2008 Soil Geochemistry. on the. Serpentinite Lakes Property,

Transcription

1 2008 Soil Geochemistry on the Serpentinite Lakes Property, Dease Lake Area (NTS 104I/06) Liard Mining Division, Northern British Columbia, for C. J. Greig & Associates Ltd., by S.T. Flasha (B.Sc.) and C.J. Greig (M.Sc. P.Geo.) February 6 th, 2009

2 TABLE OF CONTENTS 1.0 Summary of Field Program and Results Location, Access, and Physiography Claims Geologic Setting & Mineral Occurrences Previous Work Soil Geochemistry Recommendations References LIST OF FIGURES & TABLES Figure 1. Location of the Serpentinite Lakes Property, northern British Columbia Figure 2. Location of the Serpentinite Lakes Property, northern British Columbia Figure 3. Serpentinite Lakes property claim location, Liard Mining Division, northern British Columbia Figure 4. Regional geology, showing location of the Serpentinite Lakes property and significant mineral occurrences in northern British Columbia Figure soil sample locations, Serpentinite Lakes property Figure 6. Copper geochemistry in soil samples, Serpentinite Lakes property Figure 7. Nickel geochemistry in soil samples, Serpentinite Lakes property LIST OF APPENDICES Appendix I. Soil Sample Locations & Geochemistry Appendix II. Silt Sample Locations & Geochemistry Appendix III. Blank Geochemistry Appendix IV. Cost Statement Appendix V. Statement of Qualifications -i-

3 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. 1.0 Summary of Field Program and Results The Serpentinite Lakes property consists of a single 270 hectare tenure that was staked on April 8 th, 2008 to cover a possible copper-nickel-pge showing hosted by mafic-ultramafic rocks. In July 2008, a four person sampling crew spent one day on the property collecting a total of 133 soil geochemical samples, as well as 3 silt geochemical samples from nearby streams. The soil geochemical work was successful in extending and enhancing the area of anomalous copper geochemistry, but it seems clear that the copper is associated with granitic rocks and has little association with Ni. The target on the property is probably not a Cu-Ni-PGE bearing maficultramafic associated magmatic sulphide system, but a porphyry copper deposit. The total cost of exploration on the Serpentinite Lakes property in 2008 was $15,320. Further exploration is recommended, and should initially include further contour soil geochemical sampling and reconnaissance prospecting, stream sediment sampling, and mapping, primarily to the east and northeast of the known soil geochemical anomaly. 2.0 Location, Access, and Physiography The Serpentinite Lakes property is located approximately 37 kilometres east of Dease Lake, a small northern community on the Stewart-Cassiar Highway (figs. 1 and 2). Currently the most practical access to the property is by helicopter from Dease Lake. The access road to Kutcho Creek, known locally as the Boulder Road, lies only 12 kilometres south of the property, and so the Serpentinite Lakes property could be fairly readily accessed in the future by building a trail from the Boulder Road (fig. 2). -1-

4 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. & Associates Ltd. YUK ON TERRIT ORY N Atlin Atlin L Dease Lake Stikine Serpentinite Lakes Property BRITISH COLUMBIA R Li ard R Fort Nelson NWT CANADA LEGEND / LÉGENDE Provincial capital Other populated places ALASKA USA Stewart Williston L Fort St John Trans-Canada Highway Major road Ferry route Prince George Fl Fras e r International boundary Provincial boundary Bella Coola Williams Lake PACIFIC OCEAN F r ase r R Golden Kamloops AL BE R TA Kelowna Scale 100 km km Nanaimo Vancouver Trail Victoria UNITED STATES OF AMERICA Cranbrook Figure 1. Location of the Serpentinite Lakes Property, northern British Columbia. -2-

5 me 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. Serpentinite Lakes Property mn Serpentinite mn Lakes C.J. Greig & Associates mn Ltd. Date:31/10/2008 Serpentinite Lakes Property Regional Location Author: Office: Drawing: R. Greig Scale: 1: Projection: UTM Zone 9 (NAD 83) kilometres River me me me me me me Eagle Eagle Eagle Eagle Eagle Eagle Eagle Eagle Eagle Creek) Kutcho Kutcho (to (to (to (to (to (to (to (to (to Road Boulder Road m mn Dease Lake mn Dease Lake Stewart Hwy CassiarHwy Cassiar mn me me Figure 2. Location of the Serpentinite Lakes Property, northern British Columbia.

6 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. The claims are situated 2 kilometres west of the Serpentinite Lakes, within the Eagle River drainage (fig. 2). The property is snow-covered for part of the year, with field work typically limited to the months of May through October. Relief on the property is approximately 500 metres (1520 m to 2040 m), and the upper reaches of the valleys may be steep (fig. 3). Black Spruce and Balsam are the predominant tree species found on lower reaches of the property, although the majority of it is above tree line, where outcrop exposure is variable. 3.0 Claims The Serpentinite Lakes property (fig.3) consists of a single MTO (Mineral Titles Online) tenure covering a total of 270 hectares. The tenure was staked online by Charles Greig on April 8 th, The property lies within the Liard Mining Division and is in good standing until September 15 th, Geologic Setting & Mineral Occurrences According to the B.C. Government website, the Serpentinite Lakes property is underlain by a northwest-southeast trending body of ultramafic rocks of the Cache Creek Complex (fig. 4). The ultramafics are interpreted as oceanic crustal peridotite, dunite, and pyroxenite which are typically serpentized; the ultramafic rocks have been intruded by granodioritic intrusions. Although there are no documented B.C. Minfile occurrences on the property, the ultramafic rocks in the region are known to host jade, asbestos, and chromium showings. -4-

7 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd me Serplakes me me me mn mn mn mn mn mn mn C.J. Greig & Associates Ltd mn Date:31/10/2008 Serpentinite Lakes Property Claim Location Author: Office: me Drawing: R. Greig Scale: 1: Projection: UTM Zone 9 (NAD 83) Contour Interval: 20m metres 400 Figure 3. Serpentinite Lakes property claim location, Liard Mining Division, northern British Columbia me me

8 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. 6,490,000 mn 6,490,000 mn 6,465,000 mn 470,000 me 475,000 me 485,000 me 490,000 me 495,000 me 470,000 me 475,000 me 480,000 me 485,000 me 490,000 me 495,000 me 6,485,000 mn 6,485,000 mn 6,480,000 mn Stratified Rocks Pleistocene to Holocene Lower Jurassic 6,475,000 mn bimodal volcanic rocks Cache Creek Complex chert, siliceous argillite, 6,470,000 siliciclastic mn rocks Lower Jurassic 6,465,000 mn granodioritic rocks ASB (Asbestos - Cu) POLAR JADE GREEN ROCK (Jade) 6,480,000 mn 465,000 me 465,000 me argillite, greywacke, wacke, conglomerate turbidite Upper Permian to Lower Triassic undivided volcanic rocks Mississippian to Triassic Upper Mississippian to Permian Cache Creek Complex ultramafic rocks Cache Creek Complex ultramafic rocks Intrusive Rocks Author: C.J. Greig & Associates Ltd. Date:5/2/2009 Office: C Greig Drawing: S Flasha JJR (Chromium - Asbestos) 6,475,000 mn 6,470,000 mn 480,000 me Upper Mississippian to Permian Cache Creek Complex granodioritic rocks Scale: 1: Projection: UTM Zone 9 (NAD 83) 0 Serpentinite Lakes Regional Geology 2.5 kilometres 5 Figure 4. Regional geology, showing location of the Serpentinite Lakes property and significant mineral occurrences in northern British Columbia. -6-

9 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. 5.0 Previous Work The Serpentinite Lakes property was held for several years up until April 9, 2007 by Hard Creek Nickel Corporation, who staked the property as a follow-up to a Government Regional Geochemical Survey release (Northcote 2005). According to Northcote (2005), Hard Creek felt that the high Ni and Cu values reported in the RGS data, together with the presence of ultramafic rocks identified by regional mappers, was suggestive of the potential for Ni-Cu-PGE mineralization. Hard Creek undertook a program of silt (28 samples) and contour soil (335 samples at 50 metre spacings at 1600 metres elevation) geochemistry, and decided, mainly on the basis of a lack of sulphur in the ICP in soils, but also because of low PGE numbers, that the potential was not great for PGE-bearing Ni-Cu sulphide mineralization. Hard Creek did find, however, that their soil and stream sediment geochemical sampling returned elevated nickel and copper values, and they outlined several areas of anomalously high nickel. In addition to the Cuand Ni-in-soil anomalies, Hard Creek s Dease Lake-based helicopter pilot, Jim Reed, located a small malachite-chalcocite-chalcopyrite showing, now known as the Reed showing, which was located near the southeastern limit of Hard Creek s survey area, approximately 500 metres away from where some of the best Cu-in-soil anomalies were located. Selected rock samples from the Reed showing returned up to 3% Cu. The most anomalous soil geochemical samples, of which there were several, yielded between 450 and 500 ppm Cu, which was encouraging given that they were an order of magnitude or so above background. Nickel values from these same samples were moderate, and ranged from approximately 300 to approximately 900 ppm Ni; the same area yielded weakly anomalous Pd and Pt, high Mg, and spotty Au (Northcote 2005). Northcote (2005) noted that the Reed showing had not been carefully studied, and that it deserved further -7-

10 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. investigation. He recommended that further sampling, as well as prospecting and a more detailed geological examination, were warranted. Other exploration work conducted not far to the west of the Serpentinite Lakes property was documented by Payne and Fox (1985), and by Moyle (1997). 6.0 Soil Geochemistry In early July 2008, a four person crew collected 133 contour soil geochemical samples from a number of contour lines in the vicinity of the Reed showing, which lies near the centre on the tenure (fig. 5; Appendix I). Three silt geochemical samples were also collected at drainages crossed along the soil traverses (fig. 5; Appendix II). Spacing between the soil samples was approximately 50 metres. In order to keep costs down, initially only every second soil sample was shipped to the lab for analysis, and as such, a total of only 106 of the 133 soil samples which were collected were analyzed. Furthermore, only 8 of the 10 blank samples collected were analyzed. All of the silt samples were sent to the laboratory for analysis. Soil sampling on the Serpentinite Lakes property in 2008 was successful in expanding the area of anomalous copper geochemistry in the vicinity of the Reed showing (fig. 6). The antithetic copper and nickel results show quite clearly that the occurrence of copper is more likely associated with granitic rocks than it is with ultramafic rocks, but the results are nonetheless intriguing, and they do warrant further investigation(figs. 6 and 7). Although the combined dataset is still relatively small, and the coverage incomplete, the soil geochemical results from the two programs are suggestive of a sizeable copper mineralizing system, possibly on a northeast trend, and it appears as if the anomaly remains open in that direction. -8-

11 m me mn mn mn me mn mn me me me me me mn mn mn me mn mn mn KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S005 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S001 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S002 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S003 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8S004 KQRS8T001 KQRS8T001 KQRS8T001 KQRS8T001 KQRS8T001 KQRS8T001 KQRS8T001 KQRS8T001 KQRS8T KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S007 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S008 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S009 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S010 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S017 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S011 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S012 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S014 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S016 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8S018 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8T002 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S013 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S024 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S019 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S020 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S022 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S023 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8S025 KQRS8T003 KQRS8T003 KQRS8T003 KQRS8T003 KQRS8T003 KQRS8T003 KQRS8T003 KQRS8T003 KQRS8T003 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S001 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S002 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S003 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S004 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S005 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S006 MGRS8S007 MGRS8S007 MGRS8S007 MGRS8S007 MGRS8S007 MGRS8S007 MGRS8S007 MGRS8S007 MGRS8S007 KQRS8S006 KQRS8S006 KQRS8S006 KQRS8S006 KQRS8S006 KQRS8S006 KQRS8S006 KQRS8S006 KQRS8S006 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S027 MGRS8S031 MGRS8S031 MGRS8S031 MGRS8S031 MGRS8S031 MGRS8S031 MGRS8S031 MGRS8S031 MGRS8S031 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S026 KQRS8S027 KQRS8S027 KQRS8S027 KQRS8S027 KQRS8S027 KQRS8S027 KQRS8S027 KQRS8S027 KQRS8S027 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S028 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S029 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S012 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S008 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S009 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S010 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S011 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S013 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S026 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S021 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S022 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S023 MGRS8S024 MGRS8S024 MGRS8S024 MGRS8S024 MGRS8S024 MGRS8S024 MGRS8S024 MGRS8S024 MGRS8S024 KQRS8S021 KQRS8S021 KQRS8S021 KQRS8S021 KQRS8S021 KQRS8S021 KQRS8S021 KQRS8S021 KQRS8S021 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S025 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S020 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S014 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S016 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S017 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S018 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S019 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S033 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S032 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S034 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S035 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S036 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S037 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S038 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S040 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S039 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S041 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S042 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S043 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S044 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S046 MGRS8S047 MGRS8S047 MGRS8S047 MGRS8S047 MGRS8S047 MGRS8S047 MGRS8S047 MGRS8S047 MGRS8S047 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S048 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S041 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S042 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S043 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S046 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S047 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S049 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S050 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S051 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S052 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S033 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S028 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S029 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S031 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S032 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S034 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S040 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S035 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S037 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S038 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S039 KQRS8S036 KQRS8S036 KQRS8S036 KQRS8S036 KQRS8S036 KQRS8S036 KQRS8S036 KQRS8S036 KQRS8S036 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S048 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S049 MGRS8S050 MGRS8S050 MGRS8S050 MGRS8S050 MGRS8S050 MGRS8S050 MGRS8S050 MGRS8S050 MGRS8S MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S052 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S055 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S051 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S053 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S054 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S061 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S056 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S057 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S058 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S059 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S062 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S068 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S063 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S064 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S065 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S066 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S067 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S089 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S083 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S084 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S085 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S086 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S087 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S088 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S091 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S076 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S069 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S070 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S071 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S072 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S073 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S074 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S082 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S077 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S078 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S079 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S080 MGRS8S081 MGRS8S081 MGRS8S081 MGRS8S081 MGRS8S081 MGRS8S081 MGRS8S081 MGRS8S081 MGRS8S081 C.J. Greig & Associates Ltd. Serpentinite Lakes Property Silt and Soil Sample Locations 200 metres 400 Silt Soil Projection: UTM Zone 9 (NAD 83) Contour Interval: 20m Drawing: R. Greig Author: Office: 100 Date:31/10/2008 Scale: 1: Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. Figure soil sample locations, Serpentinite Lakes property. -9-

12 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd me me me mn mn mn mn mn mn mn Cu (ppm) to 510 (2) mn 446 to (1) to 446 (4) 71.7 to (5) 1 to 71.7 (11) Cu (ppm) C.J. Greig & Associates Ltd mn 942 to 1,580 (3) 598 to 942 (3) 299 to 598 (5) 156 to 299 (17) 86 to 156 (27) 0 to 86 (54) Date:4/11/2008 Author: Office: Drawing: R. Greig Scale: 1: Serpentinite Lakes Property Soil Geochemistry Cu (ppm) Projection: UTM Zone 9 (NAD 83) Contour Interval: 20m metres me me Figure 6. Copper geochemistry in soil samples, 2005 and 2008, Serpentinite Lakes property. -10-

13 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd me me me mn mn mn mn mn mn mn mn mn Ni (ppm) C.J. Greig & Associates Ltd. 2,350 to 2,990 (3) 2,210 to 2,350 (3) Date:4/11/2008 Author: Serpentinite Lakes Property Soil Geochemistry Cu (ppm) 1,970 to 2,210 (5) 1,680 to 1,970 (17) 885 to 1,680 (27) 2 to 885 (54) Office: Drawing: R. Greig Scale: 1:10000 Projection: UTM Zone 9 (NAD 83) Contour Interval: 20m metres me me Figure 7. Nickel geochemistry in soil samples, Serpentinite Lakes property. -11-

14 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. Where possible, soil samples were collected from the B horizon, at an average depth of approximately 10 to 15 centimetres. A mattock was used to dig the holes, and the soil was placed by hand into standard Kraft paper soil sample bags that were labelled with sample numbers. Control on locations was provided by hand-held GPS, and sample sites were marked with flagging tape labelled with sample numbers. The soil samples were analyzed at ALS Chemex Laboratories in Vancouver, British Columbia. To evaluate reproducibility, 8 blank samples were collected from a common location, inserted in the sample sequence, and sent to ALS Chemex along with the samples collected from the property (Appendix III). The blank samples show very little variability, particularly in the elements of interest. Therefore, the results of the blank sampling, along with the internal lab standards, suggest that the data from ALS Chemex is generally of excellent quality. 7.0 Recommendations Copper-in-soil geochemistry on the Serpentinite Lakes property outlines an area of at least 1 km in its long direction that shows good indications of copper mineralization. The suite of elevated elemental geochemistry in the soils suggests that the most likely source of this mineralization are granitic rocks, and given the relative proximity of the Eaglehead copper porphyry deposit, and the relative ease of access, the anomaly merits follow-up work. Initially, that follow-up work should include further soil geochemical contour sampling to the east and northeast and downslope from the anomalous area, plus reconnaissance prospecting, stream sediment sampling, and mapping. -12-

15 2008 Soil Geochemistry on the Serpentinite Lakes Property, C. J. Greig & Associates Ltd. 8.0 References Moyle, F Prospector s Report On the Snow Group, Liard Mining Division, British Columbia, Canada, NTS Map Sheet 104I/06W, Centered at Latitude N, Longitude W; unpublished report for Cusac Gold Mines Ltd., Demand Gold Ltd., and Pacific Bay Minerals Ltd.; B.C. Ministry of Energy, Mines and Petroleum Resources, Assessment Report #24,936, 32p. Northcote, B.K Reconnaissance Geochemical Survey of the Serp Property, Liard Mining Division, British Columbia; Unpublished Assessment Report on behalf of Hard Creek Nickel Corp.; British Columbia Ministry of Energy and Mines, Assessment Report No. 27,777, 64p. Payne, C. W. and Fox, P.E Geological and Geochemical Report on the Frik 1 to 4, AND #1 and Frak 1, 4 Claims. Unpublished report of Getty Canadian Metals Ltd., Liard Mining Division, NTS 1041/6, 11; 52 28'N 'W; B.C. Ministry of Energy, Mines and Petroleum Resources, Assessment Report #14,006, 36p. -13-

16 Appendix I. Soil Sample Locations & Geochemistry

17 Sample UTME UTMN Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Th Ti Tl U V W Zn ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % ppm % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm % ppm ppm ppm ppm ppm KQRS8S < <10 90 <0.5 < < <10 < < < < < <10 <10 26 <10 63 KQRS8S < < < < <10 < < < <10 <10 64 <10 61 KQRS8S < <2 < <0.5 <2 0.4 < < < < < <10 <10 37 <10 82 KQRS8S DNA KQRS8S < <10 40 <0.5 < < < < <2 5 7 < <10 <10 25 <10 43 KQRS8S DNA KQRS8S < <10 < < <2 6 4 < <10 <10 25 < KQRS8S DNA KQRS8S < < <10 < < < <10 <10 37 <10 67 KQRS8S DNA KQRS8S < < < <10 < < < < <10 <10 34 <10 43 KQRS8S < <10 30 < < <10 < < < < < <10 <10 59 <10 51 KQRS8S < <10 20 < < < < < < < <10 <10 72 <10 55 KQRS8S < <2 <10 20 <0.5 < < < <1 < <2 6 8 < <10 <10 83 <10 58 KQRS8S015 blank < < < < <10 <10 68 < KQRS8S < <10 20 <0.5 < < < < <1 < < < <10 <10 82 <10 93 KQRS8S < <2 <10 20 <0.5 < < < < < < < <10 < <10 71 KQRS8S < <10 20 <0.5 < < <10 < < <1 < < < <10 <10 58 <10 45 KQRS8S < <2 <10 20 <0.5 < < <10 < < < <2 7 5 < <10 <10 59 <10 43 KQRS8S < <10 30 < < <10 < < < < <10 <10 49 <10 48 KQRS8S < <2 <10 10 <0.5 < < <10 < < < <2 5 3 < <10 <10 20 <10 41 KQRS8S < <10 10 < < <10 < < <1 < < < <10 <10 76 <10 41 KQRS8S < <2 <10 10 <0.5 < < <10 < < < < < < <10 <10 79 <10 37 KQRS8S < <10 10 < < < < <1 < <2 7 5 < <10 <10 48 <10 43 KQRS8S < <2 <10 20 <0.5 < < < < < < < < <10 < <10 61 KQRS8S < <10 20 <0.5 < < <10 < < < < < <10 <10 79 <10 41 KQRS8S < <10 20 <0.5 < < <10 < < < < < < <10 <10 58 <10 56 KQRS8S < < < < < < < <10 <10 72 <10 90 KQRS8S <0.005 < < < < < < < < <10 <10 56 <10 61 KQRS8S030 blank < < < < < < <10 <10 72 < KQRS8S < <10 70 <0.5 < < < < < < <10 <10 44 <10 50 KQRS8S < < < < <10 < < < < <10 <10 76 <10 57 KQRS8S < < < < < < < < <10 <10 72 <10 67 KQRS8S < < < < <10 < < < < <10 <10 62 <10 55 KQRS8S < <10 80 <0.5 < < <10 < < < < <10 <10 45 <10 48 KQRS8S < <10 70 <0.5 < < <10 < < < < <10 <10 38 <10 44 KQRS8S < <10 10 <0.5 < < <10 < < < <2 4 2 < <10 <10 13 <10 38 KQRS8S < <10 40 <0.5 < < <10 < < <2 7 7 < <10 <10 41 <10 56 KQRS8S < <10 10 <0.5 < < <10 <1 <0.01 < < < <2 4 1 < <10 <10 16 <10 40 KQRS8S < <2 10 <10 <0.5 < < <10 <1 <0.01 < <1 < < <2 5 1 < <10 <10 9 <10 21 KQRS8S <0.005 < <2 10 <10 <0.5 < < <10 <1 <0.01 < < < <2 6 1 <20 <0.01 <10 <10 13 <10 21 KQRS8S < <2 <10 10 <0.5 < < <10 <1 < <1 < < < <10 <10 14 <10 32 KQRS8S < < < < <10 < < < < <10 <10 45 <

18 KQRS8S044 blank DNA KQRS8S045 blank < < < < < < <10 <10 70 < KQRS8S DNA KQRS8S < <2 <10 30 <0.5 < < <10 < < < <2 6 5 < <10 <10 19 <10 45 KQRS8S DNA KQRS8S < <2 <10 10 <0.5 < < <10 < < < <2 5 2 < <10 <10 15 <10 32 KQRS8S DNA KQRS8S < <2 <10 30 <0.5 < < <10 < < < <2 5 5 < <10 <10 21 <10 51 KQRS8S DNA MGRS8S <0.005 < < < < <10 < < < < <10 <10 41 <10 49 MGRS8S < < < < <10 < < < < <10 <10 38 <10 75 MGRS8S <0.005 < <10 40 <0.5 < < <10 < < <2 7 8 < <10 <10 34 <10 44 MGRS8S DNA MGRS8S < < < < <10 < < < <2 5 3 < <10 <10 14 <10 39 MGRS8S DNA MGRS8S <0.005 < <10 20 <0.5 < < <10 < < <2 5 5 < <10 <10 18 <10 40 MGRS8S DNA MGRS8S < <2 <10 10 <0.5 < < <10 < < <2 5 3 < <10 <10 13 <10 39 MGRS8S DNA MGRS8S < <10 <10 <0.5 < < <10 <1 <0.01 < < < <2 5 1 < <10 <10 12 <10 29 MGRS8S DNA MGRS8S < <2 20 <10 <0.5 < < <10 <1 <0.01 < < < <2 4 1 <20 <0.01 <10 <10 9 <10 35 MGRS8S DNA MGRS8S015 blank < < < < < < < <10 <10 69 < MGRS8S DNA MGRS8S <0.005 < <2 <10 10 <0.5 < < <10 < < < <2 4 2 < <10 <10 14 <10 40 MGRS8S < < <0.5 < < <10 < <1 < < <2 5 3 < <10 <10 16 <10 44 MGRS8S < <0.5 < < <10 < < < <2 7 4 < <10 <10 22 <10 40 MGRS8S < <10 20 <0.5 < < <10 < < < < < <10 <10 56 <10 61 MGRS8S <0.005 < <10 10 <0.5 < < <10 < < < < <2 4 8 < <10 <10 41 <10 31 MGRS8S < <2 <10 <10 <0.5 < < <10 < < <1 < <0.01 <2 6 9 < <10 <10 38 <10 50 MGRS8S < <2 <10 <10 <0.5 < < <10 < < < < <2 7 8 < <10 <10 53 <10 39 MGRS8S < <2 <10 <10 <0.5 <2 0.4 < <10 < < <1 < <0.01 <2 6 8 < <10 <10 33 <10 30 MGRS8S < <10 <10 <0.5 < < <10 < < < < <2 7 4 < <10 <10 44 <10 22 MGRS8S < <2 <10 10 < < <10 < < < < < <10 <10 52 <10 26 MGRS8S < <10 70 <0.5 < < < < < < < <10 <10 90 <10 65 MGRS8S < <10 50 < < <10 < < < < < <10 <10 65 <10 41 MGRS8S < <10 30 <0.5 < < < < < < < <10 <10 80 <10 43 MGRS8S030 blank < < < <10 < < < <10 <10 69 < MGRS8S < < < < < <1 < < < <10 <10 70 <10 52 MGRS8S < <2 <10 60 <0.5 < < <10 < < < < <10 <10 60 <10 54 MGRS8S < <10 40 <0.5 < < < <1 < < < <10 <10 76 <10 52 MGRS8S < <10 40 <0.5 < < <10 < < <2 9 9 < <10 <10 55 <10 54 MGRS8S < <10 40 <0.5 < < <10 < < <0.01 < < <10 <10 47 <10 45 MGRS8S < < < < < < <10 <10 50 <

19 MGRS8S < < < < < < < < <10 <10 44 <10 66 MGRS8S < < < < <10 < < < < <10 <10 59 <10 70 MGRS8S < <2 <10 40 <0.5 < < <10 < < <2 6 7 < <10 <10 32 <10 44 MGRS8S DNA MGRS8S < <2 <10 30 <0.5 < < <10 < < <2 6 5 < <10 <10 29 <10 47 MGRS8S DNA MGRS8S < <2 <10 20 <0.5 <2 0.1 < <10 < <1 < <2 5 3 < <10 <10 17 <10 50 MGRS8S DNA MGRS8S045 blank < < < < < <0.01 < < <10 <10 67 < MGRS8S DNA MGRS8S < <2 <10 50 <0.5 < < <10 < < < < <10 <10 47 <10 58 MGRS8S < <10 60 <0.5 < < <10 < < < < <10 <10 56 <10 60 MGRS8S < <10 70 <0.5 < < <10 < < < < <10 <10 55 <10 51 MGRS8S < <10 40 < < <10 < < < < <10 <10 58 <10 62 MGRS8S <0.005 < <2 <10 40 <0.5 < < <10 < <1 < < < <10 <10 37 <10 44 MGRS8S < <10 20 <0.5 < < <10 < < <2 6 6 < <10 <10 30 <10 45 MGRS8S < <2 <10 40 <0.5 < < < < < < <10 <10 59 <10 58 MGRS8S < <10 80 <0.5 < < <10 < < < <10 <10 64 <10 69 MGRS8S < <2 <10 10 <0.5 <2 0.3 < <10 < < <1 < <0.01 <2 4 5 < <10 <10 59 <10 18 MGRS8S < < < < <10 < < < < <10 <10 57 <10 65 MGRS8S < <2 <10 30 <0.5 < < <10 < < <1 < <0.01 < < <10 <10 40 <10 45 MGRS8S < <10 70 <0.5 < < <10 < < < < <10 <10 36 <10 46 MGRS8S < <2 <10 70 <0.5 < < <10 < < < < <10 <10 45 <10 62 MGRS8S060 blank < < < <10 < < < <10 <10 69 < MGRS8S < <2 <10 40 <0.5 < < <10 < < <1 < <0.01 <2 5 9 < <10 <10 34 <10 34 MGRS8S < <10 70 <0.5 < < <10 < < < < <10 <10 48 <10 55 MGRS8S < <2 <10 40 <0.5 < < <10 < < <1 < <0.01 < < <10 <10 41 <10 40 MGRS8S < <2 <10 40 <0.5 < < <10 < < < < <10 <10 40 <10 50 MGRS8S < <2 <10 20 <0.5 < < <10 < <1 < <0.01 <2 4 4 < <10 <10 20 <10 39 MGRS8S DNA MGRS8S NSS < <2 <10 20 <0.5 < < <10 < <1 < <0.01 <2 5 3 < <10 <10 18 <10 40 MGRS8S DNA MGRS8S NSS < <2 <10 20 <0.5 <2 0.1 < <10 < <1 < <0.01 <2 4 3 < <10 <10 16 <10 40 MGRS8S < <0.5 < < <10 < <1 < < <2 3 2 < <10 <10 12 <10 36 MGRS8S < <0.5 < < <10 < > <1 < <0.01 <2 9 6 < <10 <10 31 <10 54 MGRS8S < <2 <10 10 <0.5 < < <10 < <1 < < <2 4 2 < <10 <10 14 <10 24 MGRS8S NSS < < <0.5 < < <10 < > < < < <10 <10 47 <10 82 MGRS8S < < < <10 < <1 < < <2 5 3 < <10 <10 18 <10 37 MGRS8S075 blank < < < < < <0.01 < < <10 <10 66 < MGRS8S < < <0.5 < < <10 < <1 < <2 6 4 < <10 <10 21 <10 40 MGRS8S <0.005 < <2 <10 20 <0.5 < < <10 < <1 < <0.01 <2 5 4 < <10 <10 18 <10 38 MGRS8S DNA MGRS8S < <2 <10 10 <0.5 < < <10 < < <1 < <0.01 <2 5 2 < <10 <10 16 <10 37 MGRS8S DNA MGRS8S < <2 <10 10 <0.5 < < < < <1 < <0.01 <2 6 3 < <10 <10 17 <

20 MGRS8S DNA MGRS8S NSS < <2 <10 40 <0.5 < < <10 < <1 < <0.01 <2 8 5 < <10 <10 30 <10 47 MGRS8S DNA MGRS8S < <2 <10 70 <0.5 < < <10 < < < < <10 <10 39 <10 57 MGRS8S DNA MGRS8S NSS < <2 <10 40 <0.5 < < <10 < <1 < <0.01 <2 7 3 < <10 <10 25 <10 43 MGRS8S DNA MGRS8S < <2 <10 30 <0.5 < < < <1 < <0.01 <2 5 4 < <10 <10 21 <10 38 MGRS8S090 blank DNA MGRS8S <0.005 < <2 <10 30 <0.5 < < <10 < <1 < <0.01 <2 5 5 < <10 <10 23 <

21 VA Finalized CLIENT : "GREIG - C.J. Greig And Associates Ltd." # of SAMPLES : 75 DATE RECEIVED : DATE FINALIZED : PROJECT : "Serpentinite" CERTIFICATE COMMENTS : "ALL:NSS is non-sufficient sample. " PO NUMBER : " " Au-AA23 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 SAMPLE Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Th Ti Tl U V W Zn DESCRIPTION ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % ppm % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm % ppm ppm ppm ppm ppm KQRS8S < <10 90 <0.5 < < <10 < < < < < <10 <10 26 <10 63 KQRS8S < <2 < <0.5 <2 0.4 < < < < < <10 <10 37 <10 82 KQRS8S < <10 40 <0.5 < < < < <2 5 7 < <10 <10 25 <10 43 KQRS8S < <10 < < <2 6 4 < <10 <10 25 < KQRS8S009 < < <10 < < < <10 <10 37 <10 67 KQRS8S < < < <10 < < < < <10 <10 34 <10 43 KQRS8S < <10 20 < < < < < < < <10 <10 72 <10 55 KQRS8S < < < < <10 <10 68 < KQRS8S < <2 <10 20 <0.5 < < < < < < < <10 < <10 71 KQRS8S < <2 <10 20 <0.5 < < <10 < < < <2 7 5 < <10 <10 59 <10 43 KQRS8S < <2 <10 10 <0.5 < < <10 < < < <2 5 3 < <10 <10 20 <10 41 KQRS8S < <2 <10 10 <0.5 < < <10 < < < < < < <10 <10 79 <10 37 KQRS8S < <2 <10 20 <0.5 < < < < < < < < <10 < <10 61 KQRS8S < <10 20 <0.5 < < <10 < < < < < < <10 <10 58 <10 56 KQRS8S029 <0.005 < < < < < < < < <10 <10 56 <10 61 KQRS8S < <10 70 <0.5 < < < < < < <10 <10 44 <10 50 KQRS8S < < < < < < < < <10 <10 72 <10 67 KQRS8S < <10 80 <0.5 < < <10 < < < < <10 <10 45 <10 48 KQRS8S < <10 10 <0.5 < < <10 < < < <2 4 2 < <10 <10 13 <10 38 KQRS8S < <10 10 <0.5 < < <10 <1 <0.01 < < < <2 4 1 < <10 <10 16 <10 40 KQRS8S041 <0.005 < <2 10 <10 <0.5 < < <10 <1 <0.01 < < < <2 6 1 <20 <0.01 <10 <10 13 <10 21 KQRS8S < < < < <10 < < < < <10 <10 45 <10 69 KQRS8S < < < < < < <10 <10 70 < KQRS8S < <2 <10 30 <0.5 < < <10 < < < <2 6 5 < <10 <10 19 <10 45 KQRS8S < <2 <10 10 <0.5 < < <10 < < < <2 5 2 < <10 <10 15 <10 32 KQRS8S < <2 <10 30 <0.5 < < <10 < < < <2 5 5 < <10 <10 21 <10 51 MGRS8S001 <0.005 < < < < <10 < < < < <10 <10 41 <10 49 MGRS8S003 <0.005 < <10 40 <0.5 < < <10 < < <2 7 8 < <10 <10 34 <10 44 MGRS8S < < < < <10 < < < <2 5 3 < <10 <10 14 <10 39 MGRS8S007 <0.005 < <10 20 <0.5 < < <10 < < <2 5 5 < <10 <10 18 <10 40 MGRS8S < <2 <10 10 <0.5 < < <10 < < <2 5 3 < <10 <10 13 <10 39 MGRS8S < <10 <10 <0.5 < < <10 <1 <0.01 < < < <2 5 1 < <10 <10 12 <10 29 MGRS8S < <2 20 <10 <0.5 < < <10 <1 <0.01 < < < <2 4 1 <20 <0.01 <10 <10 9 <10 35 MGRS8S < < < < < < < <10 <10 69 < MGRS8S017 <0.005 < <2 <10 10 <0.5 < < <10 < < < <2 4 2 < <10 <10 14 <10 40 MGRS8S < <0.5 < < <10 < < < <2 7 4 < <10 <10 22 <10 40 MGRS8S021 <0.005 < <10 10 <0.5 < < <10 < < < < <2 4 8 < <10 <10 41 <10 31 MGRS8S < <2 <10 <10 <0.5 < < <10 < < < < <2 7 8 < <10 <10 53 <10 39 MGRS8S < <10 <10 <0.5 < < <10 < < < < <2 7 4 < <10 <10 44 <10 22 MGRS8S < <10 70 <0.5 < < < < < < < <10 <10 90 <10 65 MGRS8S < <10 30 <0.5 < < < < < < < <10 <10 80 <10 43 MGRS8S < < < < < <1 < < < <10 <10 70 <10 52 MGRS8S < <10 40 <0.5 < < < <1 < < < <10 <10 76 <10 52 MGRS8S < <10 40 <0.5 < < <10 < < <0.01 < < <10 <10 47 <10 45 MGRS8S < < < < < < < < <10 <10 44 <10 66 MGRS8S < <2 <10 40 <0.5 < < <10 < < <2 6 7 < <10 <10 32 <10 44 MGRS8S < <2 <10 30 <0.5 < < <10 < < <2 6 5 < <10 <10 29 <10 47 MGRS8S < <2 <10 20 <0.5 <2 0.1 < <10 < <1 < <2 5 3 < <10 <10 17 <10 50 MGRS8S < < < < < <0.01 < < <10 <10 67 < MGRS8S < <2 <10 50 <0.5 < < <10 < < < < <10 <10 47 <10 58 MGRS8S < <10 70 <0.5 < < <10 < < < < <10 <10 55 <10 51 MGRS8S051 <0.005 < <2 <10 40 <0.5 < < <10 < <1 < < < <10 <10 37 <10 44 MGRS8S < <2 <10 40 <0.5 < < < < < < <10 <10 59 <10 58 MGRS8S < <2 <10 10 <0.5 <2 0.3 < <10 < < <1 < <0.01 <2 4 5 < <10 <10 59 <10 18 MGRS8S < <2 <10 30 <0.5 < < <10 < < <1 < <0.01 < < <10 <10 40 <10 45 MGRS8S < <2 <10 70 <0.5 < < <10 < < < < <10 <10 45 <10 62 MGRS8S < <2 <10 40 <0.5 < < <10 < < <1 < <0.01 <2 5 9 < <10 <10 34 <10 34 MGRS8S < <2 <10 40 <0.5 < < <10 < < <1 < <0.01 < < <10 <10 41 <10 40 MGRS8S < <2 <10 20 <0.5 < < <10 < <1 < <0.01 <2 4 4 < <10 <10 20 <10 39 MGRS8S067 NSS < <2 <10 20 <0.5 < < <10 < <1 < <0.01 <2 5 3 < <10 <10 18 <10 40 MGRS8S069 NSS < <2 <10 20 <0.5 <2 0.1 < <10 < <1 < <0.01 <2 4 3 < <10 <10 16 <10 40 MGRS8S < <0.5 < < <10 < > <1 < <0.01 <2 9 6 < <10 <10 31 <10 54 MGRS8S073 NSS < < <0.5 < < <10 < > < < < <10 <10 47 <10 82 MGRS8S < < < < < <0.01 < < <10 <10 66 < MGRS8S077 <0.005 < <2 <10 20 <0.5 < < <10 < <1 < <0.01 <2 5 4 < <10 <10 18 <10 38 MGRS8S < <2 <10 10 <0.5 < < <10 < < <1 < <0.01 <2 5 2 < <10 <10 16 <10 37 MGRS8S < <2 <10 10 <0.5 < < < < <1 < <0.01 <2 6 3 < <10 <10 17 <10 38 MGRS8S083 NSS < <2 <10 40 <0.5 < < <10 < <1 < <0.01 <2 8 5 < <10 <10 30 <10 47 MGRS8S < <2 <10 70 <0.5 < < <10 < < < < <10 <10 39 <10 57 MGRS8S087 NSS < <2 <10 40 <0.5 < < <10 < <1 < <0.01 <2 7 3 < <10 <10 25 <10 43 MGRS8S < <2 <10 30 <0.5 < < < <1 < <0.01 <2 5 4 < <10 <10 21 <10 38 MGRS8S091 <0.005 < <2 <10 30 <0.5 < < <10 < <1 < <0.01 <2 5 5 < <10 <10 23 <10 36 KQRS8T < <2 <10 40 <0.5 < < <10 < <1 < < < <10 <10 31 <10 45 KQRS8T < <2 <10 20 <0.5 < < < <1 < <0.01 <2 7 8 < <10 <10 38 <10 35 KQRS8T < <2 <10 10 <0.5 <2 0.5 < < < <1 < <0.01 <2 6 8 < <10 <10 44 <10 36