Title Page 2005 Kelly Lake.Cdr

TYPE OF WORK IN EXTENT OF WORK PROJECT COSTS THIS REPORT (IN METRIC UNITS) ON WHICH CLAIMS APPORTIONED (incl. support) GEOLOGICAL (scale, area) Ground, 1:5,000; 1:10,000 ~10 square km Mar 42, 106, 109, 113; Stag 1-2; William 1 $ 44,335.66 Photo interpretation GEOPHYSICAL (line-kilometres) Ground Magnetic Electromagnetic Induced Polarization Radiometric Seismic Other Airborne GEOCHEMICAL (number of samples analysed for ...) Soil Silt Rock 99 samples analyzed for whole rock constituents Mar 42, 106, 109, 113; Stag 1-2; William 1 $ 2,920.50 Other DRILLING (total metres; number of holes, size) Core Non-core RELATED TECHNICAL Sampling/assaying Petrographic Mineralographic Metallurgic PROSPECTING (scale, area) PREPARATORY/PHYSICAL Line/grid (kilometres) Topographic/Photogrammetric (scale, area) Legal surveys (scale, area) Road, local access (kilometres)/trail Trench (metres) Underground dev. (metres) Other TOTAL COST $47,256.16 GRAYMONT WESTERN CANADA INC. 2010 GEOLOGIC MAPPING AND SAMPLING OF THE KELLY LAKE LIMESTONE DEPOSITS, MARBLE RANGE WEST OF CLINTON, BRITISH COLUMBIA Clinton Mining Division MAR 42, 66-69, 101-102, 105-106, 109, 113 WILLIAM 1, MARY 1, AND STAG 1-5, 9-11 Geographic Coordinates 51° 08' 00" N 121° 52' 05" W NTS Sheet 92P/04 Owner & Operator: Graymont Western Canada Inc. 260, 4311 - 12 Street NE Calgary, Alberta T2E 4P9 Consultant: Dahrouge Geological Consulting Ltd. 18, 10509 - 81 Avenue Edmonton, Alberta T6E 1X7 Authors: P. Kluczny, B.Sc., P.Geol. Date Submitted: March 21, 2011 TABLE OF CONTENTS Page 1. Introduction ................................................. 1 1.1 Geographic Setting.............................................. 1 1.1.1 Location and Access...................................... 1 1.1.2 Topography, Vegetation and Climate. 2 1.2 Property ................................................. 3 1.3 History and Previous Investigations.. 4 1.3.1 Investigations by Officers of Government Agencies. 4 1.3.2 History of Property Acquisitions. 5 1.3.3 Exploration by Graymont Western Canada Inc.. 7 1.4 Purpose of Work................................................ 8 1.5 Summary of Work............................................... 8 2. Regional Geology ................................................. 9 3. Property Geology ................................................. 11 3.1Stratigraphy ................................................. 13 3.1.1 Unit C2 ................................................. 13 3.1.2 Unit C4 ................................................. 14 3.2Structure ................................................. 16 3.2.1 Early Thrust Faults........................................... 17 3.2.2 Other Faults................................................ 17 4. Results of 2010 Exploration............................................. 18 5. Discussion and Conclusions............................................ 19 6. References ................................................. 21 LIST OF TABLES Page Table 1.1 List of Kelly Lake Claims ......................................... 3 Table 1.2 List of Surveyed Lots at Marble Range. 6 Table 3.1 Lithologic Units of Marble Range. 13 LIST OF FIGURES Fig. 1.1 Location Map................................................. F1 Fig. 1.2 Regional Access............................................... F2 Fig. 1.3 2010 Exploration and Property Geology. .(In . pocket) Fig. 1.4 Claim Map ................................................. F3 Fig. 2.1 Regional Geology..............................................(In pocket) LIST OF APPENDICES Appendix 1: Itemized Cost Statement for the 2010 Exploration. A1 Appendix 2: Analytical Laboratory Information and Techniques.. A3 Appendix 3: Assay Results - Central Analytical Laboratory of Graymont Western U.S. Inc. ................................................. A4 Appendix 4: 2010 Sample Descriptions and Assay Results from the Kelly Lake Area. ................................................. A6 Appendix 5: Statement of Qualifications. A15 1 1. INTRODUCTION Throughout this report, the term "Kelly Lake limestone deposits" refers to two limestone units (about 19 km long and up to 4 km wide) primarily within the first two mountain ridges on the southwest side of Marble Range. Most of the claims which encompass these limestone deposits were acquired by Graymont Western Canada Inc. (nee Continental Lime Ltd.) in 1992, 1993 and 1996. Others were held by BMC Lime Ltd. since the early 1970's. Three two-post claims, Stag 9 to 11, were staked by Ecowaste Industries Ltd. on the southwest side of the First Ridge in November, 2000. All of the Ecowaste and BMC claims were transferred to Graymont in 2007 for consistency of their B.C. properties. Graymont Western Canada collected and analyzed samples, and conducted geologic mapping of the Kelly Lake limestone deposits on multiple occasions from 1992 to 2005. This report describes the 2010 geologic mapping and sampling conducted on the Kelly Lake claims along First and Second ridges. The focus of exploration was to target areas that had seen only limited exploration during past programs. The geological map was compiled from the 2010 field work and from previously collected analytical and geological data. Structural measurements were obtained at stations throughout the property. A magnetic declination of 21° E was used. Attitudes of bedding and other planar features are given as A°/B° NW, where A° is the azimuth of the strike (right-hand rule) and B° is the amount of dip in the direction indicated. Where bedding has been obscured by structure, stratigraphic thicknesses were calculated using orientations from adjacent units. Where more than one bedding orientation was measured, the mean orientation was used. Throughout this report informal names have been applied to previously unnamed creeks, mountains, and other features to facilitate reference to geographic locations. A statements of work have been filed with respect to the exploration described in this report (Event Number 4820005). 1.1 GEOGRAPHIC SETTING 1.1.1 Location and Access The Kelly Lake limestone deposits are in the Intermontane Belt of southwestern British Columbia, 16 km west of the town of Clinton (Fig. 1.1). Clinton is 381 km from Vancouver via Highways 1 and 97, and 327 km via the British Columbia Railways. From Clinton, the Kelly Lake limestone deposits are easily reached by driving southwesterly on the paved Kelly Lake road which 2 parallels the BCR rail line for about 18 km and then northwesterly on the gravel Jesmond road (Fig. 1.2). Jesmond Road, which is about ½ km northeasterly from Kelly Lake, parallels the southwestern flank of Marble Range to its northern terminus and beyond. The ridge closest to Jesmond Road is termed ‘First Ridge’ and the next ridge to the northeast termed ‘Second Ridge’. Between Jesmond Road and First Ridge are two corridors for powerlines of the British Columbia Hydro and Power Authority. Local access to the Kelly Lake limestone deposits is by several four-wheel-drive (two-wheel-drive in good weather) powerline, logging and mining roads, which turn northeasterly off Jesmond Road (Fig. 1.3). At about 5½, 14 and 18 km from the Jesmond Road turnoff near Kelly Lake, are the Porcupine Creek, Lot-1284 and Trail Creek roads. The Porcupine Creek and Lot-1284 roads were originally constructed in the early 1970s for limestone exploration. At Line Creek the road to Jesmond Quarry has been washed out and the last few kilometres are accessible either by ATV or by foot. 1.1.2 Topography, Vegetation and Climate The Kelly Lake limestone deposits include two roughly parallel northwesterly trending ridges of rugged mountains cut by deep valleys with southwesterly flowing creeks. Locally precipitous cliffs rise to the tops of both First and Second ridges. First Ridge, with a maximum elevation of about 1830 m atop Dome Mountain, extends northwesterly from Two Mile Creek to just south of Trail Creek. North of Dome Mountain, First Ridge is topographically subdued and narrower than the more rugged Second Ridge. Second Ridge, with an elevation of up to 2,240 across from Dome Mountain, extends from the northern to southern extremes of the property. The areas investigated during 2010 include three locations along the middle part of Second Ridge, the northwest flank of Trail Mountain, Indecision Ridge, Bobcat Ridge and Dome Mountain, and along the northerly powerline (Fig. 1.3). Tree cover at First Ridge is sparse; it consists predominantly of stunted lodgepole pine with lesser amounts of Douglas Fir. Climate is alpine with average summer temperatures of 20° to 25°C and winter temperatures of -15° to -20°C, with extremes of 34°C and -41°C. Rainfall averages about 32 cm per year with maximum snowfall in December and January which averages 31 to 36 cm. 3 1.2 PROPERTY The Kelly Lake limestone deposits were acquired by Graymont Western Canada Inc. and its predecessor Continental Lime Ltd. in 1992, 1993 and 1996 (Fig. 1.4). BMC Lime Ltd., a subsidiary of Continental Lime Ltd., held claims in the Marble Range since the early 1970's. During 2001 three two post claims, Stag 9 to 11, were staked on the southwest side of First Ridge by Ecowaste Industries Ltd. (Table 1.1, Fig. 1.4). All of the Ecowaste and BMC tenures were transferred to Graymont in 2007. TABLE 1.1: LIST OF KELLY LAKE CLAIMS Current Expected Claim Name Tenure Number Record Date Expiry Date Expiry Date Stag 1 208888 1989 09 30 2010 12 31 2012 12 31 Stag 2 208889 1989 09 29 2010 12 31 2011 12 31 William 1 208932 1989 11 24 2010 12 31 2011 12 31 Mary 1 208933

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