ASSESSMENT REPORT TITLE PAGE AND SUMMARY

Transcription

1 ASSESSMENT REPORT TITLE PAGE AND SUMMARY TITLE OF REPORT: Assessment Report June 216 Rock Project Geological Report Mineral Claim TOTAL COST:$425 AUTHOR(S): Gary Nordin, PGeo SIGNATURE(S): NOTICE OF WORK PERMIT NUMBER(S)DATE(S): STATEMENT OF WORK EVENT NUMBER(S)DATE(S ): YEAR OF WORK:216 PROPERTY NAME:Rock Project CLAIM NAME(S) (on which work was done): COMMODITIES SOUGHT: Dimension Stone MINERAL INVENTORY MINFILE NUMBER(S),IF KNOWN: MINING DIVISION: Nanaimo NTS BCGS: 92L 55 LATITUDE: _ LONGITUDE: 5 W 33 N (at centre of work) UTM Zone: 9N EASTING: 634, NORTHING: 5,61, OWNER(S): Polaris Materials Corporation MAILING ADDRESS: West Georgia Street, Vancouver, BC, V6E3R5 OPERATOR(S) [who paid for the work]: Polaris Materials Corporation MAILING ADDRESS: West Georgia Street, Vancouver, BC, V6E3R5 REPORT KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude. Do not use abbreviations or codes) REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: Assessment Report 36215

2 TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT (in metric units) APPORTIONED (incl. support) GEOLOGICAL (scale, area) Ground, mapping 1m by 15m $ 425 Photo interpretation GEOPHYSICAL (line-kilometres) Ground Magnetic Electromagnetic Induced Polarization Radiometric Seismic Other Airborne GEOCHEMICAL (number of samples analysed for ) Soil Silt Rock Other DRILLING (total metres, number of holes, size, storage location) Core Non-core RELATED TECHNICAL Sampling Assaying Petrographic Mineralographic Metallurgic PROSPECTING (scalearea) PREPATORY PHYSICAL Linegrid (km) TopoPhotogrammetric (scale, area) Legal Surveys (scale, area) Road, local access (km)trail Trench (numbermetres) Underground development (metres) Other TOTAL COST $425 Page 2 of 2

3 Assessment Report June 216 Rock Project Geological Report Mineral Claim Port McNeill, Northern Vancouver Island, BC Nanaimo Mining Division Owner Gary Dale Nordin Operator Gary Dale Nordin NTS 92L 55 Longitude 127 degrees 12 minutes W Latitude 5 degrees 33 minutes N UTM Coordinates 634, E 5,61,N By Gary Nordin PGeo BC June, 216

4 Table of Contents Summary Page 1 1- Infrastructure Page 1 2- Location and Access Page 2 3-Claim Data Page 2 4-Physiography Page 2 5-Exploration Program Page 2 6-Budget Page 3 7-Geology Page Regional Geology Page Bedrock Geology Page Surficial Geology Page Local Geology Page 4 8. Data Entry Page 4 Signature Page Page 4 Curriculum Vitae Page 5-6 List of Maps Map Figure 1 -Location Map Figure 2 -Regional Geology-Property Location Map 3 Port McNeill Rock Claim Map Figure 4 Local Detailed Property Geology

5 SUMMARY The 216 exploration program in the Port McNeill Rock Project was conducted over a 4 day period from March 2-5, 216 and consisted detailed surface geological mapping. Work was conducted over a broad 1m outcrop ridge in the centre of Claim primarily exposed along logging roads. Outcrop consists of massive dark green Upper Triassic Karmutsen Fm. Massive to amygdaloidal basic volcanic rocks. Map Figure 2-3. Mapping has indicated competent volcanic rocks are present along the entire ridge. The area is easily accessed by branches of the Cabin Main logging road branching off the West Main logging located 5 kilometres west and 2 kilometres south of Port McNeill. It is an area of moderate relief from 22 to 3 metres elevation. 1-INFRASTRUCTURE Port McNeill is located 35 kilometers northwest of Vancouver, British Columbia at Latitude 5 degrees 3 seconds and longitude 126 degrees 17 seconds, NTS Map 92 L55.(Figure 1-2). Port McNeill is a forest-based town with a population of 3,. The town has a good supply of skilled industrial workers. Two logging companies Western Forest Products and Island Timberlands provide the majority of employment in the area. Fishing and tourism are the other main industry employers. Access is via ferry from Vancouver to Nanaimo and a 3.5 hour drive north on Island Highway# 19. Daily scheduled air flights by Pacific Coastal Airlines are available from Vancouver to Port Hardy, which is located 4 kilometers northwest of Port McNeill. Port Hardy has a population of 5,. Charter aircraft and helicopters are located both at Port McNeill and Port Hardy. A network of private logging roads maintained by Weyerhaeuser and Western Forest Products provide excellent access to the project area. The area has been extensively logged over the last 1 years. Northern Vancouver Island has a typical, west coast marine climate, which brings cool, moist weather to the area for most of the year. Annual rainfall ranges from 375 mm. to 5 mm. Temperature variations are moderate with an average annual temperature of 8 degrees Celsius (46 degrees Fahrenheit). The summer months, May through September, are considerably drier than the winter. Temperatures average 17.4 degrees Celsius (63 degrees Fahrenheit) in July and August, with hot, sunny days and some cooler days as well. Rarely does the temperature fall below degrees Celsius (32 degrees Fahrenheit) in the winter. 1

6 2-LOCATION AND ACCESS Map Figure 1-2 The project is located 9 kilometres south west of Port McNeill. Access is via Island Highway 19 for 3 km west of the Port McNeill turnoff to the West Main logging road, then south 1 kilometre to the Cabin Main logging road and 4 kilometres southeast to a spur road leading south onto the claim area. Accommodation and services are located in Port McNeill. 3-CLAIM DATA Map 2 The PORT MCNEILL ROCK mineral claim title Number is with Issue Date 215jun3 and comprises an area of hectares and is registered to GARY DALE NORDIN. 4-PHYSIOGRAPHY Northern Vancouver Island consists of three major physiographic units: the Nahwitti Lowland, the Susquash Basin and the Vancouver Island Mountains (Figure 6). The Nahwitti Plateau and the Susquash Basin are the main physiographic units in the proposed exploration area with the Vancouver Island Mountains located immediately to the south. The Nahwitti Plateau dominates the northern tip of Vancouver Island, principally to the west of the coastal exploration area. It is characterized by low relief and a smoothed upland, remnants of a dissected Tertiary erosional surface, which slopes northward towards Cape Scott. The Susquash Basin is a triangular shaped area along the eastern margin of the Nahwitti Lowland extending between Port Hardy and Port McNeill and it constitutes the bulk of the study area. It is characterized by gentle rolling to level topography below 3 meters elevation with scattered uplands or hillocks. The lowlands are underlain by gently dipping Cretaceous age sedimentary rocks of the Nanaimo Group with the hillocks made up of Triassic age sediments volcanics of the Vancouver Group. Erosion and glaciation of the soft Cretaceous sediments in the basin has produced the lowland topography. 5-EXPLORATION PROGRAM Consisted of a 4 day mapping program March 2-5, 216. Work was principally along a 1 metre elevated outcrop ridge in the centre of the mineral claim

7 6-BUDGET Geologist 3 days at $6 day = $ 18 Geological assistant 3 days at $ 25day = $75 Room and Board 4 days at $225day = $ 9 Truck Rental and Fuel 4 days at $2 day = $8 Total = $ GEOLOGY 7.1-Regional Geology-Map Figure 3 The most recent publication describing the surficial geology of northern Vancouver Island is contained in the Ministry of the Environment, APD Bulletin No. 5 by D.E. Howes, Terrain Inventory and Geological Hazards: Northern Vancouver Island (Appendix 2). Regional Bedrock Geology of the Port McNeill Area is described in detail by BC Geological Survey Geoscience Map 26-2 Geology of Quatsino-Port McNeill Area, Northern Vancouver Island- NTS 92 L 11,11E by G.T.Nixon, J.L Hammack, V.M. Koyangi, G.J. Payle, J.W. Haggart, M.J. Orchard, T.Tozer, D.A Archibald, R.M.Friedman, J.Palfy and F.Cordy. 7.2-Bedrock Geology Bedrock geology of the Port McNeill area is shown on Map Figure 3. The area is complex consisting of Mesozoic age volcanic and sedimentary rocks of the Karmutsen and Quatsino Formations that have been intruded by Jurassic age granites and overlain by coeval extensive volcanic rocks of the Bonanza Formation and sediments of the Cretaceous Nanaimo Group and Quaternary fluvial sediments. The Black Bear Project area is underlain exclusively by Upper Triassic age Karmutsen Formation basic tholeiitic submarine basalts which are conformably overlain by Quatsino limestones to the north of the mineral claim and are in fault contact with Upper Cretaceous Nanaimo group sandstones. The Nanaimo sediments are in turn overlain by Quaternary sand and gravel deposits. 6.3-Surficial Geology The bedrock has been extensively modified by glaciers during the Pleistocene period. In general most of the surficial material shown on the maps are related to the most recent glacial episode, the Fraser Glaciation, which occurred 9, to 25, years ago. During the maximum extent of the Fraser glaciation about 15, years ago, ice from the Coast Mountains on the mainland overrode the east coast of Vancouver Island in a northwesterly direction across the then ice-free Nahwitti lowlands in the Port Hardy- Port McNeill area. The glaciers began receding 13, years ago with the uplands and mountain peaks emerging first. Vast amounts of melt waters flowed from the decaying ice masses in the Vancouver Island Mountains and the Nahwitti lowlands. Thick sequences of sand and gravel were deposited around the bedrock highs and decaying ice masses in the Susquash basin in deltas where the waters emptied into the sea. A large complex delta was formed in the Port McNeill area over an area measuring 5 kilometers (east-west), by 5 kilometers (north-south) along the eastern side of the Cluxewe River. Large braided and pro-grade sand and gravel deltaic deposits were formed along the eastern side of the Cluxewe River. 3

8 7.4-Local Geology-Map Figure 4 Polaris Materials mapping at a scale of 1:5 has defined a broad rock outcrop ridge of competent Karmutsen massive to amygdaloidal basaltic volcanics. The outcrop ridge is approximately 1 metres wide along a 2 metre east west strike in the centre of the claim block from the 2 to 4 metre elevation. The area is bounded steep outcrop cliffs on the west and east above logging access roads Detailed mapping throughout the volcanic bench area along road cuts and in rocky bluffs throughout the bench area has defined hard competent uniform Karmutsen basaltic volcanic material. The mapped Karmutsen basic volcanics are a highly competent uniform rock with a consistant joint set spacing of 5-17 cm with fresh unaltered joint faces throughout the area. Rock outcrop areas were located by GPS waypoints with detailed descriptions of hardness-colourfracture density and orientation - bedding features and joint set orientation and spacing were noted and recorded on field notes and spreadsheets. The principal geological features noted were rock hardness and joint set orientation and spacing. Two principal joint directions were mapped; one set NW from 3-34 degrees azimuth with 5-7 degree dips and a second set NE 4-8 degrees azimuth with 5-8 degree dips; bedding was also mapped in several places measuring degrees azimuth and dips of 25-4 degrees. 8-Data Entry All geological core data was digitized from field sheets using rock codes noting rock type-fracture and jointing spacing and orientation and alteration with nominal accuracy of 2-5 metres. Gary Nordin P. Geo., BC June 5, 216 4

9 Curriculum Vitae Gary D Nordin Geologist PGeo BC EDUCATION B.Sc. Geology Honors, University of Alberta, 197. REGISTRATIONS SPECIALISATION P. Geol.-Association of Professional Engineers and Geoscientists of British Columbia Fellow- Geological Association of Canada Selection- Acquisition-Exploration and Development of Precious Metal Projects leading to Production. EXPERIENCE 2-Present Discovery Resource Corp. Private Geological Consulting-Investment Company 22-Present Canasil Resources Inc,, Galileo Resources Minerals- Consultant-Director, Delta Minerals- Consultant-Advisor Expertise Research and identification of viable precious metal projects Worldwide Polaris Minerals Corporation Consultant,Director Research-exploration and acquisition of crushed rock and sand and gravel aggregate projects in coastal British Columbia. Selection of the quarry sites and resource definition at Orca Quarry, Port McNeil and Eagle Rock, McTush quarry, Port Alberni Eldorado Gold Corporation(TSE) Founder, Director, Vice President, Chief Geologist Founder of Eldorado Gold. Selection of project areas throughout USA, Mexico, South America and Turkey. Directed all geological aspects of exploration, development and acquition of projects leading to productionacquisition decisions at: La Colorado, Mexico; La Trinidad, Mexico; SaoBento, Brazil; Efemcukuru and Kisladag, Turkey. 5

10 Bema Gold Corporation Founder, Director, Vice President Exploration, Chief Geologist Founder of Bema Gold. In charge of review and selection of projects and all geological aspects of a project leading to a production decision. Reviewed and directed geology and recommended acquisition of Champagne Mine, USA, Ogilvy Imperial Gold Project (Indian Rose-Ocotillo Gold Project) Imperial County, California, USA; Refugio Gold Mine, California Consultant Oil Industry Well site consultant, Blue Sky Oil and Gas, Calgary Alberta Exploration Geologist Exploration for iron ore- copper porphyry deposits in British Columbia, Alaska, Costa Rica for: -Anaconda American Brass, British Columbia -Texada Mines Ltd- Kaiser Exploration, British Columbia- Alaska -Cities Services Corp, British Columbia- Costa Rica -British Columbia Department of Mines- Geochemical survey Cassiar-Prince Rupert -Northair Mines Ltd- Bralorne-Pioneer Mine area, Banks Island, British Columbia Summers Echo Bay Mines- Port Radium,NWT Inco- Thompson, Manitoba 6

11

12 'W Port McNeill ± Keogh Mainline Cabin Mainline Mineral Claim # Highway 'N 5 1, 1,5 2, 2,5 Meters 1:25, Datum: Rock Project GCS North American 1983 Projection: Location Map for Claim # NAD 1983 UTM Zone 9N Document Path: C:\Users\enord\Desktop\Polaris Data\Claim_Location_ mxd Date Version Fig No June, 216 A 1

13 'W ± Port McNeill TAv ukn 564 Cluxewe Mtn. utrq utrk 5 33'N utrq Mineral Claim # Map Key utrk 56 Mineral Claim # Nanaimo Group Island Intrusive Bonanza Group Quatsino Fm. Karmutsen Fm. Alert Bay utrk :3, 3 km Rock Project Regional Geology Datum: Projection: Date Version GCS North American 1983 June, 216 NAD 1983 UTM Zone 9N A Fig No 2

14 632, 632,5 633, ,5 634, 634,5 635, 635,5 636, 1 ^ G.N ' E 26 MILS 1 5,62,5 8 5,62,5 Õ Magnetic North ,5 18 ' E 32 MILS UTM GRID AND 215 MAGNETIC NORTH DECLINATION AT CENTER OF SHEET Map Key 1 5,62, 14 Fault-Fracture Fracture Joint 5,62, o D Bedding Shear Joint- vertical Fracture Zone 12 GPS Waypoints 1 Fault Zone 423 Joint; M422; Az= 27; Dip= Joint; M422; Az= 34; Dip= Joint; M428; Az= 35; Dip= Joint; M431; Az= 1; Dip= Joint; M137; Az= 32; Dip=4 2 Joint; M136; Az= 33; Dip= Joint; M127; Az= 24; Dip=6 22 Joint- vertical; M129; Az= 25; Dip=9 34 5,6,5 D Joint- vertical; M134; Az= 6; Dip=9 Joint; M137; Az= 3; Dip=45 5,6, Joint- vertical; M125; Az= 65; Dip=9 34 Joint- vertical; M133; Az= ; Dip= Fracture Zone 3 m wide Joint; M99; Az= 2; Dip=75 Joint; M121; Az= 4; Dip=5 14 Shear; M111; Az= 5; Dip= Fracture; M114; Az= 24; Dip=5 136 Joint- vertical; M124; Az= 65; Dip= Joint- vertical; M96; Az= 4; Dip= Joint- vertical; M1; Az= 32; Dip= Joint; M12; Az= 16; Dip=7 ; M19; Az= ; Dip= 12 D Joint; M113; Az= 5; Dip= Joint; M12; Az= 27; Dip=7 Fracture Zone 3 m wide 1m wide shear 575East Fracture-vertical; M18; Az= 32; Dip=9 15 Fracture; M13; Az= 1; Dip= Fault-Fracture; M16; Az= 5; Dip= M Joint- vertical; M123; Az= 65; Dip= Fracture Zone 123 Joint- vertical; M131; Az= 5; Dip=9 Joint-vertical; M17; Az= 12; Dip= Joint; M43; Az= 35; Dip=75 43 Joint; M12; Az= ; Dip=8 12 Joint; M118; Az= ; Dip= ,61, 14 5,61, Joint; M119; Az= ; Dip=8 Amgydaloidal Basalt Karmutson Group (Upper Triassic Age) Outcrop Area Mineral Claim # Mineral Claim # ,61,5 Joint; ; Az= 28; Dip=75 5,61,5 Joint; ; Az=8; Dip=65 Fracture Zone 5m wide Fracture Zone, Minor Shearing ,6, 16 5,6, , , 5,599,5 5,599, , , , 634,5 635, 635, , :5, 8 636,5 1, Meters Project Name Rock Project Datum: Document Path: C:\Users\enord\Desktop\Map92L55_Structural_Geology_map_1_5 scale\rock Project 1-5 scale data\rock_project_1_5 scale.mxd GCS North American 1983 Projection: NAD 1983 UTM Zone 9N Drawn By: Date June, 216 Structural and Bedrock Geology Approved By: Version A Fig No 4

15 PcNeill Rock Claim Legend m. This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, or otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION. Map center: 5 32' 44 N, 127 6' 17 W Scale: 1:3,69