DOCSLIB.ORG

Gold Bridge Properties

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Gold Bridge Properties Gold Bridge Properties ASSESSMENT REPORT ON THE GEOCHEMICAL, AND PROSPECTING THE GOLD BRIDGE MINERAL CLAIMS Tenures 696374, 704730, 704734, 704752, 708922 Lillooet Mining Division Property Location Southern British Columbia BCGS 82L.008 Longitude and Latitude 50°8773 N 122°756 W By David A. Wallach For DW Exploration Ltd July 18, 2012 Page 1 of 28 Table of Content 1.0 Introduction........................................................... 3 2.0 Summery............................................................... 3 3.0 List of Mineral Tenures and Status........................ 4 4.0 Access and Location............................................. 5 5.0 Regional Geology.................................................. 5 6.0 Physiography, Vegetation and Climate.................. 5 7.0 Location Map.......................................................... 6 8.0 Claim Map.............................................................. 7 9.0 Rock Sample locations Map.................................. 8 10.0 Sample Analysis Map............................................ 9 11.0 Certificates of Analysis.......................................... 10 12.0 Conclusion.............................................................. 25 13.0 Statement of Costs................................................. 25 14.0 References............................................................. 26 15.0 Qualifications.......................................................... 27 Page 2 of 28 1:0 INTRODUCTION This report has been prepared David A Wallach of DW Exploration Ltd., 5241 Cobble Crescent, Kelowna, B.C. in compliance with current assessment report standards for the Province of British Columbia, Event number 5394165. David A. Wallach holds title to the Carpenter Lake 2, 3, 4, 5, and 8 Mineral Claim’s, located 236 Km north from the City of Vancouver, B.C. The report summarizes the results of geochemical sampling program carried out on the Carpenter Lake 2, 3, 4, 5, and 8 Mineral Claim’s during the month of June and July of 2012. 2:0 SUMMARY The Gold Bridge property is located in the Lillooet Mining Division of south Western British Columbia. Acceptable access to the property is found 79.5 km north of Pemberton along Meadows road and Hurley River Forest Service road off Provincial Hwy 99. 897.43 hectares consisting of 5 claims make up the total inventory of the Gold Bridge property, which are owned 100% by David A. Wallach (FMC 146010). Historical records report production of stibnite rich “ore” from the Reliance adit in 1917. Although there are numerous other small workings on the property there is little reported production. The Imperial Zone very near the Senator workings was discovered in 1985. The property is underlain by intensely deformed portions of the Paleozoic Cadwallader Group metasediments, and ophiolitic Bridge River Complex (Pioneer Group) metavolcanics. Both terranes have an oceanic provenance. These rocks have been intruded by the protracted Late Cretaceous to Early Tertiary Coast Plutonic Complex. All of the Lode gold mineralization in the area is temporally and spatially related to portions of this protracted intrusive episode. The mineralization on the Reliance property appears to be related to and controlled by several subparrallel northwest striking apparently NE dipping shears, and often contained within second and or third order discreet and anastomozing south striking moderately to steeply west dipping reverse faults and shears. This structural style has similarities to the nearby Minto Mine and other polymetallic vein systems. From May 1 to September 30, 2008 Reliance completed a $677,905.72 3052.63 metre diamond drilling program in two areas of the property. The first area tested was where moderate gold, arsenic antimony MMI soil anomalies were located. The drill holes confirmed the soil anomalies, however no economic grades of gold mineralization were intersected. The best MMI targets could not be reached by this program due to unroaded very steep topography of the area. The second area tested was the Imperial Zone which is the best known drill target on the property. The Imperial zone is north striking and steeply west-northwest plunging. Several historical holes were “twinned” and additional ones designed to infill and extend the zone. This program was very successful in confirming the widths of earlier drilling, grade however although encouraging did not match the earlier results. The drilling also confirmed that the Imperial Zone is open at depth to the west. Page 3 of 28 3:0 TENURES The Gold Bridge Claims consist of 5 tenures; 696374, 704730, 704734, 704752, 708922 Tenure Tenure Tenure Sub Map Good To Number Claim Name Owner Type Type Number Issue Date Date Status Area (ha) 696374 CARPINTER LAKE 2 146010 (100%) Mineral Claim 092J 2010/jan/08 2014/may/15 GOOD 40.8057 704730 CARPINTER LAKE 4 146010 (100%) Mineral Claim 092J 2010/jan/25 2014/may/15 GOOD 428.3678 704734 CARPINTER LAKE 3 146010 (100%) Mineral Claim 092J 2010/jan/25 2014/may/15 GOOD 244.8639 704752 CARPINTER LAKE 5 146010 (100%) Mineral Claim 092J 2010/jan/25 2014/may/15 GOOD 20.4167 708922 CARPENDER LAKE 8 146010 (100%) Mineral Claim 092J 2010/feb/27 2014/may/15 GOOD 162.9655 4:0 LOCATION AND ACCESS The Gold Bridge Mineral Claim’s are located approximately 236 kilometers north from the City of Vancouver, B.C. (see Figure 3-1). Access to the claim area is by paved highway to Lillooet, B.C. Lillooet can be reached from Vancouver via Squamish and the Duffey Lake road (Highway 99), or via Lytton in the Fraser Canyon (Highways 1 & 12). From Lillooet, the road along the north shore of Carpenter Lake is taken westerly to a point approximately 12 kilometers east of Gold Bridge, B.C. (see Figure 3-2). The Tyax claims are accessed though a gravel road northerly towards the claim area and the nearby Tyax Mountain Resort. This gravel road is followed northerly for a distance of approximately 4 kilometers (see Figure 4-1). At this point, about 1.5 kilometers south of the south end of Tyaughton Lake, a main logging haul road is taken North-easterly towards the claim area. Several branch roads off this main haul road provide good access to the claim area. The Truax W4 is accessed 4 Km south of Gold Bridge, via right hand turn on Lillooet Pioneer Rd for 1 Km with a Left turn on Lost Lake trail, then left on Truax Mt trail, then keep left at old workings for a total of 3 Km. Due to the very steep terrain and heavy avalanche season, the Trail has been severely wiped out in several places, making travel though this area very difficult. The Truax NW3 is accessed 4 Km North-east of Gold Bridge, via Truax Creek Road then Gray Road and right turn on Steep Creek Road for 300 meters and left on Girl Creek trail for 3 Km until the summit is reached. The McDonald Lake Claim is accessed from Gold Bridge via Truax Creek Road then Gray Road and right turn on McDonald Creek Road for 1.5 Km until you end up at an old mining camp at the head of McDonald Lake. A broad northeast-trending ridge is the most prominent topographic feature of the south-central claim area. Elevations on the claims range from about 2300 meters on the south border of the claims to about 1450 meters at the northeast comer of the claims. A large portion of the claim area covered by the 1996 soil geochemical grid (see Figure 4-1) has been logged off. This logging was not recent, as evidenced by the size of stumps and the height of the sporadic new growth. There was no evidence of standing or running water on the property Page 4 of 28 at the time the geochemical sampling was carried out (September, 1996). 5:0 REGIONAL GEOLOGY The regional geology of the Pemberton area has been compiled most recently in 1977 by the Geological Survey of Canada as a portion of Open File Map #482. The pertinent area of this map is reproduced as Figure 5-1A. Description of the various rock units is shown in the map legend, Figure 4B. Triassic and Jurassic Bridge River (Fergusson) Group rocks underlie the main portion of the study area. These rocks (Unit 3 in Figure 5-1A) consist of sediments, some volcanics and their weakly-metamorphosed equivalents (greenstone, basalt, chert, argillite, phyllite, minor limestone, serpentine and serpentinized peridotite). Page 5 of 28 A recent volcanic event, some 2400 years in age has deposited a layer of volcanic ash over the entire area. This ash layer lies close to the surface, usually within about 15 centimeters. The thickness of this ash layer varies with local topography. On side hills the ash layer may only be 20 to 30 centimeters in thickness. In flat areas and depressions the ash layer may be up to 70 centimeters in thickness 0:6 PHYSIOGRAPHY, VEGETATION AND CLIMATE The Gold Bridge property is located in the Cadwellder Range in the Truax Mountains. Elevations range approximately 2,379 meters above sea level on top of Truax Mountain. Steep tree-less peaks form the upper parts of the mountains with deeply incised drainages creating steep valley flanks. July is warmest with an average temperature of 12.5 °C at noon. January is coldest with an average temperature of -18 °C at night. Mount Truax has temperate cold and warm seasons, like winters and summers. Temperatures drop sharply at night. Winter has prolonged freezing periods, with the coldest month most often being December. July is on average the month with most sunshine. The wet season has a rainfall peak around November, the dry season is around the month of August. Mount Truax has a humid (> 0.65 p/pet) climate. The land area is not cultivated, most of the natural vegetation is still intact. The landscape is mostly covered with sparse vegetation. The climate is classified as a dry continental (dry warm summers), , with a boreal moist forest biozone . The soil in the area is high in podzoluvisols, luvisols (pd), soil with clay-enriched lower horizon with deeply tongued albic horizon Mount Truax can have strong (vi) earthquakes (on average one every 50 years), with occurrences at 5-6 Richter.
Load more

Recommended publications
  • 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
    [Show full text]
  • Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996
    Upper Bridge River Valley Official Community Plan Bylaw No. Bylaw 608, 1996 CONSOLIDATED COPY May 2016 IMPORTANT NOTICE THIS IS AN UNOFFICIAL CONSOLIDATION OF BYLAW NO. 608 WHICH HAS BEEN PREPARED FOR CONVENIENCE ONLY. Although the Squamish-Lillooet Regional District is careful to assure the accuracy of all information presented in this consolidation, you should confirm all information before making any decisions based on it. Information can be confirmed through the SLRD Planning Department. Bylaw 608 ( Consolidated for Convenience Only) May 2016 SUMMARY OF AMENDMENTS CONSOLIDATED FOR CONVENIENCE ONLY Consolidated bylaws are consolidated for convenience only and are merely representative. Each consolidated bylaw consists of the original bylaw text and maps, together with current amendments which have been made to the original version. Copies of all bylaws (original and amendments) may be obtained from the SLRD Planning and Development Department. BY-LAW NO. DATE OF ADOPTION 1022 – 2006 Major Review of Upper Bridge River Valley OCP January 28, 2008 Rezoning a parcel of unsurveyed Crown land from Resource 1094 – 2008 October 26, 2009 Management to Industrial Tyax Real Estate Ltd. text and map amendments plus 1305 - 2014 housekeeping amendment July 28, 2014 PID 024-877-638 (Lot 5, DL 4931, Plan KAP67637, LLD) Creating a Medical Marihuana Production Facility 1309 - 2014 February 25, 2015 Development Permit Area 1440 - 2016 OCP amendments to the Tyax Staff Housing May 25, 2016 Official Community Plan Bylaw No. 608 Page 2 Bylaw 608 ( Consolidated for Convenience Only) May 2016 SQUAMISH LILLOOET REGIONAL DISTRICT BYLAW NO. 1022, 2006 A bylaw of the Squamish Lillooet Regional District to amend the Upper Bridge River Valley Official Community Plan Bylaw No.
    [Show full text]
  • Brief on Mining and “Backcasting from Principles of Sustainability”
    Creating Resilience in the SLRD The Report of the SLRD Energy Resilience Task Force FINAL REPORT February, 2011 © 2011, Squamish-Lillooet Regional District. All Rights Reserved. The preparation of this sustainable community plan was carried out with assistance from the Green Municipal Fund, a Fund financed by the Government of Canada and administered by the Federation of Canadian Municipalities. Notwithstanding this support, the views expressed are the personal views of the authors, and the Federation of Canadian Municipalities and the Government of Canada accept no responsibility for them. FINAL REPORT February, 2011 A partial list of things made from Oil… Solvents Diesel fuel Motor Oil Bearing Grease Ink Floor Wax Ballpoint Pens Football Cleats Upholstery Sweaters Boats Insecticides Bicycle Tires Sports Car Bodies Nail Polish Fishing lures Dresses Tires Golf Bags Perfumes Cassettes Dishwasher parts Tool Boxes Shoe Polish Motorcycle Helmets Caulking Petroleum Jelly Transparent Tape CD Player Faucet Washers Antiseptics Clothesline Curtains Food Preservatives Basketballs Soap Vitamin Capsules Antihistamines Purses Shoes Dashboards Cortisone Deodorant Footballs Putty Dyes Panty Hose Refrigerant Diapers Life Jackets Rubbing Alcohol Linings Skis TV Cabinets Shag Rugs Electrician's Tape Tool Racks Car Battery Cases Epoxy Paint Mops Slacks Insect Repellent Oil Filters Umbrellas Yarn Fertilizers Hair Colouring Roofing Toilet Seats Fishing Rods Lipstick Denture Adhesive Linoleum Ice Cube Trays Synthetic Rubber Speakers Plastic Wood Electric Blankets
    [Show full text]
  • LITTLE GEM (Northern Gem) COBALT-GOLD
    Geological Report on the LITTLE GEM (Northern Gem) COBALT-GOLD PROPERTY Gold Bridge/Bralorne Area South-Central British Columbia NTS 92J15W 500 53’47”N, 1220 57’12” W R.H. McMillan Ph.D., P.Geo. 15 January 2007 Table of Contents page 1 Introduction -- Synopsis 2 2 Location and Access 2 3 Claim Status 5 4 Physiographic and Vegetation 5 5 Past Exploration Work 5 6 Geology 6 7 Mineralization, Alteration and Veining 7 8 Mineral Resources 11 9 Metallurgy 11 10 Present Exploration Work 12 10 Conclusions and Discussion 12 11 Recommendations 13 12 Bibliography 14 List of Figures 1 Location Map and Generalized Geology - Little Gem Property 1 2 Claim Map - Little Gem Property 3 3 Surface Plan – Little Gem Property (after Lammle, 1986) 4 4 Regional Geology, Little Gem area (after Massey et al, 2005) 8 5 Little Gem Mine – plan of principal surface showings and underground workings (after Stevenson, 1948) 9 Tables 1 Little Gem Property Claims 3 2 Assays – Little Germ Mine Property (after Stevenson, 1948) 10 3 GPS Locations 12 Appendices 1 Statement of Expenditures 15 2 Certificate 16 LEGEND Granitic intrusions TT TT Tyaughton trough TT TT BR Ultramafite Gabbro CD Cadwallader Group BR Bridge River Complex O TT 51 00’ Fault - inferred CD CD Fault - thrust S hu la ps R BR an ge BR BR BR Little Gem Co-Au Deposit BR BR C ar pe nte e r k La n u La G ke BR Gold Bridge BR CD 122O 30’ Do wn tow n L ake BR CD BR Bralorne CD Bendor Range N O C 51 45’ o a st R a n g e CD CD BR BR BR 1:250 000 CD 0 6 kilometres Figure 1 - Location map and generalized geology - Little Gem Property (after Church, 1995) 1 1 Introduction -- Synopsis A potentially economic deposit of cobalt-gold mineralization with minor associated uranium is partially developed by three adits in the Gold Bridge area - the vein-type mineralization is hosted in granitic rocks of the Coast Range Igneous Complex and is part of the Bridge River gold mining district (Church, 1995).
    [Show full text]
  • Hope Creek Property
    c~- GEOCHEMICAL & GEOLOGICAL ASSESSMENT REPORT on the Hope Creek Property Lillooet Mining Division, British Columbia Field Work: Sept 5 to Sept 9,200O Claims: TW, TW l-4, Grill 1 Location: l 30 Km South of Gold Bridge, B.C. l NTS Map No. 92J/lOW l Latitude: 50’ 35.5 ’ North l Longitude: 122” 58.8 ’ West Prepared By: TABLE OF CONTENTS Page SUMMARY ................................................................................................................................. 1 lNTRODUCTION.. ..................................................................................................................... .2 LOCATION AND ACCESS, ........................................................................................................ 2 TERRAIN .................................................................................................................................... 2 PROPERTY ................................................................................................................................ .3 HISTORY Regional.. ..................................................................................................................................... 3 Local.. ............................................................................................................................ 3 PHYSICAL WORK.. ................................................................................................................... .4 GEOLOGY AND MINERALIZATION Regional .......................................................................................................................
    [Show full text]
  • Wildsafebc Squamish-Lillooet Regional District Annual Report
    WildSafeBC Annual Report 2020 Squamish-Lillooet Regional District Prepared by: Devin Pawluk, WildSafeBC Squamish-Lillooet Regional District Coordinator 0 WildSafeBC Squamish-Lillooet Regional District 2020 Annual Report Executive Summary This report describes the activities of the WildSafeBC Squamish-Lillooet Regional District (SLRD) Program between May 1st and November 30th, 2020. This program is new to the SLRD and complements the work being doing in the Bear Smart Communities of the District of Squamish and the Resort Municipality of Whistler. The SLRD consists of four member municipalities (District of Lillooet, Village of Pemberton, Resort Municipality of Whistler, District of Squamish) and four unincorporated rural Electoral Areas (A, B, C, D) (Figure 1 and Figure 2). While Squamish and Whistler have their own education programs, there was a recognized need for a human-wildlife conflict reduction education in the rural areas and smaller communities. The WildSafeBC SLRD Program focused on the communities of Britannia Beach, Furry Creek, Squamish Valley, Pemberton Meadows, and Lillooet. The SLRD is located within the traditional territories of the Líl'wat, Squamish, St'at'imc, Stó:lō, Tsleil-Waututh, Nlaka'pamux, Tsilhqot'in, and Secwepemc Nations. Pemberton serves as the approximate geographic center of the region and hosts the SLRD office. This season was unusual in that there were several reports of grizzly bears in both Squamish and Whistler. In addition, near Lillooet there were three separate incidents where people were attacked by either a black bear, grizzly bear, or a cougar. Black bears remain the most commonly reported species for the area followed by cougars and coyote.
    [Show full text]
  • Broadcasting Decision CRTC 2021-266
    Broadcasting Decision CRTC 2021-266 PDF version Ottawa, 5 August 2021 Canadian Broadcasting Corporation Across Canada Various television and radio programming undertakings – Administrative renewals 1. The Commission renews the broadcasting licences for the television and radio programming undertakings set out in the appendix to this decision from 1 September 2021 to 31 March 2022, subject to the terms and conditions in effect under the current licences. The Commission also extends the distribution orders for the television programming undertakings CBC News Network, ICI RDI and ICI ARTV until 31 March 2022.1 2. In Broadcasting Decision 2020-201, the Commission renewed these licences administratively from 1 September 2020 to 31 August 2021, and extended the distribution orders for CBC News Network, ICI RDI and ICI ARTV until 31 August 2021. 3. This decision does not dispose of any issue that may arise with respect to the renewal of these licences. Secretary General Related documents Various television and radio programming undertakings – Administrative Renewals, Broadcasting Decision CRTC 2020-201, 22 June 2020 Distribution of the programming service of ARTV inc. by licensed terrestrial broadcasting distribution undertakings, Broadcasting Order CRTC 2013-375, 8 August 2013 Canadian Broadcasting Corporation – Licence renewals, Broadcasting Decision CRTC 2013-263 and Broadcasting Orders CRTC 2013-264 and 2013-265, 28 May 2013 This decision is to be appended to each licence. 1 For ICI RDI and CBC News Network, see Appendices 9 and 10, respectively,
    [Show full text]
  • BC Geological Survey Assessment Report 29489
    ……. 2 INDEX Page i…… Copy of Tenure Renewal 1…… Cover Page 2…… Index 3…… Introduction / Location / Access / History 4…… History continued / Regional Geology 5........ Previous Work & Area Geology 6........ Summary / Conclusion / Work Record 7........ Work Evaluation & Cost Statement / Attending Parties & Qualifications / Affidavit 8....… General Location Reference Map - Map 1 9…… Work Area Map - Map 2 10….. Contour Map - Map 3 Note: Unless otherwise referenced, map submissions are enhanced excerpts from the BC Ministry's Provincial Mapping System. Scale as that shown. Event 4165978 ……. 3 Introduction The Coon Tree property, tenure # 540035, a four cell claim comprising 81.57 hectares, was staked on August 28, 2006. The claim lies in the Bridge River Mining Camp, well renowned in mining history as a major gold producing region, dating back to the late 1800s, and continues as such today, with ongoing explorations by varied interests.. Location The Coon Tree claim is located within Map Sheet 092J086 in the Lillooet Mining District, on the northwest shore of Gun Lake in the Bridge River Mining Camp, centered on coordinates 122° 53’ 43.1” W Longitude, 50° 52’ 36.6” N Latitude, approximately 4.7 kilometers northwest from Gold Bridge, BC, 68 kilometers west-northwest of Lillooet or 200 kilometers north of Vancouver. The south end of the claim extends into Gun Lake, where Walker Creek cuts the property from a northwest to southeasterly direction, flowing into Gun Lake. The elevation ranges from the 880 metre level along the lake, to 1200 metres in the northwest portion of the claim. Access Access to the property may be gained from either of two directions.
    [Show full text]
  • Bridge River Valley Community Directory in 2013
    2013 $5.00 BBrriidd ggee RRiivveerr VVaalllleeyy CCoommmm uunniittyy DDiirreeccttoorryy wwwwww..bbrriiddggeerriivveerrvvaalllleeyy..ccaa PRODUCED BY: BRIDGE RIVER VALLEY COMMUNITY ASSOCIATION PHONE: 250-238-2534 EMAIL: [email protected] PILLOWS FLUFFED DAILY. PHOTO: JORDAN MANLEY JORDAN PHOTO: Ridiculously awesome catskiing just 30 minutes north of Whistler. 1.604.894.7669 SNOWCATS.CA 2 BCSC-2011-PiqueFAQ-4.125x6.375 blackcomb0613.pdf 1 6/11/13 1:08 PM C M Y CM MY CY CMY K "Proudly serving the Gold Bridge, Bralorne and Gun Lake areas since 1985" 20 Helicopters • 7 Airplanes • 8 Bases • 1 Phone Call Gun Lake 250.238.0194 blackcombaviation.com Toll Free 800.330.4354 3 Highland Cream LEAVE CIVILIZATION BEHIND AND GET INTO THE WILD Resort Gun Lake, BC P/F: (250) 238-­‐2362 Photo credits to Jordan Manley, Geoff Playfair & Sterling Lorence. [email protected] Always Dreamed of a Spectacular BOOK YOUR ADVENTURE TODAY! ŏ ŏđŏŏ ŏŏđŏŏ ŏ ŏŏđŏŏ ŏŏ get away? Discover Highland! ŏđŏŏ ġŏ ŏđŏ ŏ ŏĒŏ tyaxadventures.com l [email protected] l 888.892.9288 www.highlandcreamresort.com Tyax Adventures @ Tyax Wilderness Resort & Spa, Gold Bridge, BC 4 CONTENTS TOURIST INFORMATION 7 ACCOMMODATION 8-11 CAMPING 12-13 RESTAURANTS & DINING 14-15 FOOD SERVICES & CATERING 16 WILDERNESS ADVENTURES 17-20 RECREATION 21-25 FESTIVALS & EVENTS 26-27 GAS & AUTO SERVICES 28 COMMUNITY CENTRES & AMENITIES 29-31 COMMUNITY SERVICES 32 EDUCATIONAL FACILITIES 32 HISTORIC FACILITIES 33-34 5 MEDICAL & HEALTH SERVICES 35 PUBLIC WORKS & SERVICES 36 ROADS
    [Show full text]
  • Connection Call 604-230-8167 [email protected] Frankingham.Com
    YOUR PEMBERTON Real Estate connection Call 604-230-8167 [email protected] FrankIngham.com FRANK INGHAM GREAT GOLF, FANTASTIC FOOD, EPIC VIEWS. EVERYONE WELCOME! R E A L E S T A T E Pemberton Resident For Over 20 Years 604-894-6197 | pembertongolf.com | 1730 Airport RD Relax and unwind in an exquisite PEMBERTON VALLEY yellow cedar log home. Six PEMBERTON & AREA HIKING TRAILS unique guest bedrooms with private bathrooms, full breakfast ONE MILE LAKE LOOP 1 and outdoor hot tub. Ideal for 1.45km loop/Approx. 30 minutes groups, families and corporate Easy retreats. The Log House B&B 1.3km / 1 minute by vehicle from Pemberton Inn is close to all amenities and PEMBERTON LOCAL. INDEPENDENT. AUTHENTIC. enjoys stunning mountain views. MEADOWS RD. Closest to the Village, the One Mile Lake Loop Trail is an easy loop around the lake that is wheelchair accessible. COLLINS RD. Washroom facilities available at One Mile Lake. HARDWARE & LUMBER 1357 Elmwood Drive N CALL: 604-894-6000 LUMPY’S EPIC TRAIL 2 BUILDING MATERIALS EMAIL: [email protected] 9km loop/ Approx. 4 hours WEB: loghouseinn.com Moderate 7426 Prospect street, Pemberton BC | 604 894 6240 URDAL RD. 1.3km / 1 minute by vehicle from Pemberton The trail is actually a dedicated mountain bike trail but in recent years hikers and mountain runners have used it to gain PROSPECT ST. access to the top of Signal Hill Mountain. The trail is easily accessed from One Mile Lake. Follow the Sea to Sky Trail to EMERGENCIES: 1–1392 Portage Road IN THE CASE OF AN EMERGENCY ALWAYS CALL 911 URCAL-FRASER TRAIL Nairn Falls and turn left on to Nairn One Mile/Lumpy’s Epic trail.
    [Show full text]
  • Metallogeny of the Bridge River Mining Camp (092J10, 15 & 092O02)
    GeoFile 1999-01 Metallogeny of the Bridge River Mining Camp (092J10, 15 & 092O02) Originally created as a web article in 1999, this document was re-released, with slight modifications, as a GeoFile in 2019. By: B.N. Church (P.Eng.) and L.D. Jones (P.Geo.), 1999 Abstract The Bridge River mining camp, known principally for gold-quartz mineralization, is remarkably similar to the Mother Lode camp of California in terms of ore mineralogy, wallrock alteration, and geological setting. In both camps, ore veins occupy major fault zones in belts of elongated serpentinite bodies flanked by granitic plutons. The camp encompasses five former mines including two large gold producers (Bralorne and Pioneer), three small producers (Wayside, Minto, and Congress), and more than 60 surrounding mineral prospects. It is underlain by Paleozoic, Mesozoic, and Tertiary volcanic and sedimentary beds and igneous intrusions. The Bralorne intrusions and Pioneer volcanic rocks are the most consistently mineralized rocks in the area. The intrusions form small gabbro and diorite stocks aligned along the Cadwallader fault zone and in the Shulaps complex. Zircon from a coarse-grained phase of the Bralorne diorite yielded a U-Pb date of 293± 13 Ma indicating that the intrusions are among the oldest in the area. These rocks have 45-55% SiO2 (averaging 50.8%), similar to the Pioneer volcanic rocks, but have relatively high Mg and low Ti and iron oxides. The Bralorne and the Pioneer rocks are clearly discriminated on Ti versus felsic index (Qz+Or+Ab) plots. The Bralorne intrusions are further characterized by Ti/V values close to the 10 line and resemble ocean island arc magmas.
    [Show full text]
  • Community Emergency Plan Bralorne & Gold Bridge
    Community Emergency Plan Bralorne & Gold Bridge Table of Contents Key definitions .............................................................................................................................................. 3 Introduction ................................................................................................................................................. 4 Community Overview ................................................................................................................................... 5 Demographics .......................................................................................................................................... 5 Land Use ................................................................................................................................................... 5 Critical infrastructure ............................................................................................................................... 5 Response Capabilities .............................................................................................................................. 5 Hazard, Risk and Evacuation ........................................................................................................................ 7 Evacuation Routes ................................................................................................................................... 7 Interface Fire ...........................................................................................................................................
    [Show full text]