by: j.k. fila, p. geo. october 20, 2005

DIAMOND DRILL REPORT

FOR

PELANGIO MINES INC.

ON THE

SIMON COPPER PROSPECT

IN

DENBIGH AND L YNDOCH TOWNSHIPS

SOUTHERN ONTARIO MINING DIVISION, ONTARIO

NTS 31 F/3

BY: J.K. Fila, P. Geo. October 20, 2005

TABLE OF CONTENTS

Part 1:

Introduction ..................................................................................... 1 Property, Location, and Access .............................. " ............................. 1 Topography and Vegetation ................................................................ 2 Area and Property History ................................................................... 2 Survey ControL ................................................................................. 4 Geology

Area Geology .......... " ............................................................... 4 Property Geology ..................................................................... 5 Economic Geology and Mineralization ........................................... 5 Discussion of Recent Drill Program ............................................... 6

Quality Control Procedures .................................................................. 10 Conclusions and Recommendations ...................................................... 1 0 Bibliography Certificate

Appendix 1: Copies of Original Assay Certificates Appendix 2: Lithology Legend for Sections Appendix 3: Qualtiy Control Standard Data

Figures:

Figure 1: General Location Map Figure 2&2A: General Geology Maps Figure 3: Property Geology Map Figure 4: Claim Map Figure 5: Compilation Map and Drill Hole Location Map Figure 6: Section for SC Drill Holes 4,5, & 8 (Base Metal Assays Shown) Figure 6A: Section for SC Drill Holes 4,5, & 8 (Precious Metal Assays Shown) Figure 7: Section for SC Drill Holes 6, 7 (Base Metal Assays Shown) and

Historical Noranda Hole 1 Figure 7A: Section for SC Drill Holes 6,7 (Precious Metal Assays Shown) and

Historical Noranda Hole 1 Figure 8: Longitudinal Section

Part 2: Copies of Original Drill Hole Logs

80"

~----- ~ c?t QU EBEC

-~ --~..,

Abitibi Greenstone Belt

68°

500

KILOMETERS

"* SIMON COPPER

SIMON COPPER GENERAL LOCATION MAP

Figure 1 October, 2005

INTRODUCTION

During the fall of 2004 Pelangio Mines Inc. initiated a phase 2 drill program on its Simon Copper Prospect in Lyndoch and Denbigh Townships in Southeastern Ontario. The recent five hole (1008 m.) drill program was designed to further test the down plunge extension of the Simon Copper South (SCS) Zone and evaluate proximal anomalies defined by both airborne and ground geophysical surveys.

In the early 1960's, the SCS Zone was explored by both Noranda Mines and Young Davidson Mines (YDM). YDM reported a mineral inventory of 253,000 tons @ 1.09% Cu on the South Zone, the majority of exploration work and the known mineral inventory is above 106 meter elevation. (T.Keast, 2000) Subsequent work by Pelangio in 2000-2001 successfully intersected the South Zone Deposit and extended the zone's known vertical depth to 155 meters below surface. This initial drilling showed that copper grades, zinc grades and associated alteration on the deposit were improving significantly at depth, suggesting some potential for higher grade mineralization and possibly better widths at depth. Based on some preliminary success Pelangio completed an airborne geophysical survey over the property to evaluate the entire claim block for a similar geophYSical signature found at the deposit. This survey outlined a number of excellent EM and magnetic signatures consistent with the response found over the deposit. The priority targets were followed up with ground geophysics to better define the targets. During the course of the 2004 program only two new targets were tested and the balance of the drilling allocated to evaluating the SCS Zone at depth.

This report will document the results of the most recent drilling program and also provide a limited summary of the work carried by Pelangio since the year 2000.

PROPERTY,LOCATION, AND ACCESS

Pelangio's Simon Copper Property is located in Southeastern Ontario, approximately 135 km west of Ottawa Ontario. (fig.1) More specifically the project is located in Denbigh and Lyndoch Townships at a latitude 45 degrees 10 min. North and longitude of 77degrees 20 min. West. The property is comprised of twelve contiguous claims (92 units) which cover an area of approximately 1472 hectares. The claims are numbered SO 1236668 to SO 1236673 inclusive. (fig. 4)

The claims are situated approximately 8 km north of the village of Denbigh. The property is easily accessed by travelling north along Highway 41

1

from Denbigh and utilizing the Slate Falls Road. The Slate Falls road is oriented in an northwesterly direction and connects with a northwesterly oriented bush roads that cross the property. The distance from Highway 41 along the Slate Falls and bush roads to the eastern property boundary is approximately 6 km.

TOPOGRAPHY. AND VEGETATION

The Simon Copper Property is located in an area or rolling terrain with a number of lakes and streams. Watercourses drain in a northward direction towards the Madawasaga River. Elevations on the property range from 335 meters to 485 meters above sea level.

Vegetation consists mainly of hardwood trees, mainly hemlock, with some oak. There appears to be minimal underbrush.

AREA AND PROPERTY HISTORY

From fig. 2 it can be seen that the Simon Deposit is hosted within a northeasterly trending belt of rocks approximately 175 km long. This belt hosts a series of deposits along with the Simon Deposit; one of these was a former producer, the New Calumet Mine. This mine produced approximately 3.4 million tonnes@ 6.0% Zn, 1.7% Pb, 124gft Ag and 0.65gft gold. The number of deposits along this prospective belt suggests that some serious exploration efforts have been initiated over the years and also demonstrates that this area in general has potential to host economic deposits. (Map, R. Dahn, Noranda 1992)

Closer to Denbigh and the known the Simon Copper Property historical prospecting efforts were focused on a variety of commodities including gold, base metals, uranium, garnet and graphite. During 1902 and 1903 a small graphite mine operated in Denbigh Township. (T. Keast, 2000)

On the Simon Property early exploration efforts were carried out by Mr. Eugene Simon who exposed what is known as the North Zone in the mid 1950's. Mr. Simon carried out trenching and some limited shallow diamond drilling on this zone. This zone is a chalcopyrite rich zone associated with iron formation, pyrrhotite, and pyrite. In the 1960's the Simon Property was worked by Noranda and Young Davidson Mines Ltd. Their work was focused on what is today known as the South Zone. Work by these two companies established a resource of 253,000 tons @ 1.09% Cu down to the 106 meter level. (T. Keast, 2000)

In the early 1990's Noranda did not control the original Simon Patents it did in the 1960's but did control certain land holdings that hosted the extrapolated down dip extension of the South Zone, North Zone, and East Zone. (fig.5) The East Zone was a zone found in the hanging wall of the South Zone during the course of

drilling in the 1960's by Noranda and Young Davidson. Noranda drilled two separate holes to test the down dip extent of the South Zone and North Zone. Each hole intersected its respective target, but no assays were reported; however drill logs indicated the presence of chalcopyrite and sphalerite in both intersections. (T. Keast, 2000)

In the year 2000 Pelangio completed three short holes to further evaluate the deposit down dip and along the plunge to the west. The program was very successful in extending the mineralization approximately 50 meters below the previously known extent of the mineralization and demonstrated that there was potential for better grades at depth and possibly a larger system due to the associated alteration zone. Results from the 2000 program are tabulated below in the accompanying table:

TABLE1: ASSAY DATA FOR SIMON COPPER DRILL HOLES YEAR 2000 PROGRAM Hole From To Meters Cuok Zn% Co% Au gIt Ag gtt .

SC-OO-1 131 136 5 0.74 0.21 0.012 0.055 1.34 i

Includes 131 133.22 2.2 1.44 0.35 0.022 0.104 2.58 Includes 132.18 133.22 1.04 2.94 0.57 0.045 0.21 5.12

145 146.06 1.06 0.66 0.18 NA 0.74 1.21 Includes 145 145.6 0.6 0.659 0.239 NA 1.28 1.3

• SC-OO-2 121 129.47 8.47 0.68 0.38 0.014· 0.05 1.25 Includes 122 124.45 3.45 1.08 0.86 0.019 0.044 2.07 Includes 124.95 125.45 0.5 3.81 0.236 0.04 0.06 7.2

SC-OO-3 119 121.9 2.9 1.74 0.79 0.024 0.09 2.6 Includes 120.35 121.9 1.55 2.88 1.21 0.038 0.15 4.18 Includes 120.35 120.77 0.42 5.63 0.99 0.058 0.13 8.6

121.9 128 6.1 0.099 NSV NSV NSV NSV 138.94 141.8 2.86 0.22 NSV NSV NSV NSV

161 179 18 0.012 NSV NSV NSV NSV !

In 2003 Pelangio completed an airborne survey over the entire property in order to define other potential base metal targets. This survey outline four distinct target areas. A ground follow up was completed in 2004 to better define these targets. This ground work showed that three of the four airborne anomalies originally defined were significant and warranted drill evaluation. During the course of the ground survey a secondary target was detected in the hangingwall of the South Zone; this hangingwall target was also recommended for drill evaluation.

In 2004 Pelangio drill tested two of the four new geophysical targets and continued to evaluate the South Zone; this program is described within the context of this report.

o New Calumet (Mined Out)

3.400.000 tons @ 6% Zinc. 1.7% Lead. 1 24gpt Silver. 0.65 gpt Gold

16"

20

Figure 2 South Eastern Ontario General Geology - Pelangio Mines Inc. - Simon Copper Property

, Sunon COpe)er ~ nickel

2 MocOlsa COA)er - nickel 3 RoQIOI'l copper. nlC_1

4 lIIewDora Iron - tnonlum

.. Copper. n Icke I

• Iron - titanium o Iron t titanium t cnromlt«

FIG 2A: Regional Geology Map, Adapted from tIM Bulletin .March, 1985

SURVEY CONTROL

Up to this point in time there has never been a control grid cut by Pelangio. Drill holes and some drill holes by previous operators have been tied in by chaining from known control points from surveyed township fabric and in some instances a hand held GPS unit was utilized.

Geophysical grids (including the area around the SCS Zone) utilized by Mr. J. Grant were flagged grids and the main target conductor axis's were given a GPS co-ordinate as noted in the Grant report. It should be noted that Mr. Grants report uses NAD 27 co-ordinates; and the initial airborne geophysical survey was also in NAD 27. New topographic maps from the government now utilize maps in NAD 83 and thus diamond drill hole co-ordinates shown in logs are in NAD 83 (Zone 18). The government topographic maps were also utilized for elevations once the drill holes had been plotted on them.

On some of the logs a grid co-ordinate as well as the UTM co-ordinate are given. The grid co-ordinate was for reference simplicity and in anticipation of a grid that was laid out and eventually will be cut out of necessity in future.

Because of the significant amount of work completed on this property a control grid is very much needed prior to completing any further work around the SCS Zone. This grid could be laid out so that it could be expanded at some future date to cover other areas of interest.

GEOLOGY

The geological section of this report has been adapted from a previous corporate intemal report for Pelangio written by Mr. T. Keast (April 2000). an independent geological consultant.

Area Geology

The regional general geological picture relative to the current subject property and the surrounding area is shown in the accompanying figs. 2 and 2A. The Simon Copper Property is within what is known as the Central Metasedimentary Belt of the Grenville Province (fig.2A). The Grenville Province is considered to be a complex orogenic belt that is 1.1 billion years in age; this belt is known to truncate several other geologic provinces. The Central Metasedimentary Belt is thought to be a major Mesoproterezoic accumumlation of supracrustal rocks intruded by compositionally diverse plutonic rocks of various ages. All of these rocks have been metamorphosed to grades varying between greenschist to granulite facies.

20 Limestone, Shale

1~. lcarbonatite Alkalic Complex

14

13

12

11

10

o

Felsic Igneous

Mafic & Ultramafic Igneous

Carbonate Metasediments

Clastic Metasediments

Mafic to Felsic Metavolcanics

LEGEND

Map Modified from OGS Map 2392: Ontario Geological Map Southern Ontario

Scale - kilometres

5 10

Property Geology Pelangio Mines Inc.

Simon Copper Property Fig. 3

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315000

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\, . . -,

320000

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SIMON COPPER CLAIM LOCATION MAP

Figure 4 October, 2005

The Simon Copper prospect is located with an un-subdivided area of the Bancroft Domain. The presence of metavolcanic rocks in this area rare to absent. The Bancroft terrane is dominated by calcitic marbles, graphitic and quartzofeldspathic gneisses derived from siliceous clasitic and sedimentary rocks. In the southwest portion of the Bancroft terrane volcaniclastic sediments are abundant. Intrusive rocks consist of tonalite-granodiorite and gabbro-diorite-syenite complexes. The Bancroft terrane is dominated by marble breccia zones and abundant high strain zones indicative of a structurally complex geology. The metamorphic grade in this area is considered to be upper amphibolite.

In general Denbigh and Lyndoch Townships are underlain by medasedimentary rocks which have been folded into major antiform/synform features. These large scale fold structures have been disrupted by the intrusion of the Weslemkoon granite.

Property Geology

The Simon Copper property is underlain by a wide belt of amphibolite gneiss; this gneiss is intercalated with minor marble, quartzite, and quartzfeldspar paragneiss. The stratigraphy on the property strikes in a north-south direction and dips moderately to the east. The units have been folded such that the mineralized surface occurrences on the property lie on the western edge of a large fold structure with numerous associated paraSitic folds, all plunging 40-60 degrees to the east. (Cochrane,1964)

The most common rock type in the vicinity of the Simon Prospect is amphibolite. This unit is a black, fine to medium grained; this unit is also a well layer foliated rock composed essentially of hornblende and plagioclase with locally abundant garnet, biotite and quartz. Other accessory minerals include sphene, epidote, apatite, chlorite carbonate, pyrite, pyrrhotite, and magnetite.

The quartz feldspar paragneiss is essentially a white rock that is fine grained and made up of quartz, plagioclase and minor biotite. The intrusive gabbro unit has a similar appearance to the amphibolite as it is also black and foliated. This unit is made up of a coarse grained aggregate of plagioclase, hornblende and relict pyroxene. A report by Cochrane (1964) suggests that the pyroxene in this unit has been replaced by amphibole, epidote, chlorite and carbonate.

Economic Geology and Mineralization

In general very limited work has been carried out on Pelangio's Simon Copper Property. The majority of concentrated exploration has been limited to an area approximately 500 by 500 meters in the immediate vicinity of the South Zone representing approximately 2% of the current Pelangio land holdings.

Noranda also carried out some limited geophysics on the property consisting of magnetics and a primitive EM survey; in total it is estimated that 8-10% of the project has had any recorded exploration. (See compilation map, fig. 5)

Despite the limited amount of work on the project a small deposit which has been designated the South Zone was outlined by Noranda and Young Davidson Mines. The deposit is reported to host a resource of 253,000 tons of 1.09% copper in the mid 1960's. (T. Keast, 2000) Noranda completed a single hole to test the down dip and down plunge extension of this zone in the early 1990's and intersected the zone; no assays were reported but the logs indicate the core contained both chalcopyrite and sphalerite mineralization.

Prior to the discovery of the South Zone, exploration efforts had been concentrated on a zone known as the North Zone. The showing is hosted within a gabbro and consists of chalcopyrite and pyrrhotite within a lens of massive magnetite that is 0.3 to 1 meter wide and 5 meters in length (Cochrane 1964). Grab samples by Noranda in the 1990's return values of up to 11.2% Cu. (Noranda, R. Dahn, 1992).

Limited pack sack drilling under the North Zone by prospector E. Simon intersected the zone in five of six holes (328.7m). No assays were submitted for this drilling, but logs show that magnetite and chalcopyrite mineralization ranging in thickness from 0.61 to 3.66 meters were intersected in this drilling. Noranda drilled a deep hole to intersect this zone in the early 1990's and intersected two narrow magnetite rich zones with pyrite, chalcopyrite and pyrrhotite mineralization. No assays were reported by Noranda.

During the course of drilling on the South Zone .in the 1960's, a hangingwall lense was intersected, this zone was designated the East Zone. A single drill hole in this zone intersected 0.95% Cu over 2.5 meters; sphalerite was also reported in this zone but no assays were taken for zinc. (Noranda. R. Dahn. 1992)

The approximate location for this zone is shown on the accompanying fig. 5 as per information taken from Noranda data. (R. Dahn. 1992)

The presence of the three aforementioned zones located in a very small 500 by 500 meter area suggests there may be possibilities for a series of stacked en-echelon copper zinc sulphide lenses on this prospect.

Discussion of the Recent Pelangio Drill Program

The focus of the recent five hole drill program (1008 m.) by Pelangio was to further test the down plunge extension of the South Zone mineralization and

evaluate two new geophysical anomalies proximal to the South Zone. A summary of the program results are tabulated below in Table 2. More in depth details on mineralization and geology are presented on a hole by hole basis in the following portions of this section.

TABLE 2' SIGNIFICANT ASSAY DATA for 2004 . Hole No From To Meters Cu% Zn% Au Ag glt Comment

g/t SCD04 ·70.77 71.77 1.00 0.182 0.091 NIL 0.8 Up Dip portion Simon Cu South

(SCS) Zone?

SCDS ** 116.93 131.41 14.48 0.543 0.76 NSV NSV Simon Cu South Zone includes 116.93 120.16 3.23 1.11 2.81 NSV NSV Simon Cu Upper South Zone includes 116.93 117.58 0.65 0.204 4.14 NSV NSV Simon Cu Upper South Zone includes 118.92 120.16 1.24 2.78 5.07 0.34 5.3 Simon Cu Upper South Zone includes 123.82 125.40 1.58 2.00 0.82 0.17 3.95 Simon Cu lower South Zone

SCOD6 39.48 41.16 1.68 0.32 NSV NSV NSV Qtz Vein above South Zone includes 39.48 39.90 0.42 1.03 NSV NSV NSV

108.85 109.55 0.70 0.172 1.16 NSV NSV E. Zone?(South Zone Hangingwall)

177.70 182.36 4.66 0.30 NSV NSV NSV Simon Cu Upper South Zone

190.75 200.65 9.90 0.40 NSV NSV NSV I Simon Cu lower South Zone includes 190.75 198.05 7.3 0.49 NSV NSV NSV Simon Cu lower South Zone includes 193.75 195.70 1.95 0.69 NSV NSV NSV Simon Cu lower South Zone

SCDD7 180.41 180.93 0.52 2.86 0.425 NSV NSV Simon Cu South Zone

SCDDa 144.44 145.49 1.05 0.41 0.122 NSV NSV Simon Cu Upper South Zone?

168.25 168.77 0.52 0.281 NSV NSV NSV Simon Cu lower South Zone? NOTE: NSV denotes no slgmficant value obtained.

**SC5 failed to intersect hanging-wall geophysics anomaly, but intersected SCS Zone.

Drill Hole SC004 Section 143 North:

Hole SCOO4 was collared to test an EM anomaly supposedly located in the hangingwall of the SCS Zone on flagged grid Line 0 Station 70 East on Grid A. (Grant, J., 2004) The actual UTM co-ordinate in Nad 83 for the EM axis located in the field is 318450 E and 5008791 N. The actual axis is designated by a blazed tree at the aforementioned co-ordinates for future reference purposes.

The top of the EM target was anticipated to be present at approximately 90 meters below the surface anomaly axis point and have a dip that was close to vertical. Hole SC004 could not be collared exactly along the same line that the

I I

I

i

I

geophysics was carried out on due to topographic conditions and was moved 20-25 meters grid north (Az. 020 deg.). The hole was however drilled parallel to the geophysics grid line azimuth which was 290 degrees.

Hole Se004 failed to intersect a conductor at the proposed target depth. The conductor may have been missed because of hole deviation or the fact that the hole was not drilled on the same line as the geophysics surveyor a combination of both issues. From a review of Grant's geophysical profiles it is evident that the conductors appear to have a short strike length at any specific elevation suggesting it may be very easy to cross over the top or below a specific plunge of a conductor. Again, this may have happened in this instance.

The drill hole did however intersect a small sulphide zone with minor eu values at 70.77 to 71.77 meters. This hole distinctly resembles the ses zone in texture and lines up very well with the ses Zone on section, but the dominant sulphide in the zone is pyrite rather than pyrrhotite typically found with chalcopyrite and sphalerite in the ses Zone. This intercept is a significant distance up dip and above the known plunge; thus is may represent the barren periphery of the ses Zone with somewhat different sulphide mineralization or it may be another sulphide lense in the same plane as the ses Zone. (see fig. 5, 6 &6A)

If the upper sulphide zone found in Hole Se004 is the equivalent of the ses Zone then there are two large unexplained anomalies in the footwall of the ses Zone. One of these is the target that Se004 was originally targeted to intersect and missed and a second large anomaly originally thought to be the ses Zone on flagged grid LO St. 50 W. Grid A as shown in the Grant report profiles. For future reference purposes flagged grid LO BLO on Grid A is located at 318405 E. and 5008798 N. in Nad 83. There are known copper bearing sulphide occurrences in the footwall of the ses such as the North Zone which was a surface zone reported by R. Dahn of Noranda in his compilation in 1992. (see fig. 5)

In any event, Hole Se004 appears to have failed to explain the cause of the anomaly on Grid A LO St 70E; however information from Se004 now suggests that there may be two unexplained anomalies in the FW of ses Zone as discussed above. A further review of the geophysics profiles is recommended in light of what Se004 has shown and perhaps some consideration should be given to investigating this area further with some down hole geophysics.

Drill Hole SCaa5 Section 143 North:

This hole was targeted to intersect a weak conductor axis on flagged Grid A, LO St.175 E. (see Grant, J. 2004) or UTM 318601 E and 508756 N in NAD 83.

At the time the drilling was carried out there was only a flagged geophysics grid in this area for control. A strong magnetic anomaly is present around the current SC005 collar; this magnetic anomaly extends up to and slightly beyond LO St.175 E. The magnetics caused approximately 20 degrees of deviation in the compassed flagged line and the presence of this deviation was not immediately recognized. Consequently, hole SC005 was drilled coincident to the flagged line; this orientation tested the conductor axis but resulted in a hole with an original attitude of 270 degrees azimuth or about 20 degrees off from other holes drilled to date by Pelangio. (see fig. 5 6, and 6A)

Hole SC005 failed to intersect the anticipated conductor but intersected the SCS Zone slightly to the north of earlier drilling conducted by Pelangio during the year 2000. The intersections obtained from the SCS Zone intercept are shown in accompanying Table 2 above.

Again since the original target zone for this hole was not intersected a review of the ground geophysics data in conjunction with drill hole data should be considered. If warranted perhaps some down hole geophysics might also be considered at some future date to assist with interpretation.

Drill Hole SCaa6 and SCaa7 Section 216 North:

An old Noranda hole from 1994 (NRSH001) was collared at the same location as Pelangio holes SC006 and SC007; the Noranda hole was drilled Significantly steeper than the Pelangio holes and slightly off section to the Pelangio holes. The Noranda logs denote a fairly significant sulphide intersection on what has been interpreted to be the SCS Zone; however no assays were provided. (see fig. 5,7 and 7A)

The Pelangio holes were drilled to test the up dip extension of the SCS Zone to ascertain what type of values were present in this portion of the SCS Zone. Hole SC006 intersected two sulphide zones in the vicinity of the SCS Zone designated the SCS Zone Lower and Upper.(see Table 2 above) This is typical of what was found in the Noranda holes and early drilling in Pelangio drill holes within the upper portions of the SCS Zone. The Lower Section of the SCS Zone is associated with stringer and disseminated mineralization with a garnet rich amphibolite crosscut by small felsic dykes which are also mineralized. The garnet rich amphibolite is sometimes almost made up totally of garnets; this may be an alteration system related to the sulphide zone. The intercept obtained from the Lower SCS Zone and accompanying mineralization below it assayed 0.40% Cu over 9.9 meters while the Upper SCS Zone assayed 0.3% Cu over 4.66 m. The

intervals particularly the lower interval suggest there may be good potential for wider sections of base metal mineralization at depth in this system.

Hole seooe also cut a small copper rich quartz vein near the collar; the relationship of this vein system to the known copper bearing zones on the property in unknown. Also, seooe intersected a small sulphide rich zone which may be related to a previous zone designated as the East Zone in Noranda data. (see fig. 5). This intercept and other historical intercepts suggest that there may be potential for a hangingwall sulphide zones above the ses Zone as well as footwall zones as discussed previously above in the section of the report pertaining to hole Se004.

Drill Hole SC008 Section 143 North:

Hole seoos is drilled slightly to the north of Se004 and Se005 but for presentation and interpretative purposes is presented on Section 143 North. This hole intersected only two small intercepts of sulphide mineralization. The ses Zone is thought to have been displaced to some extent by a fault, and as a result seoos likely only caught a peripheral portion of the ses Zone.

QUALITY CONTOL PROCEDURES

During the course of the recent program the company carried out quality control procedures. In every batch of 20 assay samples a standard and blank sample were submitted for assay. The standards submitted were from Analytical Solutions Ltd.; more specifically standard No's. Oreas 50p and 51 p. Details on this standard are shown in Appendix 3. The blank material was new building brick material. Aside from the quality control samples submitted to the lab by Pelangio the laboratory also carried out quality control work. The results of the quality control samples show the work carried out by the lab to be industry standard and no serious anomalous results or errors were noted.

CONCLUSIONS AND RECOMMENDATIONS

The most recent diamond drill program by Pelangio focused on further evaluating the ses Zone along strike to the NE and evaluation of two new geophysical anomalies proximal to the ses Zone. The highlight of the program was hole SeODe which intersected a broad low grade intercept within the ses Zone assaying 0.4% eu over 9.9 m. It appears that the ses Zone is becoming somewhat larger to the NE and associated with a garnet rich alteration zone. Substantial mineralization was also found within this alteration zone proximal to

the main sulphide rich zones. This alteration zone is considered very important because it suggests a large mineralizing system. Further, during the drilling program previous to this program hole Se003 (Filo, J.K., 2001) was stopped within a similar alteration package below the ses Zone as the significance of this alteration was not known at the time. Again these alteration systems suggest there is potential for large mineralized zone(s); the presence of the alteration system below the ses Zone lends credence to the fact that there may be multiple lenses of mineralization on this prospect.

Anomaly drilling proximal failed to intersect any major new significant lenses proximal to the ses Zone. However, in the case of hole Se004; geological interpretation suggests that the target for Se004 was missed due to hole deviation and that the actual target lies in the footwall of the ses Zone. Again this suggests potential for a series of stacked lenses of mineralization on this property which could significantly improve tonnage potential on this property.

In light of the positive results obtained on this project over the past few years the following recommendations should be carried out:

1) In the holes Se004 and Se005 where the proposed geophysical target was missed a review of the geophysics profiles and new geological data from drilling should be considered prior to any further drilling.

2) Anomalies Band e in the Grant report still remain untested. If a review of geophysical profiles is carried out with respect to item one above a review of profiles for anomalies Band e can be carried out as well prior to drilling.

3) Some consideration should be given to some down hole EM or IP surveys to further evaluate the extent of the ses Zone to the northeast and evaluate the stratigraphy above and below the ses Zone for other copper zinc bearing sulphide lenses. Surveying may be required in a number of holes; this program should be designed and completed in conjunction with a geophYSicist prior to any further drilling.

4) If possible some consideration should be given to some MMI {mobile metal ion} geochemical surveying along the projected strike of the ses Zone and perhaps over the vicinity of anomalies Band e prior to drilling.

5) At present there is no control grid on the property. To date drill holes and occurrences etc. have been chained in the township survey fabric and UTM co-ordinates obtained with a GPS. At this point in time a good control grid should be cut around the ses Zone to provide control for any future geophysics or geochemical work in that area.

This grid could be expanded if necessary to tie in other priority areas such as the Anomaly Band C areas if required.

ReSpeCtfo .. , Uy SUb. m .... itteZ/d. . .. ' d ,p'/z~

J. Keyin ~o. P.Geo. (Of1~;"B.C.) .,--". ""'~:

BIBLIOGRAPHY

Carter, T.R. et al. 1985: Metallic Mineral Deposits of the Grenville Province, Southeastern Ontario; Canadian Institute of Mining and Metallurgy, Bulletin, March 1985, p.95-106.

Carter, T.R. 1984: Metallogeny of the Grenville Province, Southeastern Ontario; Ontario Geological Survey Open File Report 5515.

Cochrane, D.R. 1964: A Copper Deposit near Denbigh Ontario. Unpublished MSc. Thesis,

Queens University, Kingston Ontario. Dahn, R.

1992: Project Summary and Proposed Exploration Program on the Central Basin Project Denbigh Area, Southern Ontario, Unpublished Internal Report for Noranda Exploration Company, Limited, Timmins Ontario.

Filo, J.K. 2001: Diamond Drill Report for Pelangio Mines Inc. on the Simon Copper

Prospect in Denbigh and Lyndoch Townships Southern Ontario Mining Division, Ontario NTS 31 F/3; Unpublished Internal Corporate Report for Pelangio Mines Inc., Timmins Ontario.

Grant, J. 2004: Geophysical Report for Pelangio Mines Inc. on the Simon Copper Unpublished Internal Corporate Report for Pelangio Mines Inc., Timmins

Ontario.

Keast, T. 2000: Valuation Report on the Simon Copper Prospect; Unpublished

Internal Corporate Report for Pelangio Mines Inc., Timmins, Ontario.

McGill, D. 2003: Didgem Survey Report for Pelangio Mines Inc. on the Simon Copper Property, Unpublished Internal Corporate Report for Pelangio Mines Inc., Timmins Ontario.

Noranda Exploration 1994: Assessment File Report 2.15698 from the Resident Geolgoists

Office, Tweed Ontario.

CERTIFICATE

I, J. Kevin Filo of 535 Sartleman St. of the City of Timmins do hereby certify:

1) I have personally written this drill report on the Simon Copper Property for Pelangio Mines Inc., and I have based the opinions contained in this report on a review of the drill core, assay data, and other pertinent reports written by previous operators, Pelangio Mines Inc. and independent consultants.

2) I further certify that I have a royalty interest in the subject property, and I hold a substantial share position in Pelangio Mines Inc.

3) I hold an Honours SSc. (1980) in Geology from Laurentian University in Sudbury Ontario. I have been practicing my profession as both a mining geologist for the past twenty-five years in Canada, Mexico and Southeast Asia. Prior to carrying out work as a consulting geologist I was employed by various mining and exploration companies. Some of these included T exasgulf Exploration, Amax Exploration. Urangesellschaft Canada, Cominco (Pine Point Mines) Pamour Porcupine Mines, Necro Con Mine and Freeport McMoran.

4) I am a professional geologist in good standing with the Association of Professional Engineers and Geoscientists of B.C. (Reg.#18677) and the Association of Professional Geoscientists of Ontario. (Reg.#0220).

J. Kevin Filo, P.Geo.

APPENDIX 1: COpy OF ORIGINAL ASSAY RESULTS

Swastika Laboratories Ltd Established 1928 Assaying - Consulting - Representation

ilssay £7erti/icate

Company: Project: Attn:

PELANGIO MINES INC. Simon Copper K. Filo

We hereby certify the following Assay of 57 Core samples submitted DEC-06-04 by .

Sample Number

51501 51502 51503 51504 51505

51506 51507 51506 5150S 5151C

5151] 5151~

51513 515H 51515

51516 51517 51518 51 51 9 :;;~ A ., ;.),'\ I\; t'l

51520 13 t-Il JIIIlt-

51521 51522 51523 51524 51525

51526 51527 5152'8

Au g/tonne

0.01 0.01 0.03 0.01 Nil

Nil Nil Nil

0.08 0.03

0.01 0.04 0.02 0.02 0.03

Nil Nil Nil

0.72 Nil

ill

0.05 Nil

0.01

0.17 Nil Nil

51529 Nil 51530 Nil

Au Check g/tonne

0.06

0.14

Ag g/tonne

0.1 0.1 0.1 0.2 0.1

----------0.1 0.1 0.1 1.2 0.1

0.2 0.1 0.1 0.1 0.1

0.1 0.1 0.1 2.4 0.1

0.1 0.3 0.7 0.2 0.4

0.3 0.1 0.1 0.1 0.1

Certified by

Cu %

0.012 0.005 0.005 0.033 0.006

----- .... - --0.004 0.009 0.010 1. 03

0.005

0.196 0.017 0.006 0.007 0.005

- - - - -- ... - --0.008 0.007 0.007

0.67 0.001 - - -- --0.008 0.026 0.172 0.015 0.057

0.036 0.001 0.003 0.001 0.020

Zn %

0.003 0.004 0.004 0.007 0.004

0.004 0.006 0.001 0.006 0.001

0.002 0.001 0.004 0.005 0.008

0.007 0.005 0.005 0.006 0.004

0.016 0.062 1.16

0.014 0.025

0.026 0.007 0.002 0.004 0.012

----------------

) Cameron Ave., P.O. Box 10, Swastika, Ontario POK ITO Telephone (705) 642-3244 Fax (705) 642-3300

Page 1 of 2

4W-2761-RAl

Date: DEC-14-04

- - - - - ------------


Page 1 of 2

Assay Certificate 4W-2772-RAI

Company: PELANGIO MINES INC. Date: DEC-15-04 Project: Simon Copper Attn: K. Fila


Sample Number

Au g/tonne

Nil 0.02 0.01 0.01

Au Check g/tonne

Ag g/tonne ------

0.1 0.1 0.1 0.1

Cu Zn !ir %

--------- --- ------ --------0.004 0.004 0.007 0.003 0.007 0.004 0.008 0.001

51573 51574 51575 51576 51577 0.01 0.1 0.006 0.003

51578 51579 -;TI'rPIIO /'f R, D 51580 fi.l..I'IAJ IL

51581 51582

51583 51584 51585 - -51586 51587

Nil 0.72 Nil Nil Nil

Nil Nil Nil Nil

0.01

51588 Nil 51589 0.01 51590 Nil 51591 Nil 51592 Nil

51593 51594 51595 51596 51597

51598 51599 51600 51601 51602

0.03 0.01 Nil

0.06 Nil

Nil Nil Nil Nil Nil

- ---

0.1 0.002 0.004 2.4 0.67 0.006 0.1 O.OOl 0.004 0.1 0.001 0.003 0.1 0.003 0.005 --------_. -----------0.1 0.003 0.004 O.l 0.00:2. 0.004 0.1 0.002 0.003 0.1 0.007 0.001 0.1 0.004 0.002 --------- - -- -- -- - - - --

0.1 0.008 0.001 0.1 0.002 0.001 0.1 O. all 0.004 0.2 0.021 0.001 0.1 0.008 0.004

0.1 0.004 0.004 0.3 0.018 0.004 0.1 0.006 0.006 0.1 0.007 0.006 0.3 0.027 0.004 --- - -- --0.2 0.012 0.009 0.1 0.001 0.006 0.1 0.005 0.005 0.1 0.006 0.005 0.1 0.006 0.005

- -- -

- - - -

Certifiedlly ~~ 1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK ITO

Telephone (705) 642-3244 Fax (705) 642-3300

- - -

- - -


Assay Certificate

Company: PELANGIO MINES INC. Project:

Attn:

Simon Copper K. Filo


Sample Number

51603 51604 51605 51606 51607

51608 51609 51f.}N f<}i\-Q, 1;)

51610 J3...AN Ii..

51611 Blank

STD OxK18

Au g/tonne

Nil Nil

0.02 Nil

0.02

Nil 0.75 0.03 0.02 Nil

3.40

Au Check g/tonne

Ag g/tonne -------

0.1 0.1 0.1 0.1 0.1

0.1 2.3 0.1 0.1

--------

Cu

" ------0.009 0.007 0.00:3 0.006 0.00·1

0.001 0.6'7

0.001 0.012

Zn %

0.005 0.005 0.004 0.008 0.004

0.002 0.006 0.003 0.010

Page 2 of 2

4W-2772-RAl

Date: DEC-15-04

Cenijied by j'ifL~ ~~ 1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK 1 TO

Telephone (705) 642-3244 Fax (705) 642-3300


Assay Certificate

Company:

Project:

Attn:

PELANGIO MINES INC. Simon COppt· K. Filo

We hereby certify the following Assay of 57 Core samples submitted DF~-06-04 by .

Sample Number

Au g/tonne

Au Check g/tonne

Ag g/tonne

Cu %

Zn %

Page 2 of 2

4W-2761-RAI

Date: DEC-14-04

- - - -- ---------- - - - --51531 51532 51533 51534 51535

51536 51537 51538 51539 ~ rAwDlrnO

51540 i;' '-!£W Ii 51541 51542 51543 51544 51545

51546 51547 Blank STD OxK18 51563

51564 51565 51566 .51567 51568

5i569 51570 515701 51572

0.01 Nil Nil

0.10

0.05

0.03

0.33 Nil

0.75 Nil

Nil Nil Nil Nil. Nil

Nil Nil Nil

3.48 Nil

Nil Nil Nil Nil

0.04

Nil Nil Nil Nil

0.11

0.1 0.2 0.1 0.4 2.1

0.6 0.5 0.6 2.4 0.1

0.3 0.2 0.1 0.1 0.2

0.1 0.2

0.1 - - - --0.1 0.1 0.1 0.1 0.9

0.2 0.3 0.1 0.1

0.005 0.023 0.001 0.210 0.80

0.160 0.268 0.260 0.67

0.001

0.086 0.042 0.011

0.005 0.013

0.008 0.015

0.009 ------~

0.009 0.0013 0.008 0.023

0.60

0.037 0.074 0.009 0.009

0.006 0.071 0.020 0.298 0.133

0.060 0.035 0.045 0.006 0.005

0.137

0.043 o 010 0.005 0.005

0.007 0.006

0.005

0.005 0.005 0.005 0.006 0.008

0.004 0.005 0.005 0.004

Certified by If) ~ ~ 1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTO

Telephone (705) 642-3244 Fax (705) 642-3300


ilssay l7ertijicate

Company: Project: Attn:

PELANGIO MINES LTD Simon Copper K. Filo

We hereby cenify the following Assay of 55 Core samples submitted DEC-I1-04 by .

Sample Number - --- ... ------51612 51613 51614 51615 51616

51617 51618 31619 51620 51621

51622 51623 S1624 51625 S1626

"i1627 ;1628

::i 16 2 9 ':5 'rfl(Jv f.J1's f?/P 516 3 0 P~t-ft1\I f{. ·1631

::>1632 51633

1634 1635

51636

1637 _1638

5163~

1640 1641

Au g/tonne

---------0.03

Nil Nil Nil Nil

Nil Nil Nil Nil Nil

0.03 0.02 Nil Nil Nil

0.01 Nil

0.74 Nil

0.01

0.01 0.01 0.01 Nil

0.01

Nil Nil Nil Nil Nil

Au Check g/tonne -- .... -

Nil

0.01

Ag g/tonne

0.1 0.4 0.4 0.1 0.1

0.1 0.1 0.1 0.1 0.1

0.8 0.2 0.3 0.1 0.7

0.3 0.2

2.4 0.1 0.1

0.1 0.1 5.5 0.3 0.4

0.4 0.8 0.1 0.1 0.2

Cu

0.012 0.066 0.051 O.Oll

0.009

0.006 0.018 0.001 0.001 0.017

0.022 0.013 0.065 0.008 0.129

0.045 0.019

0.68 0.001 0.009

0.011 0.018 2.86

0.028 0.032

0.098 0.214 0.011 0.012 0.012

Zn

0.012 0.022 0.024 0.010 0.039

0.006 0.026 0.009 0.005 0.011

0.137 0.017 0.287 0.009 0.184

0.049 0.019 0.006 0.004 0.013

0.011 0.090 0.425 0.016 0.009

0.012 0.012 0.006 0.005 0.008

Page 1 of 2

4W-2828-RAl

Date: DEC-16-04

CertifiedbY.0~ ~ I Cameron Ave., P.O. Box 10, Swastika, Ontario POK I TO

Telephone (705) 642-3244 Fax (705) 642-3300


Assay Certificate

Company: PELANGIO MINES LTD Project: Attn:

Simon Copper K. Fila

We hereby cenify the following Assay of 55 Core samples submitted DEC-ll-04 by .

Sample Number

51642 51643 51644 51645 51646

51647 51648 51649 t'1'/\ I\JOA(t'l

51650 1$ {.../J\ ",Ii.,

51651

51652 51653 51654 51655 51656

51657 51658 51659 51660 51661

51662 51663 51664 51665 51666

Blank STD OxK18

Au Au Check g!tonne g!tonne

0.01 Nil

0.02 0.01 Nil

Nil Nil

0.73

Nil Nil

Nil Nil Nil

0.01 0.01

Nil Nil Nil Nil Nil

Nil Nil

0.01 0.01 Nil

Nil 3.36

0.01

Nil

0.02

Ag g!tonne

0.1 0.1 0.1 0.1 0.1

0.1 0.1 0.1 0.1 0.1

0.1 0.1 0.1 0.1 0.2

0.4 0.4 0.8 0.1 0.1

0.1 0.1 0.1 0.1 0.1

CeniJied by

Cl.I

0.008 0.011 0.008 0.007 0.016

0.012 0.004 0.69

0.001 O.OOB

0.005 0.006 0.002 0.010 0.019

0.052 0.084 0.18:2 0.003 0.001

0.007 0.006 0.013 0.007 0.007

Zn %

0.014 0.004 0.004 0.004 0.006

0.004 0.004 0.006 0.004 0.006

0.005 0.006 0.004 0.006 0.016

0.069 0.064 0.091 0.003 0.003

0.007 0.005 0.005 0.005 0.004

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK ITO Telephone (705) 642-3244 Fax (705) 642-3300

Page 2 of 2

4W-2828-RAI

Date: DEC-16-04

Swastika LaboraLvJ.ies Ltd Estab: 18 Assaying - Consulting - Representation

Geochemf.' inaiy sis, '.1 rtificate

Company: pj ,GIO MINES LTD Project: Si ," ,opper Ann: K.

We hereby c. , submitted D'

[he followL Geochemical Analysis of 42 Core samples ,-04 by .

Sample Number

51548 51549 51550 51551 51552

51553 51554 51555 51556 51557

51558 51559 5rp.") f) .... n-o 51560 B .... /\IIJK

51561 51562

-~ 51667 51668 51669 ~ rl\v{;)Afl-/)

51670 R.tAAI/i. 51671

51672 51673 51674 51675 5167C

- - -- - - --51671 51675 5167, 51680 516Bl

- - - - - - - -- -- --

Au Au Check g,' lne g/tonne

hI 0·,08 0.03 Nil Nil

(1.12 0.32 Nil Nil Nil

0.09 0.47 Nil

0.05 Nil

Nil Nil

0.43 Nil

0.05

0.02 ).10 J,02 0.37 0.02

0.03 Nil Nil

0.01 0.29

0.03

O.lB

0.32

0.32

Ag g/tonne

0.1 1.0 1.0 0.2 0.9

1.0 1.1 0.7 0.4 0.2

.... _--------0.3 2.6 0.1 0.3 0.2

0.1 0.1 2.7 0.1 0.1

0.2 0.3 0.2 5.3 0.4

0.2 0.1 0.2 0.5 5.6

Cu %

0.017 0.81 0.79

0.028 0.61

0.71 0.75

0.463 0.345 0.045

0.096 0.73

0.002 0.273 0.042

0.007 O. 018

0.72 0.001 0.007

0.025 O. 20·~ 0.060

2,78 0.104

0.017 0.051 0.037 0.301

2.74

Zn %

0.010 0.025 0.024 0.012 0.014

0.025 0.024 0.014 0.014 0.013

0.010 0.006 0.005 0.011 0.009

0.008 0.007 0.006 0.004 0.007

0.015 4.14

0.091 5.07

0.124

0.017 0.016 0.017

0.63 0.87

Page 1 of 2

4W-2831-RGI

Date: DEC-17-04

---------------

Certified by ,.i)~ ci,;o-L <,

. Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTO Telephone (705) 642-3244 Fax (705) 642-3300

Swastika Laboratories Ltd Establ:,led 1928 i )saying - Consulting - Representation

Geochemical Analysis Certificate

Company: Project:

Ann:

PELANGIO MINES LTD Simon Copper K. Fila

We hereby certify the following Geochemical Analysis of 42 Core samples submitted DEC-14-04 by .

Sample Number

51682 51683 51684 51685 51686

51687 51688 51689 ·::iIA,.J/~lHti,;)

51690 /1 ... "'1111(.

51691

51692 51693 Blank STD OxK18

Au Au Check g/tonne g/tonne

0.04 Nil Nil Nil Nil

0.01 Nil

0.40 Nil Nil

0.21 0.01 Nil

3.41

0.20

Ag g/tonne

2.3 0.3 0.4 0.3 0.8

0.4 0.1 2.7 0.1 0.1

-------------0.1 0.1

Cu

1. 27 0.049 0.155 0.01'7

0.262

0.081 0.008

0.72 0.001 0.006 -------0.006 0.007

Zn

0.76 0.062 0.038 0.030 0.063

0.034 0.004 0.005 0.004 0.008

0.006 0.008

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK lTO Telephone (705) 642-3244 Fax (705) 642-3300

Page 2 of 2

4W-2831-RGI

Date: DEC-17-04


Assay Certificate 4W-2862-RAI

Company: PELANGIO MINES INC. Simmon Copper

Date: DEC-20-04 Project: Attn: K. Filo


Sample Number

-----------------~

51694 51695 51696 51697 51698

~-------------

51699 51700 51701 51702 51703

51704 Blank STD OxK18

JAN 0 5

Au g/tonne

Nil Nil

0.03 Nil

0.05

0.04 Nil Nil Nil

0.01

0.06 Nil

3.39

Au Check Ag g/tonne g/tonne -----------

0.1 0.1

0.03 0.7 0.1 0.1

-----------------0.03 0.1

0.1 0.1 0.2 0.4

0.2

Certified by

Cu Zn % %

----------------0.008 0.008 0.040 0.013 0.410 0.122 0.023 0.023 0.011 0.011 -----------------

0.009 0.005 0.029 0.011 0.038 0.016 0.032 0.018 0.281 0.019

0.032 0.007

1 Cameron Ave., P.O. Box 10, Swastika, Ontario POK 1T0 Telephone (705) 642-3244 Fax (705) 642-3300

- _ .. _----------

---------------

APPENDIX 2: LITHOLOGY LEGEND FOR SECTIONS

Code for Simon Copper Lithology

Name Casing Amphibolite Gneiss Garnet Amphibolite Gneiss Amphibolite Garnet Amphibolite Felsic Intrusive Diorite Intrusive Mafic Intrusive Semi Massive Sulphide Massive Sulphide Stringer & Disseminated Sulphide Magnetite Iron Formation Quartz/Mica Band Quartz Vein Fault Zone

Code Cas AGN GAGN AM GAM FI 01 MI SMS MS SDS MIF QMS QV FZ

APPENDIX 3: QUALITY CONTROL STANDARD DATA REFERENCE

•

ANALYTICAL SOLUTIONS LTD.

Gold Standards

Standard 10 Matrix Au Grade 95% Confidence

Cu Grade Ag Grade Cost ($C/kg) Interval

OREAS4Pa Greywacke 52 ppb ± 3 ppb $75.00

OREAS44P Laterite 67 ppb ±2 ppb MULTI-ELEMENT $110.00 Ferruginous

OREAS43P Greywacke 73 ppb ±2 ppb MUL TI-ELEMENT $100.00

OREAS42P Greywacke 91 ppb ± 3 ppb MUL TI-ELEMENT $100.00

OREAS 52P aMP 0.182 ppm ± 0.012 ppm 0.389% $75.00


OREAS 51P aMP 0.426 ppm ± 0.021 ppm 0.729% 2.7 ppm $75.00


OREAS 6Pb Greywacke 1.422 ppm ± 0.026 ppm $75.00

OREAS 17Pb Basalt 2.56 ppm ± 0.06 ppm $75.00

OREAS 60P Meta-andesite 2.61 ppm ± 0.003 ppm 4.8 ppm $75.00

OREAS 7Pa Greywacke 3.00 ppm ± 0.06 ppm $75.00

OREAS 18Pa Basalt 3.36 ppm ± 0.05 ppm $75.00

OREAS 61Pa Meta-andesite 4.45 ppm ± 0.012 ppm 8.5 ppm $75.00

OREAS 61Pb Meta-andesite 4.75 ppm ± 0.07 ppm 8.8 ppm $75.00

OREAS 62Pa Meta-andesite 9.62 ppm ± 0.19 ppm 18.7 ppm $75.00

OREAS 62Pb Meta-andesite 11 .27 ppm ± 0.025 ppm 21.4 ppm $75.00

• Available in 60 gm sealed foil pouches. • Shipping and taxes extra. • Handling fee of $30 for orders less than 2 kg.

. .. 2

Platinum Group Elements Standards

Description of material Item code Au Grade 95%. Pt Grade Confidence Interval (Au)

MUL TJ-ELEMENT STANDARDS (-4011)

Gabbronorite OREAS 13P 48 ppb ± 3 ppb 47 ppb

Massive Sulphide OREAS 14P 51 ppb ± 1 ppb 99 ppb

• Available in 60 gm sealed foil pouches.

Base Metal Pulp Standard

Description of material Item code Metal 95% Concentration Confidence

Interval

Base metal sulphide ore OREAS 33 (-401l) As 1517 ppm ± 55 ppm

Cd 95 ppm ±3ppm

Cu 3425 ppm ±67 ppm

Au 0.521 ppm ± 0.011 ppm

Fe 16.54% ± 0.36%

Pb 7.06% ± 0.11%

Mn 349 ppm ± 20 ppm

Ag 73 ppm ±'I ppm

Zn4.04% ± 0.07%

• Shipping and taxes extra. • Handling fee of $30 for orders less than 2 kg.

For further information contact: Analytical Solutions Ltd.

Lynda Bloom, M.Sc., P.Geo 1214-3266 Yonge Street, Toronto, ON M4N 2L6 Canada

Tel: 416-462-9124; Fax: 416-462-1637 [email protected]

Please visit us at www.explorationgeochem.com

Pd Grade Price per kg

$Canadian

69 ppb $90

150 ppb $90

Price per kg

$Canadian

$30/50g

Additional standards are being finalized to expand the range of standards that we offer.

___ 5D09.0oo mN

5008900 mN

50088DO_mN __

! /

! / , , ,

! , / , , , , , ,

/

*

! , ! , ,

SOUTH ZONE

, , , , , , / , ,

/

/ . / :/ , , ,

/ : , / , ,

/ , ,

* NORTH ZONE

w E g ~ 00

;;i: ....................

NRSH002 154.23m

1---

ui E

~ 00

M

------------------""-----r:---__ ~ ~h -----__

* EAST ZONE

§ - --------------

NRSH001 251.?6m

1- -

0-- __ --..

NRSH002

(~, :....~V

--

seDD6 SeDD?

NRSH001

O"""",~"""._"",,!~20 _____ .:s...i\40 - meters

Note: 1)Assays .

Cu, Zn0.41 2)Lithology

c;-O cF (j . o

0.1ifSin%

see appendix for legend 3)Cu & Zn Values

>0.01% . ··4)GFidfeferericeliriesribl

cut, just reference lines

PELANGIO MINES INC.

Oats:14110/2005

Au(hDr_

Sc~kI: 1:503

SIMON COPPER DRILL PLAN

(OLD & NEW HOLES)

Figure 5

ELEV350 m

ELEV 300 .ffi ..

.ELEV .250 m .

.ELEV .200.m ..

ELEV 1.50,m ..

" j , "IG'1\r yl

/ " /

...qGIv i

j/ G

1Gtv .; SC004 146.42m

/

meters

/ SC005 193.9m

/

/ ,

/ /

/ " /

... ... .. .. f,

,/

-z SC008 221.34m

, /

.'

i 7

, /

I -I

/ ·ON /

'ON " ;,/ ... . J

O'ON /

/ I

I

/

I

Note: 1)Assays

Cu, Zn 0.41 ~n % 2)Lithology


>0.01%

I 4 )Section along hole SC004

with holes 005 & 008 projected to section 0.4;

5) MAIN SULPHIDE LENSE

6) Holes SC005 & SC008 projected into section

PELANGIO MINES if\JC.

0""'4/1012005 ~ A,lhoc. -\

SIMON COPPER SECTION 143N

DOH SC004,005,008 1-0_'_ilc_" ___ 1

I~O'~~:vin:g~' ___ !i __ ~_~~ _ _____ ___ _____ _

Scale: 1:1000 I Figure 6

2 • 308 6 0 cl>

c,<:l

c." c;

ELEV350 m ;,. ",<' ",'" .., c,<:l 0<:l

''''-C; C;

" .. r.

"0. '" "0 'eN "i " ... / ::-"11

"'"" '"" " ~O""

'c...., " ,.' 1,0" .,. ~O.

.;.'/ ..y.\. , .... / ~~

"" c~ , \ . / o~ ,1 1' I

• " .-Ie..., I

~~ i

"e" / ,. I

ELEV 300m

., <,

'. :,\'

""'" :--'.

'" ~It .. I ,

l\\I" ,

'"" I .s' I -.,

,.," 'e,

tA " , .., ,,' 1,1 ".> .,..

,r' " " " :: !~ - " " j.r'1

"eN , ;,. I ,..' ~ ~I' ~, " ~) "

<, j

" I " .,' I

.,. <0" Co ,'\ .... I~. ..;:.t~,

'e~ ,.,.

022[; .7 , "'"

, J~E , ! '10.". ;.r, / ,l

"'c>, I ., , ,"" I o.~

ELEV 250 m "'G.t, ~{s> I •• gl ' I ....::.! It R

.. .. , . .. . /;,\" " . ...... f

.I . ,~I\ ~.1 (? f . .•. ....... . ...

"e se004

"'0. 'It;:t.< 1" ~" "'e, I .., . .C' ,

146.42m ,'- , I" 0..- /

,1 11 .11

! Note: I'~ r'

, 1)Assays

,,; l' III

I I Au, Ag 0.41 0.165 f

f'" 2)Lithology --111 ' :.10

"';~f

" . see appendix for legend . ,

'" Sos 3)Au & Ag Values .,. " "

" .... , / >0.01 & >1 .0 in glt

1111 i ~G'~,

4)Section along hole SC004 , with holes 005 & 008 ELEV 200 m <, projected to section

"e" sea05 Sf,,~.

5) MAIN SULPHIDE

193.9m " LENSE

I 6) Holes SC005 & SC008

c"'c'v projected into section

I , PElANGIO MINES INC. ! , 2S " metors

, " i

, , f

I ! I

~~ --:-::-:::I SIMON COPPER

ELEV1 50m

0010:1·1110/2005 1 -- SECTION 143N

,

t~_ I - DDH SCOO4,OO5,OO8 I

---I ! Offlco:

se008 -- ---' I

221.34m Dm, .. "O' , -Scale. 1.1000 I Figure 6A I

I

I

350 mN

300mN

250mN

200.mN

150.mN .

secos 2l &.2Sm

/

I

SeG07 22~ ,3Sm

.~:; ' .I

~I RSHOO I ~5 1.7ijm

i i !

~Js ./

/ /

I

/

I «"", I i

/ , I

/ /

I

0, /

!

!

:2 · 30860

Note: 1)Assays

Cu, ZnOA1 0.165 2)Lithology


>0.01%

4)Old Noranda hole projected into section

5) _ MAIN SULPHIDE ZONE

3) .. w·' FAULT ZONE

meters " 5

~_P.....,E_L_A_N_G_IO_M_IN_E_S_IN_C_·_--1 1

II I SIMON COPPER I.

I :::,~~_/OS_r2lJ_o5 .....:1 SECTION 216 N II ,0 ",ffi'::."'~' _ _ Ii--_D_D_H_ N_o_r_1_, S_C_O_O_6,_O_O_7 _

11 I ~'w";'l Figure 7 i I ~S"~"'='~~~----------~i j

350mN

300mN

250mN

200mN

'<',

150 mN

'" Q.l l ..

, ,

/ SCOOO 2 10 ~Om

I

se007 ;!:1835'1I

"<t,

"-0 / ,> ,-

.' / NRSHOOt 251.76m

./

/

i

/

i

/

/ /

/

/ I

/ I

- -,/ ,j ( i "

<.,; "

, --- - - -

Note: 1)Assays

ALi,Ag 0.410,165 glC 2)Lithology

see appendix for legend 3)Au & Ag Values

>0,1 & >1 ,0 glt

, , ....... - "

--'

4)Old Noranda hole projected into section

5) _ MAIN SULPHIDE ZONE

3) '-" FAULT ZONE

! '\ ,

PELANGIO MINES INC.

Oale:1 4/0S/2005 1 SIMON COPPER SECTION 216N

DOH Nor 1, SC006, 007

Dr.:lwing: ' I--------;--.~-------------------------~

Scale: 1:1000 Figure 7 A

-

2 .. 3 0 8 6 0 SOUTH ZONE 2.00/0 Cu I 12.2 meters

O)z 00 1::0 0) ..... s-O) 0)

NORTH ZONE

Norex Grabs Avg. 1.20/0 Cu, 4.00/0 Zn - I:: 0) ._

D::...J

I.F. Grabs Up To 11.20/0 Cu

400m

Figure 8

Compned Irom Pelongio / Norondo dolo ond mte.-prelolions

H-12

• • H-3

• H-4 • H-5 • 1.1% Cu/9.2m

H

1.43%

Legend

. 86% Cu/6.1m 2.96% Cu/2.7m H-11 Mod. Zinc •

-1 65-3 •

50

SCALE BAR

D,nterpreted Mineralized Zone

~Pelongio . Pierce Point (2000)

Cu%/ m

• Pelongio Pierce Point (2004)

Cu%/m

• Historical Pierce Point (Noranda/Young Davidson)

Cu%/m

EB Noranda Early 1990's

Cu%/m

1

H-6 •

65-5

H-8 • H-9

65-6

1.42'cu/3.4m

H-10 •

Elev.

~~--------------~~--r---------------------t-------------------~~3go~om~----------------t---------~ 0.95% Cu Elev.

SC-00-2 0.68% Cu/8.47m

0.74% "UI".uum A

SC-00-3

SC-00-5 0.543% Cu/14.48m

• 1.74% Cu/2.90m

etres

• SC-00-8 0.41 % Cu/1.05m

• SC-OO-8 0.28% Cu/0.52m

. SC-00-6 0.30% Cu/4.66m

• SC-00-6 0.40% Cu/9.90m -

SC-00-7 2.86% Cu/O.52m

_____ Noranda

Sulphide Intercept ~ (No Assays)

Z *(1)

~~ ~&

Pplongio Mi nes Inc Simon Copper Project

Longitudinal Section

Longitudinal Section Orientation Azimuth 020'

200m Elev.

100m

Notes: *(1 )Misplot of this hole in original report, now plotted with more accurate field information .

October, 2005 NTS: 31 F / 3

a)Other values like Zn & previous metals can be found on logs & sections

b)Some higher grade intercepts may be found within intervals shown in long section

DIAMOND DRILL REPORT

FOR

PELANGIO MINES INC.

ON THE

SIMON COPPER PROSPECT

IN

DENBIGH AND L YNDOCH TOWNSHIPS

SOUTHERN ONTARIO MINING DIVISION, ONTARIO

NTS 31 F/3

- e.CE\VEO PART 2 OF PART 2 R

O'J Q 3 1005

GEOSC\ENC~~S~ESSMENT

2 ~08 60

DRILL HOLE SC-04-04 SUMMARY PAGE

Exploration Company: Pelangio Mine Inc. Property Name: Simon Copper Property Drilling Company: Forage M. Lafreniere

Hole Started: Hole Completed: Logged By:

October 31, 2004 November 2, 2004 J. Kevin Filo, P.Geo.

Date Logged: December 4, 2004 to December 6, 2004

Survey Data:

Summary Log:

From To 0 12.65

12.65 19.47 19.47 21

21 27.5 27.5 32.72

32.72 38.41 38.41 52.57 52.57 70.77 70.77 71.77 71.77 73.3 73.3 117.35

117.35 118.03 118.03 127.78 127.78 128.6 128.6 136.85

136.85 146.42

EOH: 146.42

Rocktype Cas AGN

FI AGN

GAGN AM

GAGN AM

SMS FI

AM FI

AGN FI

AGN GAGN

Collar: 129 North 271 East UTM: 5008767 North 318547 East Azimuth: 290 Degrees Collar: -47 deg.

76m: Az: 288; Dip: -49 146m: Az: 303: Dip: -60

Note: See Code for lithological legend in Appendix 2 in report.

~v"

a fir " .

~/ ;/.

DRILL LOG SC-04-04 DRILL LOG PAGE 1 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g1tAu g1tAg

m. m. Type m. m. m. 0.00 12.65 Case Casing left in hole 12.65 19.47 Amphibolite -- this unit is an amphibolite gneiss with darker grey black mafic

Gneiss sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 10:90, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the lO's of em, banding or fabric present within these larger bands fairly distinctive banding is orinented 80-85 deg. to CA; schistose like appearance on broken section of core; orientation of mica noted -very blocky broken core with a few minor slips oriented at 20 deg. to CA, numerous fractures parallel to banding, some oxidation noted on slips -felsic pegmatitic dykes from 14.74 to 15.23 and 15.32 to 16.90, dykes principally made of K-spar and plagiocla<;e with some mica and minor mafic minerals -a few quartz stingers noted generally parallel to banding, these make up a maximum of I % of unit and these are generally a few mm. to a cm. or so wide -no significant mineralization noted -unit is very soft to moderately hard, more micaceolls sections softer -no response to magnet -no response to HCL -lower contact with dyke sharp and at 87 dee. to CA

19.47 21.00 Felsic Dyke -this is a coarse grained pegmatitic dyke made up of K-spar, plagioclase, quartz some mica an minor mafic minerals -competent lInit -no significant mineralization or sulphides -lower contact sharp at 45 del!:. to CA. .. -~~~ ....

-=this unit is an amphibolite gneiss with darker grey black mafic 21.00 27.50 Amphibolite Gneiss sections and lighter more felsic sections that are light grey to off

white in color. .... -~. ___________ M._

DRILL LOG SC-04-04 DRILL LOG PAGE 2 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg

m. m. Type m. m. m. Amphibolite -darker more mafic sections made up of hornhlende. chlorite, hiotite. Gneiss and some quartz and plagioclase, lighter sections mainly quartz. Continued plagioclase, biotite and some minor mafic minerals

-proportion of lighter to darker sections within this interval roughly 15:85. generally lighter hands med gr. hut coarser than darker hands -rare red garnet noted -handing in this unit ranges from a few mm. to a few cm. some banding noted in the 10'5 of cm , handing or fabric present within these larger bands -fairly distinctive banding is orinented 80-85 deg. to CA. -competent unit with a few fractures at 80-85 deg. to CA -some minor quartz noted a few stingers and veinlets: a few mm. to a cm. or so wide; these make up <1% of unit -unit is non-manetic -no signiticant sulphides noted -no HCL reaction -unit moderate to soft. can be scratched with knife with ease -lower contact gradational

27.50 32.72 Garnet -this unit is a garnet amphibolite gneiss with darker grey black mafic Amphibolite sections and lighter more felsic sections that are light grey to off 51(,49 standard #50p 0.69 0.006 0.73 0.1 Gneiss white in color. 51650 blank 0.001 0.004 NIL 0.1

-darker more mafic sections made up of hornblende. chlorite, biotite. and some quartz and plagioclase, lighter sections mainly quartz, plagiociase, biotite and some minor maiic minerals -proportion of lighter to darker sections within this interval roughly 51651 2852 29.27 0.75 0.008 0.006 NIL 0.1 15:85, generally lighter bands med gr. but coarser than darker bands 51652 29.27 30.80 1.53 0.005 0.005 NIL 0.1 -substantial amount of red anhedral garnets noted throughout 10-15% 51653 30.80 32.32 1.52 0.006 0.006 NIL 0.1 -banding in this unit ranges from a few mm. to a few cm. some 51654 32.32 32.72 0.40 0.002 0.004 NIL 0.1 banding noted in the I O's of cm . banding or fabric present within these larger bands -fairly distinctive banding is orinented 80-85 deg. to CA. -competent unit for the most part a few fractures at 80-85 deg. -a few minor quartz veins with occasional speck of sulphide. quartz veins a few mm. up 3-4 cm., these make up less than 1 % of unit


m. m. Type m. m. m. Garnet -this section also contains a few minor diorite dykes 15 -20 cm. in Amphibolite length Gneiss -overall sulphide content of this unit trace to <112% Continued

-unit is locally magnetic and this is pretty minor for the most part -weak to non-existent HCL response -moderately hard unit, distinctly harder where more garnets present -lower contact gradational

32.72 38.41 Amphibolite -this unit as per description from 21.00 to 27.50 m. above Gneiss -this unit is pretty competent with a few minor slips at 20 deg. to CA

and some fractures at 80-85 deg. to CA (same attitude as banding in this section) -occasional garnet noted in this section, increase towards lower contact -a few quartz veins and stingers noted, once again about 1-2% -this section has a few minor diorite dykes about 10- 20 cm. long -sulphide content trace -this section is non-magnetic -very weak HCL reaction -unit is moderately hard and can be scratched with knife -gradational lower contact

38.41 52.57 Garnet Amphibolite -this unit is a garnet amphibloite gneiss similar to garnet Gneiss amphiblolite gneiss sections described previously in this hole.

-like other similar units this one has darker grey black mafic sections & lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende. chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 20:80, generally lighter bands med gr. but coarser than darker bands -substantial amount of red anhedral garnets noted throughout 10- I 5% -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 1 O's of cm , banding or fabric present within these larger bands; some bands of garnet noted as well within unit -fairly distinctive banding is orinented 80-85 deg. to CA.

... -~-~ ~()rne evidence of folding in banding at 45 m .

.~ ... -~IULL LOG SC:04-04 DRILL LOG PAGE 4

r From To Rock Rock Type Description Samp. I F::.m To Samp. Cu% Zn% g/tAu g/tAg

m. m. Type m. m. Garnet -very competcnt unit with a few fractures at 80-85 deg. to CA. and Amphibolite the rare minor occasional slip at 15 deg. to CA. Gneiss -a few quartz veins and stinger ranging from a few cm. to mm. , Continued

some grayish white and others more bull white in appearance: quartz vein content in this interval of unit 1% -quartz generally parallels banding -also a few small diorite dykes noted again as well in the order of 10-20 cm: these will often contain minor red garnets as well on occasion -trace sulphides in this unit -no response to magnet -very weal response to HCL -variable hardness. moderate to hard where increased garnet content and softer in more chloritic sections. for the most part can still be scrau.:nel with knife

52.57 70.77 Amphibolite -this unit is an amphibolite gneiss with darker grey black mafic Gneiss sections and lighter more felsic sections that are light grey to off

white in color. -darker more matic sections made up of hornblende. chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 40:60. generally lighter bands med gr. but coarser than darker bands -rare red garnet noted

I -banding in this unit ranges from a few mm. to a few cm. some banding noted in the lO's of cm. banding or fabric present within these larger bands, but for the most part thin banding predominates -fairly distinctive banding is orinented 80-85 deg. to CA. -section within this unit; possible sub unit with little or no banding interspersed with banded sections from 59.76 to 65.95 as per original unit -some quartz noted in this interval principally in stringers and small veins, quartz content for entire unit estimated at 1-2%, most of this in section form 52.57 to 59 meters

_ ~_ ~RILL LOG SC-04-04 DRILL LOG PAGE 5

I From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg m. m. Type m. m. m.

Amphibolite -occasional sulphides notcd in some small quartz stingers towards 51655 65.85 67.38 1.53 0.010 0.006 0.01 0.1 Gneiss lower contact 51656 67.38 68.90 1.52 0.019 0.016 0.01 0.2 Continued -fairly competent unit with some minor fractures parallel to banding 51657 68.90 69.90 1.00 0.052 0.069 NIL 0.4 described for this unit and some minor slips and fractures oriented at 51658 69.90 70.77 0.87 0.084 0.064 NIL 0.4 20-30 deg. to CA: also some slips sub parallel to CA such at 61.60 to 62 , once again fairly minor -sulphide content in the entire interval about 1/2 to I % the vast majority of this being in fine sulphides in the last 5 meters above lower contact. main sulphide is pyritc with a speck or two of chalco -unit is non-magnetic -weak to non-existant HCL reaction -unit moderately hard and can be scratched with knife -lower contact gradational into sulphide rich zone but associated with small diorite dyke

70.77 71.77 Semi -initally this sections starts off with stringers and grades into a 51659 70.77 71.77 1.00 O.IS2 0.091 NIL O.S Massive section with poorly developed net texture and a few small sections Sulphide of semi-massive sulphide over \0 em or so and then back into

stingers and disseminated mineralization towards lower contact -overall sulphide content about 10-15%. this is predominantly pyrite -host rock of this sulphide zone is amphiblite typical of that described in numerous instances in this hole. somewhat sheared for about 10-15 cm before lower contact -lower contact "«f\(,j"tf'cI with quartz vein at 42 deg. to CA

71.77 73.30 Felsic -as stated above the first 10 cm or so of this unit is a quartz vein. then 51660 71.77 72.40 0.63 0.003 0.003 NIL 0.1 Intrusvie from 71,9 to 72.40 hcavily altered and greenish in color (altered 51661 72.40 73.30 0.90 0.001 0.003 NIL 0.1

feldspar); beyond altered section unalterd K-spar and plagioclase and some biotite mica make up unit. all of this unit is pegmatitic and coarse grained -trace of sulphide within unit, occasional speck or chalcopyrite -lower contact sharp and at 50 deg. to CA.

73.30 117.35 Amphibolite @72.30 to 87 m. 51662 73.30 74.00 0.70 0.007 0.007 NIL 0.1 Gneiss this unit is an amphibolite gneiss with darker grey black mafic 51663 74.00 75.00 1.00 0.006 0.005 NIL 0.1

sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende. chlorite. biotite, and some quartz and plagioclase. lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval approx. 40:60

~m DRILL LOG SC-04-04 DRILL LOG PAGE 6 ... -. __ . To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. Type m. m. m. Amphibolite -medium grained unit for most part, darker sections slightly more Gneiss finer grained than lighter grained Continued -this section primarily made up of bands of mm to cm or two wide

-banding generally orinented at 80-85 deg. to CA. -in this particular interval of unit some minor small patches with a few red garnets over 20 to 50 cm. -some minor quartz veins and stringer in this interval of unit; I % quartz maximum in a few stingers a mm. or so to a cm. or two in width generally parallel to banding as well -this unit considered relatively competent, a small number of fractures at 80-85 to CA, also a few minor slips at 15-20 deg. to CA. -moderately hard unit; can be scrathed with knife -trace of sulphide in this section -unit is non-magnetic -weak 10 non-existent HCL reaction

@ 87 m to 90.5 m -this is very similar to unit above except in contains significantly more garnets; perhaps about 7-10%. possible sub interval of unit -few slips in this section at 10 deg. to CA., very minor fault with a little gouge at 90.2, orinentation 35-40 deg. to CA. some minor fractures generally parallel to banding at 80-85 deg. to CA. -this interval has some sections that look somewhat silicified and thus unit is considered hard to moderately hard, more difficult to scratch silicifed portions with knife -no significant sulphides once again -weak HCL music -no response to magnet

@ 90.5 to 93.35 -once again a section as at 72.29 to 87 m., banding not as pronounced -few minor quartz stingers. generally parallel to banding at 85-90, quartz stingers, I % max -no significant sulphides and no response to magnct

~. -moderately hard unit that can be scratched with knife

DRILL LOG SC-04-04 DRILL LOG PAGE 7 -----.

From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg m. m. Type m. m. m.

Amphibolite -weak to non existant HCl response Gneiss -few minor slips in this section at 15 to 20 deg. to CA and fractures Continued parallel banding

@93.35 to 96.75 -this section basically as per section from 87 to 90.5 meters -once again about 7-10% garnets -still some banding and in the mm to em range with respect to widths and description of bands compositions as per the initial description in this unit from 72.29 to 87 m except some more garnets in this interval; this is a possible sub interval within unit -once again a few quartz stingers in this section from a few mm. to a cm. or two, these make up about I % of unit maximum -trace of sulphide generally on fracture plane -again a few minor slips at 10 deg. to CA.; and a few fractures as well parallel to banding at 80-85 deg. to CA. -occasional small diorite intrusive in this section 10 -15 cm long max. -trace of sulphide, pyrrhotite -overall this unit is non-magnetic -no significant HCL reaction -moderately hard unit again. some sections harder to scratch with knife because of garnets

@96.75 to 111.59 -again this is an amphibloite gneiss as per original description for this unit with darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase. lighter sections mainly quartz. plagioclase, biotite and some minor mafic minerals, rare garnet -proportion of lighter to darker sections within this interval approx. 40:60 -this section seems to have more chlorite and is moderate to soft and

~--- ... --.. fairly easily Watched with knife

~ Fro~ DRILL LOG SC·04·04 DRILL LOG PAGE 8 To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. Type m. m. m. Amphibolite -banding still of the mm. to cm. scale and at 80 to 85 deg. to CA. Gneiss -banding somewhat overprinted by mottled appearance in this section Continued -a few fractures in this interval at 80-85 deg. and 45 deg, to CA; also

a few slips at 5 deg. to CA. and 15 deg. to CA.: but overall a competent unit -no significant sulphides in this interval -no response to HCL in this interval -unit is non-magnetic in this interval -a few quartz vein ranging from 10 cm to 20 cm, two altogether, thus quartz content of this interval from vein quartz still I % max and these veins are barren

@111.59to 117,35 -this is still a gneissic amphiblolite as per description of interval immediately above this except this section is not as chloritic in appearance, not mottled and banding more distinctly evident than in interval above, banding in the mm. to cm. range in widths -lighter to darker sections about 60:40 in this section still -banding oriented at about 70 deg. to CA. -a few minor red garnets noted in this interval, pretty rare and patchy -some quartz veins in this unit in the mm. to a cm. or two in width; max 1% of unit -fairly competent interval with a few minor factures parallel to banding and some minor slips at 45 deg, to CA. -no significant sulphides noted -moderately hard unit. that can be scratched with knife some softer chloritic sections noted -no signigicant HCL reaction -lower contact sham along slip at 35-40 deg. to CA

117,35 118.03 Felsic Dyke -light colored pegmatitic dyke composed mainly of plagioclase, quartz and some biotite mica and minor manc minerals -no significant sulphides -sharp lower contact at 45 deg. to CA.

... ---~--... -- -.. ~

DRILL LOG SC-04-04 DRILL LOG PAGE 9 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. Tvpe m. m. m. 118.03 127.78 Amphibolite - this unit is an amphibolite gneiss with darker grey black mafic

Gneiss sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornhlende, chlorite. biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals, some minor sections over to's of cm with red garnets -unit is medium grainded with darker sections somewhat slightly tiner grained -proportion of lighter to darker sections within this interval approx. 40:60 -banding in this unit in the mm. to cm. range with a few intervals with bands from 10-15 cm .. handing on a smaller scale within these larger bands as well -some quartz noted within this section; in most instances quart7. vein lets and stingers are from a few mm. to cm in width and they are generally parallel to banding which is oriented at 75-80 deg. to CA. -unit is very competent, fractures are few in number and once again at about 75-80 deg. to CA., some rare minor slips also noted at 5 and 15 deg. to CA; these are pretty few in number as well -a few minor diorite dykes 10 cm or so long noted as well -sulphide content trace -unit is non-magnetic -unit has weak HCL reaction -unit is moderately hard and can be scratched with knife -lower contact with dyke sharp at 45 deg. to CA.

127.78 128.60 Felsic Dyke -corse grained pegmatitic dyke composed of plagioclase, K-spar, quartz minor biotite and mafic minerals -no significant sulphide noted -lower contact at shallow angle to CA.; 10 deg. to CA, near lower contact pegmatite dyke cuts small diorite dyke, pegmatite younger

DRILL LOG SC·04-04 DRILL LOG PAGE 10 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg

m. m. Tvpe m. m. m. 128.60 136.85 Amphibolite this unit is an Iphibolite gneiss with darker grey black mafic

Gneiss sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals and some garnets -garnets localized but may be present over 1-2 meter sections -proportion of lighter to darker sections within this interval approx. 40:60 -generally bands in the mm. to cm. range in width but some bands in the 10-15 cm range with banding present within the bands -unit is medium grained with darker sections being slightly more finer grai ned -banding at 80 deg. to CA for most part; note some evidence of folding at 129.5, banding goes from 45 to 80 over 10 to 15 cm interval this unit is a very competent interval with a few minor fractures at 80 deg. to CA and a few minor slips at 45 deg. to CA. -unit contains some minor quartz stingers and veinlets which make up about I % of unit; these are generally no more that a cm. and generally follow banding at 80 deg. to CA.: occasional clot of quartz noted as well -no significant sulphide noted in this unit, trace pyrrhotite and chalco associated with garnet rich sections -unit is non-mangetic -weak to non-existant HCL reaction -moderate to soft unit, can be relatively easily scrathed with knife -I(jwer contact gradational

136.85 146042 Garnet -this unit is a garnet amphibloite gneiss similar to garnet 51664 142.07 143.60 1.53 0.013 0.005 0.01 0.1 Amphibolite amphiblolite gneiss sections described previously in this hole. 51665 143.60 145.12 1.52 0.007 0.005 0.01 0.1 Gneiss -like other similar units this one has darker grey black mafic sections 51666 145.12 146.42 1.30 0.07 0.004 NIL 0.1

& lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite. biotite. and some quartz and plagioclase, lighter sections mainly quartz.

DRILL LOG SC·04-04 DRILL LOG PAGE 11 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. ~~~ ~ ...... Type m. m. m. . .. ~

... _--... ... __ . __ .. ..-~---...

Garnet plagioclase. biotite and some minor mafic minerals Amphibolite -proportion of lighter to darker sections within this interval roughly Gneiss 45:55, generally lighter bands med gr. but coarser than darker bands Continued

·substantial amount of red anhedral garnets noted throughout 10-\5% -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10' s of cm , banding or fabric present within these larger bands; some minor bands of garnet noted as well within unit -banding within this unit at about 85 deg. to CA. -this unit is very competent looking; a few fractures at 85 deg. to CA., and a few minor slips at about 45 deg. to CA. -unit contains some quartz veins; these make up I % max of unit and are generally a cm. or less wide and generally parallel banding -unit contains a small plagioclase rich pegmatite dyke over 14-20 em. ; outside of this no significant intrusives within unit. -unit has some trace sulphides, pyrrhotite and rare fleck of chalco -unit non-magnetic -weak HCL reaction at best -unit has variable hardness, easier to scratch with knife where no garnets; all in all of moderate hardness

E.O.H. 146.42 Core stored at Pelangio's field office in Connaught Ontario.



Hole Started: Hole Completed: Logged By: Date Logged:

Survey Data:

Summary Log:

From To 0 13.28

13.28 17.97 17.97 19.95 19.95 25.88 25.88 32.82 32.82 37.36 37.36 41.07 41.07 67

67 68.1 68.1 71.95

71.95 87.4 87.4 89.24 89.24 118.92

118.92 120.16 120.16 123.82 123.82 125.4 125.4 132.93

132.93 138.45 138.45 139.12 139.12 144.3 144.3 193.9

EOH: 193.90 meters

Rocktype Cas AGN

FI AGN

GAGN AGN

GAGN AGN

MI GAGN AGN

FI AGN

SMS/MS AGN

SMS/MS AGN

AGN/FZ AGN

FI AGN

November 2, 2004 November 4, 2004 J. Kevin Filo, P.Geo. December 6, 2004 to December 9, 2004

Collar: 162 North 283 East UTM: 5008748North 318655East Azimuth: 290 Degrees Collar: -50 deg.

117m: Az: 282; Dip: -51



m. m. Type m. m. m. 0.00 13.28 Case Casing len in hole 13.28 17.97 Amphibolite - this unit is an amphibolite gneiss with darker grey black mafic ,

Gneiss sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende. chlorite, biotite. and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals, some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 60:40, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10' s of cm . banding or fabric present within these larger bands as well -unit is medium grainded and darker sections slightly finer -banding within this unit at about 80 deg. to CA. -a few minor quartz veins noted; these are a few mm. to cm or so wide, and they make up about I % of unit maximum -fairly competent unit with a few fractures generally parallel to banding, a few minor slips noted at about 45 deg. to CA as well -a few traces of pyrrhoite in this unit -unit overall is non-magnetic -weak to non-existant HCL response -unit is moderately hard and can be scratched with knife -schistose appearance for about 40 cm. above lower contact, lower c;ontact sha,~and at about 85 deg. to CA

17.97 19.95 'Felsic Dyke -coarse grained pegmatitic dyke composed of K-spar, plagioclase, quartz and mica, no significant sulphides noted, competent looking unit with a few fractures at 70-80 deg. to CA. -lower contact sharp and at 45 deg. to CA.

19.95 25.88 Amphibolite -this unit pretty much as per description of amphibolite gneiss on Gneiss other side of dyke described above from 13.28 to 19.97

-this particular section does have a more equal proportion of light to dark colored bands 50:50 and a few more garnets sometime over 10-30 cm intervals -also a few minor slips at about 15 deg. to CA. and a few fractures parallel to banding at about 80-85 deg. to CA. -this section has a bit more of a mottled appearance and is possibly slightly more chloritic and thus moderately hard to soft, can be sratched with knife fairly easy particularly more chloritic bands

.. L--.. _


m. m. Type m. m. m. Amphibolite -once again unit is non magnetic

Gneiss -no significant HCL reaction. weak to non existant Continued -no significant mineralization noted

-lower contact gradational 25.88 32.82 Garnet -similar in composition to amphibolite;; above except significant

Amphibolite amount of garnets noted: this particular sections has about 7-10% Gneiss garnets

-the garnet amphibloite gneiss in this instance is a unit with darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende. chlorite, biotite. and some quartz and plagioclase. lighter sections mainly quartz, plagioclase. biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10's of cm . banding or fabric present within these larger bands as well -unit is medium grainded and darker sections slightly finer -banding within this unit at about 85 deg. to CA -unit competent a few fractures at 80-85 deg. to CA. -some minor quartz stringers and veinlets noted a em. or so wide; these generally make up less than I % of unit. -sulphides within this zone trace to non-existent. rare speck and or clot of pyrrhotite noted -unit is non-magnetic with the exception of rare localized spot over a few em. -weak to non-existent HCL reaction -moderately hard unit that can be scratched with knife with some difficulty :I()wer contact gradational

DRILL LOG SC-04-0S DRILL LOG PAGE 3 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu gltAg

m. m. Type m. m. m. 32.82 37.36 Amphibolite -as per previous sections of amphibolite gneiss in this hole this unit

Gneiss is made up of darker grey black malic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals. some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the I O's of em, banding or fabric present within these larger bands as well -unit is medium grainded and darker sections slightly finer -banding at about 80 deg. to CA. -competent unit rare fracture or two at 80 deg. to CA and occasional minor slip at 45 deg.to CA. and 10 deg. to CA. -a few minor quartz stingers generally under a cm.: < I % of unit -trace of sulphide, rare clot of pyrrhotite. -modrately hard unit that can be scratched with knife -weak to non-existent HCL reaction -lower contact gradational

37.36 41.07 Garnet -this garnet amphibloite gneiss is made up of darker grey black mafic Amphibolite sections and lighter more felsic sections that are light grey to off Gneiss white in color.

-darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -unit also contains approximately 10 % red anhedral garnets and occasional band of garnets a cm. or so wide. -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a lew mm. to a few em. some banding noted in the 10' s of em , banding or fabric present within these larger bands as well; banding at 85-90 deg. to CA. -unit is medium grainded and darker sections slightly finer ....... . ....

DRILL LOG SC·04-05 DRILL LOG PAGE 4 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg

m. m. Type m. m. m. Garnet -once again a competent unit with occasional slip at 10 deg. to CA; Amphibolite and a few fractures at 85 to 90 deg. to CA. Gneiss -no significant sulphides a rare quartz stinger or two noted Continued

-unit has weak HCL response -unit is moderately hard, more difficult to scratch with knife where garnets and more lighter colored silica rich sections present -unit has a gradational contact

41.07 67.00 Amphibolite -as per previous sections of amphibolite gneiss in this hole this unit Gneiss is made up of darker grey black mafic sections and lighter more

felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite. and some quartz and plagioclase. lighter sections mainly quartz. plagioclase. biotite and some minor mafic minerals, some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10's of cm . banding or fabric present within these larger bands as well -unit is medium grainded and darker sections slightly finer -banding at about 80-85 deg. to CA. ,some evidence of folding from observation of banding at 42.90 -competent unit with a minimal amount of fracture at 80-85 deg. to CA and occasional minor slip at 45 deg.to CA. and 10 deg. to CA. -sections of this unit have a more mottled look and appear somewhat more chlorite rich such as from 42 to 53 m. and 62 to lower contact -a few minor plagioclase/K-spar rich dykes noted and a few small diorite dykes in this section, these are few in number and generally under 20 cm. -some minor quartz stringers and veinlets up to a couple of cm. wide generally parallel to banding but occasional stinger at 15-20 deg. to CA; these estimated to make up < 1'1'0 of unit -trace sulghides noted at best

~ DRILL LOG SC-04-0S DRILL LOG PAGE 5 Samp. Gm From Rock Type Description To Samp. Cu% Zn% gltAu gltAg

m. m. m. Amphibolite -modrately hard unit that can be scratched with knife. mottled Gneiss sections which are thought to be more chlorite rich are slightly softer Continued -weak to non-existent HCL reaction

-lower contact associated with small diorite dyke associated with mafic intrusive below; contact sharp at 45 deg. to CA.

67.00 68.10 Mafic Dyke -very tine grained grey (chilled) mafic dyke -no sulphides -non-magnetic -lower contact associated with quartz vein at about 70 deg. to CA.

68.10 71.95 Garnet -similar in composition to amphibolites above except significant Amphibolite amount of garnets noted; this particular sections has about 7-10% Gneiss garnets

-the garnet amphibloite gneiss in this instance is a unit with darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more matic sections made up of hornblende. chlorite. biotite. and some quartz and plagioclase. lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 40:60, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. -unit is medium grainded and darker sections slightly finer -a few slips noted at 45 deg. to CA and a few fractures oriented parallel to banding which is at 80 deg. to CA.; generally a pretty competent interval -unit contains a few minor quartz stingers generally less than a cm. wide, these are generally parallel to banding and sometimes there are a few at some erratic angles; these veins make up approx. 1%. -some very minor sulphides noted <1% -unit is non-magnetic -variable hardness. unit can be scratched with knife, some chloritic sections which are softer and more garnet rich sections harder -lower contact gradational


m. m. Tvpe m. m. m. 71.95 R7.40 Amphibolite -as per previous sections of amphibolite gneiss in this hole this unit

Gneiss is made up of darker grey black malic sections and lighter more felsic sections that are light grey to off white in color. -darker more mane sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase. lighter sections mainly quartz, plagioclase. biotite and some minor manc minerals, some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm.; banding 75-85 deg. to CA. -unit is medium grainded and darker sections slightly liner -once again a lew minor slips at 15 and 40-45 deg. to CA and some fractures at about 80 deg. to CA which parallels banding, overall farily competent unit, minor fault with hematite at 74.55 to 74.85 -a few small diorite dykes and a dyke comprised mainly of coarse plagioclase and quartz and some mica (pegamatitic felsic dyke) from 81.85 to 82.40 m. -a few minor quartz veins noted, these are generally parallel to banding .• and mainly a cm or so wide maximum; these make up less than I % of unit. -sections within this unit have a mottled appearance and are somewhat more chloritic -very minor to trace sulphide note within this unit -very weak HCL reaction -unit moderately hard and can be scratched with knife. more mottled chloritic portions more easily scratched -contact with dyke below sharp and at 40 deg. to CA.

87.40 89.24 Felsic Dyke -coarse grained pegmatitic dyke primarily composed of K-spar. palgiocJase, quartz, and some biotite and minor mafic minerals -trace su Iphides -sharp lower contact associtated with slip at 15 deg. to CA.

. ...... ~

DRILL LOG SC-04-05 DRILL LOG PAGE 7 From To Rock Rock Type Description Samp.# From To Samp. Cu% Zn% g/tAu g/tAg

m. m. Type m. m. m. 89.24 118.92 Amphibolite -as per previous sections of amphibolite gneiss in this hole this unit 51667 111.59 113.11 1..52 0.007 0.008 NIL 0.1

Gneiss is made up of darker grey black mafic sections and lighter more 51668 113.11 114.63 1.52 0.018 0.007 NIL 0.1 felsic sections that are light grey to off white in color. 51669 standard #51p 0.72 0.006 0.43 2.7 -darker more malic sections made up of hornblende. chlorite. biotite, 51670 Blank 0.001 0.004 NIL 0.1 and some quartz and plagioclase. lighter sections mainly quartz, 51671 114.63 116.16 1..53 0.007 0.007 0.05 0.1 plagioclase, biotite and some minor mafic minerals, some minor red 51672 116.16 116.93 0.77 0.025 0.015 0.02 0.2 garnets noted in this interval as well. 51673 116.93 117.58 0.65 0.204 4.14 0.10 0.3 -proportion of lighter to darker sections within this interval roughly 51674 117.58 118.92 1.34 0.060 0.091 0.02 0.2 50:50. generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the lO's of cm , banding or fabric present within these larger bands as well -unit is medium grainded and darker sections slightly liner -banding at about 80-85 deg. to CA -for the most part a competent unit with some fractures parallel to banding. some minor slips noted at 15,30,45 and sub-parallel to CA.~ particularly between 96 and 100 m. -sections of this unit have a mottled texture once again and are somewhat more chloritic~ also some distinct looking chlorite altered bands as well locally -some minor quartz veins and stingers noted. these are generally under a couple of cm.: these are more prevalent between 96-1 OOm.; overall vein and stringer quartz make up a maximum of I % of unit. -this section contains some minor small diorite dykes and some smaller coarse pegmatitic dykes that are primarily plagioclase. quartz. biotite and some minor mafic minerals; the most prominent ones at 101.75 to 102.47 and 110.16 to 110.46 -for the most part pretty minimal sulphides in this unit but proximal to lower contact some clots of pyrrotite with some sphalerite over a cm. or two such as at 116.95 and 117.50 -no response to magnet and weak HCL reaction at best -moderately hard unit. can be scratched with knife, chloritic sections softer -Iowe~ontact sharg at 88 deg. to CA.

DRILL LOG SC-04-05 DRILL LOG PAGE 8 From To Rock Rock Type Description Samp.# From To Samp. Cu% Zn% gftAu gftAg

m. m. Type m. m. 118.92 120.16 Sulphide -this zone contains up approximately 25% sulphide hosted within a 51675 118.92 120.16 1.24 2.78 5.07 0.34 5.3 7.,one amphibolite zone typical of amphiblolites described previously in

this hole. the primary sulphide minerals are pyrrhotite. pyrite chalcopyrite and sphalerite, -the sulphide is semi-massive and some stringers and some bands of sulphide; it is estimated that there is 7% sphalerite. 4% chalcopyrite, 10% pyrrhotite and 4% pyrite. positive response to ohm meter -banding within this unit is at 30 deg. to core -lower contact associated with altered felsic dyke that is six cm. long, that is greenish in color (alteration of feldspars?) and contains some minor chalco. -below dyke contact sharp at 70 deg. to CA.

120.16 123.82 Amphibolite -as per previous sections of amphibolite gneiss in this hole this unit 51676 120.16 120.73 0.57 0.104 0.124 0.02 0.4 Gneiss is made up of darker grey black malic sections and lighter more 51677 120.73 122.26 1.53 0.017 0.017 0.03 0.2

felsic sections that are light grey to off white in color. 51678 122.26 122.78 0.52 0.051 0.016 NIL 0.1 -darker more malic sections made up of hornblende, chlorite. biotite. 51679 122.78 123.58 0.80 0.037 0.017 NIL 0.2 and some quartz and plagioclase. lighter sections mainly quartz. 51680 123.58 123.82 0.24 0.301 0.63 0.01 0.5 plagioclase. biotite and some minor mafic minerals. some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm.: banding 75-85 deg. to CA.; banding within this section crenualated in places suggesting some folding -unit is medium grainded and darker sections slightly tiner -occasional small diorite dyke a few cm or so wide with occasional garnet in them -a few minor quartz veins. one larger one from 123.14 from 123.58: estimated quartz content approx. 1%. -sulphide in this section pretty minor (trace), some pyrite mainly -moderately hard unit. can be scratched with knife -unit is non-magnetic -contact with sulphide zone sharp but erratic

DRILL LOG SC-04-05 DRILL LOG PAGE 9 From To Rock Type Rock Type Description Samp. # From To Samp. Cu% Zn% glt Au gltAg

m. m. I m. m. m. 123.82 125.40 Sulphide -this zone contains about 30% sulphides. this is mainly semi-massive and 51681 123.82 124.61 0.79 2.74 0.87 0.30 5.6 Zone massive sulphides: some stingers and clots and dissemianted sulphide as 51682 124.61 125.40 0.79 1.27 0.76 0.04 2.3

well, there is approximately 27% pyrrhotite and about 3% chalcopyrite -banded amphibolites host the sulphides, positive ohm meter response -the bandings is crenulated in sections of this unit and this suggests some folding of the unit -lower contact fairlv sham at about 80 deg;. to CA.

125.40 132.93 Amphibolite -as per previous sections of amphibolite gneiss in this hole this unit is 51683 125.40 126.83 1.43 0.049 0.062 NIL 0.3 Gneiss made up of darker grey black mafic sections and lighter more felsic 51684 126.83 128.36 1.53 0.155 0.D38 NIL 0.4 sections that are light grey to otT white in color. 51685 128.36 129.88 1.52 0.077 0.030 NIL 0.3 -darker more mafic sections made up of hornblende. chlorite, biotite, and 51686 129.88 131.41 1.53 0.262 0.063 NIL 0.8 some quartz and plagioclase, lighter sections mainly quartz, plagioclase, 51687 131.41 132.93 1.52 0.081 0.034 0.01 0.4 biotite and some minor mafic minerals, some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 50:50, generally lighter bands med gr. but coarscr than darker bands -banding in this unit ranges from a few mm. to a few cm.; banding 75-85 deg. to CA.; banding within this section crenualated in places suggesting some folding -unit is medium grainded and darker sections slightly finer banding in this unit at about 80-85 deg. to CA. -reasonably competent unit, a few fractures at 75-85 deg. to CA and on minor slip at 127 m. sub-parallel to CA.; becomes more blocky a couple of meteis above fault zone; few more fractures and slips above fault zone -some scattered fine sulphides noted throughout this unit; estimate about 2%, mainly pyrite, some pyrrhotite and some chalcopyrite -also a few quart stringers and veinlets generally a maximum of a cm. or so wide, these make up no more than I % of unit and sometime have mineralization within them -unit also contains minor diorite dykes 15-20 cm long. -for the most part unit is non-magnetic; rare instant where there is localized response -moderately hard unit that can be scratched with knife, some chloritic sections with a mottled texture more easily scratched -weak response to HCL, slip at lower contact and start of fault zone

DRILL LOG SC-04-05 DRILL LOG PAGE 10 From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. m. m. m. 132.93 138.45 Fault Zone of -this is a very blocky broken zone of gneissic amphibolite typical of 51688 132.93 1.B.93 1.00 0.008 0.004 NIL 0.1 Amphibolite gneissic amphiblolile described previously in this hole: there are 51689 standard #51p 0.72 0.005 0.40 2.7 Gneiss numerous slips and fractures: slips often have slickenslides evident: slips 51690 blank 0.001 0.004 NIL 0.1

are 15 deg. to CA. and or subparallel to CA. 51691 133.93 134.81 0.88 0.006 0.008 NIL 0.1 -dioriite dyke from 133.93 10 134.81 (upper contact 15 deg to CA and 51692 134.81 135.56 0.75 0.006 0.006 0.20 0.1 lower contact 85 deg. to CA) some smaller dykes above this 10-15 cm 51693 135.56 135.98 0.42 0.007 0.008 0.01 0.1 from upper contact to this main dyke -minor sulphides noted from lower dyke contact for about 75 cm below dyke; mainly pyrite and only 1-2%; some minor sulphides in dyke as well -this fault zone is non-magnetic, gneissic amphibolite is banded with light and dark bands typical of gneissic amphibolites described above, proportion of light to dark portions still about 50:50; banding at about 85 deg. to CA. -unit can be scratched with knife and is moderately hard; more chloritic sections obviously somewhat softer and diorite intrusive hard to scratch -lower contact sharp and associated with slip sub-parallel to CA; a lot of broken ground with lower contact

138.45 139.12 Amphibolite -as per description at 125.40 to 132.93 Gneiss -this section has no significant suldphide (trace sulphide)

-proportion of lighter to darker material 50:50 -banding at about 80-85 deg. to CA. -weak HCL reaction -unit moderately hard and can be scratched with knife -very locally over a cm. or two in a coupie of place unit is magnetic -sharp lower contact with dyke at 35-40 deg. to CA.

139.12 144.30 Felsic Dyke -coarse grained pegmatitic dyke composed of plagioclase, K-spar, quartz and minor biotite -occasional chalcopyrite on fractures in this dyke, minor overall -large raft of amphibolite within dyke from 142.93 to 143.81 -lower contact sharp and at 4S dei. to CA.

144.30 193.90 Amphibolite @ 144.30 to 160.37 Gneiss -as per previous sections of amphibolite gneiss in this hole this unit is

made up of darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase

DRILL LOG SC-04-05 DRILL LOG PAGE 11 From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg

m. m. m. m. m. Amphibolite biotite and some minor mafic minerals. some minor red garnets noted in

Gneiss this interval as well. Continued -proportion of lighter to darker sections within this interval roughly

50:50, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. for the most part but there are sections where bands are 20-30 cm. wide: banding is often present with these larger discrete bands that are 10' s of cm wide: generally no more than 40 cm. maximum -it should be noted that some of the lighter larger bands such at 147.30 m. exhibit textures that suggest a metamorphosed tuffaceous unit -banding generally at about 85 deg. to CA.: some banding oriented so as to suggest some folding such as at 154.60 m. -this particular interval is very competent looking with a few minor slips at 15-20 deg. to CA: a particular example of this is at 150.80 m.: fractures tend to follow banding -some quartz veining and stingers in this unit, these tend to follow banding and represent approximately I % of unit max: they are generally not more than a couple of cm. wide -occasional diorite dyke noted in this unit, main dyke noted at 158.95 to 159.36, this is associated with some slips, i.e. lower contact where slip and contact at 20 deg. to CA: upper contact of dyke at 85 deg. to CA. -sulphides within this unit trace at best -unit can be scratched with knife; TTlouerale haruness; iighter sections harder to scratch, darker sections more chloritic and easier to scratch

@160.37 to 175.61 -no real change from interval for this unit described immediately above -once again, trace of sulphides: occasional quartz stringer parallel to banding and I % maximum of unit -competent unit: rare slip or two at 45 and 15 deg. to CA, fractures parallel banding at 85 deg. to CA -unit is non magnetic and has weak HCL reaction -bands in the I O's of cm and tuffaceous looking bands not really present in this section

DRILL LOG SC-04-0S DRILL LOG PAGE 12 From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% WtAu gltAg

m. m. m. m. m. Amphibolite @175.61 to 193.90

Gueiss -distinctly similar compostionally to intervals of this unit described above Continued -distinct decrease in lighter colored (felsic) bands to darker (mafic bands);

the ratio is more like 30:70 and bands now only a few mm to a cm. or two with no bands in the 10' s of cm. as described previously above -banding generally at about 80-85 deg. to CA. -a few more garnet rich sections in this interval locally over 10-20 cm and some sporadic garnets(red in color and anhedral) -trace sulphides at best -unit has a few fractures parallel to banding some very minor slips at 45 deg. to CA and sub-parallel to CA.; one significant one over 25 cm associated with some blocky core from 179.64 to 179.89; this slip at about 5 deg. to CA.; overall a pretty competent unit -a few small plagioclase and quartz rich pegmatitic dykes generally under 20 cm. noted sporadically through the unit -very minor quartz stingers.< 1% -banding becoming less and less prominent in last few meters of core -very weak HCL reaction -unit can be scratched with knife, of moderate hardness -no response to magnet

E.O.H. 193.90 Core stored at Pelangio Mines Inc. field office in Connaught Ontario.




Survey Data:

Summary Log: From To

0 4.57 4.57 21.18

21.18 39.18 39.18 41.68 41.68 60.63 60.63 61.4 61.4 73.6 73.6 79.75

79.75 87.2 87.2 108.85

108.85 109.55 109.55 129.63 129.63 136.25 136.25 167.75 167.75 177.05 177.05 177.7 177.7 179.8 179.8 180.85

180.85 182.36 182.36 190.75 190.75 191.8 191.8 201.6 201.6 207.25

207.25 215.5 215.5 218.29

EOH: 218.29 meters

Rocktype Cas AM

AGN QV AM

AM/FZ AM

GAM AM

GAGN SDS AGN AM

GAGN AGN

FI AGN SMS

FI AM MS

GAM AM

GAM AM

November 5, 2004 November 7,2004 J. Kevin Filo, P.Geo. November 18, 2004 to November 27, 2004

Collar: 216 North 358 East UTM: 5008773 North 318744 East Azimuth: 290 Degrees Collar: -48 deg.

102m: Az: 295; Dip: -45 218m: Az: 296: Dip: -46

',.


DRILL LOG SC-04-06 DRILL LOG PAGE I From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. Type m. m. m. 0.00 4.57 Case 4.57 21.1 R Amphibolite -this unit is primarily light colored (light grey to off white) with a

few darker bands (grey black) -the mineralogy of the lighter sections is mainly quartz. plagioclase. biotite and minor muscovite mica in the lighter sections and some very minor mafic minerals; the more mafic or darker sections are dominated by hornblende. chlorite. biotite. along with quartz and plagioclase in lesser amounts -some banding evident in this unit. generally minor and more pronounced within mafic sections. note mafic sections make up about 5% of this unit; where banding is present it is generally on the 1 to 3 em scale and banding is generally oriented at 80 to 90 deg. to CA. -this unit is considered to be moderately hard and can be scratched with a knife -this unit does not respond to a magnet -the unit is generally a very competent unit with occasional fracture that generally follows banding at 80 to 90 deg. to CA; the exception to this is the start of the hole from 4.57 to 7.93 where the ground is blocky and broken up; this is likely due to proximity to surface -a small K-spar, plagioclase, and quartz rich pegmatite dyke was noted from 4.57 to 4.80 meters. the lower contact is sharp at 60 deg. to CA. -the unit has virtually nil sulphides of any sort -the occasional red colored garnet has been noted up 0.5 cm. -no significant response to HCL noted -lower contact is gradational

21.18 39.18 Amphibolite -this unit is primarily composed of grey black mafic bands (8:;-90%) Gneiss that are made up of hornblende, chlorite. biotite. and some quartz and

plagioclase; when broken a schistose like appearance is evident; quartz and plagioclase and biotite and very minor mafic minerals dominate tbe lighter grey to off white bands compositionally -banding ranges from a few mm. to a few cm .. banding is generally oriented at 60 to 70 deg. to CA. and more distinct in this unit -modrate to soft unit, light colored sections harder to scratch and darker sections easier due to chlorite -note sections of this unit with more light colored material from 32 to 34 m.; somewhat different than the norm for this unit; light colored material 60-65% for this interval -in rare instances some tiny red garnets noted -sulphide content of this unit trace at best. some minor pyrrhotite and pyrite specks noted at 27.7 meter

DRILL LOG SC·04-06 DRILL LOG PAGE 2 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gil Au gltAg

m. m. Type m. m. m. Amphibolite - grains size. lighter bands med gr. but coarser than darker bands 51501 26.22 27.75 1.53 0.012 0.003 0.01 0.1 Gneiss -no significant reaction to BCL 51502 27.75 29.27 1.52 0.005 0.004 0.01 0.1 Continued -this unit is very competent and has a few fractures. one set that is 51503 29.27 30.80 1.53 0.005 0.004 0.Q3 0.1

generall y parallel to fabric at 60-70 deg. to CA and another set that is 51504 30.80 32.32 1.52 O.m3 0.007 0.01 0.2 oriented at about 20 deg. to CA, this second set noted at 24.6 m. -in general this unit does not respond to magnet but from 26.22 to 32.32 there is strong but localized response: this is due to rare pyrrhotite and likely magnetite being present, occasional magnetite 51505 35.37 36.90 1.53 0.006 0.004 NIL 0.1 rich section over 10 em or so from interval 35.37 to 38.41 51506 36.90 38.41 1.51 0.004 0.004 NIL 0.1 -lower contact sharp at vein and at 45 deg. to CA. 51507 38.41 39.18 o.n 0.009 0.006 NIL 0.1

39.18 41.68 Quartz Vein -smoky grey blaek quartz vein 51508 39.18 39.48 0.30 O.OlO 0.001 NIL 0.1 -at 39.50 to 39.90 about 10·15% sulphide mainly pyrite and some 51509 39.48 39.90 0.42 1.03 0.006 0.07 1.2 chalcopyrite in clots. other portions of vein also contain smears and 51510 39.90 40.60 0.70 0.005 0.001 0.D3 0.1 blebs of pyrite, particularily large clot at 41.1 (pyrite). overall 51511 40.60 41.16 0.56 0.196 0.002 0.01 0.2 sulphide content of vein (both chalco and pyrite) 1-2% 51512 41.16 41.68 0.52 0.017 0.001 0.04 0.1 -unknown very hard black mineral (non-mangetic) that cannot be scratched with knife at 41 to 41.1 -quartz vein is blocky and broken with a large number of fractures. one set at 20 deg. to CA and a second set at 60-70 deg. to CA. -lower contact sharD at 45 deg. to CA

41.68 60.63 Amphibolite -this unit is primarily grey black in color with some sections of 51513 41.68 42.99 1.31 0.006 0.004 0.02 0.1 lighter grey to off white sections; the more mafic material that is grey black in color comprises about 70-80% of this unit -there is some banding in this unit but is not as pronounced as in the gneissic unit described above and thus it is designated as solely amphibolite. the units appearance with the exception of the banded sections generally the same, where banding is present it is generally at 70 deg. to CA -once again the darker grey colored mafic portion of the unit is comprised of hornblende, chlorite, biotite. quartz and plagioclase while the lighter colored portion of this unit is mainly quartz, plagioclase, biotite and possibly some minor mafic minerals -occasionally patches of small red garnets may be present -sulphide content in this section pretty minimal, local traces of pyrrhotite -a few minor rare quartz stingers occasionally noted at 80 deg. to CA -once again two sets of fractures noted, one at about 80 deg. to CA or parallel to fabric noted in unit and a second set at about 20 deg. to CA., generally a very competent unit -both lighter and darker portions of unit can be scratched with kni fe, moderately hard, more mafic darker portions of unit more easily scratched an4~lig~tly softer.

DRILl. LOG SC·04-06 DRILL LOG PAGE 3 I From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu glt Ag I

m. m. Type m. m. m. Amphibolite -no signi ficant response from magnet with the exception of where Continued speck of pyrrhotite noted.

-HCL reaction nil -lower contact sharp along fault gouge at 60.63 meters; contact 48 deg. toCA.

60.63 61.40 Amphibolite -predominantly grey black amphibolite made up of hornblende. Fault Zone chlorite, biotite and some quartz and plagioclase

-distinct gouge noted at 60.63 along slip at 45 deg. to CA.; also gouge at 61.4 and slip plane at lower contact at 25 deg. CA -some minor weak hematite stain note in fault zone, fairly broken bloc~round nOled below

61.40 73.60 Amphibolite -once again this unit is comprised of grey black sections which are more mafic in appearnce and some light grcy to off white sections which appear more felsic in appearance -the more mafic sections of this unit are comprised of hornblende chlorite, biotite and some quartz and plagicoclase while the more felsic or lighter sections are quartz. plagioclase biotite and minor mafic minerals -this section is predominantly made up of lighter colored material. approximately 80-85% and 15% mafic material. -generally lighter bands med gr. but coarser than darker bands -some local banding within this unit from few mm. to a few cm .• banding generally at 70 deg. to CA -a number of fractures present in this unit; two sets once again. one parallel to bands and a second at about 20 deg. to CA; fairly broken blocky ground from below fault above to about 68 m., also very block broken zone possible minor fault from 65.3 to 65.70 -there are also a series of minor slips at about 20 deg. to CA oriented similar to fractures described above -towards lower contact from 71.5 to lower contact there is an unusual texture where large anhedral quartz blebs and the occasional garnet has developed within the unit; at first glance these look like a dyke but they may be zones of strain and development of coarse crystals: a good example of this is from 72.15 to 72.60 -no significant mineralization noted in this unit -no response from magnet and no response to very weak HCL reaction -unit is hard but can be scratched with knife, some portions of lighter colored unit harder to scratch; likely due to quartz content

----I()wer contact gradational

,--.......

~ ...... DRILL LOG SC-04-06 DRILL LOG PAGE 4 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. Type m. m. m. 73.60 79.75 Garnet -garnet amphibolite unit is primarily made up of more mafic material

Amphibolite comprised of hornblende, chlorite, biotite and some plagioclase and quartz and numerous small garnets throughout -lighter sections which make up less than 10% of this section are mainly quartz, plagioclase and biotite. minor mafic minerals+/ occasional garnet -locally there is some minor banding in this unit at 75 to 80 deg. to CA.. some fractures at similar orientation and a few minor slips at 20 deg. to CA.. overall a very competent looking unit -fold axis at 90 deg. to CA noted at 77.85. 77.95 and 78.70 m. -at 74.35 to 74.80, section of coarser grained light colored amphibolite with coarse anhedral quartz and occasional subhedral garnet similar to that described in section above. possible zone of strai n agai n -this unit has little or no sulphides, some pyrite noted along occasional fracture plane or slip plane -moderately hard unit that can be scratched with knife -no response to magnet and no response to HCL -lower contact gradational distinct decrease in garnets over last couple of meters

79.75 87.20 Amphibolite -this section of amphibolite once again comprised of darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende. chlorite. biotite, and some quartz and plagioclase. lighter sections mainly quartz, plagioclase. biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 50:50 -banding limited to for the most part to last few meters and generally 80-90 deg. to CA. -competent unit with a few fractures at 45 deg. to CA and parallel to banding, some minor poorly developed slips at 20 deg. to CA. -a rare small garnet or two noted -no significant sulphide note -no signific;ant resQonse to magnet

DRILL LOG SC-04-06 DRILL LOG PAGE 5 -~---

From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg m. m. ~T~e m. m. m.

Amphibolite -no response to HCL Continued -lower contact gradational increasing banding towards contact and a

few more_garnets ------87.20 108.85 Garnet -garnet amphibolite unit is primarily made up of more mafic material 51514 93.29 94.82 1.53 0.007 0.005 0.02 0.1 Amphibolite comprised of hornblende. chlorite. biotite and some plagioclase and 51515 94.82 96.34 1.52 0.005 0.008 0.Q3 0.1 Gneiss quartz and numerous small garnets throughout 51516 96.34 97.87 1.53 0.008 0.007 NIL 0.1

-lighter sections which make up about 35% of this section are mainly 51517 97.87 99.39 1.52 0.007 0.005 NIL 0.1 quartz. plagioclase and biotite. minor mafic minerals and garnets

generally lighter bands med gr. but coarser than darker bands -garnets make up 10-15% of this unit -this section exhibits a gneissic texture and is stongly banded for the 51518 105.49 107.02 1.53 0.007 0.005 NIL 0.1 most part. banding ranges from a few mm. to 10' s of cm. 51519 standard #50p 0.67 0.006 0.72 2.4 -banding is at a high angle to the CA generally 75 to 90 deg. to CA. 51520 blank 0.001 0.004 NIL 0.1 -very competent looking unit with a few fractures generally parallel 51521 107.02 108.54 1.52 0.008 0.016 NIL 0.1 to banding and some very minor high angle slips between 90 to 93 51522 108.54 108.85 0.31 0.026 0.062 NIL 0.3 m. oriented at about 20 deg. to CA. -some minor quartz stingers in unit. <2% parallel to banding -at 89.45 to 89.80 small diorite dyke light colored. lots of plagioclase. erratic upper and lower contacts. -note more massive section of this unit found from 103.36 to 106 m. -this section fairly soft and relatively easily scratched with knife. possibly more chloritic -no significant sulphide noted. occasional trace particularly towards lower contact -from 107 to lower contact a few sections of light colored amphibolite that has become coarser grained and contains large anhedral quartz, possible zone of strain as described previously. boudinage like texture on more micro scale -no response from magnet and very weak to non existant reponse to HCL

----- ------------ =Iower cont~ct associated with minor slip at about 70 deg. to CA. 0.7-108.85 109.5.5 Sulphide -this section is comprised of 20-25% stringers blebs and/or poorly 5J523 108.85 109 . .55 0.70 0.172 1.16 0.0.5

Zone developed net texture, mainly 2-23% pyrite and 1 % sphalerite and 1% (:hJll(:oQYrite, does not respond to ohm meter

----

DRILL LOG SC·04-06 DRILL LOG PAGE 6 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAII gltAg

m. m. Type m. m. m. Sulphide -within this zone some very quartz rich sections, that have a drusy Zone appearance; some amphibolite also within this interval

-upper contact associated with slip at 70 deg to CA, and lower contact similarly 70 deg. to CA; note some banding within this section similarly 70 deg. to CA

109.55 129.63 Amphibolite -once again this section of amphibolite once again comprised of 51524 109.55 110.65 1.10 0.015 0.014 NIL 0.2 Gneiss darker grey black mafic sections and lighter more felsic sections that 51525 110.65 111.05 0.40 0.057 0.025 0.01 0.4 are light grey to off white in color. 51526 111.05 111.59 0.54 0.036 0.026 0.17 0.3 -darker more mane sections made up of hornblende, ch lorite, biotite. and some quartz and plagioclase, lighter sections mainly quartz, plagioclase. biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 25:75; generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. and is fairly distinctive (gneissic texture) banding is orinented 80-90 deg. to CA; schistose like appearance noted on broken section of core; orientation of mica; there is section with somewhat less banding from 118.20 to 122.85 -small dyke (diorite) composed of plagioclase, quartz and biotite and some ferro-magnesium minerals from 111.44 to 111.80, contacts sharp and at 80-90 deg. to CA; also small K feldspar dyke from 113.25 to 113.38. sharp contacts at 85-90 deg, to CA; also small K-spar; also small K spar rich pegmatite dyke from 118.20 to 118.5 upper contact at 50 deg. to CA & lower along minor slip 20 deg. to CA -generally pretty minor sulphides, (trace to <1/2%) some pyrite noted in association with a greenish colored minor felsic intrusive from from III to 111.25 this felsic intrusive somewhat greenish but similar in appearance to quartz rich sections found in sulphide rich unit above -for the most part this unit is a fairly competent unit with only a few fractures, fractures generally parallel bedding 80 to 90 deg. to CA.; some fractures noted at 20 deg. to CA; in some instances some evidence of movement along these and thus some of these considered minor slips; minor fault with gouge at 123.22 to 123.4 upper contact 20 deg. to CA and lower contact 45 deg. to CA

DRILL LOG SC·04-06 DRILL LOG PAGE 7 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/IAg

m. m. TvJlC m. m. m. Amphibolite -some minor garnets noted from 123.8 to 127 meters Gneiss -this unit moderately hard but can be seratehed with knife, more Continued mafic sections softer due to chlorite

-no real significant response from magnet -weak to non existent HCL response -lower contact gradational

129.63 136.25 Amphibolite -eompositionally this unit similar to amphibolite gneiss above; once again this section of amphibolite once again eomprised of darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 10:90; generally lighter bands med gr. but coarser than darker bands -banding within this interval significantly less, more massive in appearance;where weak fabric is present banding oriented 80-90 deg. toCA -some minor quartz stingers parallel to this banding on occasion; quartz veins <2% of unit -trace sulphide at best in this unit -very competent unit; a few minor fractures generally at 89-90 deg. toCA -unit is moderate in hardness and can be scratched with knife; also no response to magnet -very weak to non-existant HCL response -very rare occasional garnet seen in this unit -lower contact associated with small dyke, < !Ocm. diorite, lower contact of dyke at 136.25 oriented 80 deg. to CA.

136.25 167.75 Garnet -@ 136.25 to 151.22 Amphibolite -this section of garnet amphibolite gneiss is very similar in Gneiss composition previously described units with the exception that there

are red garnets within this section; estimate 10% plus garnets

DRILL LOG SC-04-06 DRII.L LOG PAGE 8 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

m. m. Type m. m. m. Garnet - this section garnet amphibolite gneiss once again comprised of Amphibolite darker grey black mafic sections and lighter more felsic sections that Gneiss are light grey to off white in color. Continued

-darker more rna tic sections made up of hornblende. chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz. plagioclase. biotite and some minor mafic minerals. both light and darker sections contain a significant number of red colored granets -proportion of lighter to darker sections within this interval roughly )0:70. generally lighter bands med gr. but coarser than darker bands -this particular interval contains a significant number of dykes; these dykes are coarse grained but not quite pegamatitic diorite dykes composed of plagioclase feldspar quartz and some biotitie mica. -dykes present at 137.45 to 138.88; 139.10 to 139.30, 146.72 to 147.03 and 149 to 149.40; there are also a series of small dykes as well generally under IOcm. contacts generally follow the banded fabric which is at about 75-80 deg to CA. -once again banding ranges from a few mm. to few cm. -very eompetent unit with a few fractures generally parallel to fabric at 75-80 deg. to CA -some quartz stingers generally under a cm and parallel to fabric present; estimate 3-4% maximum -sulphide content trace to non-existant -moderate to hard unit, that can be scratched with knife. more chloritic rich sections easier scratched -some weak HCL reaction -no significant response to magnet

@151.22to 167.75 -still garnet amphibolite gneiss as per section above. similar composition as described above -slightly more lighter material in this section light to darker material approx 40:60, generally lighter bands med gr. but coarser than I darker bands -banding intervals in this section generally a few mm. to a em. max.; banding still as approximately 80 deg. to CA; some minor quartz

DRILL LOG SC-04-06 DRILL LOG PAGE 9 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn'1'~ gil Au gil Ag

m. m. Type m. m. m. Garnel stringers generally under a cm., these make up 2-3% of unit; 51527 \62.80 163.20 0.40 0.001 0.007 NIL 0.1 Amphibolite exception of small vein at \63.2 to 163.5 51528 163.20 163.50 0.30 0.003 0.002 NIL 0.1 Gneiss -still lots of red garnets 10-15%, unit also more schistose in 51529 163.50 163.88 0.38 0.001 0.004 NIL 0.1 Continued appearance as well.

-few minor fractures once again; generally parallel to banding descrihed in this section and occasional rare minor slip at 20 deg. to CA such as at 160.45 m. -trace sulphide in this interval at hest -no significant response to HCL and no response to magnet -gradational lower contact

167.75 177.05 Amphibolite -this unit as per amphibolites and amphiholite gneiss described 51530 172.56 174.09 1.53 0.020 0.012 NIL 0.1 Gneiss previously in this hole 51531 174.09 175.61 1.52 0.005 0.006 0.01 0.1

-this section of amphibolite gneiss once again comprised of darker 51532 175.61 177.05 1.44 0.023 0.071 NIL 0.2 grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 10:90; generally lighter bands med gr. but coarser than darker bands -rare occasional red garnet note in this section -generally banding ranges from a few mm to a cm. or two; handing oriented 75-80 deg. to CA -a few minor quartz stingers noted in this section generally < 1/2 cm oriented parallel to fabric; occasional vein a cm or two. -very competent unit, with a few fractures paralle! to banding and rare minor slip noted on occasion at about 20 deg. to CA -this section contains Y2% sulphides generally sporadically disseminated and rare clot or bleb, sulphide mainly pyrite and rare speck of chalcopyrite -some minor sections in this unit respond to magnet, some magnetite thought to be present -variable hardness but still considered of moderate hardness and scratched with knife with not much difficulty -HCL reaction pretty much non existant -lower contact sharp and associated with shear on contact with lower unit at 50 de~ to CA

'-..

DRILL LOG SC-04-06 DRILL LOG PAGE 10 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% glt Au glt Ag

m. m. TVDe m. m. m. 177.05 177.70 Felsic Dyke -coarse grained K-spar rich pink colored pegmatite dyke, also 5]533 177.05 177.70 0.65 0.001 0.020 NIL 0.1

contains chloritic clots some quartz and muscovite mica -minor sulphides present, trace pyrite -unit is non magnetic hard. and has no HCL reaction -lower contact sharp at 45 deg. to CA.

177.70 179.80 Amphibolite -as per previous descriptions once again this section of amphibolite 51534 177.70 178.66 0.96 0.210 0.298 0.10 0.4 Gneiss gneiss is made up of darker grey black mafic sections and lighter 5]535 178.66 179.21 0.55 0.80 0.133 0.05 2.1

more felsic sections that are light grey to off white in color. 51536 179.21 179.80 0.59 0.16 0.060 0.03 0.6 -darker more mafic sections made up of hornblende. chlorite. biotite. and some quartz and plagioclase. lighter sections mainly quartz. plagioclase. biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 5:95, generally lighter bands med gr. but coarser than darker bands -banding within this section at 80 deg. to CA. and generally a few mm. in width to a I to 1.5 cm. max. -occasional quartz stinger parallel to banding. <2% of unit -competent unit with occasional fracture parallel to banding and rare minor slip at about 20 deg. to CA. -this unit is well mineralized with about 10% sulphides. comprised of disseminated stinger and clots of massive sulphide. estimate of about 1,4 to V2 % chalcopyrite overall and I % pyrite and 8-9% pyrrhotite -occassional plagioclase rich diorite dykes up to 15 em noted -unit is magnetic from pyrrhotite -unit soft to moderately hard. can be scratched with knife -weak to non existent HCL reaction -lower eontact erratic in appearance

179.80 180.85 Semi -mainly semi massive to net textured pyrrhotite associated with clots 51537 179.80 180.85 1.05 0.268 0.035 0.33 0.5 Massive of pyrite «2%) and some minor chalcopyrite (1/2%) Sulphide -lower contact erratic at about 40-45 deg. to CA

-reacts to ohm meter (conductive) 180.85 182.36 Felsic Dyke -this is once again a pinkish colored coarse grained K-spar rich 51538 180.85 182.36 1.51 0.26 0.045 NIL 0.6

pegmatitic dyke with some quartz and biotite mica as well 51539 standard #50p 0.67 0.006 0.75 2.4 -the unit has a high sulphide eontent. mainly pyrite. it also contains 51540 blank 0.001 0.005 NIL 0.1 some minor rafts of pyrrhotite rich amphibolite. also some minor disseminated chalcopyrite is present

DRILL LOG SC·04·06 DRILL LOG PAGE 11 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg

rn. m. Type m. m. m. -~ .. ._--Felsic Dyke -estimated sulphide content for this unit is 10% : approximately 7%

Continued pyrite, 2 to 2.5% pyrrhotite and 0.5% chalcopyrite -lower contact is sharp for dyke and associated with a shear, contact 30 deg. to CA.

182.36 190.75 Amphibolite -first 40 cm of this unit proximal to upper contact strongly sheared 51541 182.36 182.76 OAO 0.086 0.137 0.3 NIL and shear orientation or shear fabric 45 deg. to CA, some minor 51542 182.76 183.26 0.50 0.042 0.043 0.2 NIL pyrite and pyrrhotite stingers noted in this section parallel to shear 51543 183.26 184.76 1.50 0.011 0.010 0.1 NIL fabric; perhaps 2% over this 40 cm interval 51544 184.76 186.29 1.53 0.005 0.005 0.1 NIL -outside of this sheared section this is predominantly and amphibloite 51545 186.29 187.80 1.51 0.013 0.005 0.2 NIL as described previously in this hole, this section for the most part 51546 187.80 189.30 1.50 0.008 0.007 0.1 NIL except proximal to contacts (within 1 to 1.5 meters or so) is more 51547 189.30 190.00 0.70 0.015 0.006 0.2 NIL massive in appearance with some minor handing at 45 deg to CA. 51548 190.00 190.75 0.75 0.017 0.010 0.1 NIL -compositionally this unit much the same as other amphibolite units described in this hole; as per previous descriptions once again this section of amphibolite unit is made up of darker grey black malic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite. biotite. and some quartz and plagioclase. lighter sections mainly quartz. plagioclase. biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 5:95, generally lighter bands med gr. but coarser than darker bands -some red subhedral garnets noted particularily in last I to 2 meters above luwer contact -this unit contains some minor medium grained felsic dykes that are mainly quartz and plagioclase feldspar from I 84AO to 184.77 and 185.2 to to 185.6, slip associated with lower contact of 2nd dyke, slip at 20 deg. to CA.; competent unit with a few fractures at 80 deg. to CA. -rare quartz within this section.<2% in occasional stinger parallel to banding -estimate of about 0.5% sulphide. pyrite and speck or two of chalcopyrite

---

DRILl, LOG SC-04-06 DRILL LOG PAGE 12 From To Rock Rock Type Description Samp. From To Samp. CII % Zn% glt Au

.:-gltAg

m. m. Type m. m. m. Amphibolite -no magnetic response in this unit Continued -no HCL reaction

-sharp lower contact at 45 deg. to CA 190.75 191.80 Massive -mainly massive pyrrhotite (95%) with 3% chalcopyrite. also some 5]549 190.75 191.80 1.05 0.81 0.025 0.08 1.0

Sulphide minor quartz and some garnets within this interval. conductive -lower contact sharp at 65 deg. to CA

191.80 201.60 Garnet @ 191.80 to 194.20 51550 190.80 191.30 0.50 0.79 0.024 0.G3 1.0 Amphibolite - mainly grey black mafic garnet amphibolite unit with little or no 51551 191.30 193.75 1.45 0.Q28 0.012 NIL 0.2

lighter colored material, mineralogy for this unit as described 51552 193.75 194.20 0.45 0.61 0.014 NIL 0.9 previously. hornblende. chlorite, biotite mica and some plagioclase 51553 194.20 195.35 1.15 0.71 0.Q25 0.12 1.0 and quartz, some red garnets particularly proximal to upper contact 51554 195.35 195.70 0.35 0.75 0.024 0.32 1.1 -first 50 cm below upper contact contains significant garnets and 51555 195.70 196.95 1.25 0.463 0.014 NIL 0.7 well mineralized with chalcopyrite; 3% chalcopyrite 51556 196.95 198.05 1.10 0.345 0.014 NIL 0.4 - below richer interval to dyke below there is about 2% sulphide 51557 198.05 198.95 0.90 0.Q45 0.013 NIL 0.2 max; mainly disseminated sulphides; estimate max of Y2% 51558 198.95 200.00 1.05 0.096 0.010 0.09 0.3 chalcopyrite and balance pyrite and pyrrhotite 51559 standard #51p 0.73 0.006 0.47 2.6 -this section is predominantly massive in appearance 51560 blank 0.002 0.005 NIL 0.1 -note at 193.75 to 194.20 (lower contact) there is a greenish felsic 51561 200.00 200.65 0.65 0.273 0.011 0.05 0.3 dyke with a drusy appearance. (altered) diorite ?, similar to that 51562 200.65 201.60 0.95 0.042 0.009 NIL 0.2 found at 108.85 to 109.55 up in the hole with another sulphide zone -this dyke also contains sulphides; 1-1.5% chalcopyrite and similar amount of pyrrhotite, lower dyke contact 45 deg. to CA -this unit is magnetitic in certain spots where there is pyrrhotite but overall it is not really magnetic -unit is relatively competent with a few fractures generally at 80 deg. to CA. -no HC) reaction in unit -a couple of minor quartz stringers noted <1/2% of unit

@194.20 to 20).5 -this is still garnet amphibolite but within this section for approximately 80% of unit the unit is almost mono mineralic; i.e. principally red garnet -for the approximately the first 1.5 meters from approx. )94.2 to \95.7 there are numerous clots. blebs. and a few cm. of massive pyrrhotite

DRILL LOG SC-04-06 DRILL LOG PAGE 13 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gii"Ag

m. m. Type m. m. m. Garnet -the estimated sulphide content in this section is 15%; with 10%

c,_,

Amphibolite pyrrhotite, 2% pyrite and 3 % chalcopyrite Continued -below this from 195.7 to 200.65 sulphide content is about 7% and

this is about 5% pyrrhotite, 1.5% chalcopyrite and 0.5% pyrite. this mainly disseminated and occasional stringer and bleb of sulphide -once again this section is a fairly competent interval with a few fractures at 70 deg. to CA and a couple of slips at 20 deg. to CA -rare quartz stringer noted in this interval -tbis unit is magnetic where there is pyrrhotite -because of this section being principally garnet it is generally hard to scratch with knife and similarly no HCL reaction -lower contact is gradational as garnets gradually become less and less.

-"

201.60 207.25 Amphibolite -this unit is much like other amphiblolites described in this hole, 51563 201.60 203.05 1.45 0.009 0.005 NIL 0.1 however it is dominated by the more mafic dark grey material and 51564 203.05 204.58 1.53 0.009 0.005 NIL 0.1 has very little lighter more felsic material; there is also limited 51565 204.58 206.10 l.52 0.008 0.005 NIL 0.1 banding, still medimum to finer grained unit 51566 206.10 207. 25 1.15 0.008 0.005 NIL 0.1 -once again the principal mineralogy is hornblende, chlorite, biotite, some plagioclase and some quartz and a rare red garnet generally close to contacts -where minimal banding is present it is generally oriented 80 to 85 deg. to CA. -some very minor quartz stingers noted; likcly < 1/270 of unit at about 80-85 deg. to CA as well -once again a very competent unit; very minimal fractures; were present they are also at about 80-85 deg. to CA. -occassional fracture at about 45 deg. to CA as well -occassional moderate response to magnet, possible magnetite -very weak to non-existant HCL response -fairly easily scratched with knife, chloritie -minimal to trace sulphide -gra~dational lower contact

DRILL LOG SC-04-06 DRILL LOG PAGE 14 g/tA:g From To Rock Rock Type Description Samp. From To Samp. Cu% Zn%

...

g/tAu m. m. ... ~e m. m. m.

207.25 215.5 Garnet -this section of garnet amphibolite is very similar in composition 51567 207.25 207.75 0.50 0.023 0.006 NIL 0.1 Amphibolite previously described units with the exception that there are red 51568 207.75 208.10 0.35 0.60 0.008 0.04 0.9

garnets within this section; estimate 10% plus red garnets 51569 208.10 209.15 1.05 0.037 0.004 NIL 0.2 -section of garnet amphibolite gneiss once again comprised of 51570 209.15 210.68 1.53 0.074 0.005 NIL 0.3 darker grey black mafic sections and lighter more felsic sections that 51571 210.68 212.20 1.52 0.009 0.005 NIL 0.1 are light grey to off white in color. 51572 212.20 213.73 1.53 0.009 0.004 NIL 0.1 -darker more mafic sections made up of hornblende. chlorite, biotite. 51573 213.73 215.24 1.51 0.004 0.004 NIL 0.1 and some quartz and plagioclase. lighter sections mainly quartz. 51574 215.24 215.74 0.50 0.007 0.003 0.02 0.1 plagioclase, biotite and some minor mafic minerals. both light and darker sections contain a significant number of red colored granets -proportion of lighter to darker sections within this interval roughly 10:90. generally lighter bands med gr. but coarser than darker bands -fairly sparse sulphides in this unit overall I % mainly pyrrhotite and some minor chalcopyrite; minor section with about 25-30% garnets and 10-15% sulphides mainly pyrrhotite and minor chalcopyrite from 207.75 to 208.1 -banding within this unit generally a few mm. to a few cm. where present but not very pronounced. orientation varies from 45-50 deg. to CA to almost 85 deg. to CA. -occasional quartz stinger noted generally parallel to banding -also rare diorite dyke up to 30-40 cm. long -very competent unit. a few fractures at 70 deg. to CA and rare minor slip at 30 deg. to CA -outside of sections with pyrrhotite mineraliLalion lhis unit is basically non-mangnetic -moderately hard unit but can be scratched with knife more difficult where lots of garnet. -no response to HCL -lower contact gradational

215.5 218.29 Amphibolite -this unit pretty much as described from 201.6 to 207.25 -some banding within this unit but not really pronounced and where present a few mm. to a cm. or two, and generally at 85 deg. to CA. -competent unit with rare fracture or two and occasional slip at 10-15 deg. to CA. -rare to trace sulphide -rare .. garnet minor

DRILL LOG SC·04·06 DRILL LOG PAGE 15 --From To Samp. From To

---= .. Cu% Zn% gltAu

. .. -Rock Rock Type Description Samp. glt Ag

m. m. Type m. m. m. I--

Amphibolite -no HCL reaction .. - .. -

Continued -unit is non magnetic -unit is moderately hard but can be scratched with knife -occassional quartz stringer minor generally at 85 deg. to CA -rare minor diorite dyke 10-15 cm. long

E.O.H. 218.29 Core stored at Pelangio Field Office in Connaught Ontario.




Survey Data:


0 2.9 2.9 21.35

21.35 23 23 36.2

36.2 37.52 37.52 70.3 70.3 73.4 73.4 85.1 85.1 99.05 99.05 108.25 108.25 114.33 114.33 123.3 123.3 140.45 140.45 142.35 142.35 151

151 158.7 158.7 164.8 164.8 167.36 167.36 180.41 180.41 180.93 180.93 203.55 203.55 212.24 212.24 213.79 213.79 218

218 228.35

EOH: 228.35 meters

Rocktype Cas AGN

DI AGN QV

AGN AGN/FZ

AGN GAGN

FI AGN

GAGN AM FI

AGN GAGN AGN

AM/FZ AGN SMS AGN

GAGN FI

AM GAGN

November 7,2004 November 9, 2004 J. Kevin Filo, P.Geo. November 30, 2004 to December 3, 2004

Collar: 216 North 358East UTM: 5008773 North 318744 East Azimuth: 290 Degrees Collar: -58 deg.

163m: Az:296 Dip:-56 214m: Az:303 Dip:-57


DRILL LOG SC-04-07 DRILL LOG PAGE 1 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAlI gllAg

m. m. Type m. m. m. 0.00 2.90 Case 2.90 21.35 Amphibolite this unit is an amphibolite with darker grey black mafic sections 51575 2.90 3.95 1.05 0.007 0.004 0.01 0.1 Gneiss and lighter more felsic sections that are light grey to off white in 51576 3.95 4.33 0.38 0.008 0.001 0.01 0.1

color. 51577 4.33 4.88 0.55 0.006 0.003 0.01 0.1 -darker more mafic sections made up of hornblende, chlorite, biotite, 51578 4.88 5.70 0.82 0.002 0.004 NIL 0.1 and some quartz and plagioclase, lighter sections mainly quartz, 51579 standard #5Op 0.67 0.006 0.72 2.4 plagioclase, biotite and some minor mafic minerals 51580 blank 0.001 0.004 NIL 0.1 -proportion of lighter to darker sections within this interval roughly 51581 5.70 6.75 1.05 0.001 0.003 NIL 0.1 60:40, generally lighter hands med gr. but coarser than darker bands 51582 6.75 7.93 1.18 0.003 0.005 NIL 0.1 -banding in this unit ranges from a lew mm. to a few cm. and is 51583 7.93 8.20 0.27 0.003 0.004 NIL 0.1 fairly distinctive (gneissic texture) handing is orinented 80-90 deg. 51584 8.20 9.00 0.80 0.002 0.004 NIL 0.1 to CA: schistose like appearance note on hroken section of core; orientation of mica noted -note in some instances banding is at larger intervals up to 50 COl. but this is more less minor; the dominant banding is in the mm. to cm. range, this smaller banding present within the larger up to 50 cm. bands -reasonably competent interval. with some fractures at 80-90 deg. to CA.; also some fractures at 45 deg. to CA and some minor weak slips at 20 deg. to CA.; at 17.05 to 17.07 minor fault with some 51585 20.12 2135 1.23 0.002 0.003 NIL 0.1 gouge and blocky broken ground, and oxidation, upper contact 45 deg. to CA and lower 85 deg. to CA -minor diorite dyke from 3.95 to 433 mainly composed of plagioclase, quartz and some biotite mica from, rare speck of chalcopyrite and speck of pyrrhotite -outside of minralization descrihed in dyke, sulphides basically trace to non existant; exception 5m to 8m. -some quartz seen in this section as patehy sections. some minor vein lets a few crn to a few mID. wide parallel to banding. these patches, stingers and veinlets make up perhaps 2-3% of unit -overall this unit considered hard and difficult to scratch with knite because of more quartz rich portions (lighter colored bands) -no reaction to magnet in this unit with exception of where there is minor pyrrhotite i.e 501 to 8m. -no HCL reaction in this unit ... ~ ... L.. ......

..... - DRILL LOG SC-04-07 DRILL LOG PAGE 2 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg

m. m. Type m. m. m. 21.35 23.00 Diorite -upper contact of this unit sharp at 25 deg. to CA 51586 21.35 21.98 0.63 0.007 0.001 NIL 0.1

-this unit looks like the typical diorite encountered in other holes and 51587 21.98 22.50 0.52 0.004 0.002 0.01 0.1 in the minor dyke described within unit above except it is coarser 51588 22.50 23.00 0.50 0.008 0.001 NIL 0.1 grained almost pegmatitic -compositionally. plagioclase quartz and some very minor mafic minerals, also some yellowish mica (sericite? very minor) -rare speck of chalcopyrite and pyrrhotite; beyond 21.95 to 23.5 large raft of amphibolite within dyke? and/or two dykes. ~Iower contact at 23.00 sham at 10 deg. to CA

23.00 36.20 Amphibolite -as per description above from 2.90 to 21.35 51589 23.00 23.40 0.40 0.002 0.001 0.01 0.1 Gneiss -proportion of lighter to darker sections within this interval roughly

50:50. generally lighter bands med gr. but coarser than darker bands -banding within this interval generally in the mm. to cm. range. where present larger bands at 10-30 cm range havc mm. and cm. bands within; banding generally 80 deg. to CA -some quartz stingers and veinlets generally a few mm. to a couple of cm. once again note and parallel to banding. overall 2'1"0 -overall this unit pretty competent in appearance; fractures which are 51590 35.37 36.20 0.83 0.011 0.004 NIL 0.1 few in number 80 deg to CA; once again some very minor slips noted at about 25 deg. to CA. -sulphide content within this unit trace at best -unit is moderate to hard; can be scratched with knife but with difficulty particularily more lighter quartz rich sections are harder -unit has rare localized response to magnet (magnetite) -no HCL rcsponse to extremely weak response -lower contact with vein sharD at 30 deg. to CA.

36.20 37.52 Quartz Vein -mainly quartz. some smoky black grey portions but generally white 51591 36.20 37.52 1.32 0.021 0.001 NIL 0.2 and associated with some K-spar rich sections -splashes of pyrite noted with vein. overall pyrite contcnt 2% max. -this vein similar to that found in hole SC-04-06 with smoky black quartz. but no chalcopyrite in this instance -sham lower contact at 85 deg. to CA.

DRILL LOG SC-04-07 DRILL LOG PAGE 3 _.-

From To Rock Rock Type Description Samp. From To Samp. Cu % Zn% gftAu gftAg m. m. Type m. m. m.

37.52 70.30 Amphibolite @ 37.52 to 59.76 51592 37.52 38.41 0.89 0.008 0.004 NIL 0.1 Gneiss garnet amphibolite gneiss with darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite. biotite, and some quartz and plagioclase, lighter sections mainly quartz. plagioclase, biotite and some minor mafic minerals: occasional rare red garnet noted in this unit, particularly in last few meters of this interval -proportion of lighter to darker sections within this interval roughly 45:55, generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. and is fairly distinctive (gneissic texture) banding is orinented 70-80 deg. to CA; schistose like appearance note on broken section of core; orientation of mica noted -larger bands on a gross scale evident once again but mm. to cm bands dominant and present with gross scale bands (gneiss texture) -few minor quartz veins in this interval again and generally less than 2% of interval; these are generally a em or so max and generally conform to banding orientation -a few minor felsic dykes also noted; these are generally 10-15 cm. max and few in number; they are mainly plagioclase and quartz compositionally -once again a pretty competent unit; two fracture sets noted again one at 70-80 deg. to CA or paraiie] to banding and occasional fracture at 40-45 deg. to CA; rare minor slips at 20 deg. to CA -very rare to trace pyrite (sulphide) noted -very rare response to magnet -still hard unit to moderately hard unit. lighter quartz rich sections still the hardest to scratch -overall minor response to HCL, rare occasional strong response

@ 59.76 to 70.30 -as per description above, still amphibolite gneiss, banding present in 10' sol' cm but within these gross scale banded sections there are bands that are within the mm. to cm range.

DRILL LOG SC·04-07 DRILL LOG PAGE 4 From To Rock Rock Type Description Samp. From To Samp. Cli % Zn% g/tAu g/tAg

m. m. Type m. m. m. Amphibolite -once again this section has lighter and darker hands as described 51593 6S.9 69.69 0.79 0.004 0.004 0.03 0.1 Gneiss previously in interval above; proportion in this interval about 50:50 Continued -at about 61.3 meters core becomes fairly broken and blocky. minor

fault with gouge at 61.2 meters fault at 45 deg. to CA., pink felsic dyke in fault from 61.2 to 62.8, dyke is medium grained and comprised of K-spar, palgioclase and quartz -fractures in this particular interval at 70 deg. to CA.; minor slips at 45 deg. to CA and minor slips at 20-25 deg. to CA -banding in this interval generally oriented at 70 deg. to CA for most part -very rarely some minor red garnets have been noted -note from 66.4 to 67.2 some small mafic dykes a em or two wide running subparallel to CA; fine grained with some hiotite, possibly a lamprophyre (this dyke material reacts to HCLl -this section has trace su lphides at best -unit is pretty hard due to amount of quartz rich light colored sections and hard to scratch with knife, darker more chloritic rich sections of unit obviously easier to scratch -no real response to magnet -this section has a very weak to to non-existant reSDonse to HCL

70.30 73.40 Amphibolite -this is a blocky broken section of core with numerous slips and 51594 69.69 70.30 0.61 O.DlS 0.004 0.01 0.3 Fault Zone fracutures and locally some gouge 51595 70.30 71.13 0.83 0.006 0.006 NIL 0.1

-the rock within the fault is amphiblolite as described previously in 51596 71.13 71.95 0.82 0.007 0.006 0.06 0.1 this hole; it is moderately to strongly hemaiiie aliered. 51597 71.95 72.20 0.25 0.027 0.004 NIL 0.3 -slips with fault at 10-15 deg. to CA 51598 72.20 72.40 0.20 0.012 0.009 NIL 0.2 -minor quartz vein with some pyrite (2%) from 71.95 to 72.25 m. -outside of mineral in vein basically no mineralization -fault zone is non-magnetic -fault zone is soft and easily scratched with knife -some HC! reaction, generally associated with a few calcite stingers -UDDer contact 40 deg. to CA and lower contact 45 deg. to CA.


m. m. Type m. m. m. 73.40 85.10 Amphibolite -this unit is an amphibolite with darker grey black mafic sections and 51599 72.40 72.90 0.50 0.001 0.006 NIL 0.1 Gneiss lighter more felsic sections that arc light grey to off white in color.

-darker more mafic sections made up of hornblende. chlorite, biotite. and some quartz and plagioclase, lighter sections mainly quartz, plagioclase. biotite and some minor matic minerals; occasional rare red garnet noted in this unit, sporadically throughout unit: increase in garnets towards lower contact -proportion of lighter to darker sections within this interval roughly 45:55; generally lighter bands med gr. but coarser than darker bands -once again banding on a I D's of cm scale but also significant banding on a mm to cm scale within these -fairly consistent banding in the 75-85 deg range within this unit -some minor quartz stingers and veinlets from a few mm. to a cm or two in width, occasion rare veinlet parallel to CA for 10-20 cm. such as at 82.7 to 83.00; quartz content from veinlets <2%; quartz generally parallel to banding. -competetent unit after fault zone with rare fracture or slip -some minor local disseminated pyrrhotite and pyrite, sulphide content maximum of 1% -no response to magnet -unit contains some minor small dykes of diorite \0 cm. long and occasionally these have some sulphides (minor) -weak to non-existent BCL reaction, and gradational lower contact

85.10 99.05 Ganet garnet amphibolite compositionally with darker grey black mafic 51600 90.24 91.77 1.53 0.005 0.005 NIL 0.1 Amphibolite sections and lighter more felsic sections that are light grey to off 51601 91.77 93.30 1.53 0.006 0.005 NIL 0.1 Gneiss white in color. 51602 93.30 94.82 1.52 0.006 0.005 NIL 0.1

-darker more mat1c sections made up of hornblende. chlorite, biotite, 51603 94.82 96.34 \.52 0.009 0.005 NIL 0.1 and some quartz and plagioclase, lighter sections mainly quartz. 51604 96.34 97.34 1.00 0.007 0.005 NIL 0.1 plagioclase, biotite and some minor matic minerals; substantial 51605 97.34 98.34 1.00 0.008 0.004 0.02 0.1 increase in red 0.5 cm or less anhedral garnets present in this section 51606 98.34 99.05 0.71 0.006 0.008 NIL 0.1 (10% plus garnets) -proportion of lighter to darker sections within this interval roughly 10:90, darker sections or more matic sections dominant - generally lighter bands med gr. but coarscr than darker bands -banding in this unit ranges from a few mm. to a few cm. and is fairly distinctive (gneissic texture) banding is orinented 80-85 deg. to CA; schistose like appearance note on broken section of core; orientation of mica noted

.. ~

.. -~.

DRILL LOG SC-04-07 DRILL LOG PAGE 6 From To Rock Rock Type Description Samp. From To Samp. Cu % Zn% gltAu gltAg

m. m. Type m. m. m. Garnet -some quartz present in this interval as well, mainly a few mm. to a 51607 99.05 99.39 0.34 0.004 0.004 0.02 0.1 Amphibolite cm. or so and generally parallel to banding which is at 80-85 deg. for Gneiss the most part. 2-3% quartz within unit maximum Continued

-occassional minor felsic dykes 10 cm or so that look to be diorite in composition and have undergone some strain, almost boudin like textures within them occasionally -some minor pyrrhotite locally. overall trace to non existent -fairly competent interval with very few fractures, fractures parallel banding where present -weak to non existant HCL reaction -still moderately hard unit that can be scratched with knife -no response from magnet -sharp lower contact at 40 deg. to CA.

99.05 108.25 Felsic Dyke -this unit initially is composed of mainly coarse grained pegamtitic 51608 102.44 102.94 0.50 0.00 I 0.002 NIL 0.1 plagioclase. some K-spar. quartz and minor mafic minerals 51609 standard #50p 0.67 0.006 0.75 2.3 -beyond 103 to lower contact more of a dyke swarm as fair amount 51610 blank 0.00 1 0.003 0.D3 0.1 of inclusions of amphibolite within the dyke 51611 102.94 104.00 1.06 0.12 0.010 0.02 0.1 -beyond 104 meters dyke more of a swarm, and feldspars within 51612 104.00 105.00 1.00 0.012 0.012 0.D3 0.1 dyke seem to be altered to greenish color and some sulphides, mainly 51613 105.00 105.49 0.49 0.066 0.022 NIL 0.4 pyrite, pyrrhotite and minor chalcopyrite associated with dyke. 51614 105.49 106.49 1.00 0.051 0.024 NIL 0.4 within dyke swarm sulphide content I % max overall and locally 3- 51615 106.49 106.97 0.48 0.011 0.010 NIL 0.1 4%. 51616 106.97 107.80 0.83 0.009 0.039 NIL 0.1 -amphibolite within dyke typical of amphibolite in this hole. 51617 107.80 108.25 0.45 0.006 0.006 NIL 0.1 -last 40 cm or so of this unit, much more K spar in dyke and lower 51618 108.25 108.55 0.30 0.018 0.026 NIL 0.1 contact at 45 deg. to CA.

108.25 114.33 Amphibolite -garnet amphibolite gneiss with darker grey black mafic sections and Gneiss lighter more felsic sections that are light grey to off white in color.

-darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals; occasional rare red garnet noted in this unit, sporadically throughout unit; increase in garnets towards lower contact -banding within this section more on the cm 10 mm. scale and lighter material si[nificantly less lighter to darker portion 80:20

DRILL LOG SC·04·07 DRILL LOG PAGE 7 ""-

'From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg 01. m. Type m. m. m.

Amphibolite -unit is medium grained limited lighter sections medium grained but Gneiss slightly coarser than darker mafic sections. Continued -banding within this unit at about SO deg. to CA

-some pretty minor quartz noted in this unit <1 %. generally a stringer or veinlet parallel to banding, small veinlet noted at 1OS.S8 to 10S.98 -a few small felsic dykes noted within this interval, rich in Kspar, plagioclase and quartz, these are coarse to pegamtitic such as at 109.49 to 109.67,109.94 to 109.35, and 110.75 to 110.95 and 111.07 to 111.23 and also at 115.79 to 115.89 and 114.15 to 114.30 -reasonably competent unit with a few fractures at 45 deg. to CA and at 80 deg. to CA, possible minor slip 111.07 at 10-15 deg. to CA associated with felsic dyke -trace to non existant sulphides -no reaction to magnet -no HCL reaction -unit moderately hard and can be scratched with knife -gradational lower contact

114.33 123.30 Garnet - garnet amphibolite gneiss compositionally with darker grey black Amphibolite malic sections and lighter more felsic sections that are light grey to Gneiss off white in color.

-darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals; substantial increase in red 0.5 cm or less anhcdral garnets present in this section (10% plus garnets) -proportion of lighter to darker sections within this interval roughly 20:80. darker sections or more mafic sections dominant - generally lighter bands med gr. but coarser than darker bands -banding generally 70-80 degrees to CA -competent interval with some fractures at 70-80 deg. to CA; few minor slips ranging from 5-15 deg. to CA. -minor sulphides noted trace to V2% overall -a few minor quartz stingers noted <I % generally parallel to banding -moderately hard unit but can be scratched knife -non existent to weak HCL reaction -gradational lower contact

DRILL LOG SC·04·07 DRILL LOG PAGE 8 From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% gftAu gftAg

m. m. lJ'pe m. m. m. _ .. 123.30 140.45 Amphibolite -this section principally amphiblolite with some banding. generally

all medium to fine grained grey black unit comprised of hornblende. chlorite, biotite, and some plagioclase and quartz -few minor bands of lighter grey material, (plagioclase, quartz and biotite) approx. 5% of unit max. weak to moderate banding within darker sections but no change in color -banding where present is oriented at about 80 deg. to CA. -very competent looking unit with a few fractures generally parallel to banding. occasional minor slip at 15 to 20 deg. to CA and minor fault at 135.2 to 135.40 associated with blocky broken core. -some minor quartz in this unit generally at 70-80 deg. to CA. perhaps 3% of unit -from 131.4 to lower contact there is a dyke swarm (numerous small dykes 10 to 50 cm. long associated with quartz on occasion): compositionally the dykes are a coarse to almost pegamtitic diorite comprised of plagioclase quartz and some biotitie mica and possibly some other very minor mafic minerals. they occasionally have a speck or two of sulphides and a garnet or two on occasssion -these dykes represent 30% of this last section -overall this unit contains minimal sulphides trace to Y2{i'o -still moderately hard unit that can be scratched with knife -no response to magnet -no response to HCL -sharp lower contact at 80 deg. CA

140.45 142.35 Felsic Dyke -coarse grained to pegmatitic unit made primarily of plagioclase and K-spar and quartz and some mica mainly biotite and muscovite -a few fractures at 70 deg. to CA; also rare fracture at 15 deg. to CA -no sulphides noted -lower contact along slip at 45 deg. to CA.

142.35 151.00 Amphibolite - amphibolite gneiss with darker grey black mafic sections & lighter Gneiss more felsic sections that are light grey to off white in color.

-darker more mafic sections made up of hornblende. chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals; occasional rare red garnet noted -banding within this section more on the cm to mm. scale and lighter material s!gnificant~ less lighter to darker portion 20:80


m. m. Type m. m. m. Amphibolite -no real banding on a larger scale in 10's of cm. or greater Gneiss -banding that is present is oriented at 80 deg. to CA Continued -grain size in this unit is medium but darker sections slightly finer

grained -some minor quartz stingers noted in this section. generally parallel to banding; estimated % about 2%. -very competent unit for the most part a few fractures at 70-80 deg. to CA. also occasion fracture and minor slip at 10-15 deg. to CA. one small fault zone associated with blocky broken ground and some felsic intrusive at 148.54 to 149.25. contacts at ahout 15 deg. to CA. and sililarily minor fault at 150 ot to 150.20 -this unit has trace to \/2% sulphide at best -this unit is moderately hard and can be scratched with knife -unit has no response to magnet -weak to non existent response to HC) -gradational lower contact

151.00 158.70 Garnet -this section somewhat different from other garnet amphibloite 51619 154.27 155.79 1.52 0.001 0.009 NfL 0.1 Amphibolite gneiss; unit appears somewhat more silicified and is harder to scratch 51620 155.79 157.34 1.55 0.001 0.005 NfL 0.1 Gneiss generally with knife

-still bands generally on a mm. to cm scale at about 80-85 deg. to CA; bands still comprised of with darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende. chlorite. biotite. and some quartz and plagioclase. lighter sections mainly quartz. plagioclase, biotite and some minor mafic minerals; substantial increase in red 0.5 cm or less anhedral garnets present in this section (10% plus garnets) -proportion of lighter to darker sections within this interval roughly 40:60, darker sections or more mafic sections dominant -generally lighter bands med gr. but coarser than darker bands; difficult to discern bands because of overprint of silicification but bands detinitely present -

DRILL LOG SC-04-07 DRILL LOG PAGE 10 From To Rock Rock Type Description Samp. From To Samp. Cu Zn% g/tAu g/tAg

m. m. Type 1Il~_ .. m. m. % Garnet -occassional quartz vein noted in this unit <1/2%, generally <0.5 cm Amphibolite wide and usually paraliel to banding Gneiss -competent unit with a few minor slips at about 5 deg to CA: Continued

occasional rare fracture at about 80-85 deg. to CA. -sulphide content of this unit estimated at trace to 1/2% -weak to non-existent HCL reaction -no response to magnet -lower contact associated with small dyke at 85 deg. to CA.

158.70 IM.80 Amphibolite - amphibolite gneiss with darker grey black mafic sections and Gneiss lighter more felsic sections that are light grey to off white in color.

-darker more mafic sections made up of homblende. chlorite. biotite, and some quartz and plagioclase, lighter sections mainly quartz. plagioclase. biotite and some minor mafic minerals: occasional rare red garnet noted -banding within this section more on the em to mm. scale and lighter material significantly less lighter to darker portion 20:80 -banding in this section at about 80-85 deg. to CA -bands medium grained and darker bands a little finer grained -very minor quartz. occasional stringer of quartz. < I % of unit -very sparse to non-existant sulphides -fairly competent unit becomes hlocky towards fault zone, a few slips at 10-15 deg. to CA .• a few fractures at 70 and 80 deg. to CA. -small diorite dyke at start of unit with rafts of amphibolite within is for the first 35 ern of this unit: outside of this dyke few dykes in this unit -unit is non-magnetic -weak to non existent HCL reaction .moderately hard unit that can be scratched with knife -contact at fault zone sha~p and at 20 de.g. to CA

164.80 167.36 Amphiholite -this section of amphiblolite as per section above from 158.7 to 164.8 Fault Zone except it is broken and blocky with numerous slips and slickenslides

are evident on slip planes -lower contact of fault at about 5 deg. to CA.


m. m. Type m. m. m. 167.36 180.41 Amphibolite - amphibolite gneiss with darker grey black mafic sections and 51621 169.00 169.51 0.51 0.017 0.011 NIL 0.1

Gneiss lighter more felsic sections that are light grey to off white in color. 51622 169.51 170.51 1.00 0.022 0.137 0.Q3 0.8 -darker more mafic sections made up of hornblende, chlorite, biotite. 51623 170.51 171.51 1.00 0.013 0.017 0.02 0.2 and some quartz and plagioclase. lighter sections mainly quartz. 51624 171.51 172.56 1.05 0.065 0.287 NIL 0.3 plagioclase, biotite and some minor mafic minerals; occasional rare 51625 172.56 173.56 1.00 0.008 0.009 NIL 0.1 red garnet noted 51626 173.56 174.56 1.00 0.129 0.184 NIL 0.7 -banding within this section more on the em to mm. scale and lighter 51627 174.56 175.61 1.05 0.045 0.049 0.01 0.3 material significantly less lighter to darker portion 5:95 ratio 51628 175.61 177.13 1.53 0.019 0.019 NIL 0.2 ·basicallya medium to tine grained unit 51629 standard #50p 0.68 0.006 0.74 2.4 -banding in this section at about 80-85 deg. to CA 51630 blank 0.001 0.004 NIL 0.1 . fairly competent unit but a few slips generally sub-parallel toCA 51631 177.13 178.66 1.53 0.009 0.013 0.01 0.1 from J 69.5 to 172 meters; also some minor fractures basically 51632 178.66 179.66 1.00 O.OI 1 0.011 0.01 0.1 parallel to banding 51633 179.66 180.41 0.75 0.18 0.090 0.01 0.1 -some minor quartz in this unit generally parallel to banding and veinlets of a few mm. up to a 1-1.5 cm.; content of quartz < I % -unit contains patchy disseminated. clots and stingers of pyrite. pyrrhotite and chalcopyrite; overall sulphide content of this section 1-2% but locally over 15-20 cm as much as 4%, this section may represent sulphide zone target. but it has poor mineral content with the exception of small sulphide zone below -a few minor diorite dykes ranging from 10-35 cm. and also small K spar rich dyke noted from 171.25 to 171.44 -no response to magnet except very locally where pyrrhotite -weak to non-existent HCL reaction -moderately hard unit that can be scratched with knife -lower contact sharp with sulphide zone below, 75 deg. to CA.

180.41 180.93 Semi -mainly amphibloite as above with about 35-40 plus sulphide. mainly 51634 180.41 180.93 0.52 2.86 0.425 0.01 0.425 Massive semi massive to net textured. Sulphide -3-4% chalcopyrite and the balance of sulphides pyrrhotite

-some dyke like material in unit (10%) diorite green alteration -lower contact sharp along minor slip at 85 deg. to CA.

'---:=--DRILL LOG SC·04·07 DRILL LOG PAGE 12

From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg f--. m. m. Type m. m. m.

180.93 203.55 Amphibolite -amphibolite gneiss with darker grey black mafic sections and lighter Gneiss more felsic sections that are light grey to off white in color.

-darkcr more mafic sections made up of hornblende. chlorite. biotite. and some quartz and plagioclase. lighter sections mainly quartz. plagioclase. biotite and some minor mafic minerals; occasional rare red garnet noted -banding within this section more on the cm to mm. scale for the most part but there are some sections in the 10'5 of cm with band of more lighter and darker material

lighter material significantly less lighter to darker portion] 5:85 ratio -basically a medium to fine grained unit. darker portions slightly finer grained than darker sections -banding in this section at about 80-85 deg. to CA for most part -some minor quartz veining and stingers: generally a few mm. in width and parallel to banding -some small diorite dykes up to 30 cm. in the tirst few meters of this unit -very competent looking unit with few fractures generally at 80 deg. to CA. and a few minor slips at 20 deg. to CA. -unit is non-magnetic except where very minor pyrrhotite noted -sulphide content trace to non-existant -no significant HCL reaction -unit is moderately hard and can be scratched with knife -lower contact gradational

203.55 212.24 Garnet -this unit has distinct banding but mainly grey black matic bands and Amphibolite bands of garnet and little in the way Iigher colored more felsic bands: Gneiss compositionally the unit consists of a lot of red garnets (15-20%)

within a grey black amphibolite made up of hornblende. chlorite, biotite. and some quartz and plagioclase & felsic bands have quartz. plagioclase and biotite for the most part -very competent unit with a few fractures generally parallel to banding which is at about 80-85 deg. to CA. some minor slips at this orientation as well. also some fractures and a few minor slips at 15 deg. toCA. -some minor quartz stingers and vein1ets generally a cm. or less a180-85~d~. to CA.; these make up <I % of unit


m. m. Type m • m. m. .. ~-

Garnet -a few minor diorite dykes noted in this interval generally not larger 51636 203.05 204.05 1.00 0.032 0.009 0.01 0.4 Amphibolite than 20-25 cm. 51637 204.05 205.05 1.00 0.098 0.012 NIL 0.4 Gneiss -from 204.05 to 206.10 almost 60% garnets. some sections almost 51638 205.05 206.10 1.05 0.214 0.012 NIL 0.8 Continued monomineralic. this section contains about 2-3% disseminated 51639 206.10 207.63 1.53 0.011 0.006 NIL 0.1

pyrrhotite and chalcopyrite; chalcopyrite estimated at ahout '12'7'0. also 51640 207.63 209.15 1.52 0.012 0.005 NIL 0.1 some minor pyrite. very minor. 51641 209.15 210.68 1.53 0.012 0.008 NIL 0.2 -outside of the aforementioned mineralized section mineralization is 51642 210.68 212.20 1.52 0.008 0.014 0.01 0.1 generally less than 1/2% total sulphides -garnets become less and less as lower contact is approached -moderately hard unit; where garnet rich difficult to scratch with knife and very hard. -unit is pretty much non-magnetic except locally where there is some local pyrrhotite -little to no HCL reaction -lower contact sharp at 45 deg. to CA and associated with slip on contact

212.24 213.79 Felsic Dyke -this is a coarse grained pegmatitic dyke that is principally composed of K-spar, plagioclase. quartz and some minor mafic minerals and mica -no significant mineralization noted -some minor slips at 10-15 deg to CA .. overall a competent unit -lower contact sham and at 45 deg. to CA. r 2J:179 218,00 Amphibolite -unit below dyke is weakly banded at more massive in appearance -unit still comprised of hornhlende. chlorite. hiotite and some minor plagioclase, and quartz and is med. grained & grey hlack in color -rare red garnet or two noted -where there is some handing it is at about 85 deg. to CA. -some minor slips at 10-15 deg. (0 CA and the occasional fracture at about 85 deg. to CA -occasional minor quartz stinger a few mm to cm. wide max. generally oriented at 85 deg. to CA. quartz <2% of unit -unit is non-magnetic -trace sulphides -unit is relatively easily scratched with knife -occasional 10-15 cm diorite dyke noted within unit -weak to non existant HCL reaction -lower contact gradational


m. ~ f-. Tvpe m. m. m. 218.00

-_." 228.35 Garnet -garnet amphibolite gneiss with darker grey black mafic sections & 51643 218.29 219.82 1.53 0.011 0.004 NIL 0.1

Amphibolite lighter more felsic sections that are light grey to off white in color. 51644 219.82 221.34 1.52 0.008 0.004 0.02 0.1 Gneiss -darker more mafic sections made up of hornblende, chlorite, biotite. 51645 221.34 222.87 1.53 0.007 0.004 0.01 0.1

and some quartz and plagioclase. lighter sections mainly quartz, 51646 222.87 224.39 1.52 0.016 0.006 NIL 0.1 plagioclase. biotite and some minor matic minerals; numerous red 51647 224.39 224.79 0.40 0.012 0.004 NIL 0.1 garnet noted that are generally anhedral 51648 224.79 225.79 1.00 0.004 0.004 NIL 0.1 -banding within this section more on the cm to mm. scale and lighter material significantly less lighter to darker portion 5:95 ratio: occasional lighter bands in the 10-15 cm range and occasional band of garnets for a few cm. -basically a medium to tine grained unit -banding in this section at about 80-85 deg. to CA -some quartz noted within this unit perhaps 1-2% of unit generally parallel to banding, width of stingers and veins is from a few mm. to a couple of cm. -trace to !h% tine sulphide mainly pyrrhotite -unit is non-magnetic except in rare instance where there is some minor pyrite -unit is fairly soft and easily scratched outside sections with a lot of garnets -weak to non existent HCL

E.O.H. 228.35 This core is stored at Pelangio's field oftice in Connaught Ontraio.




Survey Data:


0 6.53 6.53 16.4 16.4 17.71

17.71 46.67 46.67 51

51 84.9 84.9 86.9 86.9 96.34

96.34 133.43 133.43 144.44 144.44 145.49 145.49 151

151 161.08 161.08 162.58 162.58 168.25 168.25 168.77 168.77 197.75 197.75 201.85 201.85 221.34

EOH: 221.34 meters

Rocktype Cas AGN

FI AGN

FI AGN

FI AGN

GAGN AM

SDS AM

AGN FI

AGN SMS

GAGN FI

GAGN

November 9, 2004 November 11 , 2004 J. Kevin Filo, P.Geo. December 3,2004 to December 7,2004

Collar: 162 North 313East UTM: 5008738 North 318683 East Azimuth: 290 Degrees Collar: -70deg.

141 m: Az:289 Dip:-66 221 m: Az:294 Dip:-64


DRILL LOG SC-04·08 DRILL LOG PAGE 1 -.~

From To Rock Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg m. m. Type m. m. m.

0.00 6.53 Case Casing left in hole 6.53 16.40 Amphibolite - this unit is an amphibolite gneiss with darker grey black mafic

Gneiss sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite. biotite, and some quartz and plagioclase. lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals. some minor red garnets noted in this interval as well. -proportion of lighter to darker sections within this interval roughly 60:40. generally lighter bands med gr. but coarser than darker bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10's of cm . banding or fabric present within these larger bands as well -unit is medium grainded and darker sections slightly finer grainded -banding within this unit at about 80-85 deg. to CA. -up to 112.15 m. unit is reasonably competent with a few slips at about 10-15 deg. to CA and fractures parallel to banding; minor blocky broken section at 112.15 associated with oxidized slip at 112.5 -below 112.15 very blocky and broken up with numerous fractures parallel to banding; some minor slips parallel to banding as well, it appears there is an overlap of a fault zone from this unit to the next: upper contact of fault zone not distinct but possibility it starts at about 15.72 where there is a &lip with blocky ground that is oxidized; slip at about 85 deg. to CA. -a few minor rare quartz veins and stingers noted in unit; these are parallel to CA; these represent <I % of unit -unit is non-magnetic -very weak HCL reaction -minimal sulphide content; trace at best -unit is moderately hard and can be scratched with knife, more felsic portions are harder -some bleaching of lower contact and lower contact at 85 deg. to CA and sharp; block and broken core with numerous slips and fractures down to contact

-_." DRILL LOG SC·04-08 DRILL LOG PAGE 2

From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg m. m. m. m. m.

16.40 17.71 Felsic Dyke -this looks like a re-crystalized felsic pegamtitic dyke, almost porpyhritic in appearance because of the larger feldspars; dyke principally made up of plagioclase, quartz and biotite mica and minor malic minerals -this felsic dyke is badly broken up and blocky with numerous slips at about 15 deg. to CA.; tbis dyke in thought to occupy a fault zone which extends form the unit above to the lower contact of the dyke -minimal to trace sulphides in this unit -lower contact alon2 slip at about at 5 dell.. to CA.; slip oxidized

17.71 46.67 Amphibolite @ 17.71 to 41.86 Gneiss -once again this unit is an amphibolite gneiss with darker grey black

mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite. biotite. and some quartz and plagioclase. lighter sections mainly quartz, plagioclase. biotite and some minor mafic minerals. some minor red garnets noted in this interval as well. sometimes consistent over a meter or so. -proportion of lighter to darker sections within this interval roughly 90: 10, thus distinctly different appearance that unit above: dominant mineralogy is plagioclase quartz and biotite mica because of numerous light colored bands -banding in this unit ranges from a few mm. to a few cm. some banding noted in the I O's of cm . banding or fabric present within these larger bands as well unit is mcdium grained and darker seciions slightly liner grained

-banding within this unit at about 80-85 deg. to CA. -this unit is somewhat blocky and broken up below fault zone above to about 22 m with a number of minor slips at about 10 deg. to CA; beyond 22 m vey few minor slips at about 10 deg. to CA where present and some fractures generally parallel to banding -few coarse grained felsic dykes note the biggest being a dyke from 20.65 to 21.48, this dyke is similar to the dyke described within the fault zone in unit above. a few minor small felsic dykes of similar composition noted outside of this main dyke -a few minor quartz stingers noted in this unit, generally parallel to banding; quartz still pretty minor; quartz makes up less than I % of unit

"-

~.

DRILL LOG SC-04-08 DRILL LOG PAGE 3 From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% gltAu g/tAg

m. m. m. m. m. Amphiholite -sulphide content of this unit hasically trace Gneiss -unit for the most part is moderately hard, can he scratched with knife Continued with some difficulty

-no response to magnet -very weak HCL reaction at hest

@ 41.86 to 46,67 -once again this a gneissic amphibolite but within this interval of unit there is a distinct change from the interval above as the darker more matic bands of amphibolite are dominant light to dark bands are now about 20:80 -this interval also contains a few garnets as above -handing also becoming less prominent in this interval but still present and at about 85 deg. to CA -a few rare quartz veins and stingers still which are generally parallel to CA; these once again make up a maximum of I % of unit -this interval is fairly competent with a few fractures generally parallel to CA and occasional slip at about 45 deg. to CA. -this interval has minimal to trace sulphides -small felsic pegmatite dyke mainly comprised of plagioclase, quartz and very minor mica from 44.81 to 45.3, contacts associated or proximal to slips at 45 deg. to CA. -this unit moderately hard; can be scratched with knife, some sections have a mottled appearance and are more chlantic and thus easier to scratch with a knife -weak HCL raction -this interval is also non-magnetic -lower contact ground and blocky

46.67 51.00 Felsic Dyke -this a coarse grained pegmatitic dyker made up primarily of K-spar, some plagioclase, quartz and minor mica and mafic minerals -this unit contains traces of pyrite ( some smoky black quartz in unit) -the unit is extremely broken and blocky with numerous slips at shallow angles to CA (5-15 deg): this section may represent a fault zone that is occupied hy this dyke -lower contact sharp and at 45 deg. to CA.


m. m. m. m. m. 1-----84.90 Amphibolite 51.00 @51 to 75 m.

Gneiss -once again this unit is an amphibolite gneiss with darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more matic sections made up of hornblende. chlorite, biotite, and some quartz and plagioclase. lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals. some minor red garnets noted in this interval as well. but patchy, more garnets just after upper contact -proportion of lighter to darker sections within this interval TOughly 50:50 -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10's of cm . banding or fabric present within these larger bands as well -unit is medium grained and darker sections slightly tiner grained -sections within this interval have a mottled appearance and appear to be more chlorite rich, occasionally a 3-5 cm band of very chlorite altered material noted. -banding within this unit at about 80-85 deg. to CA. -very competent unit a few fractures at 80-85 deg. to CA or parallel to banding -a few minor dykes generally not greater than 20 cm., diTOitic looking dykes that are coarser granind (pegmatitic). possibly recrystalized which number abour 5-6 small dykes generally under 15 cm and small coarse grained pegamtitic K-spar rich dyke also comprised of plagioclase and quartz from 59.7 i to 59.91: upper contact 45 and lower contact 80 deg. to CA. -a few quartz stingers noted in this unit generally less than a cm. wide: these generally follow banding and make up a 1 % of unit maximum -trace to Y2% sulphides; minor local pyrrhoite and speck or two of chalco -unit moderately hard and can be scratched with knife. mottled chloritic rich sections more easily scratched with knife -weak to non existent HCL reaction -unit is non-magnetic

... -_ .... -

DRILL LOG SC-04-08 DRILL LOG PAGE 5 ---

From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% gltAu gltAg m. m. m. m. m.

Amphibolite @ 75 to 84.90 Gneiss -this interval of gneissic amphiblolite pretty much just an extension of Continued inteval described above with a few minor differences

-competent still but a few very minor slips at about 10 to CA. and a few fractures parallel to banding as before. banding still at about 80-85 deg. to CA -few minor diorite dykes similar to that described in interval above; these are generally a couple of cm. long and very few in number -a few minor quartz stringers once again generally parallel to banding; these make up less than I % of this interval -most of this interval has a mottled appearance and interval has a lot of chlorite, some minor sections interspersed with garnets -once again trace of sulphides at best -interval is non-magnetic -interval is moderately hard, mottled chloritic sections easier to scratch -weak to non-existant HCL reaction -lower contact with dyke sharp and at 45 deg. to CA.

84.90 86.90 Felsic Dyke -very coarse grained pegmatitic dyke composed of K-spar. plagioclase, quartz and minor biotite mica -occasional red garnet noted and no significant sulphides -competent unit with a rare slip and or a fracture or two -unit is non-magnetic -lower contact sha!E. and at 60 deg. to CA

---- ---r--86.90 96.34 Amphibolite -once again this unit is an amphibolite gneiss with darker grey black

Gneiss mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals, some minor red garnets closer to lower contact. -proportion of lighter to darker sections within this interval roughly 30;10 -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10's of cm. banding or fabric present within these larger bands as well

DRILL LOG SC·04·08 DRILL LOG PAGE 6 From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% I g/tAu gltAg

m. m. m. m. m. Ampbibolite -this section has a mottled appearance and is more chloritic to about Gneiss 91.00 meters Continued -unit contains minor quartz stingers generally about a em. wide maximum

and parallel to banding; these make up <l % of unit -trace to non-existent sulphides -weak HCL reaction at best -unit can be scratched with knife but of moderate hardness; chloritic mottled sections scratched easier -unit is non-magnetic -lower contact gradational

96.34 133.43 Garnet @ 96.34 to 122.28 Ampbibolite -very similar unit to amphibolite gneiss described above except garnet Gneiss amphibolite gneiss contains signitlcantly more red garnets that are

various sizes of garnets from a few mm. to a cm. or so; these are anhedral to subhedral -once again this unit has darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor malic minerals -proportion of lighter to darker sections within this interval roughly 15:65 -banding in this unit ranges from a few mm. to a few cm. some banding noted in the lO's of em , banding or fabric present within these larger bands as well, banding evident but not as intense as in unit above -unit is medium grained and darker sections slightly finer grained -banding within this unit at about 80-85 deg. to CA. -very competent unit a few fractures at 80-85 deg. to CA or parallel to banding -this section is less chloritic and appears slightly harder when scratched with knife possibly somewhat more siliceous, very local mottled chloritic sections over a Y2 meter or so intermittently -a few small dykes of coarse grained to pegmatitic diorite (appears re-crystalized); these are generally under 20 cm and a minor component of unit -some minor quartz stingers in this unit ranges from a few mm. to a cm. or two, these make up a maximum of 1%


m. m. m. m. m. Garnet -sulphides in this unit trace to non-existant, some pyrrhotite and rare Amphibolite speck of chalcopyrite Gneiss -this unit has patchy sections that are magnetic over perhaps no more than Continned 5% of core

-very weak to non-existant HCL reaction

@ 122,28 to 133.43 -this is still a garnet amphibolite but the lighter or more felsic bands now are dominant and the lighter to darker intervals are now about 80:20 in this interval -still a very garnet rich interval -very competent interval still banded at about 80-85 deg. to CA and a few fractures parallel to this banding, no slips of any significance noted -this interval is fairly hard and appears somewhat silicified, can be scratched with knife but with some difficulty -rare coarse grained dioritic dyke or two that are up to 20 cm or so in length; these make up a minor portion of this interval -note at \30,2 to 130.3 small feldspar rich dyke that exhihits a green alteration of feldspars; this type of dyke typically seen with sulphide zones in previous holes -trace to 1/.0% sulphides; very fine where present, speck of pyrrhotite and rare speck of chalcopyrite ~unit appears non-magnetic -reaction to HCL within this zone very weak at best -lower contact gradational

133.43 144.44 Amphibolite -this unit has very minimal amount of banding and the majority of the unit is comprised of dark grey matic unit that is made up of hornblende, chlorite, biotitc, and some plagioclase and quartz -looks similar to other amphiblolites but banding not a pronounced and distincllack of more felsic sections encountcred previously -very competent unit once again, a few fractures at 80-85 deg. to CA; similar to the occasional banding found within this unit -some small coarse grained to pegmatitic diroritc dykes 10-20 cm long

DRILL LOG SC-04-0S DRILL LOG PAGE S From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% g/tAu g/tAg

m. m. ... -~. m. m. m . noted in this unit. these make up a small portion of the unit 51694 142.07 143.60 1.53 0.008 0.008 NIL 0.1

Amphibolite -medium to finer grained unit 51695 143.60 144.44 0.84 0.040 0.013 NIL 0.1 Continued -predominantly a dark grey unit -once again a few minor quartz stringers in lInit generally 85-90 to deg. to CA; these are very few in number and not really significant -some occasional bands of chlorite noted. distinct lack of mottled appearance. more siliceous and harder unit. can be scratched with difficulty -unit is non-magnetic -no significant response to HCL -traces of sulphide noted< 1/2% overall

144.44 145.49 Sulphide -initially fine disseminated sulphides and some stringers which grades 51696 144.44 145.49 1.05 0.41 0.122 O.oJ 0.7 Zone into some semi massive sulphide and then again back into disseminated

and stinger sulphides towards the end of zone -sulphide concentration over this interval 15%. dominant sulphide is pyrrhotite (10%) some pyrite 3-4% and 1% chalcopyrite maximum -within this unit occasional small felsic intrusive with green alteration of feldspars within it. typical of that found in other sulphide intersections within various holes drilled by Pelangio. portion of this unit conductive -lower contact associated with an 8 cm cherty looking zone with substantial K-spar within it (dyke???); lower contact at about 87 deg. to CA

145.49 151.00 Amphibolite -this unit is as per description of amphibolite unit just above sulphide 51697 145.49 146.65 -

1.16 0.023 0.023 NIL 0.1 zone from 133.43 to 144.40 51698 146.65 148.17 1.52 0.011 0.011 0.05 0.1 -competent unit once again. occasional fracture at about 85 deg. to CA 51699 148.17 149.70 1.53 0.009 0.005 0.04 0.1 and no significant slips or faults 51700 149.70 151.22 1.52 0.029 0.011 NIL 0.1 -one minor dyke (coarse dioritic dyke) under 10 cm. -rare quartz stinger noted -banding pretty rare. where present approaches 85 deg, to CA. tending towards massive appearance -minor sulphides localized perhaps Y1% overall. mainly pyrrhotite and speck or two of chalcopyrite


m. m. m. m. m. -unit is somewhat siliceous and hard. can be scratched with knife with

Amphibolite difficulty Continued -unit is non-magnetic and no HCL reaction

-gradational contact .---151.00 161.08 Amphibolite -once again this unit is an amphibolite gneiss with darker grey black

Gneiss mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase, lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals, rare small red garnets noted -proportion of lighter to darker sections within this interval roughly 55:45 -banding in this unit ranges from a few mm. to a few cm. some banding noted in the I O's of cm , banding or fabric present within these larger bands as well -unit is medium grained and darker sections slightly finer grained -sections within this interval have a mottled appearance and appear to be more chlorite rich, occasionally a 2-3 cm band of very chlorite altered material noted. -banding within this unit at about 80-90 deg. to CA. -very competent unit with a few fractures parallel to banding and no significant slips or faults -minor dyke noted, less than 20 cm long. coarse dioritic intrusive -sulphides trace to non-existent -unit is non-magnetic and HeL reaction is weak to non-existent -unit is of moderate hardness, softer where more chloritic, can be scratched with knife -lower contact with c!l'ke sharp and at 65 deg. to CA.

161.08 162.58 Felsic Dyke -off white colored coarse pegmatitic dyke composed mainly of plagioclase and some quartz and minor biotite mica and occasional garnet -competent unit, no significant sulphides noted -lower contact sharp and at 45 deg. to CA

... __ ...


m. m. m. m. m. 162.58 168,25 Amphibolite -this unit is basically as per thc amphibolite gneiss from I'll to 161.08 51701 166.46 167.46 1.00 0.038 0.016 NIL 0.1 Gneiss -this particular unit is once again very competent with a few fractures 51702 167.46 168.25 0.79 0.032 0,018 NIL 0.2

parallel to banding at 80-85 deg. to CA or parallel to banding within this unit -occasional rare diorite dyke generally less than 10 cm, -few minor quartz stringers generally a few mm. to a cm. max,; these make up less than I % of unit -once again sulphides pretty much trace to non-exsitant -as per unit above mottled appearance and unit moderate hardness and can be scratched with knife, more ch10ritic portions easier to scratch with knife -very weak reaction to HCL -lower contact sharp and at 75-80 deg. to CA.

168.25 168.77 Sulphide -initially from 168.25 to 168.55 mainly red garnet with some minor 51703 168.25 168.77 0.52 0.281 0,019 0.01 0.4 Zone sulphide and grading into semi- massive and conductive sulphide and then abruhtly ending at lower contact which appears to he associated with a small quartz stinger -sulphide content 30% of unit, approximately 28% pyrrhotite and balance pyrite and chalcopyrite -lower contact sharo at 80 deg. to CA.

168.77 197,75 Garnet @168.77to 187.80 51704 168.77 169.51 0,74 0.032 0.Q7 0.06 0.2 Amphibolite -very similar unit to amphibolite gneiss descrihed ahove except garnet Gneiss amphibolite gneiss contains significantly more red garnets that are

various sizes of garnets from a few mm. to a cm. or so; these are anhedral to subhedral, occasional bands of garnet up to a cm. or two -once again this unit has darker grey black mafic sections and lighter more felsic sections that are light grey to off white in color. -darker more mafic sections made up of hornblende, chlorite, biotite, and some quartz and plagioclase. lighter sections mainly quartz, plagioclase, biotite and some minor mafic minerals -proportion of lighter to darker sections within this interval roughly 60:40 -banding in this unit ranges from a few mm. to a few cm. some banding noted in the 10' s of cm , banding or fabric present within these larger bands as well; note at 175.61, changes in banding suggests some folding -unit is medium grained and darker sections slightly finer grained -banding within this unit at about 80-85 deg. to CA. in general -a few minor quartz stingers and veinlets noted, these generally follow the banding and make uo a max. of I % of unit _ ....


f--.. m • ... ~ .. ~ . _rn~ .. m. m • Garnet -at 171.3 to 171.94 coarse grained felsic dyke. upper contact at 45 and Amphibolite lower contact 50 deg. to CA.; some minor dioritic dykes as well. Gneiss generally less than 10 cm. Continued

-very competent unit with some fractures at about 85 deg. to CA .. very rare slip or two noted at 85 deg. to CA. as welL -some sections of darker bands within this unit fairly chloritic whrere there are more mafic hands and can be scratched with knife, obviously softer in more chloritic sections -this interval contains trace sulphide -unit is non -magnetic and weak HCL reaction

@187.80to 197.75 -very similar to interval ahove except felsic section of gneiss becoming even more dominant lighter to darker bands now about 75:25 -also increase in garnets and occasionally 20-30 cm bands of almost pure gamet, similar to what is found proximal to sulphide zones on this property -knots of garnet noted as well, and these seem to have been rotated to some extent within bands -still banding similar to what was described in previous interval for this unit except handing more like 80 deg. to CA. in general -occassional quartz stingers up to a few cm .. these are pretty minor and make up <I % of this interval -some chloritic alteration of more mafic sections noted -this unit is pretty hard and can be scratched with diftlculty due to presence of more quartz rich felsic sections and more garnets -no significant sulphides noted -this interval has no reaction to magnet -weak to non-existent HCL reaction -sh~ lower contact along dyke at 70 deg. to CA.

. .. -197.75 201.85 Felsic Dyke -very coarse grained pegmatitic unit mainly comprised of K-spar;

plagioclase, quartz and some mica -some minor amphiblolite within this unit -no significant mineralization -lower contact at 70 deg. to CA

DRILL LOG SC-04-0S DRILL LOG PAGE 11 From To Rock Type Rock Type Description Samp. From To Samp. Cu% Zn% gltAu g/tA~

m. m. m. m. m. 201.85 22L34 Garnet -this unit is as per garnet amphibolite gneiss from 168.77 to 197.75

Amphibolite -very competent unit, some fractures generally parallel to banding 75-85 Gneiss to CA; no major slips or faults noted

-no significant mineralization -weak to moderate HCL reaction -fairly hard unit; can be scratched with knife with difficulty, some mafic sections contain chlorite and are somewhat softer -some minor quartz stingers a few mm. to a em or so maximum, these make up I % of unit maximum -this section is fairly light in color and light to dark banded sections or felsic to mafic sections are similar in proportion to last portion of unit above or 75:25

E.0.H.221.34

This drill core is stored at Peiangio's field office in Connaught Ontario.

by: j.k. fila, p. geo. october 20, 2005

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