Volume 5D, ESA – Trans Mountain Pipeline ULC Socio-Economic Technical Reports Trans Mountain Expansion Project Traditional Land and Resource Use Technical Report Gathering Places Aseniwuche Winewak Nation community members did not identify any gathering places during the TLU for the Project. No mitigation was requested for gathering places by Aseniwuche Winewak Nation. Sacred Sites Aseniwuche Winewak Nation community members did not identify specific sacred sites during the TLU for the Project. Community members explained that the Hinton area is culturally important and presently used by Aseniwuche Winewak Nation community members, whereas the Valemount area is also culturally important, but not currently used. Community members did not expect to find sacred sites during ground reconnaissance due to extensive industrial development in Hinton and surrounding areas (Aseniwuche Environmental Corporation 2013). Aseniwuche Winewak Nation requested notification if culturally relevant sites are found during Project construction and that the sites are protected by a 100 m buffer. 5.2 Hargreaves to Darfield Segment The results of TLU studies conducted to date have identified TLU sites potentially affected by the Hargreaves to Darfield segment and associated Project components requiring mitigation. 5.2.1 Lheidli T’enneh Lheidli T’enneh elected to conduct a third-party TLU study for the Project. A third-party consultant, Chignecto Consulting Group conducted a map review, community interviews and ground reconnaissance that focused on Crown lands within the asserted traditional territory of Lheidli T’enneh. The findings of the TLU study have not been reviewed or approved by Lheidli T’enneh Chief and Council or community. The interim report is considered draft and any changes resulting from review with the Lheidli T’enneh community will be incorporated into the final report.
    [Show full text]
  • Emory Creek Nickel Project
    Emory Creek Nickel Project Claim ID Numbers: 845260, 848432 New Westminster Mining Division NTS 092H05 Project Area Location: UTM NAD 83: Zone 10, 605000 East, 5481000 North Registered Owner: Doug Warkentin Operator: Crucible Resources Ltd. Upper Emory Area - Exploration and Geochemical Sampling Report July 19, 2012 Prepared By: Doug Warkentin, P.Eng Page 2 TABLE OF CONTENTS Introduction ……..………….3 Location and Access ……….………..3 Tenure Information ……….………..3 Regional Geology ….……..………6 Local Geology …………..…….6 Property History ……………..….8 Summary of Work …………..….…9 Work Program …………..……10 Sampling and Data Collection ……….……....10 Interpretation of Results ……….……….11 References …………….….11 Author’s Qualifications …………….….13 Statement of Costs …………….….14 FIGURES 1 Emory Creek Nickel Project Location Map ……..………….4 2 Project Tenure Outline ………..……….5 3 Regional Geology ………..……….7 4 Airborne Magnetic Images ………………...8 TABLES 1 Emory Creek Nickel Project Mineral Tenures ……..………….5 2 Rock Sample Analytical Results ……………..…10 Appendix 1 – Sample Location Maps Appendix 2 – Assay Reports CRUCIBLE RESOURCES LIMITED Page 3 Introduction Location and Access The Emory Creek property lies in the Southern Lillooet Ranges of the Coast Mountains, approximately 12 km northwest of Hope, BC and 10 km west of the community of Dogwood Valley on the Trans Canada Highway. The general project location is shown in Figure 1. The south eastern portion of the property has limited four wheel drive or ATV access along BC Hydro power line access roads and old logging roads in the upper Emory Creek valley. While some of these roads are in good condition, the original access along the lower part of Emory Creek from the Trans Canada Highway has been cut off by landslides, requiring access from Stulkawhits Creek to the south along a north-south BC Hydro access corridor that connects to the old Emory Creek Road from BC Nickel Mine Road.
    [Show full text]
  • Nd ISOTOPIC SIGNATURES AN]) STRATIGRAPIIIC CORRELATIONS: EXAMPLES from WESTERN PACIFIC MARGINAL BASINS and MIDDLE JURASSIC ROCKS of the SOUTHERN CANADIAN CORDILLERA
    Nd ISOTOPIC SIGNATURES AN]) STRATIGRAPIIIC CORRELATIONS: EXAMPLES FROM WESTERN PACIFIC MARGINAL BASINS AND MIDDLE JURASSIC ROCKS OF THE SOUTHERN CANADIAN CORDILLERA by J. Brian Mahoney B.S., University of Wisconsin-Madison, 1983 M.S., Idaho State University, 1987 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES DEPARTMENT OF GEOLOGICAL SCIENCES We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA August, 1994 © J. Brian Mahoney, 1994 ______________________________ In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of Bntish Columbia, I agree that the Ubrary 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 or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. (Signature Department of éZ)Lc2tcr <_tG’CL The University of British Columbia Vancouver, Canada ci Date ‘‘ U ‘ld?,EYL DE-6 (2/88) ABSTRACT The purpose of this investigation is twofold: 1) to evaluate the applicability of Nd and Sr isotopic analyses of fine grained clastic sediments to basin analysis and stratigraphic correlation; and 2) to document the lithostratigraphic, biostratigraphic, geochemical and isotopic characteristics of Lower to Middle Jurassic strata in tectonostratigraphic terranes of the southern Canadian Cordillera in order to evaluate potential terrane linkages. Isotopic analyses of Neogene strata from three western Pacific marginal basins (Shikoku Basin, Sea of Japan, Sulu Sea) permit evaluation of isotopic analyses to basin discrimination and stratigraphic correlation.
    [Show full text]
  • Th* Varsity Outdoor Qub \ Journal
    Th* Varsity Outdoor Qub \ Journal i VOLUME XXIV 1981 ISSN 0524-5613 Vancouver, Canada 7Ae Umveuibj of IkitUh Columbia PRESIDENT'S MESSAGE March, 1982 Another school year has passed and so have many memorable moments in the V.O.C. This year was a good one for the V.O.C. We have seen our membership grow to a recent high of over 250. For many, the club has opened up a whole new world of adventure and challenge. For others, the club has continued to be a central part of their lives adding new memories and aspirations. The success of our club has always been in the strength of our active members. This year, again, active members gave their time unselfishly to such things as leading trips, cabin committee meetings and social functions, not to mention many others. It is these people I would like to thank most for making my job, as President, that much more enjoyable. For those of you who have participated in club activities for the first time, I urge you to take an active part in helping to run the club. I am sure you will find that the rewards far exceed the time and effort involved. As a club whose major interests lie in the outdoors, I feel we as a membership have helped people become more aware of what is beyond the campus of U.B.C. British Columbia offers a wealth of wilderness which is accessible to everyone. It is important that as a club we continue to pass on our knowledge about outdoor activities and wilderness areas.
    [Show full text]
  • Description of Non-Commercial Winter Recreation Zones
    Descriptions of Non-Commercial Winter Recreation Zones Sea-to-Sky Land and Resource Management Plan The information contained in this document is from the report “Recommendations for Management of Winter Backcountry Recreation in the Lillooet River Drainage and the Sea-to Sky LRMP Area – Appendix A” (Gordon Erlandson, 2008), with minor revisions to ensure direction is consistent and accurate with LRMP zoning. The management direction referenced is not policy, but rather provides advice and guidance for the management of the non-commercial winter recreation zones established in the Sea-to-Sky Land and Resource Management Plan (S2S LRMP) amendment, Section 4.4.3, Map 15A. Commercial recreation management direction for the Squamish Nation Land Use Agreement area is established in Appendix 5 of the S2S LRMP. Should there be any discrepancies in references to commercial recreation between this document and Appendix 5, then please refer to the latter. The non-commercial winter recreation zones in the S2S LRMP area are: Non-motorized use (RA1) Self propelled activities that do not rely on a motorized vehicle for access or recreation use within a designated zone. Acceptable Uses / Activities: Existing motorized and / or non-motorized commercial recreation uses and activities are acceptable if present. Backcountry skiing, ski touring / mountaineering, cross-country / Nordic skiing, dog- sledding, snowshoeing Non-motorized transport only. New non-motorized uses may be considered. Non-motorized use with air access (RA1-A) Self propelled activities that do not rely on a motorized vehicle for recreation use within a designated zone. Acceptable Uses / Activities: Same uses as RA1, but aerial transport is allowed for drop off / pick-up of day use or multi-day recreation users.
    [Show full text]
  • 199503-85.Pdf
    1985 ANNUAL REVIEW OF ACTIVITIES Institute of Ocean Sciences Institute of Ocean Sciences, Patricia Bay 1985 ANNUAL ItEVIEW OF ACTIVITIES Institute of Ocean Sciences PATRICIA BAY, SIDNEY, B.C. .... I Government Gouvernement ".... of Canada du Canada Fs 1-26/1985 ISBN 0-662-14796-0 For additional copies or further information, please write to: Department of Fisheries and Oceans Institute of Ocean Sciences p.o. Box 6000 Sidney, British Columbia, Canada V8L 4B2 Contents DEPARTMENT OF FISHERIES AND OCEANS 7 Director-General's Foreword 9 Hydrography 11 Field Hydrography 13 Chart Production and Distribution 15 Tidal and Current Surveys 18 Engineering Services 20 Oceanography 25 Ocean Physics 27 Fjords and Channels 27 Straits 27 Continental Shelf 28 Deep Sea 30 Forecasting 30 Processes 31 Observational Techniques 31 Computing Services 33 Ocean Chemistry 34 Pollution Research 35 Climate Studies 39 Chemical Traces of Water Masses 42 Ocean Ecology 42 Plankton 42 Benthos 46 Ocean Information 49 Climatology 51 Environmental Advisory Services 52 Information Management 53 Public Information 55 Ships 57 Management Services 63 DEPARTMENT OF ENVIRONMENT 67 Atmospheric Environment Service 69 Canadian Wildlife Service 73 DEPARTMENT OF ENERGY, MINES AND RESOURCES 7S Earth Physics Branch and Geological Survey of Canada 77 Director's Foreword 77 Marine Sedimentology 78 Marine Geology- Bedrock Geological Studies 82 Palaeontology 8S Multiparameter - Geophysical Surveys 86 Juan de Fuca Ridge and Offshore Mapping 87 International Ocean Drilling Project 88 Seismological Service 89 Gravity 92 Geothermal Studies 93 Geomagnetism 9S Geodynamics 98 Boundary Studies 100 Technical Support 100 APPENDICES I. Contracts 103 II. Publications 109 III. Permanent Staff 120 DEPARTMENT OF FISHERIES AND OCEANS 7 Director-General's Foreword In October of this year, Mike Bolton retired as Director of the Pacific Region of the Canadian Hydrographic Service located at the Institute of Ocean Sciences (IOS).
    [Show full text]
  • Glaciers of North America— GLACIERS of CANADA
    Glaciers of North America— GLACIERS OF CANADA HISTORY OF GLACIER INVESTIGATIONS IN CANADA By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The earliest recorded description of a Canadian glacier was in 1861. Since that time, various glaciological investigations have been conducted in the several glacierized regions of Canada (for example, Coast Mountains, Interior Ranges, Rocky Mountains, and Arctic Islands), including mass balance, modeling, dendrochronology, climatology, ice chemistry and physics, ice-core analyses, glacier-surge mechanics, and airborne and satellite remote sensing CONTENTS Page Abstract ------------------------------------------------------------------------------ J27 Occurrence of Glaciers----------------------------------------------------------- 27 FIGURE 1. Index map of the glaciers of western Canada -------------------- 29 2. Index map of the glaciers of arctic and eastern Canada---------- 34 TABLE 1. Summary of historical information on glaciers of western Canada --------------------------------------------------------- 30 2. Summary of historical information on glaciers of arctic and eastern Canada ------------------------------------------------- 32 3. The glacierized areas of Canada --------------------------------- 35 Observation of Glaciers ---------------------------------------------------------- 35 Historic (Prior to World War II) ------------------------------------------
    [Show full text]
  • British Columbia – VE7)
    Summits on the Air Canada (British Columbia – VE7) Association Reference Manual Document Reference S61.1 Issue number 1.6 Date of issue 01-Apr-2018 Participation start date 01-Nov-2010 Authorised Date: 01-Apr-2018 obo SOTA Management Team Association Manager Nathon Hall VE7ETS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Summits on the Air – ARM for Canada (British Columbia – VE7) Table of Contents 1 ASSOCIATION REFERENCE DATA................................................................................. 6 1.1 PROGRAM DERIVATION ..................................................................................................................... 8 1.2 GENERAL INFORMATION ................................................................................................................... 8 1.3 FINAL ASCENT AND ACTIVATION ZONE ............................................ ERROR! BOOKMARK NOT DEFINED. 1.4 RIGHTS OF WAY AND ACCESS ISSUES ................................................................................................ 9 1.5 MAPS AND NAVIGATION .................................................................................................................... 9 1.6 SAFETY CONSIDERATIONS .............................................................................................................. 10 1.7
    [Show full text]