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Electoral Area Directors Committee Agenda October 9, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood Street, Pemberton, BC
Electoral Area Directors Committee Agenda October 9, 2019; 10:30 AM Pemberton Community Church - Meeting Room 7420 Dogwood Street, Pemberton, BC Item Item of Business and Page Number Page 1. Call to Order We would like to recognize that this meeting is being held on the Traditional Territory of the Líl’wat Nation. 2. Approval of Agenda 3. Electoral Area Directors Committee Closed Meeting THAT the Committee close the meeting to the public under the authority of Section 90(1)() of the Community Charter. 4. Rise & Report from the Closed Electoral Area Directors Committee Meeting 5. Consent Agenda (Voting rule on each item may vary; unanimous vote required) Items appearing on the consent agenda which present a conflict of interest for Committee Members must be removed from the Consent Agenda and considered separately. Any items to be debated or voted against must be removed from the Consent Agenda and considered separately. THAT the resolutions set out in the Consent Agenda be approved, and those Consent Agenda items which do not have resolutions related thereto be received. 5.1 Approval and Receipt of Minutes 5.1.1. Electoral Area Directors Committee Meeting Draft 5 - 11 Minutes of September 5, 2019 THAT the Electoral Area Directors Committee Meeting Minutes of September 5, 2019 be approved as circulated. 5.2 Staff Reports & Other Business 5.2.1. September 2019 Select Funds Report 12 - 16 THAT the following resolution of the September 5, 2019 Electoral Area Directors Committee meeting with respect Item Item of Business and Page Number Page -
Radiogenic Age and Isotopic Studies: Report 3
GSCAN-P—89-2 CA9200982 GEOLOGICAL SURVEY OF CANADA PAPER 89-2 RADIOGENIC AGE AND ISOTOPIC STUDIES: REPORT 3 1990 Entity, Mtnat and Cnargi*, Mint* M n**ouroaa Canada ftoaioweat Canada CanadS '•if S ( >* >f->( f STAFF, GEOCHRONOLOGY SECTION: GEOLOGICAL SURVEY OF CANADA Research Scientists: Otto van Breemen J. Chris Roddick Randall R. Parrish James K. Mortensen Post-Doctoral Fellows: Francis 6. Dudas Hrnst Hegncr Visiting Scientist: Mary Lou Bevier Professional Scientists: W. Dale L<neridj:e Robert W. Sullivan Patricia A. Hunt Reginald J. Theriaul! Jack L. Macrae Technical Staff: Klaus Suntowski Jean-Claude Bisson Dianne Bellerive Fred B. Quigg Rejean J.G. Segun Sample crushing and preliminary mineral separation arc done by the Mineralogy Section GEOLOGICAL SURVEY OF CANADA PAPER 89-2 RADIOGENIC AGE AND ISOTOPIC STUDIES: REPORT 3 1990 ° Minister of Supply and Services Canada 1990 Available in Canada through authorized bookstore agents and other bookstores or by mail from Canadian Government Publishing Centre Supply and Services Canada Ottawa, Canada Kl A 0S9 and from Geological Survey of Canada offices: 601 Booth Street Ottawa, Canada Kl A 0E8 3303-33rd Street N.W., Calgary, Alberta T2L2A7 100 West Pender Street Vancouver, B.C. V6B 1R8 A deposit copy of this publication is also available for reference in public libraries across Canada Cat. No. M44-89/2E ISBN 0-660-13699-6 Price subject to change without notice Cover Description: Aerial photograph of the New Quebec Crater, a meteorite impact structure in northern Ungava Peninsula, Quebec, taken in 1985 by P.B. Robertson (GSC 204955 B-l). The diameter of the lake is about 3.4km and the view is towards the east-southeast. -
Pliocene and Pleistocene Volcanic Interaction with Cordilleran Ice Sheets, Damming of the Yukon River and Vertebrate Palaeontolo
Quaternary International xxx (2011) 1e18 Contents lists available at SciVerse ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Pliocene and Pleistocene volcanic interaction with Cordilleran ice sheets, damming of the Yukon River and vertebrate Palaeontology, Fort Selkirk Volcanic Group, west-central Yukon, Canada L.E. Jackson Jr. a,*, F.E. Nelsonb,1, C.A. Huscroftc, M. Villeneuved, R.W. Barendregtb, J.E. Storere, B.C. Wardf a Geological Survey of Canada, Natural Resources Canada, 625 Robson Street, Vancouver, BC V6B5J3, Canada b Department of Geography, University of Lethbridge, 4401 University Drive, Lethbridge, Alberta T1K 3M4, Canada c Department of Geography, Thompson Rivers University, Box 3010, 900 McGill Road, Kamloops, BC V2C 5N3, Canada d Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada e 6937 Porpoise Drive, Sechelt, BC V0N 3A4, Canada f Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, BC V2C 5N3, Canada article info abstract Article history: Neogene volcanism in the Fort Selkirk area began with eruptions in the Wolverine Creek basin ca. 4.3 Ma Available online xxx and persisted to ca. 3.0 Ma filling the ancestral Yukon River valley with at least 40 m of lava flows. Activity at the Ne Ch’e Ddhäwa eruptive center overlapped with the last stages of the Wolverine Creek eruptive centers. Hyaloclastic tuff was erupted between ca. 3.21 and 3.05 Ma. This eruption caused or was coincident with damming of Yukon River. The first demonstrable incursion of a Cordilleran ice sheet into the Fort Selkirk area was coincident with a second eruption of the Ne Ch’e Ddhäwa eruptive center ca. -
Preliminary Results of Field Mapping, Petrography, and GIS Spatial Analysis of the West Tuya Lava Field, Northwestern British Columbia
Geological Survey of Canada CURRENT RESEARCH 2005-A2 Preliminary results of field mapping, petrography, and GIS spatial analysis of the West Tuya lava field, northwestern British Columbia K. Wetherell, B. Edwards, and K. Simpson 2005 Natural Resources Ressources naturelles Canada Canada ©Her Majesty the Queen in Right of Canada 2005 ISSN 1701-4387 Catalogue No. M44-2005/A2E-PDF ISBN 0-662-41122-6 A copy of this publication is also available for reference by depository libraries across Canada through access to the Depository Services Program's website at http://dsp-psd.pwgsc.gc.ca A free digital download of this publication is available from GeoPub: http://geopub.nrcan.gc.ca/index_e.php Toll-free (Canada and U.S.A.): 1-888-252-4301 All requests for permission to reproduce this work, in whole or in part, for purposes of commercial use, resale, or redistribution shall be addressed to: Earth Sciences Sector Information Division, Room 402, 601 Booth Street, Ottawa, Ontario K1A 0E8. Authors’ addresses K. Wetherell ([email protected]) B. Edwards ([email protected]) Department of Geology Dickinson College P.O. Box 1773 Carlisle, Pennsylvania U.S.A. 17013 K. Simpson ([email protected]) 605 Robson Street, Suite 101 Vancouver, British Columbia V6B 5J3 Publication approved by GSC Pacific Original manuscript submitted: 2005-04-21 Final version approved for publication: 2005-05-26 Preliminary results of field mapping, petrography, and GIS spatial analysis of the West Tuya lava field, northwestern British Columbia K. Wetherell, B. Edwards, and K. Simpson Wetherell, K., Edwards, B., and Simpson, K., 2005: Preliminary results of field mapping, petrography, and GIS spatial analysis of the West Tuya lava field, northwestern British Columbia; Geological Survey of Canada, Current Research 2005-A2, 10 p. -
Electoral Area Directors Committee Agenda December 5, 2018; 10:30 AM Room B, Pemberton Community Centre 7390 Cottonwood St
Electoral Area Directors Committee Agenda December 5, 2018; 10:30 AM Room B, Pemberton Community Centre 7390 Cottonwood St. Pemberton, BC Item Item of Business and Page Number Page 1. Call to Order by Corporate Officer We would like to recognize that this meeting is being held on the Traditional Territory of the Líl’wat Nation. 1.1. Election of 2019 Electoral Area Directors Committee Chair 1.2. Election of 2019 Electoral Area Directors Committee Vice-Chair 2. Approval of Agenda 3. Electoral Area Directors Committee Closed Meeting THAT the Committee close the meeting to the public under the authority of Section 90() of the Community Charter. 4. Rise & Report from the Closed Electoral Area Directors Committee Meeting 5. Delegation (1:00 PM) 5.1. Mark Mendonca, President, Tourism Pemberton 4 - 11 • Request for funding of $4,000 from Area C Select Funds to match the Village of Pemberton Community Initiative & Opportunity Fund funding for a part-time marketing coordinator. • Request for support for the Economic Impact Study of Tourism in the Pemberton & District and surrounding area. 6. Consent Agenda (Voting rule on each item may vary; unanimous vote required) Items appearing on the consent agenda which present a conflict of interest for Committee Members must be removed from the Consent Agenda and considered separately. Any items to be debated or voted against must be removed from the Consent Agenda and considered separately. THAT the resolutions set out in the Consent Agenda be approved, and those Consent Agenda items which do not have resolutions related thereto be received. Item Item of Business and Page Number Page 6.1 Approval and Receipt of Minutes 6.1.1. -
USGS Open-File Report 2009-1133, V. 1.2, Table 3
Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041 -
CHAPTE,R 3 STRUCTU'w and Metamorpili!SM
Ministry of Employment and Investment CHAPTE,R3 STRUCTU'W AND METAMORPIlI!SM"- OVERVIEW rassic or Early Cretaceous deformationis also doclimented locally within the area, an by angular unconformity separat- The structure of the Taseko Bridge River areais domi- - ing the lower and upper unitsthe of Relay Mountain Group nated by a systemof northwest to north-trending faults that east of Lake. However, the extent of Jura!:sic and reflect a complex history of mid-Cretaceous to Tertiary con- Lorna Early Cretaceous deformation remains poorly undmtood. tractional, strikeslip and extensional deformation.The old- Although the Middle Jurassic has been pslulateli as the est map-scale structures include systems of mainly time of initial thrust-amalgamation ofCadwallader Terrane southwest-vergent thrust faults that have been mapped with the Bridge River andShulaps complexes (Pottf r, 1986; within several discontinuousbelts extending from the south- Rusmore et al., 1988). the present study documens struc- east comer of the map area toBig Creek. These faults are, tures of this age only in Bridgethe RiverComplex, and pro- at least in part, Cretaceous in age and are inferred to be vides no clear evidence for thrust imbrication and .lplift of broadly synchronouswith deposition of synorogenicclastic adjacent terranes until the mid-Cretaceous. rocks of the mid-Cretaceous Taylor Creek Group and Sil- verquick formation; angular unconformities beneath the Within the Taseko - Bridge River map area, i~enetra- Hauterivian unit of the Relay Mountain Group, the Albian tively deformed metamorphic rocks are restricted to the Taylor Creek Group, and the Upper Cretaceous SilverquickShulaps Range and contiguous Mission Ridge,whxe they and Powell Creek formations may relate to this protracted are represented mainly by the Bridge River schists (Potter, interval of deformation. -
Canada and Western U.S.A
Appendix B – Region 12 Country and regional profiles of volcanic hazard and risk: Canada and Western U.S.A. S.K. Brown1, R.S.J. Sparks1, K. Mee2, C. Vye-Brown2, E.Ilyinskaya2, S.F. Jenkins1, S.C. Loughlin2* 1University of Bristol, UK; 2British Geological Survey, UK, * Full contributor list available in Appendix B Full Download This download comprises the profiles for Region 12: Canada and Western U.S.A. only. For the full report and all regions see Appendix B Full Download. Page numbers reflect position in the full report. The following countries are profiled here: Region 12 Canada and Western USA Pg.491 Canada 499 USA – Contiguous States 507 Brown, S.K., Sparks, R.S.J., Mee, K., Vye-Brown, C., Ilyinskaya, E., Jenkins, S.F., and Loughlin, S.C. (2015) Country and regional profiles of volcanic hazard and risk. In: S.C. Loughlin, R.S.J. Sparks, S.K. Brown, S.F. Jenkins & C. Vye-Brown (eds) Global Volcanic Hazards and Risk, Cambridge: Cambridge University Press. This profile and the data therein should not be used in place of focussed assessments and information provided by local monitoring and research institutions. Region 12: Canada and Western USA Description Region 12: Canada and Western USA comprises volcanoes throughout Canada and the contiguous states of the USA. Country Number of volcanoes Canada 22 USA 48 Table 12.1 The countries represented in this region and the number of volcanoes. Volcanoes located on the borders between countries are included in the profiles of all countries involved. Note that countries may be represented in more than one region, as overseas territories may be widespread. -
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TITLE OF REPORT: VERITAS Assessment Report 2013 TOTAL COST: $8,247.37 AUTHOR(S): Alex BURTON P. Eng., P. Geo., Consulting Geologist SIGNATURE(S): NOTICE OF WORK PERMIT NUMBER(S)/DATE(S):N/A June 6 to July 9, 2013 STATEMENT OF WORK EVENT NUMBER(S)/DATE(S ): 5459603 2013/Jul/19 YEAR OF WORK: 2013 PROPERTY NAME: VERITAS CLAIM NAME(S) (on which work was done): 1019139 COMMODITIES SOUGHT: Gold MINERAL INVENTORY MINFILE NUMBER(S),IF KNOWN: 092 J NE 031 MINING DIVISION: Lilloet NTS / BCGS: 92 J 086 LATITUDE: _ 50 _________° _50 _________’ 30__________" LONGITUDE: _122 _________° _ 54 _________’ __ 55________" (at centre of work) UTM Zone: 10 EASTING: 506063 NORTHING: 5632098 OWNER(S): LEE Michael Richard (147295) (100%) MAILING ADDRESS: 60562 Granville Park, Vancouver, B. C. V6H 4B9 OPERATOR(S) [who paid for the work]: LEE, Michael Richard MAILING ADDRESS: 60562 Granville Park, Vancouver, B. C. V6H 4B9 REPORT KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude. Do not use abbreviations or codes ) Bridge River and Bralorne Complex with Augite diorite and Soda granite next to Veritas quartz vein in contact with Hurley Formation REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: 6971, 14390, 15209, 18436, 33415. TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT (in metric units) APPORTIONED Technical (incl. support) 375m 101939 GEOLOGICAL (scale, area) linear Ground, mapping Photo interpretation GEOPHYSICAL (line-kilometres) Ground Magnetic Electromagnetic -
Documentation of a Holocene Volcanic Cone in the Tuya-Teslin Volcanic Field, Northern British Columbia
Geological Survey of Canada CURRENT RESEARCH 2006-A1 Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia K. Simpson, B. Edwards, and K. Wetherell 2006 CURRENT RESEARCH Natural Resources Ressources naturelles Canada Canada ©Her Majesty the Queen in Right of Canada 2006 ISSN 1701-4387 Catalogue No. M44-2006/A1E-PDF ISBN 0-662-42326-7 A copy of this publication is also available for reference by depository libraries across Canada through access to the Depository Services Program's Web site at http://dsp-psd.pwgsc.gc.ca A free digital download of this publication is available from GeoPub: http://geopub.nrcan.gc.ca/index_e.php Toll-free (Canada and U.S.A.): 1-888-252-4301 Critical reviewers Mark Stasiuk Authors’ addresses K. Simpson ([email protected]) Geological Survey of Canada 605 Robson Street, Suite 101, Vancouver, British Columbia V6B 5J3 B.Edwards ([email protected]) K. Wetherell ([email protected]) Department of Geology, Dickinson College, P.O. Box 1773, Carlisle, Pennsylvania 17013 U.S.A. Publication approved by GSC Pacific, Vancouver Original manuscript submitted: 2005-09-13 Final version approved for publication: 2005-11-03 Correction date: All requests for permission to reproduce this work, in whole or in part, for purposes of commercial use, resale, or redistribution shall be addressed to: Earth Sciences Sector Information Division, Room 402, 601 Booth Street, Ottawa, Ontario K1A 0E8. Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia K. Simpson, B. Edwards, and K. Wetherell Simpson, K., Edwards, B., and Wetherell, K., 2006: Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia; Geological Survey of Canada, Current Research 2006-A1, 7 p. -
Anil Iralnnte March)
THE PROSPECTOR WEDNESDA Y MAY 15, 1985 \ \ 4 ^ THE PROSPECTOR WEDNESDA Y MAY IS, 1985 Wekmat to tfje Ifctbge Hiuer Balterj Gold Bridge & District Chamber of Comm• erce and the advertisers present this brochure where ATV-assisted ac• In the 1880s, after upstream from the Fra- trails which remain for lorne (see map below) ditions permit snowmo- Logging activities in about an historic and rugged recreation retreat ser River, panning in today's outdoors enthu• can be gained from Hwy biling right to their do• recent years also have cess to wilderness camp• 168 air-kilometres [105 air miles] due north of paying 25 cents a head ing can erase civilizati• to cross the toll bridge hopes of locating the siasts to explore. Glim• 99 at Pemberton via the orsteps. However, even opened Pearson Cr. Rd. Vancouver,BC. mother lode. pses of history, as well High Line Rd. (for 4x4s, if lower elevations have (#4), Downton Lk. Rd. on's "rat race" from the The map inside pinpoints 30 local spots whose superceding the natives' as spectacular mountain thawed or been plowed (#15) and Kingdom Lk. mind.However, many bridge which gave the Eventually their tena• March through Novem• numbers reappear in articles and photo captions city left Bridge River vistas beckon. ber) or Hurley River for loggers, arrange• Forest Access Rd. (#21 Forest Service Recreati• on the front and back pages. Bridge River its name, Backroad access to Forest Access Rd. (for ments can be made with and 24), where thous• on Sites also are avail• prospectors could begin country laced with a network of roads and Gold Bridge and Bra- pick-up trucks in sum• those same businesses to ands of hectares of rol• able for those who pre• their arduous journey mer or snow vehicles be met enroute. -
Distribution, Nature, and Origin of Neogene–Quaternary Magmatism in the Northern Cordilleran Volcanic Province, Canada
Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada Benjamin R. Edwards* Igneous Petrology Laboratory, Department of Earth and Ocean Sciences, James K. Russell } University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada ABSTRACT Cordillera, driven by changes in relative these diverse volcanic rocks in space and time. plate motion between the Pacific and North We then use the compiled petrological and geo- The northern Cordilleran volcanic province American plates ca. 15–10 Ma. chemical data to address the origins of this alka- encompasses a broad area of Neogene to Qua- line magmatism and the structure of the litho- ternary volcanism in northwestern British Keywords: alkaline basalt, Canada, Cordil- sphere beneath the northern Cordilleran volcanic Columbia, the Yukon Territory, and adjacent leran, magmatism, Quaternary, volcanism. province. Specifically, we determine the source eastern Alaska. Volcanic rocks of the north- region characteristics of northern Cordilleran ern Cordilleran volcanic province range in INTRODUCTION volcanic province magmas using trace element age from 20 Ma to ca. 200 yr B.P. and are and isotopic data, and we produce a petrological dominantly alkali olivine basalt and hawai- Neogene to Quaternary magmatism in the image of the lithosphere using phase equilibria ite. A variety of more strongly alkaline rock Cordillera of North America is closely related to calculations for lavas and mantle peridotite types not commonly found in the North the current tectonic configuration between the xenoliths. Results of this analysis provide a basis American Cordillera are locally abundant in North American, Pacific, and Juan de Fuca plates on which to amplify the tectonic model we have the northern Cordilleran volcanic province.