Diamond Drilling on the. Scadding Gold Property. Scadding Township, Ontario. Drill Holes TRM to TRM Mavros Whissell B.A.

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1 Diamond Drilling on the Scadding Gold Property Scadding Township, Ontario Drill Holes TRM to TRM by Mavros Whissell B.A. Robert Komarechka B.Sc., P.Geo, P.Geol Lindsay Moss B.Sc. Date: April 30, 2010

2 Table of Contents Introduction... 4 Location... 4 Access... 5 Property Description... 5 Previous Work... 7 Summary of Work... 8 Drilling... 8 Summary of Drilling Undertaken... 8 Table 1: Drilling Summary for Plan Map of DDH Locations Surveying Logging Core Cutting and Sampling Observations Drilling Lithological Historical drilling Conclusion Recommendations APPENDIX 1: DDH Logs TRM TRM TRM TRM TRM TRM TRM TRM TRM TRM TRM

3 TRM TRM TRM TRM TRM TRM TRM TRM APPENDIX 2: DDH Sections 2009 Lithology Drill Location Map Section Location Map TRM TRM and TRM TRM and TRM TRM TRM TRM TRM TRM and TRM TRM and TRM TRM TRM TRM TRM TRM and TRM

4 Introduction This report covers the Scadding Gold Mine Site and the adjacent staked and optioned claims (the Property ) by Trueclaim Exploration Inc. ( the Company ) for its potential to host gold mineralization that could be economically exploited. At the time of this report the Property consists of 7 mining leases which contain a total of 56 contiguous mining claims, as well as?? optioned and staked claims for a total area of approximately 37,000 acres. The Property is predominantly underlain by Early Proterozoic age sediments of the Huronian Supergroup, specifically the Serpent, Espanola and Bruce Formations of the Quirke Lake Group which have been intruded by Early Proterozoic age (Nipissing) gabbro and diabase. The gold mineralization occurs in what is thought to be younger than 1700 Ma (million year old) bodies of hydrothermal breccia made up of coarse fragments of the Serpent Formation with abundant chlorite alteration and as much as 5% iron sulfide content. Based on previous drilling a noncompliant resource of 539,049 tons containing 165,525 oz of gold which represented a grade of oz gold per ton, was reported on the property. It is the purpose of this work to determine if significant mineralization existed on the property worthy of a further Phase II drill program to delineate a resource evaluation. This report discloses the data from the drill program undertaken in Work undertaken on this property and this report was supervised by Bob Komarechka P.Geo. of Bedrock Research Corp. Location The Property is located in Scadding Township, District of Sudbury, Ontario between Wanapitei and Ashigami Lakes, about 50 kilometers northeast of Sudbury, Ontario at 46 o -38 N latitude, 80 o -37 W longitude. The Property includes the former Scadding Gold Mine ( ) located in Concessions II and III, Lots 5 and 6, Scadding Township, Sudbury Mining Division.

5 Access Access to the old mine workings and the 2009 Phase 1 DDH program is provided via the well maintained gravel Kukagami Lake Road. Travelling on this road which runs near north from Highway 17 for?? km. will bring one to a gravel road to the west. Taking this road leads to the old minesite and the area of drilling. See figures 1 & 2. Add figure 1 General Location Map here Property Description The following table shows the extent of the property as held at the time of the initiation of drilling: Figure 2: True Claim Land Position, September 29, 2009.

6 Figure 3: Scadding Gold Property Lease Map

7 Previous Work The following is a summary of the key Property highlights as previously written by L.D.S. Winter, P.Geo. and later paraphrased or duplicated. Previous to Trueclaim Exploration Inc. operations, a total of meters of diamond drilling in 221 surface holes have been drilled on the Property and most of this work was restricted to four mining claims. In 1980 P.C. McLean calculated a non-compliant resource for the Property of 539,049 tons containing 165,525 oz of gold which represented a grade of oz gold per ton. The estimated resource base in 1983 was 152,895 tons at an estimated undiluted grade of oz gold per ton which represents approximately 57,000 contained ounces. The Scadding Gold Mine produced approximately 914 kg of gold from 127,000 tonnes (t) of ore grading 7.2 Au/t (29,400 ounces of gold from 139,742 short tons of ore grading 0.21 oz/ton) during the period 1984 to 1990 from three shallow open-cuts (North, East-West and South Zones) and underground development of the Central (Intermediate) Zone. The estimates from 1983 combined indicated and inferred categories which is not permitted under current CIM Reserve and Resource Standards as required by NI This information is historical data and should only be considered as such. It does not represent current resources compliant with CIM Standards as required by NI The Scadding Gold Mine was run as an extraction project without any attempt to build a sustained mining operation or to evaluate the potential of the Property. Previous to the Company s operations, the most recent work was carried out by JML Resources Ltd. in A preliminary drilling program confirmed the presence of gold at one of the known historic gold zones (North Zone) and confirmed that historic gold zones are associated with broad chlorite and albite-rich alteration envelopes. Geophysical surveys identified 7 distinct linear zones and that within 3 of the zones historical gold development had occurred. Based on the historical work (1973 to 1990) on the Property and the work in the last 10 years by Currie Rose Resources Inc. and JML Resources Ltd., it is considered that the Property has the potential to host additional mineralization.

8 Summary of Work Drilling Trueclaim contracted Mallette Drilling from the period of November 10 th to December 16 th 2009 to complete the Phase 1 drill program. In total 19 NQ diamond drill holes were drilled over an area covering 4 of the 7 leases that comprise the Scadding Gold Property. The total meters drilled during this program was m. Orientation of the drill hole was surveyed at approximately regular 50m intervals. These tests were done using a Reflex tool by the drillers. Readings were documented by the driller once the hole was terminated. Drill casings were left in the ground with the driller requested to supply and attach caps. These caps were later labeled with a punch showing the hole number. Summary of Drilling Undertaken On November 11 th, 2009 drilling commenced. The first hole was located in the South Pit area on claim TRM was drilled about 10m from the edge of the south pit. Present within the historical data there was indication that hole W36 drilled by Watt and McLean in 1984 contained a large intercept of gold mineralization. The first Trueclaim hole was scouted by Paul McLean and was meant to target this intercept. A large diabase dyke was intersected and seemed to end at the point that Paul McLean thought we would intersect chlorite breccia. For this reason, we measured out a second drill hole about 20m to the west and attempted to hit the chlorite unit again. Successfully, we intersected very little diabase and more chlorite. While drilling the first two drill holes water was taken from the south pit using a pump. As there was blasting to remove the material from the south pit, the drillers has some struggles collaring in this area due to the fragmented nature of the rock near the pit. After the first two drillholes we moved to the north zone. Holes TRM-09-03, TRM and TRM were drilled in attempt to extend the north zone towards the north-east. The quartzite was less altered here and the drillers had a very hard time finding the right bit that would last. During the drilling of these holes numerous bits were ordered and tested until a bit that suited the rock was found. In this area water for the drilling was taken from the North Pit and pumped about 100m to the drill. In these drillholes quartzite, chlorite breccia and carbonate breccia were encountered.

9 The drill was moved into the north zone to twin one of the Currie Rose holes (CR42) in order to gain more confidence in the historical data. TRM was drilled vertically within half a meter to the east of the old collar. The lithological contacts seemed to be consistent with what was documented in the logs. While we were drilling in this location, some personnel from the Ministry of Labour appeared for a site visit and inspection of the drill. TRM-09-07, TRM and TRM were all drilled in the south pit area. During inspection of the drill core from hole TRM during logging visible gold was observed. These observations warranted more drilling around the south pit to determine the orientation of the mineralized zone. TRM was drilled about 20m north of the second hole to see if we would intersect the zone when we stepped back. Some chlorite breccia was intersected in this hole. It was then decided that we should drill 20m further to the west and attempt to intersect the zone with TRM This drillhole was unsuccessful and the majority was drilled into the Espanola Limestone. TRM was a vertical hole drilled on the south side of the pit to see if the mineralization occurred in this location. A small interval of chlorite breccia was intersected followed by the contact with the Espanola Formation. The Currie Rose New Zone was always an area of interest that needed some follow up. Sporadic vertical historical drillholes occur throughout this area. It seemed that there was something interesting going on in this area structurally. Four holes (TRM-09-10, TRM-09-11, TRM and TRM-09-13) were drilled into this zone all oriented towards the south. All four holes intersected chlorite breccia, diabase and were terminated in Espanola Limestone. Drilling in this location was smooth and with no major problems. Water was pumped from the East-West Pit to the drill shack. There was very limited drilling between the central mined zone and the north pit, it seemed like this was one of the areas needing further exploration. Drillhole TRM was an attempt to determine if there was continuity between the two zones. During drilling water was used from the North Pit. The logging revealed that there was chlorite breccia present in that location. This hole was terminated within the Carbonate breccia. A few hundred meters to the south-west, TRM was drilled targeting a small intersection of gold assays found during drilling in 2004 by JML Resources. Numerous meters of quartzite and carbonate breccia were intersected with very little chlorite. The pump shack was located at the South Pit and no bulldozing occurred as the pad was built on an old drill road.

10 10 targets were identified by geophysics run by Currie Rose. All of them were clearly marked using a solid t-bar and had an engraved plaque attached to it marking the Target number and what geophysical anomaly it was targeting. We decided to test Target 4 which was located about 200m north of the North Pit. This area was exposed while trenching the area a few weeks prior. This was mostly a swampy area and several chloritic boulders had been pulled out of the muck. TRM was stepped back 40m south of the T-bar for Target 4. Very little chlorite, alteration and mineralization were present in the core. TRM was drilled 100m down strike of TRM As we had intersected some intervals of chlorite breccia in this earlier hole, we decided to see if we could pick it up 100m to the north east. About 10m to the north of the drill was hole an old Northgate hole drilled vertically and producing water. The last two holes of this drilling program were TRM and TRM both were drilled from the same point located between the Currie Rose New zone and the East-West Pit. The first hole was drilled vertically and interested weakly mineralized chlorite breccias and the second hole was drilled to the north and also intersected some chlorite breccia intervals. On December 16th, TRM was in barren looking quartzite and there was a general consensus that this would mark the end of the 2009 drilling program. This gave us an opportunity to catch up on the logging and sampling. We wanted to ensure that all samples were at the laboratory prior to Christmas break.

11 Table 1: Drilling Summary for 2009 Hole # Easting Northing Azimuth Dip Depth Drilling Drilling Logger(s) Logging Logging Started Finished Started Finished TRM /11/ /11/2009 Robert Komarechka 11/11/ /11/2009 TRM /11/ /11/2009 Robert Komarechka 13/11/ /11/2009 TRM /11/ /11/2009 TRM /11/ /11/2009 TRM /11/ /11/2009 Lindsay Moss 15/11/ /11/2009 Robert Komarechka Robert Komarechka 18/11/ /11/2009 Lindsay Moss Robert Komarechka 21/11/ /11/2009 TRM /11/ /11/2009 Lindsay Moss 24/11/ /11/2009 TRM /11/ /11/2009 TRM /11/ /11/2009 Robert Komarechka 26/11/ /11/2009 Lindsay Moss Lindsay Moss 28/11/ /11/2009 TRM /11/ /11/2009 Lindsay Moss 29/11/ /11/2009 TRM /11/ /12/2009 Lindsay Moss 01/12/ /12/2009 TRM /12/ /12/2009 Lindsay Moss 02/12/ /12/2009 TRM /12/ /12/2009 Robert Komarechka 05/12/ /12/2009 TRM /12/ /12/2009 TRM /12/ /12/2009 Robert Komarechka 06/12/ /12/2009 Lindsay Moss Lindsay Moss 07/12/ /12/2009

12 Hole # Easting Northing Azimuth Dip Depth Drilling Drilling Logger(s) Logging Logging Started Finished Started Finished TRM /12/ /12/2009 Robert Komarechka 10/12/ /12/2009 Lindsay Moss TRM /12/ /12/2009 Lindsay Moss 11/12/ /12/2009 TRM /12/ /12/2009 Robert Komarechka 12/12/ /12/2009 TRM /12/ /12/2009 Lindsay Moss 14/12/ /12/2009 TRM /12/ /12/2009 Roebrt Komarechka 19/12/ /12/2009 Lindsay Moss

13 Plan Map of DDH Locations

14 Surveying In October, Global Surveying Services was hired by Trueclaim Exploration to more accurately locate features found in the field. Lindsay Moss spent several weeks compiling data for assessment work and putting together a map of historical drillholes. This map was taken in to the field with the GSS crew and as many drillholes we could find were located with the GPS. About 30% of the historical holes were located in the field. Holes that were not found in were most commonly positioned either in pits or cemented if located above the underground workings. Most recent drillholes from Currie Rose (1997) and JML Resources (2003 and 2004) were in a similar position to what was documented on the map. Currie Rose holes were very well marked with 4 inch by 4 inch block of wood chiseled into a round point at the bottom and hammered into the casing. JML drillholes were easily spotted because the drilling was so recent that pads had not become over grown. As well, many drillholes away from the mine area were drilled on their cut grid, the lines are still in pretty good condition. JML marked most drillholes with a 2 inch by 2 inch wooden picket often with flagging tape tied around the base. Older drillholes were more difficult to locate. About half of Northgate and Gulf holes drilled away from mine workings were found in the field. These drillholes were often intensely rusted and very difficult to find due to the brown colour being similar to the trees. Only one hole drilled by Watt and McLean in the early 1980`s was found and it is still questionable as to whether this drillhole actually belongs to this group. Where we found the collar, about 300m east from the south pit there should have been two collars as one was failed. There was only one collar located in this area and it was a different orientation from what was documented. During this surveying program two wells were discovered on the property. No documentation of these were found in the historical data, but it is believed that these were used for hydrological studies. Several other points of interest were surveyed during the two week period, including all roads and trails on the minesite, the waste pile, the portal and the pits. Some pickets still remain from old cut lines and these were surveyed, but there weren`t enough points and it was impossible to determine which pickets these were as they had no markings, so that data is unusable. Global Surveying placed several iron bars around the property, so we have something concrete for future surveying to tie into.

15 Logging Prior to drilling an excel logging sheet was created designed based on what historical data deemed important to capture. Both alteration and mineralization seemed to play an important role in the gold mineralization. Logging by Bob Komarechka and Lindsay Moss began soon after drilling commenced. A stereomicroscope was used in conjunction with logging to better view small flecks of visible gold as well to aid in identifying unknown phases. Magnetic susceptibility readings were taken sporadically using a KT5 Magnetic susceptibility meter by Exploranium, mainly in attempt to identify intrusive lithologies. Logging occurred in a garage rented just off of Highway 17 at 300 Kukagami Lake Road. Within the garage is a logging bench and 5 core racks built by Stanley Kowal. The garage was heated with a portable oil furnace rented from Able in Sudbury. In order to get heat from one side of the garage to the other, we needed to drill a hole through the wall for the heating vents to pass through. The core is currently stored on the property with significant intervals stored inside and locked. Remaining core from 2009 is located in racks outside of the garage and covered with tarps to prevent the wood from rotting. Core Cutting and Sampling Core cutting was undertaken by Stanley Kowal. A saw was rented from Exploration Services for the purpose of cutting core. Two 14 inch diamond blades were purchased for the saw. A separate room away from the logging area housed the saw and all cutting materials. Prior to cutting blanks and standards were organized. Standards were acquired from CCIC in Sudbury and blanks were created from white quartz. The main problem encountered with cutting was our water supply to the saw. There was no running water in the shack and there was only a rain barrel outside the shack for water. The people who rented the house next door have a well and were kind enough to fill our barrel. When temperatures dropped it was near impossible to keep this water from freezing solid. We got a few large plastic water containers from Mohawk Garnet and stored the water inside the heated shack. Cut core was stored in the cutting shack and sampling was done periodically. Half core samples were placed in thick plastic sample bags with their corresponding sample tag. A portion of the sample tag

16 with the sample number was stapled into the bottom of the core box. Standards were inserted every tenth sample and blanks were inserted every fiftieth. Sample bags were closed with zip ties and put in rice bags in groups of 10. Samples were taken to the lab when we accumulated about 10 bags of core. When drilling commenced we were transporting our samples to SGS Laboratories in Sudbury and duplicate samples or field samples were being sent to Swastika Laboratories in Swastika. At SGS Laboratories it was taking a significant amount of time for results, so all samples were transferred to AGAT Laboratories on highway 17 in Sudbury.

17 Observations Drilling During the 2009 drilling program several observations were made regarding the drilling at the Scadding Mine Site. Bits for drilling should be specifically for hard rock like the quartzite. Water on site is readily available and easily accessible from almost anywhere on the property. It was noted that rock is highly fragmented due to blasting around the pit areas which can cause problems during casing. Also to note, the Espanola Limestone drills very rapidly with the hard rock bits. The drillers can almost double their speed while drilling through Espanola Formation. Lithological While logging core we were able to identify that there were several different types of chlorite alteration found on the Scadding Mine site. These chlorites can be distinguished primarily by their appearance. One chlorite phase often associated with sulphides in a medium green is colour and rather pervasive in its alteration around the quartzite fragments. The other chlorite observed seems slightly lighter in colour and tends to have a sharper contact with fragments. The later chlorite is rarely mineralized by sulphides. While running the drill program we found a pile of ore assumed to be from the underground working. These rocks were composed almost completely of chlorite and contained large 1-5cm cubic pyrite crystals. Visible gold was identified within 3 of the first 4 holes of this program. The gold identified was commonly found under the stereomicroscope. It seems as if the gold is very fine grained and therefore difficult to find with the naked eye. Gold was found in strongly chloritized areas in association with sulphide minerals. Alteration was somewhat variable throughout the drilling. It seems like there is much more hematite alteration present in the south pit than there is in the north pit. Within TRM we noticed that the visible gold was in chlorite beside a strongly hematitically altered fragment. Where as in TRM we still observed visible gold in the chlorite of the chlorite breccia units, however the quartzite fragments are commonly white to tan in colour. While drilling in the north it was observed that the quartzite was not or weakly altered by hematite when in the zone where chlorite breccia occurs. Commonly there is a distinct point at which chlorite

18 alteration become carbonate alteration. At this point the quartzite fragments become salmon pink in colour due to the intense pervasive chlorite alteration. We have not yet concluded the relationship between hematite alteration and gold mineralization. Historical drilling After all of the compilation, field work and drilling completed by Trueclaim Exploration there are a few observations made about historical data and historical drilling. It seems as if mineralization and chlorite breccia are both occurring in the general areas they were documented as occurring. While compiling data before drilling occurred there were numerous holes in the assessment reports. Some of these missing documents were acquired from sources who worked on the property and others still have not surfaced. There is no record of any assays from the Gulf drilling program we just have lithological logs. For the work done by Watt and McLean most of the data was compiled, however no drill collars were found to confirm they exist. As for Northgate, we have only found a few collars because most were drilled into the area of the underground mining and therefore cemented during mining. We have compiled all of the data from Northgate and it seems that most data fits what was intersected. Currie Rose drillholes were definitely the easiest to find being marked with a block of wood. In the JML drilling assessment report it seem like most of their results and logging were pretty close to what was intersected in the Currie Rose drillholes, some assays varied due to gold flecks. It seems like data from Currie Rose and JML Resources is far more reliable than the other historical data.

19 Conclusion Through the compilation of historical work done on the Scadding Mine site it seemed as if the drilling programs in the past were rather small and somewhat inconclusive. I was stated by several documents and people that there is still potential for expansion as well as new discoveries on the property. The primary goal of this preliminary phase of drilling was to establish the accuracy of historical records and determine whether or not there is current potential on the Scadding Gold Mine property. To date we have been able to rank the historical data based on accuracy as well as determine that there is still potential for expanding old deposits and finding new ones. It was determined that there is still gold present in the ground as we observed visible gold in holes drilled in the north (about 75m away from the open pit) and in the south zones. Lithologically, chlorite breccia is confirmed in places where it was documented by historical drilling. It seems as if there are physically different types of chlorite present on the mine site which contain variable amounts of sulphide mineralization. Alteration is variable throughout the site, most commonly hematite which is stronger in the south pit area and weaker in the north pit.

20 Recommendations More diamond drilling needs to occur on the Scadding site. Most historical drilling was concentrated on the 5 deposits within the mine area. Not much drilling was done outside of this area until JML Resources drilling program in 2003 and Several small sniffs of gold mineralization were detected outside of the main zones which need to be followed up in future drilling programs. In this drilling program it was determined that the mineralization is sporadic and commonly contained within the mineralized chlorite breccia units. In order to get a better idea of the way these bodies are sitting in space it is recommended that the historical and current drilling are modeled in a 3D program. Through modeling the ore zones and location of the chlorite breccia more accurate drill targeting can be achieved. The North Zone seems to be the largest drilled zone of mineralization not mined on the property. More detailed drilling in this area would allow magnetic and geochemical tests which can be useful to determining controlling factors related to gold mineralization. In the 3D modeling program, geochemical results can be plotted to see which elements are more closely related to gold. Magnetic susceptibility readings will be useful in determining whether an airborne magnetic survey would benefit Trueclaim in identifying more pockets of mineralized chlorite breccia. As well, the geochemistry can be used to define a way of differentiating mineralized verses non-mineralized chlorites.

21 APPENDIX 1: DDH Logs TRM E, N. Logged by R. Komarechka from the 11 th to 13 th of November TRM Lithological Logs From To Lithology Description 0 6 Casing Overburden to 5.9m Olivine Diabase Medium grey, mottled with white and black, medium crystalline, massive. 65% white plagioclase, 30% pyroxene and amphibole, minor pyrrhotite. It is magnetic and rather blocky. From 25.0m to the end of the interval is a finer grained chill margin. There is an abrupt contact with the quartzite below. Mag readings between 20-25ams SF Quartzite Breccia 90% fragments, 10% matrix, fragments consist of flesh colour to brown coloured microcrystalline showing variations in alteration with lighter colours along the edge of fragments and within fractures, fragments of various size, generally up to meter sized with breccia zones containing more abundant matrix in between. Erratically distributed matrix with local areas containing up to 20-30% chlorite in irregular open fractures with associated crushed quartzite, minor amounts of white calcite also noted. Chlorite is a dark greenish grey and there does not appear to be a particular trend to the chlorite filled fractures. Finely crystalline pyrite within the breccia matrix composing about 3-5% of the composition of the matrix. Quartzite is a pinkish colour, probably sodium metasomatism with weak hematization. Mag readings between ams SF Quartzite Light to medium khaki grey, finely crystalline, well sorted, banded. Also has fractures that are surrounded by cream white zones about cm wide. Mag readings between ams SF Quartzite Breccia Lacking hematite alteration as observed in above breccia unit. Colour is a cream grey to white and khaki with chlorite mottling and khaki colour bands. Same type of quartzite as before, fine crystalline, moderately sorted. Contains large decimeter scale quartzite fragments with matrix of mottled chlorite with a matrix of quartz and white carbonate. Matrix material composes about 30% over discrete areas.

22 From To Lithology Description SF Quartzite Serpent quartzite fine to crystalline, light grey to khaki grey, banded, consists of very fine to crystalline well consolidated quartz. These bands which are diffuse vary in width from 2-30cm wide and vary in colour and shape. There appears to be a secondary white soft mineral possibly associated with chlorite found uniformly distributed in lighter sections of core comprising up to 50%, but more commonly about 5% SF Quartzite Breccia Brecciated serpent formation consisting of colour from light grey through flesh colour to brown. Diffuse varicoloured consists of 70% breccia fragments which are albitized and have very irregular outlines. Fragments are coated with a rim of chlorite. The matrix of the breccia consists of white calcite with fenestral greenish grey chlorite. The carbonate in the matrix is white coloured. Fragment sizes are in the order of 10 to 30cm and there are occasional fractures containing greenish grey chlorite SF Quartzite Medium grey to light and dark grey, banded quartzite. Finely crystalline, flesh pink coloured mottling in areas near the upper contact. A minor breccia located at m containing about 3% pyrite. The fragments of the breccia show some bleaching along the margins. Near base of unit begins to develop small dark grey bands SF Quartzite Medium grey to dark grey banded quartzite, finely crystalline with dark thin bands of intrusive lamprophyre. Contacts between lamprophyre and quartzite are irregular Lamprophyre SF Quartzite Breccia Very dark grey, very fine to crystalline, massive, uniform colouration. Irregular contacts with surrounding quartzite. Minor hairline fractures with calcite and serpentine. Mag readings between 24-29ams. Varicoloured quartzite breccia varying from cream white through brown to dark grey. Highly variable texture consisting of large blocks of quartzite and localized areas of smaller fragments. The matrix of the breccia comprises about 20 to 30% and the matrix consists of a creamy white carbonate. Some of the fragments contain white flecks of possible leucoxene SF Quartzite It is a light brown to dark grey. The material is finely crystalline quartz and is slightly banded. The core in this interval is very broken up. There are some thin minor fractures with associated bleaching. Minor area of brecciation located at 69.7m SF Quartzite Breccia Brown grey to pink flesh colour, primarily 90% fragments, 10% matrix. The matrix consists of quartzites that are finely crystalline. The matrix is composed of carbonate EF Limestone Light green to white with thin bands of black and brown. Grain size if fine to extremely fine.

23 From To Lithology Description SF Quartzite Dark grey to medium grey banded quartzite with bands varying in size from 2 to 10cm. They are finely crystalline composed primarily of quartz and compose about 30% dark mafic material SF Quartzite Light tan grey to brownish grey, banded finely crystalline. Some local areas with some dark green and pistachio green alteration, possibly chlorite and epidote. Developing dark argillaceous bands towards base of unit SF Argillite Dark grey, hypo-crystalline contains occasional thin white crackle textured calcite veinlets. Local development of minor chlorite EF Limestone Consists of light grey to pink limestone bands separated by numerous dark argillaceous bands and occasional fragments of argillite. The limestone is very finely crystallite, massive, occurs in bands with a variation between light grey and pink. The band width ranges from 8-20cm and they are separated by medium to green grey argillite. Some of the argillaceous bands towards the base of the unit become fractured with infillings of greenish white carbonate EF Limestone Pastel grey green to light brown diffusely banded limestone containing dark grey thin argillite layers. Thin argillite layers are becoming more pervasive and defined towards the end of the unit. E.O.H. 101 EOH TRM Mineralization Log From To Sulphide Mineral % Mineralization Type Comments Pyrrhotite 0.1 Disseminated Pyrite 5 Disseminated Pyrite 0.1 Disseminated Associated with chlorite Pyrite 3 Breccia Matrix Pyrite 1 Disseminated within albitized quartzite Pyrite 0.5 Stringer Associated with chlorite in hairline fractures Pyrite 0.5 Breccia Matrix Pyrite 0.5 Disseminated Very fine grained Pyrite 0.5 Disseminated

24 TRM Structural Log From To At Structure Angle T.C.A. Comment Structure is chaotic Bedding 65 Alteration occurring along layers in the bedding Bedding 50 Bands are uniform in orientation 46 Bedding 80 Thin hairline fractures rimmed with light coloured bleaching 49.5 Bedding Bedding Bedding Bedding Bedding Bedding 65 TRM Alteration Log From To Alteration Mineral 1 % Alteration Style 1 Alteration Mineral 2 % Alteration Style Hematite weak to moderate Fracture fill Albite moderate Pervasive Chlorite Weak Breccia Matrix Albite Weak Fracture fill Albite weak to moderate Other weak to moderate Carbonate Weak Breccia Matrix Albite Strong Pervasive Albite Weak Pervasive Chlorite Chlorite weak weak Albite Moderate Pervasive Carbonate strong Albite Weak Pervasive Albite Moderate Pervasive Carbonate moderate Carbonate Weak Fracture fill Breccia Matrix Fracture fill Breccia matrix Breccia Matrix Chlorite Weak Vein Other weak Vein Chlorite Weak Fracture fill Hematite Weak Fracture fill Comment White fuzzy specks pervasive over narrow interval of 0.5m Chlorite (~4%) and disseminated throughout Epidote and chlorite alteration confined to particular bands Increasing towards the base of the unit TRM Samples From To Sample # Lithology Comments H SF Quartzite Breccia H SF Quartzite Breccia H Lamprophyre For Whole rock Geochem H SF Quartzite Breccia

25 TRM Reflex Tests Depth Azimuth Dip Reflex Magnetic Field Magnitude Robert G. Komarechka, P.Geo, P.Geol

26 TRM E, N. Logged by R. Komarechka from the 11 th to the 13 th of November, TRM Lithological Log From To Lithology Description Casing Overburden to 4.5m Olivine Diabase This interval is a chilled margin that is dark grey, finely crystalline, massive. Composed of pyroxene, plagioclase with minor amounts of pyrrhotite. Mag readings at 26-30ams SF Quartzite Varicoloured, dark grey to flesh pink to orange fine crystalline, massive, contains splotches up to 10cm of chlorite near the bottom which contains an irregular zone of chlorite which contains about 8% pyrite, subhedral and about 1cm in diameter SF Quartzite Breccia SF Quartzite SF Quartzite Breccia SF Quartzite SF Quartzite SF Quartzite Breccia SF Quartzite Breccia Orange salmon to medium grey in localized zones, consists of very finely crystalline quartz with fractures delineated by orange bleached areas, some areas show brecciation and some areas are not as brecciated. The amount of breccia fragments is on the order of 95% and matrix material is less than 5%. The matrix is primarily silica. The salmon colour is probably due to hematization. Dark grey, very finely crystalline, massive with occasional alteration along fine fractures (orange coloured). Occasionally discordant thin white calcite veinlets. Varying in colour from dark grey to salmon, there are fractures filled with chlorite and calcite (hairline fractures). Finely crystalline and massive. Dark grey quartzite, finely crystalline, massive containing numerous fractures filled with quartzite and a slight aureole of orange hematite. Dark grey quartzite, finely crystalline, massive with minor white calcite filled fractures. Similar to the unit above except less calcite fracturing. Minute crystals of carbonate scattered throughout. Salmon coloured to medium grey, develops specks of chlorite which become more abundant towards the base. Similar to the unit above, except pyrite is beginning to develop, hematization is less pervasive and becoming more fracture filled. Brownish grey, finely crystalline, mottled with black to dark green flecks containing scattered blebs of pyrite. Pyrite is also found within chlorite specks and within chlorite filled fractures SF Quartzite Breccia SF Quartzite Breccia SF Chloritized Quartzite Weakly brecciated quartzite with a chlorite matrix. The quartzite is very finely crystalline varying in colour from pinkish brown to grey. Brecciated with chlorite coming in along layers of quartzite broken apart as well as in specks. Local patchy areas of chlorite which seem to have replaced some fragments. There is pyrite which appears to be constrained along fractures that have become bleached and more so along the intersection of these fragments. Pyrite is also developed in subhedral masses, they are coarse grained blebs which are scattered throughout. Quartzite is salmon coloured to brown, finely crystalline, the breccia has a matrix of chlorite in fractures. There is pyrite associated with chlorite. Similar to previous interval but lacks hematitic alteration. Grey in colour, finely crystalline containing finely disseminated pyrite and possible magnetite, pervasively moderately chloritized. Unusual mag reading of 179. Only the upper part of this zone has higher mag. 70% chlorite and about 30% quartz, patchy chlorite becomes merged together into a more pervasive alteration.

27 From To Lithology Description SF Quartzite Breccia SF Quartzite Breccia Quartzite breccia that is salmon coloured to light brown, very finely crystalline, with numerous fractures filled with chlorite containing pyrite. VG noted in the chlorite. Mag readings between 17 and 20ams. Grayish in colour, but ranges from medium grey to salmon tan coloured. Very finely crystalline quartzite, brecciated with some chlorite present in fractures. Chlorite is not as pervasive as the previous section. Much darker than the previous section due fine grained pervasive pyrite mineralization, also present with a dark sub-metallic mineral (magnetite?). Mag readings between 11 and 47.2ams. Lower mag readings in areas with hematization, higher readings with areas of increased chlorite SF Quartzite Breccia SF Quartzite Breccia SF Quartzite Breccia SF Chloritized Quartzite SF Quartzite Breccia SF Quartzite Breccia SF Quartzite SF Quartzite Breccia SF Quartzite SF Quartzite Breccia SF Quartzite Breccia SF Quartzite Breccia Patchy chlorite in rock. This unit is dark grey with patches of sand tan coloured fragments of quartzite. 30% sand brown quartzite fragment and 70% chloritic matrix material. Fine magnetite and pyrite disseminated throughout, as well pyrite is observed in blebs. Mag reading between 22 and 25ams. Numerous fractures, the rock is mottled dark grey to beige. Beige colouration appears to be aureoles around dark coloured green magnetite fractures. Fracture infilling changes from chlorite to magnetite as we move into this interval. Mag readings between 11 and 35ams, increasing down interval. Similar to the unit above, but having more numerous darker areas. Dark areas caused by fine disseminated pyrite and magnetite. Small interval that is dark grey. Mag readings between 0.4 and 0.9ams. Medium grey in colour, finely crystalline. Homogenous, massive, a few white calcite veins. Numerous fragments with chlorite and magnetite fractures. Original fragments are dark brown and contain fine inclusions of magnetite and pyrite. Fractures becoming infilled with pink calcite. The rock has a crazed appearance due to the numerous fine magnetite veinlets. Pyrite occurs in some of the larger veinlets and in blotches. Numerous salmon to tan coloured fragments with diffuse edges in a dark green chlorite matrix, 80% fragments, 20% matrix. Minor pyrite in chlorite although locally up to 15% and occasionally forming euhedral crystals in fragments. 18 cm green gray band of chloritized quartzite at 44meters. Alternating medium gray and tan brown bands of very finely crystalline quartzite. Gray bands have tiny specks of chlorite while tan bands have very minor chlorite with pervasive hematization. Salmon orange with diffuse areas of medium gray. Local clouds of disseminated pyrite framboids containing up to 30% pyrite. Pyrite also found in chlorite fractures. Khaki tan to light brown, diffusely banded, very siliceous, minor chlorite concordant with banding. Mottled salmon to khaki brown fragments, fragments often with khaki brown interiors, with numerous fractures defined by light lines. Siliceous matrix with occasional green chlorite and localized areas of chlorite speckling. Unit core surface has a very smooth polish suggesting a high silica content. Medium gray to khaki bands, partially brecciated with banded sections with dark green chlorite infilling thin fractures. Medium gray to khaki gray, slightly brecciated, pervasively chloritized with minor disseminated pyrite. Weakly fractured with chlorite alteration along fractures. Previous mild hematization.

28 From To Lithology Description SF Argillite SF Quartzite Breccia Dark grey, uniform contains faint light grey wispy bands more silica rich with very weak hematite alteration. Unit contains very fine grained pyrite although there are local areas where blebby pyrite occurs. There is carbonate present within the matrix. It is flesh pick to khaki in colour, mottled, matrix is composed of white carbonate and some quartz. The fragments constitute 20% of the material and the matrix 80%. Towards the base of the unit there is less brecciation and some relic banding becoming apparent SF Argillaceous Siltstone Dark to medium grey, uniform with minor areas of fractures filled with white calcite. Some local banding and possible fragments of lighter coloured hematized quartzite. Towards the base of the unit there is a transition to lighter grey, gradation into the unit below SF Orthoquartzite SF Quartzite Breccia EF Limestone Light grey orthoquartzite, uniform, massive. Contains minor very fine disseminated pyrite. Thin white discontinuous fractures of white carbonate, faint banding present. Quartzite breccia with a carbonate matrix, likely limestone. The fragments comprise about 70% of the rock, 30% matrix. The fragments vary in colour from tan brown to medium grey. The matrix is speckled grey limestone. There are fractures throughout the fragments, but not the matrix and are composed of white carbonate. Varicoloured flesh pink to medium grey, more flesh coloured towards the top of the unit. Displays banding which is chloritized near the top of the unit. Epidote developed in some areas along the bands, khaki green coloured. Alteration blebs of tan coloured carbonate rims with cores of epidote towards the base of the unit EF Siltstone EF Silty Limestone EF Silty Limestone Dark green, banded with light grey, occasionally locally brecciated with white carbonate veins. Light pastel grey with occasional dark grey lines. Some diffuse pink bands. Minor amount of epidote bands which are a darker green colour. Banded silty limestone containing numerous irregular bandwidths of epidote, these vary in colour from dark green to pistachio green. Slight brecciation at the base of the unit with carbonate in a fractured matrix EF Silty Limestone Light grey with some thin bands of light pink and some bands of epidote EF Argillite EF Limestone Dark grey with faint areas of light grey, black uniform, non-descript, occasional white carbonate filled fractures. Minor amounts of disseminated pyrite. Consists of 70% varicoloured green epidote bands and 30% silty limestone. Epidote is mottled, lighter green pistachio coloured developing after a dark green epidote development EF Limestone Light grey limestone with bands of epidote, green in colour EF Limestone breccia EF Limestone EOH Varicoloured from dark grey pink to green and brecciated throughout. Matrix material consists of white carbonate, often pistachio green with epidote. Classic Espanola formation, consists of light grey limestone with shades of pink developing numerous dark bands, slightly contorted. Discrepancy between drillers block and our measurements. Block was missed up hole. End block shows 95.0m. Our measurement indicate 92.0m

29 TRM Mineralization Log From To Sulphide Mineral % Mineralization Type Pyrrhotite 0.5 Disseminated VG Specks Pyrite 8 Blebby With chlorite Pyrite 10 Blebby Pyrite 12 Blebby, fracture fill Pyrite 6 Blebby, fracture fill Several smaller flecks Pyrite 15 Fracture fill Pyrite 2 Fracture fill Comments VG in chlorite matrix associated with pyrite, free gold in chlorite cluster Gold occurs within chlorite fractures Pyrite 4 Fracture fill Associated with chlorite breccia matrix Pyrite 15 Finely disseminated pyrite 10 Disseminated and blebby Pyrite 1 Fracture fill Pyrite 0.5 Fracture fill Pyrite 30% Fracture fill 10% magnetite More pyrite (15%) noted locally (36.5m) in association with magnetite in fractures VG in chlorite matrix 0.46 AMS VG in chlorite matrix VG in chlorite matrix 0.36 AMS VG in chlorite matrix VG in chlorite matrix Pyrite 5 Fracture fill with pyrite Pyrite 20% Disseminated Pyrite 8 Disseminated Pyrite 5 Disseminated Also observed as fracture filling Pyrite 6 Disseminated and blebby Pyrite 0.5 Disseminated Pyrite 8 Disseminated Pyrite 0.5 Disseminated and blebby Pyrite 0.5 Disseminated Pyrite 0.5 Disseminated Right above odd alteration blebs

30 TRM Structural Log At Structure Angle T.C.A Bedding Bedding Banding Banding Banding Banding Banding Banding Banding Banding Banding Banding Banding Banding 48 Comment TMR Alteration Log From To Alteration Mineral 1 % Alteration Style 1 Alteration Mineral 2 % Alteration Style 2 Comment Hematite Weak Fractures developing into blebs Albite Moderate Pervasive Chlorite Weak Fracture filling Hematite Strong Pervasive Albite Weak to moderate Pervasive Hematite Weak Fracture filling Hematite Moderate Fractures and pervasive Chlorite Moderate Fracture filling Hematite Moderate Fracture filling Chlorite Moderate Fracture filling Hematite Moderate Pervasive Chlorite Moderate Fracture filling Hematite Weak Pervasive Chlorite Strong Fracture filling Hematite Weak Patchy Hematite Weak Fracture filling Chlorite Strong Fracture filling Chlorite Strong Patchy to pervasive Hematite Strong Pervasive Chlorite Moderate Fracture filling Hematite Moderate Pervasive Magnetite Moderate to strong Pervasive Chlorite Strong Breccia matrix Hematite Moderate Pervasive Magnetite Moderate Disseminated Magnetite Moderate Fracture filling Chlorite Strong Pervasive Magnetite Moderate Pervasive Carbonate Weak Veins Hematite Strong Pervasive Chlorite Moderate Fracture filling Hematite Weak Pervasive Magnetite also noted as cloudy like inclusions Calcite veining parallel to one another minor white thin parallel calcite veins Hematite Strong Pervasive Chlorite Moderate Pervasive Hematite Moderate Pervasive Chlorite Weak Hematite Moderate Pervasive Silica Strong Pervasive Hematite Weak Pervasive Chlorite Weak Fracture filling Hematite Weak Pervasive Carbonate Weak Fracture filling Chlorite Moderate Pervasive