GRAVITY WEST MINING CORP. MACKENZIE JAIMS

Transcription

1 GRAVITY WEST MINING CORP. MACKENZIE JAIMS REPORT ON PHASE 2 - Chief Bay Road & Drake Hill Areas DIAMOND DRILLING PROGRAM VOLTAIRE LAKE PROPERTY, DISTRICT OF THUNDER BAY, ONTARIO by Colin Bowdidge, Ph.D., P.Geo., and Dawn-Ann Metsaranta, M.Sc.,

2 Table of Contents Introduction... 3 Property, Location and Access... 3 History... 8 Nickel-Copper-PGE Exploration in the Nipigon-Sibley Basin... 8 Lake Nipigon Geoscience Initiative... 8 Post-LNGI Exploration... 9 Uranium Exploration in the Sibley Basin... 9 Geology Diamond Drilling Program Chief Bay Road Area Drilling Drake Hill Area Drilling Discussion and Conclusions Figures: 1: Ontario Location Map 2: Claim Map 3: Geology 4: Drill hole locations, Plan View 5: Inverted EM data and Geology Interpretation Appendix A: Diamond drill hole logs Appendix B: Assay Certificates Plates: Cross Sections of diamond drill holes 2

3 Introduction This report summarizes the winter diamond drilling program carried out by Gravity West Mining Corp. and Mackenzie Jaims in the Voltaire Lake area. This second phase of drilling followed up on Phase 1 drilling completed during the fall of 2007 and took place from October 2007 to February 2008, totaling meters. The drilling focused on two areas, the Drake Hill area and the Chief Bay road area. Drilling in the Chief Bay area attempted to intersect a section of the Black Sturgeon fault as interpreted from modeling of VTEM data. Drilling in the Drake Hill area followed up on Cu-Ni-PGE mineralization encountered in hole VL-07-03A from Phase 1 of drilling. Property, Location and Access The Voltaire Lake property consists of 130 mining claims comprising 1822 claim units. Table 1 lists these claims. The recorded holders are Mackenzie Jaims and Gravity West Mining Corp. The claims in the area of the Phase 2 - diamond drilling program are shown in Figure 2. Figure 1 shows the general location of the Voltaire Lake property which lies in the Voltaire Lake, Candide Lake, Kitchen Lake, Ruffo Lake, Chief Bay, Caribou Island and Grand Bay areas of the Thunder Bay mining Division, Ontario. The property is about 130 km north of the city of Thunder Bay. Assess is by provincial highways 527 and 811, and a network of active and non-active logging roads. 3

4 TABLE 1: List of Claims for Gravity West Mining Corp. Claim # Record Date Expriy Date Claim Sheet No. of Units Ass. Work Required /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 8 $3, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 15 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 4 $1, /31/ /31/2007 Kitchen Lake 15 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 5 $2, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Kitchen Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Candide Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6,400 4

5 /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Voltaire Lake 16 $6, /31/ /31/2007 Kitchen Lake 6 $2, /5/2006 5/5/2008 Kitchen Lake 7 $2, /1/2006 5/1/2008 Kitchen Lake 8 $3, /5/2006 5/5/2008 Kitchen Lake 16 $6, /1/2006 5/1/2008 Kitchen Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 6 $2, /1/2006 5/1/2008 Ruffo Lake 4 $1, /1/2006 5/1/2008 Ruffo Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 11 $4, /1/2006 5/1/2008 Ruffo Lake 11 $4, /1/2006 5/1/2008 Ruffo Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 16 $6, /1/2006 5/1/2008 Ruffo Lake 7 $2, /1/2006 5/1/2008 Kitchen Lake 5 $2, /24/2006 5/24/2008 Voltaire Lake 16 $6, /24/2006 5/24/2008 Voltaire Lake 16 $6, /24/2006 5/24/2008 Chief Lake 15 $6, /24/2006 5/24/2008 Chief Lake 11 $4, /24/2006 5/24/2008 Voltaire Lake 16 $6, /24/2006 5/24/2008 Voltaire Lake 16 $6, /24/2006 5/24/2008 Voltaire Lake 13 $5, /24/2006 5/24/2008 Voltaire Lake 15 $6, /24/2006 5/24/2008 Voltaire Lake 14 $5, /10/2006 7/10/2008 Voltaire Lake 15 $6, /24/2006 5/24/2008 Voltaire Lake 16 $6,400 5

6 /24/2006 5/24/2008 Voltaire Lake 16 $6, /24/2006 5/24/2008 Voltaire Lake 16 $6, /24/2006 5/24/2008 Voltaire Lake 11 $4, /24/2006 5/24/2008 Voltaire Lake 14 $5, /10/2006 7/10/2008 Voltaire Lake 8 $3, /10/2006 7/10/2008 Voltaire Lake 13 $5, /10/2006 7/10/2008 Voltaire Lake 15 $6, /10/2006 7/10/2008 Voltaire Lake 13 $5, /14/2007 8/14/2009 Voltaire Lake 5 $2, /14/2007 8/14/2009 Caribou Lake 11 $4, /14/2007 8/14/2009 Voltaire Lake 15 $6, /14/2007 8/14/2009 Caribou Lake 14 $5, /14/2007 8/14/2009 Voltaire Lake 16 $6, /14/2007 8/14/2009 Caribou Lake 10 $4, /14/2007 8/14/2009 Voltaire Lake 16 $6, /14/2007 8/14/2009 Caribou Lake 16 $6, /14/2007 8/14/2009 Caribou Lake 3 $1, /14/2007 8/14/2009 Voltaire Lake 16 $6, /14/2007 8/14/2009 Caribou Lake 16 $6, /14/2007 8/14/2009 Caribou Lake 5 $2, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 16 $6, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 16 $6, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 4 $1, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 8 $3, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 16 $6, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 4 $1, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 15 $6, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 13 $5, /14/2007 8/14/2009 Grand Lake (Lake Nipigon) 3 $1, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 16 $6, /1/2008 2/1/2010 Voltaire Lake 7 $2, /1/2008 2/1/2010 Voltaire Lake 14 $5, /1/2008 2/1/2010 Voltaire Lake 14 $5, /15/ /15/2009 Voltaire Lake 16 $6,400 6

7 360,000 me 350,000 me 340,000 me 330,000 me 320,000 me 5,510,000 mn ,500,000 mn ,490,000 mn LEGEND Phase 1 - Diamond Drilling Program - Fall Phase 2 - Diamond Drilling Program. Winter GRAVITY WEST MINING CORP Date:21/5/2008 Author: D.Metsaranta Voltaire Lake Project Phase 2 Diamond Drilling Program Winter Office: T.Bay Figure 2 - Claim Map Drawing: Scale: 1: ,480,000 mn Projection: UTM Zone 16 (NAD 83) kilometres 5

8 History The property has seen little in the way of previous exploration. The western part of the property covers exposed Archean basement, specifically the eastern end of the Garden Lake greenstone belt. Like most greenstone belts in the Canadian Shield, it has been explored in the past for gold and base metals. However, none of this prior work has taken place in or near the Voltaire Lake property, and so will not be referred to here. Nickel-Copper-PGE Exploration in the Nipigon-Sibley Basin In 1997, Robert Fairservice, a Thunder Bay prospector, discovered platinum-group element (PGE) mineralization in a weathered peridotite near Seagull Lake, 75 km southeast of the Voltaire Lake property. This discovery led to widespread exploration for nickelcopper-pge mineralization in the Nipigon basin. These programs invariably targeted airborne magnetic and/or electromagnetic anomalies. A number of Proterozoic mafic to ultramafic intrusions were discovered which had previously not been recognized. Two programs were carried out in the area of the present property. In 2002, Gitennes Exploration Inc. tested a coincident magnetic-electromagnetic anomaly that straddles the western boundary of claim Ground magnetic and EM surveys were carried out to define the anomaly and three drill holes were put down. All three holes intersected mafic volcanics, tuffs, clastic metasediments and magnetite-chertsulphide iron formation interbedded with pyrite-rich graphitic argillite. All sulphidebearing material was analysed and no anomalous gold, PGE or base metal values were returned. In 2001, Canplats Resources Corp. and Colby Resources Corp. drilled five airborne EM anomalies near the eastern end of the main claim block of the present property. One of these holes was abandoned in overburden or weathered bedrock, and one cut only diabase and gabbro (possible an Archean gabbro in the basement, but this cannot be positively determined from the drill log). Three holes penetrated the diabase sill and (in two cases) underlying Sibley sediments and entered Archean basement. Of these three holes, JP cut biotite schist, and JP cut mafic volcanics with a band of magnetite-chert iron formation and graphitic argillite, and GR-01 cut granite gneiss. No anomalous metal contents were detected in the samples sent for analysis. The depth to basement information from this drilling is pertinent and useful information for the present program, showing that the basement lies well within the depth penetration capabilities of modern time-domain EM systems. Lake Nipigon Geoscience Initiative Largely as a consequence of the discovery of magmatic sulphide mineralization in the Seagull intrusion and the intense exploration activity for PGEs that followed, the Lake Nipigon Geoscience Initiative (LNGI) was conceived. The LNGI was a multi-year (2002 8

9 to 2005), multidisciplinary study of the Lake Nipigon area, focusing on the Sibley basin and especially on magmatic events within the basin. The LNGI was funded by the Northern Ontario Heritage Fund Corporation and managed by the Ontario Prospectors Association. It drew on the technical resources of the Ontario Geological Survey (OGS), Lakehead University and the Geological Survey of Canada. Although the uranium potential of the Sibley basin was not an issue when the LNGI began, much of the data generated by the LNGI was of a general nature and can be used to help select targets for uranium exploration. These included: the first detailed geological maps of much of the Sibley Basin; a high resolution airborne magnetic and gamma-ray spectrometer survey; detailed lake-sediment geochemical surveys; a medium-resolution gravity survey; a comprehensive synthesis of the stratigraphy and structure of the Sibley basin; and audiofrequency magneto-telluric profiling of the Sibley basin. The recent geological mapping of the Garden Lake belt by the OGS was not part of the LNGI, but was part of the government activity that resulted from the renewed interest in the area. The LNGI project area covers the eastern part of the Voltaire Lake property. An additional source of data is an airborne magnetic-em survey carried out by the OGS in 1999 over the Garden Lake and Obonga Lake greenstone belts (OGS, 2003), which covers the western part of the Voltaire Lake property. Post-LNGI Exploration One salient result of the LNGI was the discovery of a prominent positive gravity anomaly in the Kitchen Lake area. This anomaly occupies most of the area of the Stares Contracting Corp. claims (see fig. 3), but also extended somewhat further to the west, where Robert Fairservice held claims that expired in In 2004, he carried out prospecting, but located only outcrops of Nipigon diabase. In 2005, Rampart Ventures Ltd. Optioned the Stares Contracting Corp. claims and drilled a single hole (KL05-01) into the axis of the gravity anomaly. It passed through an unusually thick diabase sill and underlying Sibley sediments before entering the basement, which consisted of mafic volcanics without mineralization. Uranium Exploration in the Sibley Basin In the late 1970s and early 1980s, the unconformity-related uranium deposit model that had emerged from the Athabasca basin became better understood, exploration activities for uranium started to spread to other mid-proterozoic sedimentary basins. During this period a number of exploration programs were carried out in the Sibley basin, but it must be observed that, considering its relative accessibility, the Sibley basin was, and still remains, the least-explored of all such basins in Canada. All of the uranium exploration in that era took place well to the south of Voltaire Lake, and there is no documentary evidence that the Voltaire Lake property was ever prospected for uranium. 9

10 Since 2005, there has been renewed interest in the uranium potential of the Sibley basin. Companies active in the area include RPT Uranium Corp. (formerly Rampart Ventures Ltd.), Mega Uranium Ltd. and Benton Resources Ltd. with its partners Grandcru Resources Corp. and Tri-Gold Resources Corp. Geology The western part of the property covers the eastern end of the Garden Lake greenstone belt, a typical volcano-sedimentary belt of the Wabigoon subprovince, a structural domain within the Superior province. The eastern part of the property lies in the Sibley- Nipigon basin. Basement rocks are covered by flat-lying Sibley group sediments of mid- Proterozoic age, which are in turn intruded by Nipigon diabase sills of Keweenawan age. Diabase is the outcropping lithology over most of the basin part of the property. The eastern claim block of the Voltaire Lake property covers part of the Black Sturgeon fault. This is a structure that was active during and after the deposition of the Sibley sediments. It divides the Sibley basin into a two parts: a thicker western section and a much thinner eastern section. The fault has a substantial downthrow to the west, possibly several hundred meters. Figure 3 is a geological map taken from the Geology of Ontario. 10

11 E 360,000 me 350,000 me 340,000 me 330,000 me 320,000 me 5,520,000 mn GEOLOGICAL LEGEND Nipigon sills : Diabase sills Metamorphosed Felsic to intermediate intrusive rocks Mafic to intermediate metavolcanic rocks Tonalite to Granodiorite Foliated-Archean Intrusive Rocks Phase 2-Diamond Drilling Program Winter Phase 1-Diamond Drilling Program Fall ,510,000 mn Gravity West Mining Corp. Claim outline. Holes VL and VL ,500,000 mn Holes VL to VL ,490,000 mn GRAVITY WEST MINING CORP Voltaire Lake Project PHASE 2 Diamond Drilling Program Date:21/5/2008 Author: D.Metsaranta Figure 3 GEOLOGY MAP Office: T.Bay Drawing: Scale: 1: Projection: UTM Zone 16 (NAD 83) kilometres kilometres 55

12 Diamond Drilling Program Table 2 gives a summary of the Phase 2 diamond drilling program. The program consisted of eight drill holes totaling meters. Holes VL to VL were drilled in the Chief Bay Road Area. These holes were drilled vertically along a roughly east-west line running perpendicular to the interpreted strike of the Black Sturgeon Fault. Holes VL and VL were drilled in the Drake Hill area at the same location as hole VL-07-03A which contained promising Cu-Ni and PGE assays. All drilling was completed by Discovery Diamond Drilling Ltd. of Morinville, Alberta and Dorion, Ontario. Figure 4 shows the drill hole locations with topography in plan view. Drill Logs are given in appendix A, assay certificates are in appendix B and cross sections are attached. Table 2- Summary of Phase 2-Diamond Drilling Program at Voltaire Lake Hole ID Easting Northing Elevation (m) Azimuth Dip Depth (m) Date Started Date finished VL Oct. 21, 2007 Nov. 1, 2007 VL Nov. 2, 2007 Nov. 3, 2007 VL Nov. 4, 2007 Nov. 26, 2007 VL Nov. 27, 2007 Nov. 29, 2007 VL Nov. 29, 2007 Jan. 25, 2008 VL Dec. 3, 2007 Dec. 8, 2007 VL Feb. 1, 2008 Feb. 8, 2008 VL Feb. 9, 2008 Feb. 16, 2008 Chief Bay Road Area Drilling Holes VL to VL were drilled in attempt to locate the Black Sturgeon Fault, a major regional fault structure that appears to cross through the area. The target area was selected based on a conductivity-depth section derived from VTEM data by Condor Consulting Ltd. using Layered Earth proprietary software on license to Condor, which was interpreted to show a major offset of Sibley Group sedimentary rocks and diabase sills (Figure 5). The planned strategy employed to locate the fault was to drill holes on both sides of the interpreted fault structure and then to use the elevation differences between major contacts such as the Sibley Group/Archean unconformity as a vector to the actual fault location. VL was drilled to a depth of meters. VL intersected overburden to meters followed by Sibley Group sediments to meters, the hole then encountered a thick diabase sill to a depth of meters where the hole passed thorough Sibley Group sediments to and then entered Archean basement rocks consisting of hematized and fractured granite. 12

13 VL was drilled 100 meters to the east of VL After 3.90 meters of overburden (diabase boulders) hole VL passed through Sibley Group Sediments from 3.90 to 7.18 m then diabase, ending at meters. The next hole was drilled 100 meters to the west of VL Hole VL passed through meters of overburden, followed by Sibley Group sandstone to meters where it then entered magnetic Sibley Group sandstone to meters. The hole then entered and diabase, ending at a depth of meters. VL was drilled 200 meters east of VL VL intersected meters of diabase; it then entered Sibley Group sandstone until meters where it then entered a small section of diabase to a depth of meters. The hole intersected Sibley sandstone from to meters, followed by another section of diabase to m, then back into sandstone to meters, with more diabase until meters. One last section of sandstone was intersected at to meters with the hole ending in diabase at meters. VL was drilled in between holes VL and VL-07-09, approximately 150 meters east of VL It passed through meters of overburden, then diabase to a depth of meters, followed by two packages of Sibley Group Sediments, the first was sandstone from to meters and the second from to meters which were magnetic sediments. VL then penetrated a diabase sill to the bottom of the hole ending at meters, with a small Sibley sandstone package at to meters. The hole was abandoned because the drill rods became stuck. Hole VL was drilled in the middle of VL and VL-07-06, just 50 meters east of VL VL cut diabase to a depth meters, followed by Sibley Group Sediments to meters, it then passed through a thin diabase sill and entered back onto Sibley Group sediments from to meters. The hole then entered a thick diabase sill to a depth of meters. The hole then passed through Sibley sandstone to a depth meters where it intersected the unconformity. Basement rocks consisted of altered granite and the hole was stopped at meters. Drilling of holes VL to VL did not succeed in intersecting what might be a simple Fault. However, it does show the possibility of a more complex fault system with a number of smaller structures. Based on the cross-section of the drill holes, a significant elevation difference between the unconformity elevation in VL and VL may exist and could represent the fault. However, as VL was abandoned before it intersected the unconformity, and the exact magnitude of the elevation difference remains unknown. Much more geologic information could have been gained through drilling all of the holes through to the Archean basement rocks. Drake Hill Area Drilling VL and VL were designed to follow up mineralization present in VL-07-03A drilled during the Phase 1 drill program and to explain a VTEM conductor that was 13

14 not clearly intersected by VL-07-03A. All three holes were collared at the same location and 157 degree azimuth with VL-07-03A drilled at a 60 degrees dip, VL drilled at a 50 degree dip and VL at a 70 degree dip. Hole 12 cut diabase from 6.39 to metres and Sibley Group sedimentary rocks from to the unconformity at metres. Basement rocks consisted of metagabbro to pyroxenite with a minor felsic to intermediate phase to a depth of , followed by: a siliceous, sulfide bearing cherty unit to metres, a sulfide-rich graphitic schist with quartz veining to metres, a mix of mafic metavolcanic rocks and felsic to intermediate intrusive to , a second graphitic unit including massive pyrrhotite to metres and diorite to the end of the hole at metres. 262 samples were sent for assay with a few returning Cu, Ni and Zn assays in the few thousand range. All assay results are shown on the logs in Appendix A. Hole 13 cut diabase from 2.30 to metres and Sibley Group sandstone from to the unconformity at metres. Basement rocks consisted of pyroxenite to metres followed by a porphyritic mafic intrusion to metres, diorite to metres, a sulfide-rich breccia to metres, diorite with a minor diabase intrusion to metres, another sulfide-rich breccia zone to metres and diorite to the end of the hole at metres. 50 samples were sent for assay and again several sections returned assays up to a few thousand Cu, Ni or Zn. The highest grade samples included Cu over 0.30 metres and another assayed Cu over 0.28 metres. Again all assay results are shown on the logs in Appendix A. 14

15 27 5,504,000 mn 346,000 me 348,000 me 350,000 me 352,000 me 354,000 me VL VL ,502,000 mn ,500,000 mn VL VL VL VL VL ,498,000 mn VL GRAVITY WEST MINING CORP Date:21/5/ Author: D.Metsaranta Office: T.Bay Drawing: Voltaire Lake Project PHASE 2 Diamond Drilling Program Figure 4 Drill hole Locations-Plan View 300 Scale: 1:20000 Projection: UTM Zone 16 (NAD 83) ,000 metres

16 MAGNETIC PROFILES "''''''''' LAYERED EARTH INVERSION OF EM DATA GEOLOGICAL INTERPRETATION BLACK STURGEON "' ' sediments I Diabase sill Diabase sill I Sibley sediments Sibley se... U1ments Basement I I I I "''''00 Basement VOLTAIRE LAKE PROPERTY - EAST BLOCK - GEOPHYSICAL INTERPRETATION Figure 5 - Layered Earth Inversion of EM Data and Geological Interpretation

17 Discussion and Conclusions Drilling in the Drake Hill area has continued to intersect significant Cu-Ni-PGE mineralization and also shows potential for VMS style base metal mineralization. Further drilling of conductive anomalies is warranted. Drilling in the Chief Bay area did not succeed in its goal of intersecting the Black Sturgeon Fault. However, the holes that were not drilled through to basement could be extended to better evaluate evidence for a fault related offset of the unconformity and possibly determine the location of the fault. No anomalous radioactivity was found during the Phase 2 drill program. However, the discovery of graphitic basement units is promising from the standpoint of uranium mineralization and should be further evaluated by drilling particularly targeting conductors closer to the Sibley Group-Archean unconformity or major structural features. Respectfully Submitted Colin Bowdidge, Ph.D., P.Geo. Dawn-Ann Metsaranta, M.Sc. 17

18 Appendix A

19 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -90 Dip and Directional Tests Azimuth 0 Depth Dip Azimuth Total Depth m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone 16 Elevation 267 Collar coordinates (local) Date Started October 21, 2007 Date Finished Nov. 1, 2007 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes Locate the Black Sturgeon Fault Comments

20 VL Diamond Drill Log 1 of 1 FROM (M) TO (M) LITHOLOGY DESCRIPTION Overburden Pebbles, boulders Silty sandstone Very fine grained, white/green colour, very chalky looking, frequent light grey coloured, rounded spots throughout core. Core does not fizz when touched by acid. Sharp contact with diabase below, chill margin (3-4cm, 80 degrees to core axis). No visible sulphides, local quartz pods at 29.88m, white/yellow colour Diabase Fine grained to medium grained, grey/black colour, equigranular for the most part with occassional medium to coarse grained sections. Strongly magnetic, local blebs and patches of alteration (sericite?) to a light green grey colour. From 55.70m to 86.70m coarse grained section; at m core becomes coarse grained again with light coloured (silvery sheened) minerals, possibly orthopyroxene?, core is more broken up and veinlets of serpentine at 60 degrees to core axis Fault Gauge Very broken up, looks like cement with sandy groundmass and sandstone pebbles, dark brown red black colour, red and green sandstone pieces Diabase Fine grained, dark grey black, very broken up, strongly magnetic Fault Gauge Very broken up, groundmass is greenish and purplish with green and red sandstone pebbles Silty sandstone Fine grained, banded light green/dark green colour. Bands are 0.3cm to 0.5cm thick Sandstone Fine grained, banded red and green, commonly spotted, bedding is typically 0.5cm up to 25cm thick Foliated Granite Medium grained, white/pink colour, hematite blebs/spots (10%), foliated 50 degrees to core axis, lots of chlorite along foliated planes, some chlorite veinlets 10 degrees to core axis, local potassically altered patches, no visible sulphides. 20% hematized, local epidote veinlets/veins, chlorite veinlets range from 20 degrees to 60 degrees to core axis. At m, core becomes lighter orange white colour and gradually becomes more iron stained into an orange colour. Core looks brecciated by chlorite veins at m. At m, shart contact, 90 degrees to core axis, core is grey green pink to From to , core is pinkish green, abundant chlorite veinlets, very broken in places, foliated 45 degrees to core axis. From m to m, core is grey white, hematite veinlets (light pink), deep purple hemtite blebs and spots, 5%. At m, Epidote, hematite vein, 30 degrees to core axis, 1/2 cm thick. From m to m, core becomes dark greyish with less hematization than previously END OF HOLE

21 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -90 Dip and Directional Tests Azimuth 0 Depth Dip Azimuth Total Depth 63.67m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone 16 Elevation 273 m Collar coordinates (local) Date Started Nov. 2, 2007 Date Finished Nov. 3, 2007 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes Locate Black Sturgeon Fault Comments

22 VL Diamond Drill Log 1 of 1 From (m) To (m) Lithology Description Overburden Diabase boulders, pebbles, gravel Sandstone Light white/green colour, looks very mottled together in places, soft sediment textures visible, darker green colour has light coloured sediments falling into them, spotted and finely laminated, contact with lower unit is 80 degrees to core axis Diabase Medium grained, veinlets of chlorite (black) range from 10 to 60 degrees to core axis, no visible sulphides, dark grey black colour, equigranular, massive, strongly magnetic, one spec of chalcopyrite at 53.20m From to 54.12m, 2-3% chalcopyrite blebs and specs m END OF HOLE

23 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -90 Dip and Directional Tests Azimuth 0 Depth Dip Azimuth Total Depth 75.29m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone 16 Elevation 276 m Collar coordinates (local) Date Started Nov. 4, 2007 Date Finished Nov. 26, 2007 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes Locate Black Sturgeon Fault Comments

24 VL Diamond Drill Log 1 of 1 FROM (M) TO (M) LITHOLOGY DESCRIPTION Overburden Diabase boulders, pebbles, clay, sand Sandstone (Rossport Formation) Fine grained, light white green colour, bedding 50 degrees to core axis, local veinlets and patches of hematization, red wine colour (2.4%). 10% of core has patches and veinlets that look more weathered and broken up. 5% of core has local white specs and spots (0.5cm in size) Sandstone Fine grained, light white pink colour, some patches and beds of light white green. Bedding is 45 degrees to core axis. Fractures 60 and 45 degrees to core axis (in opposite direction to bedding) Magnetic Sandstone Fine grained, medium green blue colour, strongly magnetic, magnetite is visible as blebs, veinlets and patches. Bedding 55 degrees to core axis. Local brecciated sections, 2-3cm, light orange red and white with medium green pieces, local mottled sections and white patchy alteration sections??, this unit could be and exo-scarn?? Diabase Fine grained at contact with scarn? And transitions into medium grained. Massive, dark grey black colour, strongly magnetic, local (2%) black chlorite veinlets, 0 and 60 degrees to core axis END OF HOLE

25 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -90 Dip and Directional Tests Azimuth 0 Depth Dip Azimuth Total Depth m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone 16 Elevation 276 m Collar coordinates (local) Date Started Nov. 27, 2007 Date Finished Nov. 29, 2007 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes Locate Black Sturgeon Fault Comments

26 VL Diamond Drill Log 1 of 1 FROM (M) TO (M) LITHOLOGY DESCRIPTION Diabase Medium grained, magnetic, dark grey/black colour, local brecciation with black chlorite, 2-3cm thick. Fractures 60 and 20 degrees to core axis, black chlorite veins and veinlets, 2-5%. Contact with lower unit 40 degrees to care axis Sandstone Fine grained, light green white colour with patches and bloches or red-pink hematization (10%). Bedding 50 degrees to core axis, some local areas of bedding are at 10 degrees to core axis, this unit looks very mottled and melanged together. Contact with lower unit 40 degrees to core axis, small 2-3cm unit of fault gauge just at contact Diabase Medium grained, magnetic, very broken core, chlorite on fracture planes, 60 degrees to core axis m Sandstone Same as above, 15cm of fault gauge at top of unit, bedding 60 and 80 degrees to core axis, 25% hematized red-pink beds Diabase Medium grained, dark grey black colour, magnetic, contact at top is 30 degrees to core axis, fractures 30 and 10 degrees to core axis Sandstone Fine grained, light green white colour, 2% hematization only in two small veins around 103m and m (1cm each). Local sections look very melanged and blochy to a more white colour. 2-3% chloritized veinlets, contact 80 degrees to core axis Diabase Medium to fine grained, magnetic, first 10cm not as magnetic as rest of unit, chlorite veinlets 20 and 10 degrees to core axis. Contact at bottom 80 degrees to core axis Sandstone Medium green cream grey colour, first 10cm of sediments are magnetic and finely laminated with black chlorite and magnetite beds. Bedding 80 degrees to core axis, 5% hematized spots from m to m. Contact at bottom 90 degrees to core axis Diabase Fine to medium grained, gradually transitions into medium grained for remainder of hole. Black chlorite veinlets 20 and 60 degrees to core axis. Magnetic, dark grey black colour, very broken core from 140m to m END OF HOLE

27 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -90 Dip and Directional Tests Azimuth 0 Depth Dip Azimuth Total Depth m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone 16 Elevation 268 m Collar coordinates (local) Date Started Nov. 29, 2007 Date Finished 25-Jan-08 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes Locate Black Sturgeon Fault Comments Hole 10 was stopped on Dec then restarted after Hole 11 was finished on Dec. 8, Hole 10 needed to go farther to reach the fault.

28 VL Diamond Drill Log 1 of 1 FROM (M) TO (M) LITHOLOGY DESCRIPTION Overburden Diabase boulders and pebbles Diabase Dark grey black colour, medium grained, locally fractured 60 and 10 degrees to core axis, black chlorite visible along fracture planes. Magnetic, sharp contact with lower unit at 60 degrees to core axis. Loca 5-10cm sections of brecciation/fault gauge Sandstone Fine grained, medium green grey colour, looks silicified and is much harder when scratched than regular sediments. Green chlorite veinlets and patchy bleached spots throughout, no visible bedding Magnetic sediments Fine grained, medium green grey colour, silicified, magnetic, bedding 70 degrees to core axis, chloritized, very crumbly and broken up from 98m to m. Local 10cm patches of strong chloritization, local 15cm patches of bleached white rock at 101m Diabase Medium to coarse grained, dark grey black colour, fractures degrees to core axis, one vein (2cm) of black chlorite and carbonate 0 degrees to core axis (down the core axis) at 104m. Black chlorite veins/veinlets throughout, 10%, range from 0 to 90 degrees to core axis. Locally strongly chloritized (black) sections where core looks chlorite flooded, trace pyrite. From m to m, m to m and m to m, 5% hematized, coarse grained, magnetic, no sharp contacts, 15-20% feldspar, gabbro pods possibly dykes, 2-5% pyrite along fractures, 60 degrees to core axis. From m to m, m to m and m to m, coarse grained here. From m to m, very broken up. From m to m, very broken up m Sandstone Fine grained, very crumbly and soft, medium brown to medium green colours, first 0.50m is very brecciated and looks like fault gauge. No distinct bedding angle visible, looks very mottled and melanged. Sharp contacts at top and bottom, both 80 degrees to core axis. Local 10-20cm patches of reddish iron staining Diabase Same as before. Medium to coarse grained, dark grey black colour, fractures degrees to core axis. Black chlorite veins/veinlets throughout, 10%, range from 0 to 90 degrees to core axis. Locally strongly chloritized (black) sections where core looks chlorite flooded, trace pyrite. From m to m, very broken crumbly sections of core END OF HOLE

29 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -90 Dip and Directional Tests Azimuth 0 Depth Dip Azimuth Total Depth m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone 16 Elevation 275 m Collar coordinates (local) Date Started Dec. 3, 2007 Date Finished Dec. 8, 2007 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes Locate the Black Sturgeon Fault Comments

30 VL Diamond Drill Log 1 of 1 FROM (M) TO (M) LITHOLOGY DESCRIPTION Diabase Boulders, pebbles Sandstone (Rossport Formation) Chalky white colour, fine grained, top and bottom sections look mottled green and red colour, middle looks solid one colour (white) sandstone, gradual contacts, shart contacts with diabase above and below, both 90 degrees to core axis Diabase Magnetic, fine grained, dark grey black colour, massive Sandstone Grey green colour, fine grained, local sections mottled with red colour, sharp contacts with diabase above and below, both 90 degrees to core axis Diabase Magnetic, dark grey black colour, massive, medium grained with 2m section at top of fine grained. Black chlorite veinlets along fractures degrees to core axis, starting at m, more broken core segments than before to m Clay Very fine grained, light grey green colour, soft and falling apart, lots of lenghths of core lost here, not sure of exact depth Diabase Same as before. First 20cm is brecciated and melanged with white carbonate, very broken core from 305m to m Sandstone Fine grained, very broken core starting from 339m, light green grey colour, locally pink grey. Bedding visible at 60 degrees to core axis, core has been melanged in several places causing bedding angles to be disrupted, some core looks brecciated Foliated Granite Light grey to medium grey, medium grained, local alteration of hematite (20%), foliated 60 degrees to core axis. Local 20cm sections of strong chloritization. Fractures 60 degrees to core axis END OF HOLE

31 GRAVITY WEST MINING CORP. VOLTAIRE LAKE PROPERTY DIAMOND DRILL LOG Hole No. VL Hole No. VL Collar Dip -50 Dip and Directional Tests Azimuth 157 Depth Dip Azimuth Total Depth m Claim Local Grid Collar coordinates (UTM) UTM Datum NAD 83 Zone Elevation 307 m Collar coordinates (local) Date Started Feb. 1, 2008 Date Finished Feb. 8, 2008 Drilled By Logged By Core Size Casing Left In Purpose of hole Discovery Diamond Drilling L. Rajnovich NQ Yes To re-test conductor Comments A total of 262 samples were analysed.

32 VL Diamond Drill Log 1 of 8 From (m) To (m) Lithology Description Sample # From (m) To (m) Length (m) Au Pt Pd Cu Ni Pb Zn Overburden Diabase Medium to coarse grained, dark grey black colour, strongly <15 < magnetic, trace disseminated pyrite, fractures range from 25 to 50 degrees to core axis. Local green chlorite veins, 2%, 45 degrees to core axis. Core gradually changes to fine to medium grained size around 45 meters. Local green chlorite and feldspar veins (1-2cm), 20 degrees to core axis <5 <15 < <5 19 < < <5 <15 < <5 <15 < <5 <15 < <5 <15 < <5 15 < <5 <15 < <5 <15 < <5 17 < <5 20 < <5 <15 < <5 <15 < <5 <15 < <5 <15 < <15 < <5 <15 < <5 16 < <5 <15 < <5 20 < <5 15 < < < < <5 <15 < <5 <15 < < < <5 18 < < < <5 < <5 <15 < <5 <15 < <5 <15 < <5 22 < <5 26 < < <

33 VL Diamond Drill Log 2 of 8 From (m) To (m) Lithology Description Sample # From (m) To (m) Length (m) Au Pt Pd Cu Ni Pb Zn Limestone Very fine grained, pale grey green colour, bedding 50 degrees to core axis. Local hematized veinlets/patches, 5-7%. Moderately magnetic. Contact at top 50 degrees to core axis, contact at bottom melanged up, looks conglomeratic/brecciated Metagabbro to Pyroxenite <5 24 < <5 20 < <5 18 < <5 16 < <5 15 < <5 28 < < < < <5 22 < <5 21 < <5 20 < Coarse grained, dark grey green colour, very broken up at top meters, local hematized patches/blobs with in broken up core (these areas are not magnetic). Overall unit is strongly magnetic, no visible sulphides at top. Starting approximately m, presence of sulphides begins as disseminated, blebs and patches, up to 15-20% pyrite. Core is bery coarse grained starting at 153 meters. Fractures are typically 25 and 50 degrees to core axis. Local blebs and pods of cubic pyrite, 5%. From m to m, Quartz/Feldspar vein, 20 degrees < to core axis, slightly hematized to a pale pink colour. At m, Quartz/Feldspar vein (1-2cm) same as above < From m to m, brecciated section, altered < From m to m, altered section, light white grey < colour, minerals look elongated, 50% disseminated pyrite. From m to m, Quartz/Feldspar/Epidote vein, degrees to core axis, 5-7% pyrite. From m to m, Blobs/vein of pyirte, 50%, vein is 20 degrees to core axis From m to m, vein with 3-5% pyrite and epidote, degrees to core axis. From m to m, Blob/vein of pyrite, vuggy in centre, 40% pyrite, 5-7% chalcopyrite. From m to m, Altered section, slightly < hematized, 10% epidotized < <5 28 <

34 VL Diamond Drill Log 3 of 8 From (m) To (m) Lithology Description Sample # From (m) To (m) Length (m) Au Pt Pd Cu Ni Pb Zn < < < < < <5 <