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Drillhole Log-MQ-13-011 Drillhole Log Units Meters North American Nickel Inc. Hole Type North American Nickel hole Claim/Permit 2011/54 Length 101.00 Project Maniitsoq District Date Started 27/06/2013 Province/State/Region Area Greenland, Maniitsoq Area Date Completed 28/06/2013 Zone/Prospect Collar Survey Hand-held GPS Date Logged 28/06/2013 Co-ordinate System UTM WGS84 Greenland Zone 22 UTM North 7216150 Local Grid E Azimuth Grid (°) Grid ID UTM East 461980 Local Grid N Azimuth Astro. (°) 189.00 NTS Sheet UTM Elevation 285.00 Grid Elevation Dip (°) -50.00 Logged By Johan D. Krebs Core Storage Nuuk Project Supervisor Jim Sparling Core Size BTW Finalized Drill Contractor Westcore Core Reduction(s) 1> 100.25 2> By Casing 1 Steel 1.20 Distance Azimuth (°) Dip (°) Use Survey MethodMag. Field Comments Casing 2 Grid Astronomic Test (nT) Casing Pulled 0.00184 -50 Compass Makes Water 22.00189.5 -50.6 Reflex EZ 5328 Plugged Plug Depth 52.00187.1 -50.3 Reflex EZ 5472 Capped 82.00188.3 -49.8 Reflex EZ 5471 Pulsed Pulse Depth 101.00 Geophysics Contractor Crone Geophysics Purpose Testing Maxwell plate, anomaly P97 Results Comments MQ-13-011 Page 1 of 8 Lithology Ni Cu Co Pt Pd Au S From To Sample # From To Len. ppm ppm ppm ppb ppb ppb % 0.00- 0.75 0100 Casing/overburden BTW casing, no grout 0.75- 20.33 1920 Granodiorite Granodiorite intrusive. N236016 15.00 17.002.0037 15 15 2.5 0.5 0.5 0.07 Leuco to mesocratic, medium grained, massive, non to poorly N236017 17.00 17.960.9688 14 22 2.5 0.5 0.5 0.04 foliated, unit is moderate to weakly magnetic throughout. Locally N236018 17.96 19.001.04238 19 36 2.5 0.5 0.5 0.04 sections with up to 2-3% magnetite occur. Few cm sized k-spar rich pegmatite veins are hosted within the unit. First meter of unit carries N236019 19.00 20.331.33289 34 37 2.5 0.5 0.5 0.08 a weak foliation Average composition of unit. Plagiclase (labadorite) 50-60% Quartz 40-50% Biotite 3-5% Magnetite 0.5-1% Lower contact is gradational, but seems to be @ 62deg TCA Structure: 1.00- Foliation 52° to c/a Moderate foliation MQ-13-011 Page 2 of 8 Lithology Ni Cu Co Pt Pd Au S From To Sample # From To Len. ppm ppm ppm ppb ppb ppb % 20.33- 31.76 1500 Norite / Gabbronorite Norite N236020 20.33 22.001.6768 69 30 2.5 0.5 0.5 0.18 Mesocratic, dark green, medium to fine grained, non foliated, N236021 22.00 24.002.0089 76 31 2.5 0.5 0.5 0.18 massive. Unit is moderately magnetic through out. Unit carriers 5- N236022 24.00 25.651.65518 51 55 2.5 0.5 0.5 0.13 10% leucocratic labradorite rich cm thick veins. Over all these veins have a composition similar to the granodiorite intrusive described N236023 25.65 27.001.35200 69 34 2.5 10.5 0.12 above. Magnetite and biotite is higher at the contact between the N236024 27.00 28.281.28143 77 21 2.5 0.5 0.5 0.14 granodiorite veins and the norite. N236025 28.28 29.741.46400 130 49 2.5 12 0.24 Average composition of the norite: N236026 29.74 31.001.26589 191 61 5 10.5 0.33 Plagioclase (labradorite) 50-60% N236027 31.00 31.760.76871 272 78 7 22 0.49 Pyroxene 30% Hornblende 1-5% Biotite 1-5% (only found at contact with granodiorite veins) Trace, Po, Py and Cpy Lower contact is fairly sharp @ 38deg TCA Structure: 20.33- Contact 62° to c/a unit contact MQ-13-011 Page 3 of 8 Lithology Ni Cu Co Pt Pd Au S From To Sample # From To Len. ppm ppm ppm ppb ppb ppb % 31.76- 35.98 1530 Norite / gabbronorite with weak sulphides - up to 5% total Sulphides N236028 31.76 32.490.731020 397 83 13 42 0.71 Norite with up to 5% total sulphides N236029 32.49 33.501.011250 513 80 14 55 0.95 Mineralized norite N236031 33.50 34.000.50673 201 57 10 31 0.36 Mesocratic, dark green,medium to fine grained, non foliated, N236032 34.00 34.730.732210 724 111 50 21 14 1.54 massive, unit moderate to strongly magnetic (strongly magenetic arround sulphide blebs). As previous norite unit described above unit N236033 34.73 35.530.802870 769 135 70 29 12 1.93 carries 5-10% leucocratic labradorite rich veins of similar composition N236034 35.53 35.980.453150 1110 135 64 32 20 2.2 to the granodiorite intrusive described at the beginning of the hole. The mineralized norite has a composition and texture similar to previously described norite less the sulphides. The sulphides occor as isolated frothy blebes consisting of Po, Py and Cpy. The sulphides of the individual frothy blebs are interconected over distances of 20- 30mm howere the blebs are isolated from one another (tested withn ohm-meter) Average composition of mineralized norite: Plagioclase (labradorite) 50-60% Pyroxene 30% Hornblende 1-5% Biotite 1-5% (only found at contact with granodiorite veins) 2% Po as frothy blebs 2% Py as frothy blebs 0.5-1% Cpy as fine disseminated grains witin the frothy Py-Po blebs. Structure: 31.76- Contact sharp 38° to c/a unit contact MQ-13-011 Page 4 of 8 Lithology Ni Cu Co Pt Pd Au S From To Sample # From To Len. ppm ppm ppm ppb ppb ppb % 35.98- 63.00 1500 Norite / Gabbronorite Norite N236036 35.98 37.001.02310 61 30 2.5 20.5 0.13 Mesocratic, dark green, medium to fine grained, non foliated, N236037 37.00 38.001.00388 57 48 2.5 10.5 0.13 massive. Unit is moderately magnetic through out. Unit carriers 2-5% N236038 38.00 39.001.00410 77 52 2.5 10.5 0.15 leucocratic labradorite rich cm think veins. Over all these veins have a composition similar to the granodiorite intrusive described in the N236039 39.00 40.001.00547 177 52 8 21 0.18 beginning of the hole. N236040 40.00 41.001.00748 222 69 10 41 0.4 N236041 41.00 42.001.00595 237 69 5 24 0.31 Average composition of the norite: Plagioclase (labradorite) 50-60% N236042 42.00 44.002.00449 81 59 2.5 10.5 0.16 Pyroxene 30% N236043 44.00 46.002.00471 85 62 5 10.5 0.15 Hornblende 1-5% N236044 46.00 48.002.00460 84 59 2.5 10.5 0.15 Biotite 1-5% (only found at contact with granodiorite veins) N236045 48.00 50.002.00472 87 60 2.5 10.5 0.15 Trace, Po, Py and Cpy as local blebs N236046 50.00 52.002.00461 88 61 5 10.5 0.16 Lower contact is faulted and sharp @ 35deg TCA N236047 52.00 54.002.00449 81 62 2.5 10.5 0.19 N236048 54.00 56.002.00332 47 43 2.5 10.5 0.1 N236049 56.00 58.002.00469 88 59 8 21 0.16 N236051 58.00 60.002.00367 60 48 8 30.5 0.12 N236052 60.00 62.002.00452 63 60 6 10.5 0.14 N236053 62.00 63.001.00316 43 45 5 10.5 0.08 Structure: 35.98- Contact sharp 62° to c/a unit contact 63.00- 76.42 0300 Fault - Brecciated Fault zone N236054 63.00 64.001.0063 6 10 2.5 0.5 0.5 0.01 Fault zone starting off with pegmatite followed by a gabbro rich N236056 64.00 65.001.00422 59 53 6 20.5 0.1 section, grading into a cataclastite ending with a section of mylonitic N236057 65.00 66.321.3266 2 9 2.5 0.5 0.5 rock. See minor litho for details N236058 66.32 67.000.68463 83 56 5 10.5 0.06 Lower contact sharp @ 60deg TCA N236059 67.00 68.001.00421 68 55 2.5 10.5 0.08 N236060 68.00 69.221.22374 66 46 2.5 10.5 0.09 63.00- 66.32 0900 Pegmatite - Massive Pegmatite Leucocratic, pink, coarse grained, massive, non foliated. MQ-13-011 Page 5 of 8 Lithology Ni Cu Co Pt Pd Au S From To Sample # From To Len. ppm ppm ppm ppb ppb ppb % Composition Quartz 40% Plagioclase 40% K-spar 15% Biotite 5% 66.32- 69.22 1400 Gabbro - mod-intensely Altered Mesocratic, dark green, fine to medium grained, massive, non foliated, brecciated. Average composition Hornblende 60% Plagioclase 30% Biotite 5% minor trace Py 69.22- 71.68 0320 Gouge Fault Section with cataclastic fabric, protolith likely same gabbro as described above. The rock is so ground up that it beginning to develop a new foliation 71.68- 76.42 0200 Mylonite Mylonitic section, mixture of gabbro and pegmatite fragments. Lower contact is sharp. Structure: 63.00- Contact sharp 35° to c/a Fault contact 66.32- Contact sharp Sharp contact between gabbro and pegmatite 71.00- Foliation 55° to c/a Foliation caused by faulting, fine grained cataclastite 74.00- Foliation 54° to c/a Foliation casused by faulting, fine grained cataclastite. MQ-13-011 Page 6 of 8 Lithology Ni Cu Co Pt Pd Au S From To Sample # From To Len.
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