report of physical work on the new kirkland project … · 4.0 geology 3 4.1. regional geology 3...

REPORT OF PHYSICAL WORK ON THE NEW KIRKLAND PROJECT

BAYLY TOWNSHIP, ONTARIO Larder Lake Mining Division, Ontario

NTS 31M13

January 4th, 2012 Prepared By: Jared Shilson

Supervised: Thomas Hart, P.Geo.

i

Table of Contents

1.0 INTRODUCTION 1

2.0 PROPERTY LOCATION, ACCESS, AND DESCRIPTION 1

3.0 PREVIOUS WORK 3

4.0 GEOLOGY 3

4.1. REGIONAL GEOLOGY 3

4.2. LOCAL GEOLOGY 7

4.3 TRENCH GEOLOGY 8

4.3.1 TRENCH STRUCTURE 9

4.4 PROSPECTING 9

5. WORK PROGRAM 10

5.1. PHYSICAL WORK 10

5.2 PROSPECTING 10

5.3 SAMPLING 10

5.4 STATEMENT OF EXPENDITURES 11

6. CONCLUSIONS 12

7. RECOMMENDATIONS 13

8. REFERENCES 14

9. STATEMENT OF THE AUTHORS 15

APPENDIX A: DAILY SUMMARY OF WORK 17

APPENDIX B: TRENCH MAPS AND PROPERTY MAP 20

APPENDIX C: SAMPLES DESCRIPTIONS 29

APPENDIX D: ALS ASSAY CERTIFICATES 34

ii

List of Tables

Table 1: List of claims composing the New Kirkland Property

Table 2: Summary of previous work

Table 4: Statement of expenditures

List of Figures

Figure 1: Location of New Kirkland Project

Figure 2: Regional geology map

Figure 3: Local geology Map

Figure 4: Photo of narrow fracture zone

Appendix A: Daily Summary of Work

Table A1: Daily summary of work

Appendix B: Trench Maps and Property Maps

Figure B1: Property map with trench locations, scale 1:4240.

Figure B2: Detailed sampling and Geology of Trench 1

Figure B3: Detailed sampling and Geology of Trench 2

Figure B4: Detailed sampling and Geology of Trench 3, scale 1:65.





Appendix C: Sample Descriptions

Table C1: Sample Descriptions

Appendix D: ALS Assay Certificates

1

1.0 INTRODUCTION

This report has been prepared by Transition Metals Corp. to provide documentation of a program of

physical work completed on a property located in Bayly Township, Larder Lake Mining District between

August 22th and August 28th, 2011. The company conducted the work to expand on the Bute-Larder gold

occurrence located north of Wendigo Lake. The content of this report is believed by the author to be

current, as of December 1st, 2011.

2.0 PROPERTY LOCATION, ACCESS, AND DESCRIPTION

The New Kirkland property consists of one 1.6 km by 1.6 km claim block north of Wendigo Lake

in mid-central Bayly township at approximately 597670E, 5303930N (Zone 17; NAD 83 ) (Figure

1; Table 1). At the time of the work program, there were no other claims staked in Bayly

Township. Numerous pits and trenches dating pre-1940 are found on the property and have

been exposed to varying degrees by present and past logging operations.

The trenches are located at a point of locally higher elevation with downward slopes to the

west, south and east. The property contains a combination of dry hummocky higher ground and

wet, swampy low ground. Drainage is towards Wendigo Lake, and there are few sources of

water on the property other than small beaver ponds.

The property is accessible via a winter logging road, referred to as the Gogo road by local

cottagers, exiting south from highway 624 approximately 12 km south of Larder Lake. The

logging road is roughly 16 km long from the highway to the trenching locations. During the field

visit in August, the road was driveable by truck for a few kilometres only, after which ATV’s

were required due to poor road conditions. The property can also be accessed by boat via

Wendigo Lake with a short (< 1 km) hike from the lake shore.

2

Figure 1. Location of New Kirkland project (yellow star), claim 4260273 in green.

Table 1: New Kirkland property claim.

Claim No Units Hectares Twp / Area Mining Div. Project Name Claim Status

4260273 16 256 Bayly Larder Lake New Kirkland Active

3

3.0 PREVIOUS WORK

Table 2 presents a summary of previous work conducted on and around the property.

Table 2. Summary of previous work

Date Description of Work

1938 Approximately 240 m of pits and trenches were dug by Bute Larder Gold Mining Syndicate Ltd. The showings were then explored for Bute Larder Gold Mining Syndicate Ltd. by Sylvanite Gold Mines Ltd.

1963 Limited geological mapping was performed by Peerless Canadian Explorations Ltd.

1971 Asarco Exploration Ltd. Conducted ground-based magnetometer and electromagnetic surveys as well as geological mapping on a property optioned to Asarco by Hudson Bay Mines Ltd.

1974-5 Lovell, H.L., Ploeger, F., and de Grijs, Jan mapped Bayly township for the Ontario Geological Survey.

1987 H. Ferderber Geophysics Ltd. Flew a combined airborne geophysical survey and collected magnetic and VLF-electromagnetic data on the property of Premier Explorations Inc.

1989 H. Ferderber Geophysics Ltd. Flew a combined airborne geophysical survey and collected magnetic and VLF-electromagnetic data on the property of Carl Forbes

4.0 GEOLOGY

4.1. Regional Geology

The following description of the Abitibi greenstone belt was summarized by Hart (2011), and was extracted from Ayer et al. (2002, 2005) and Thurston et al. (2008) and on the references found in those papers. The Abitibi greenstone belt is composed of east-trending synclines of mainly volcanic rocks and intervening domes cored by synvolcanic and/or syntectonic plutonic rocks (gabbro-diorite, tonalite, and granite) alternating with east-trending bands of turbiditic wackes (Figure 2). Most of the volcanic and sedimentary rock dip vertically and are generally separated by east-trending faults with variable dips. Some of these faults, such as the Porcupine-Destor fault, display evidence for overprinting deformation events including early thrusting, later strike-slip and extension events. There are two ages of unconformable successor basins, early, widely distributed “Porcupine-style” basins of fine-grained clastic rocks,

4

followed by later “Timiskaming-style” basins of coarser clastic and minor volcanic rocks which are largely proximal to major strike-slip faults (e.g. Porcupine-Destor, Larder-Cadillac). Numerous late-tectonic plutons from syenite and gabbro to granite with lesser dikes of lamprophyre and carbonatite cut the belt.

Metavolcanic and metasedimentary rocks of the Abitibi greenstone belt have been subdivided into a series of assemblages, the Pacaud, Deloro, Stoughton-Roquemaure, Kidd-Munro, Tisdale, and Blake River. The 2723 to 2720 Ma Stoughton-Roquemaure assemblage, characterised by broad regions of tholeiitic basalts, komatiitic basalts, and komatiites with several relatively minor felsic volcanic centers, is located on the east flank of the Round Lake batholith. Calc-alkaline intermediate to felsic volcanic rocks of the 2701 to 2696 Ma upper Blake River assemblage overlie the Stoughton-Roquemaure in the Kirkland Lake area and have been interpreted to underlie the area of the New Kirkland property (Figure 2).

Figure 2: Regional geology of the southern Abitibi greenstone belt (Ayer et al. 2002) with the

property location in orange.

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The plutonic rocks of the Abitibi greenstone belt were subdivided by Ayer et al. (2005) into synvolcanic, syn-tectonic and post-tectonic intrusions. The synvolcanic intrusions were further subdivided in to felsic to intermediate and mafic to ultramafic intrusions. Felsic to intermediate synvolcanic intrusions range in age from about 2745 to 2696 Ma and are coeval with, and geochemically similar to, the volcanic assemblages. These intrusions predate significant compressional strain, are typically foliated tonalite to granodiorite, and are found predominantly within the larger granitic complexes (e.g Round Lake batholith). Mafic to ultramafic bodies intrude the metavolcanic rocks to the north and east of the property (unit 10; Figure 3). These rocks may be part of the suite of mafic to ultramafic synvolcanic intrusions that range from approximately 2740 to 2700 Ma and mainly occur as peridotite to gabbro and diorite sills or lenticular units that cut stratigraphy at a low angle. The Archean rocks are unconformably overlain by Paleoproterozoic rocks of the Huronian Supergroup, which were deposited in a north-trending graben referred to as the Cobalt Embayment overlying the Abitibi greenstone belt (unit 16b; Figure 3). Four formations, the Gowganda, Lorrain, Gordon Lake, and Bar River, were deposited in the Embayment and form the upper most sedimentary cycle of the Huronian Supergroup collectively referred to as the Cobalt Group (Bennett et al. 1991). The Gowganda Formation has been subdivided in to the lower Coleman Member consisting of clast and matrix supported conglomerate, and the upper Firstbrook Member consisting of pebbly wacke, wacke, siltstone, mudstone, and arenite. The Coleman Member conglomerates have been interpreted to have been glacial or alternatively debris flows or turbidity currents. The finer sediments of the Firstbrook Member are interpreted to have been deposited in a deltaic environment. Gabbroic rocks of the Nipissing Intrusive event intrude all older rocks of the Cobalt Embayment forming sills, dykes and undulating sheets up to a few hundred metres thick (Bennett et al. 1991) (Unit 17; Figure 3). A two pyroxene gabbro is the most common lithology in the Nipissing but olivine gabbro, hornblende gabbro, feldspathic pyroxenite, leucogabbro, and granophyric gabbro and granophyres are also present. The 2219 Ma Nipissing gabbro may have originated from a radiating dike swarm related to the 2217-2210 Ma Ungava magmatic event located under the Labrador Trough fed via the 2216 Ma Senneterre dykes that form part of the radiating dike swarm (Ernst 2007). Locally, emplacement of the Nipissing appears to have been controlled by pre-existing structures in the Huronian and Archean basement rocks.

6

Figure 3: Regional geology of the Bayly Township area with the property outlined in red (from Geology of Ontario)

7

Supracrustal units in the Abitibi greenstone belt are dominated by east-striking volcanic and sedimentary assemblages and east-trending Archean deformation zones and folds. Larger batholithic complexes external to the supracrustal rocks (e.g. Round Lake) represent centres of structural domes. The intervening areas define belt-scale synclinoria that deformed during a number of distinct periods. This pattern is interrupted by the trends of Porcupine and Timiskaming assemblage rocks which unconformably overlie the older assemblages. Older syntectonic intrusions (2695–2685 Ma) may be related to the compressive stresses that induced early folding and faulting related to the onset of continental collision between the Abitibi and older sub provinces to the north. Younger syntectonic intrusions (2680–2670 Ma) are coeval with the Timiskaming assemblage and are spatially associated with the Porcupine Destor and Larder Lake Cadillac deformation zones. The late tectonic intrusions (2670–2660 Ma) are possibly synchronous with D4 folding within the Timiskaming assemblage rocks in the Timmins area and represent the final stage in transpressional deformation along the Porcupine Destor deformation zone and may be correlative with the D2 event identified in the Kirkland Lake–Larder Lake area. The regional deformation zones commonly occur at assemblage boundaries and are spatially closely associated with long linear belts representing the sedimentary assemblages (i.e., Porcupine and Timiskaming). It has been proposed that the regional association of the Porcupine Destor and Larder Lake Cadillac deformation zones and major assemblage boundaries are proximal to the locus of early synvolcanic extensional faults.

4.2. Local Geology

The property is underlain to the east by intermediate to felsic metavolcanic rocks interpreted to be part of the calc-alkaline 2701 to 2696 Ma upper Blake River assemblage. The metavolcanic rocks are intruded by a suite of medium- to coarse-grained gabbro and diorite bodies exposed to the north and east of the property (Lovell et al., 1976) (Figure 3). Clastic metasedimentary rocks of the Cobalt Group, Huronian Supergroup, unconformably overlie the older lithologies. A northeast-striking Proterozoic-age diabase dyke intrudes all younger units.

Intermediate to felsic rocks on the property consist of dacitic crystal tuffs, lapilli-tuffs and tuff breccias exposed to the east. The metavolcanic rocks trend to the northeast and are part of the south-eastern limb of a large anticline with an axis that strikes east through Skead Twp. (Lovell and Ploeger 1980).

A different suite of northeast-trending, medium- to coarse-grained gabbros and diorites intrude the metavolcanic rocks (Figure 3). Lovell and Ploeger (1980) mapped two major sills of high MgO tholeiite composition intruding subparallel to the bedding of the metavolcanic rocks.

Uncomformably overlying the older rocks on the west side of the property are argillites and conglomerates of the Coleman Member of the Cobalt Group, Huronian Supergroup (Lovell et al., 1976) (Figure 3). The metasedimentary rocks of the Coleman Member are relatively flat-lying, dipping approximately 20°; however steeper dips of up to 70° have been noted and are

8

interpreted to represent deposition on steep paleo-slopes of the underlying Archean basement rocks (Lovell and Ploeger 1980).

Three sets of northeast-, northwest- and east-northeast-trending faults are found locally. Most of the faults are pre-Huronian. However, some northwest trending faults cause offsets in the Huronian rocks suggesting a younger age or re-activation of pre-existing structures (Lovell and Ploeger, 1980).

4.3 Trench Geology

The main lithology exposed in all of the trenches consisted of intermediate tuff to intermediate lapilli tuff breccia (Appendix B; figures B1 to B8). Clasts in the breccias are intermediate in composition, sub angular, and range from granule to cobble sized within a fine-grain to granular matrix. In all the trenches, except trench 1, the intermediate tuff is cut by a narrow, silicified and carbonatized fracture ranging between 10 and 45 cm thick (Figure 4). The silicification and carbonatization in the trenches is discontinuous and fracture-controlled.

Weakly sheared quartz veinlets and stringers and variable sulphide mineralization occur in both the central fracture and occasionally in the minor fractures. The quartz occurs as lens-shaped veins within the fracture zone up to a few centimetres in thickness, and outside the fracture zone as fracture-fill quartz veinlets that are typically less than 4 mm thick.

Figure 4. North-trending main fracture cutting intermediate metavolcanic rocks

9

Sulphide mineralization within the main fracture is patchy and variable both within the veins

and along the vein contacts. Some patches contain up to 10% disseminated medium- to coarse-

grained chalcopyrite, trace fine-grained malachite and trace fine-grained azurite. In trench 3,

one sample contained up to 5% chalcopyrite, trace malachite, azurite and sphalerite. Trench 4

hosted a vug that contains prismatic coarse-grained quartz up to 0.5 cm long and coarse-

grained chalcopyrite up to 4 mm in diameter.

Sulphide mineralization in the narrow fracture extends no more than 10 cm to either side of the

fracture and the host rock outside of the zone remains unsulphidized with the exception of

minor joint- and fracture-fill quartz veinlets. Mineralization in the competent host rock and un-

sulphidized fractures was not sampled during this project.

4.3.1 Trench Structure

The main fracture zone extends at least 150 m along strike trending between 334° and 354°,

with dips between 80° to vertical. A second fracture was exposed in trench 6 strikes

approximately 080o and dips 81o (Figure B7). This second fracture correlates well with a 7 cm

thick quartz vein exposed in trench 7 that strikes 262o and dips 89o (Figure B8). This second

fracture and quartz vein likely intersects the main fracture but that intersection was not

exposed during this work program. It is also possible that the fracture in trench 6 and the

quartz vein in trench 7 are not related as the trench 6 fracture does not contain a quartz vein.

The character of the structure hosting the quartz vein in trench 7 is also difficult to determine

due to the poor wallrock exposure.

Jointing and fracturing in the trenches is pervasive. Jointing is weakly to moderately variable

and tend to be sub-parallel and sub-perpendicular to the main narrow fracture. In trench 1,

most of the joints and fractures contain less than 4 mm quartz veinlets. However in the other

trenches, quartz veinlets in the joints are not as pervasive.

4.4 Prospecting

Prospecting on the property confirmed the geology mapped by the Ontario Geological Survey

(Lovell and Ploeger 1980). The exception being a single conglomerate outcrop observed at

597557E, 5304270N (Zone 17; NAD 83), which is 50 m to the east of the current eastern

boundary of the Huronian Supergroup.

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5. WORK PROGRAM

The current program undertaken by Transition Metals Corp. focused primarily on stripping,

washing, and mapping of the trenches. The objective of the trenching was to expand on

exposures resulting from pits and trenches from previous work. An initial day of prospecting

was conducted on June 2nd, 2011 to locate the trenches and reconnaissance mapping on the

claim. The main physical work program was conducted from August 22nd until August 28th, 2011

and consisted of trenching and prospecting.

5.1. Physical Work

The stripping was performed by Fred Pritchard of Elk Lake Enterprises A Dahl 753 backhoe was

used to excavate the overburden of seven trench areas covering 563 m2.A high pressure water

pump and hoses were supplied by Elk Lake Enterprises, and washing of the trenches was

performed by Jared Shilson and Michaela Kuuskman. A sump excavated during construction of

the logging road was used as a water supply to wash trench 6, and a second sump was dug in a

swampy area to wash the other six trenches.

The trenches were mapped on a scale of 1: 100 as they were cleaned by either Jared Shilson or

Michaela Kuuskman. The results of the mapping are showing in Figure B2 to B8 in Appendix B.

5.2 Prospecting

On June 2nd, 2011, Greg Collins, Tom Hart, Jared Shilson and Caitlin Beland spent a day

establishing access to the property and prospecting to locate the historical trenching and pitting

reported to be present on the property. A number of samples were collected with the locations

shown in figure 4. On August 22nd, 2011, Michaela Kuuskman and Jared Shilson prospected the

area close to the trenches while searching for a suitable water source for trench washing.

5.3 Sampling

The objective of trench sampling was to determine the nature of mineralization found in the

fractures as well as evaluating mineralization associated with quartz veinlets and stringers that

could be related to the same or similar structures as the fracture zone. A total of 48 grab

samples were collected from the seven trenches by J. Shilson and M. Kuuskman using a

hammer and chisel. Sample descriptions were completed by J. Shilson and M. Kuuskman and

are located in Appendix C, table C1. Sample locations are shown in Appendix B, figures B1 to B8.

11

A total of 6 grab samples were also collected while prospecting during the June 2nd, 2011

property visit to establish access and on August 22nd while searching for a suitable pump water

source for trench washing. Locations of samples obtained while prospecting are shown in figure

B1.

All samples collected on the New Kirkland property were submitted to ALS Chemex for sample

preparation in Sudbury and analyses in Vancouver for gold and a multi-element package. Assay

certificates are found in Appendix D.

5.4 Statement of Expenditures

The total value of work done on the New Kirkland property is summarized in Table 3. A more

specific breakdown of work activities based on a daily log is provided in Appendix A, table A1.

Table 3. Summary of expenditures

Cost Category Amount

Geological Consultant $3,125

Field Geologists $6,000

Trenching $2,760

Samples $2,700

Vehicle Expenses $1,160

ATV Expenses $500

Food and Accommodations $1,085

Report Writing $1,500

Total $18,830

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6. CONCLUSIONS

The main fracture zone exposed in the trenches may be a narrow fault splay related to a west-

northwest-trending fault mapped by Lovell and Ploeger (1980). Gold mineralization is

associated with the quartz veins and sulphide mineralization that could be temporally related

to the faulting event or possibly a later mineralization event.

Assay results returned Au values range from 0.5 g/t to 6.99 g/t (Appendix C, Table C1) (Figures

B2 to B8). Additionally, a grab sample of float interpreted to be from past-trenching of trench 7

assayed up to 46.7 g/t. These assay results demonstrate the presence of gold mineralization

within two fracture zones.

The total width of the north-trending fracture system varies from less than 10 cm to 50 cm over

a strike distance of approximately 150 metres (Figure 3 and B1). Trenching did not expose any

parallel fractures that could extend the width of the main structure, however the trenches did

not expose a large area lateral to the main fracture zone (Figures B2-B8). The width of the

mineralization within the fracture zone has not been tested in detail as the samples collected

during this work program consisted of only grab samples. Channel sampling was not attempted

as in many places along the fracture zone previous trenching have removed a large portion of

the fracture and vein material leaving a narrow, steep sided channel along the fracture zone

that precluded the use of a channel saw. An alteration zone associated with the fracture was

not identified but due to the narrow nature of the trenching, it is difficult to determine if there

may be a subtle broad alteration halo around the fractures.

A fracture roughly perpendicular to the north-trending fracture zone was exposed in Trench 7

and assay results indicate that this second structure also hosts gold mineralization (Figure B8).

The assay results ranged from 0.003g/t to 0.12g/t which are lower than the north-trending

assay values. However, this west-trending structure was exposed in only the one trench and the

lateral continuity and potential for other sub parallel fractures has not been fully evaluated.

13

7. RECOMMENDATIONS

The presence of gold mineralization in the north- and west- trending structures, although

narrow in the 2011 trenches, indicates a potential for additional gold mineralization along strike

in both structures. Staking of additional claims along strike with these fracture zones has been

completed in the fall of 2011 following the receipt of the analytical results.

The trenching completed in 2011 was limited to small area to determine the potential for gold

mineralization, and did not fully test the potential for adjacent parallel or sub-parallel

structures. Additional trenching would be helpful in determining the potential for additional

structures in the immediate area of the 2011 trenches.

There is also the potential for additional gold mineralization along strike with the currently

identified mineralization, but outcropping hosting gold mineralization could be some distance

from the current trenches. The next phase of exploration should involve a program of

prospecting and mapping and grab sampling in an attempt to locate the strike extensions of

the know fracture zones as well as to identify fracture zones similar to the main fracture zone

mapped in the trenches. The extent of the west-trending 7 cm thick quartz vein in trench 7

remains unknown however the possibility that this fracture could be related to an adit located

off the claim but along strike to the east requires further investigation. Reconnaissance

mapping of the newly acquired claim should be completed as part of this program to

investigate the character of the gold occurrences in the areas to the north and how these

occurrences may relate to the gold mineralization exposed during this work program.

A geophysical survey may prove useful in locating similar structures and confirming the

continuity of the approximate 345 degree strike to the structure that runs through the trenched

area. The association of the gold mineralization with fracture zones containing only minor

sulphide mineralization suggests that VLF-EM or induced polarization survey could be useful in

tracing the structures. The perpendicular relationship between the two structures could

require any survey to be completing in two overlapping orientations.

14

8. REFERENCES Lovell, H.L., Ploeger, F., and de Grijs, Jan.1976:Bayly Township, District of Timiskaming; Ontario Div.

Mines, Prelim. Map P.1198,Geol. Ser., scale 1:15,840 or 1 inch to ¼ mile. Geology, 1974, 1975. Lovell, H.L., and Ploeger, F.R. 1980:Geology of Bayly Township, District of Timiskaming; Ontario

Geological Survey Miscellaneous Paper 88, 24p. Accompanied by Map P.1198 (revised), Scale 1:15 840 (1 inch to ¼ mile).

Ayer, J.A., Amelin, Y., Corfu, F., Kamo, S., Ketchum, J., Kwok, K., Trowell, N. 2002. Evolution of the southern Abitibi greenstone belt based on U–Pb geochronology: autochthonous volcanic construction followed by plutonism, regional deformation and sedimentation; Precambrian Research, 115 p. 63–95

Hart, T.R. 2011. 43-101F1 Technical Report on the Haultain Property Haultain and Nicol Townships –

Gowganda, Ontario (NTS 41P10); prepared for Transition Metals Corporation; dated January

13th, 2011

Thurston, P.C., Ayer, J.A., Goutier, J., and Hamilton, M.A. 2008. Depositional Gaps in Abitibi Greenstone Belt Stratigraphy: A Key to Exploration for Syngenetic Mineralization; Economic Geology, 103, p. 1097–1134.

Campbell, R.A. 1989. Report on the Combined Airborne Geophysical Survey on the Property of Carl

Forbes, Bayly Township, Larder Lake Mining Division, Ontario., R.A. Campbell, B.Sc., Geologist, H.

Ferderber Geophysics Ltd.

Campbell, R.A. 1988. Report on the Combined Airborne Geophysical Survey on the Property of Premier

Explorations Inc., Bayly Township, Larder Lake Mining Division, Ontario., R.A. Campbell,

Geologist, H. Ferderber Geophysics Ltd.

Nicholls, E.B., 1971. Geophysical Report on the Hudson Bay Mines Limited Claim Group, Bayly Township,

District of Temiskaming., E.B. Nicholls, P.eng, Geophysicist, Asarco Exploration Company of

Canada Ltd.

Brown, R.L., 1971. Geological Report on the Hudson Bay Mines Limited Claim Group, Bayly Township,

District of Temiskaming., R.L. Brown, P.eng, Asarco Exploration Company of Canada Ltd.

----~ ----:-------

9. STATEMENT OF THE AUTHORS

L Jared ShiJson, certif\ that:

1) I am an employee of Transition Metals Corp.

2) I currently reside at 77 Maitland Place, unit 140 I, Toronto. ON

3) I expect to graduate with a B.Sc. (geology and physics) from the UniYersiLy of Toronto in spring 2012.

4) I have been working as a field geologist in Canada from May 20 11 to present.

Signed this 4rh day of January. 2012 in the City of Sudbury, Ontario

f Jared Shilson}

15

L Thomas Hart do hereby certify that:

1) I reside at 2404 Algonquin Road, Sudbury, Ontario P3E 5V1,

2) I graduated with a M.Sc. (Geology) degree in 1984 from the University of Toronto.

3) I have been practicing my profession in Canada since 1984, as an exploration geologist (an employee and independent consultant) on precious and base metal projects with exploration/mining companies in Canada, and as a mapping geologist with the Ontario Geological Survey.

4) I am the proprietor of Hart Geoscience Inc., a consulting company based in Sudbury Ontario contracted by Transition Metals Corp. to provide management services with respect to on-going exploration and development activities on their properties in Ontario. In this capacity, I am authorized to act as an Agent of the Company.

5) I am a member of the Association of Professional Geoscientists of Ontario.

6) I supervised the portions of this work program and writing of the technical report.

Signed this 4th day of January, 2012 in the City of Sudbury, Ontario

Thomas Hart, M.Sc., P. Geo.

16

17

APPENDIX A: DAILY SUMMARY OF WORK

Table A1. Daily summary of work

18

Date Crew Truck ATV Water Pump

Mech Hoe

Work Done Claims

02-Jun-11 JGC,TR,JS,CB 1 2 Establish site access and prospecting 4260273

22-Jul-11 MK,JS 1 1 Check accessibility for back hoe, road block by fallen tree, checked alternate access

4260273

19-Aug-11 TR,JS 1 1 Check accessibility to site, fallen tree removed, access was good

22-Aug-11 MK,JS,FP 1 2 1 1 Looked for water source for pump, flagged other trenches, began trench stripping and washing

4260273

23-Aug-11 MK,JS,FP,TR 1 2 1 1 Washing, stripping trenches 4260273

24-Aug-11 MK,JS,FP 1 2 1 1 washing, mapping, stripping trenches 4260273

25-Aug-11 MK,JS 1 2 1 washing, mapping trenches 4260273

26-Aug-11 MK,JS 1 2 1 washing mapping trenches 4260273

27-Aug-11 MK,JS,JGC 1 2 finished trench mapping, JGC site visit, began sampling 4260273

28-Aug-11 MK,JS 1 2 finished sampling, equipment removal 4260273

29-Aug-11 JS Initial report writing


19

Date Crew Truck ATV Water Pump

Mech Hoe

Work Done Claims


30-Nov-11 JS Assessment report

01-Dec-11 JS Assessment report



20

APPENDIX B: TRENCH MAPS AND PROPERTY MAP

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597,680 mE

D Intermediate Lapilli Tuff

Not Visible


Date: Dec. 2011

Detailed Sampling Field Geolog ist J . Shilson

Trench 1 Drafting J . Shilson

Office: Sudbury

Projection : UTM Zone 17 Nad 83

597,680 mE

U1 w 0 w Co w U1

3 z

U1 w 0 w Co 1\.) U1

3 z

U1 w 0 w ~ U1

3 z

z E

0 (J) co c0 0 ('f)

Lfi

z E

0

'

1 5317~· 0_526 Sample Numt>er hJ V<We (ppm)

• <0_2ppmAu

Q <0_5ppmAil

e < 2.0 ppmAu

. >2 _0 ppmAu

597 715 mE

co ......... . co c0 0 ('f)

Lfi

z E

0 1'co c0 0 ('f)

Lfi 0

N

t Tr

Transition Metals

2.5

metres

597,715 mE

5

597 725 mE

D Intermediate Volcanic

D Brittle-Ductile Shear

Rubble

2


Office: sutuy

597,725 mE

Detailed Sampling Trench 2

Pfojection:UTM Zooe 17 Nil83

U1 w 0 w Co co 0

3 z

U1 w 0 w Co -..,J 0

3 z

z E l() (") (J)

C'i 0 (")

Lri

z E l() N (J)

C'i 0 (")

Lri

" Vein

\ Fracture/Joint

~ Shear

~ Glacial Striae

1531759 . 0.526 Sample Number Au Value (ppm)

• <0 .2 ppmAu

Q <0.5 ppmAu

e < 2.0ppmAu

• > 2.0ppmAu

N

1 Tr

Transition Metals

597 695 mE

I

597 ,695 mE



El Rubble


Date: Dec. 2011

Field_Geologist

Drafting J . Shilson

Office: Sudbury



(J1

w 0 w Co w (J1

3 z

(J1

w 0 w Co N (J1

3 z

597 ,680 mE

z E ~ (J)

C'i 0 (")

Lei

z E l{) l{) (J)

C'i 0 (")

Lei

z E

0 l{) (J)

C'i 0 (")

Lei

0

I Joint

Shear

1531759 . 0.526 Sample Number AuValue (ppm)

• <0.2ppmAu

0 <0.5ppmAu

• <2.0ppmAu

• > 2.0ppmAu

N

1 Tr

Transition Metals

1.5

metres

597 ,685 mE

3

597 ,690 mE



Rubble


Date: Dec.2011

Field Geologist J . Shilson Drafting J . Shilson

Office: Sudbury



(J1

w 0 w Co (J1 (J1

3 z

U1 w 0 w <D U1 0

3 z

(J1

w zl_~---------------------------------------,5~9~7~,6~8@5~m~E~----------------------------------~5~9~7J,6~9~0~m~E~---------~ E

z E l() OJ OJ C'i 0 (")

Lri

z E

0 OJ OJ C'i 0 (")

Lri

z E l() CXl OJ C'i 0 (")

Lri

z E 2 OJ C'i 0 (")

Lri

z E ~ OJ C'i 0 (")

Lri

z E

0 ,._ OJ C'i 0 (")

Lri

0

597 ,665 mE

" \ ~

~

'

1531 75. 0.526 Samp!e Numt>er AJJValue (ppm)

• <0_2ppmAu

Q < 0_5ppmAu

• < 2_0 ppmAu

• >2_0ppmAu

N

t

n Transition Metals

2.5

metres

597,665mE

597 ,670 mE 597 ,675 mE

5

597,670mE 597,675 mE

597 ,680 mE

D D D D

lnlermedk!te l apiiTuff


~-!e:.~olog&

r~


Office:sutuy

Pfojectioo:UTMZooe17Nil83

0• • • • ~2

::: 1;~1·6:~ :~ ... ·2 ~ .. • • • • • • • • , I ••••• 1531613 0.048

• • • • • • • • - ~ I • 1531612 . 0.016

-:-~ \ ! 1531611 . 0.021 . " \

597,680mE

597 ,685 mE

(J1

w 0 w Co 8 3 z

(J1

w 0 w Co ffi 3 z

(J1

w 0 w Co ~ 3 z

(J1

w 0 w Co Ul 3 z

0 (")

Lfi

z E

0

0 -<i 0 (")

Lfi

z E ~ 0 -<i 0 (")

Lfi

z E

0 0 0 -<i 0 (")

Lfi

z E ~ (J)

C'i 0 (")

Lfi

597 660 mE 597 665mE

" \ ~

-->---¥8-

f ............. ,-

' '

153175. 0.526 Sample Numt>er AJJ Value (ppm)

• <0_2ppm Au

Q < 0_5ppm AIJ

e <2.0 ppm AIJ

. >2_0 ppmAu

N

1

Tr

Transition Metals

0 2 4 1"""""""~~1111111111"""""""'

·metres 597,660mE

/ 86

~

---------

1531752

153175~7/; 81 0.002 I I

597 ,665 mE

86

597 670 mE 597 675 mE



LJ Rubble

1.005


Date: Dec. 2011 Detailed Sampling ~-ie:.~olog&

r~ Trench 6 Office:sutuy

Projectioo:UTMZooe17Nil83

597 ,670mE 597,675mE

(J1

w 0 .!>.

~ 0 3 z

(J1

w 0 .!>. 0 ~ 3 z

(J1

w 0 .!>. 0 0 0 3 z

(J1

w 0 w Co ffi 3 z

'<t 0 (")

Lfi

z E

0

0 -<i 0 (")

Lfi

z E ~ 0 -<i 0 (")

Lfi

z E 8 0 -<i 0 (")

Lfi

597 ,645 mE

1531759. 0.526 Sample Number Au Value (ppm)

• <0.2 ppmAu

0 <0.5 ppmAu

• < 2.0ppmAu

• > 2.0ppmAu

"y Fracture

I Joint

Vein

' Quartz Vein

N

t

0 1.5 3 ~""""'iiiiii~~~""""'l

metres

597 ,645 mE

597 ,650 mE 597 ,655 mE



D Rubble

•• "1?3162_71'.'0.Q04 ' ...... -~

:~.:.:.:.: ·~·: •••• ~15~3 "7"':16:-:2-:"16~0.004 .............. ~- .... 0 . - . - . . . . . . -·-

0.003

-. -. . . . .- .- -. -. . .


597,650mE

Date: Dec. 2011

Field Geologist J . Shilson

Drafting J . Shilson

Office: Sudbury


Pro·ection : UTM Zone 17 Nad 83

597,655 mE

z

(J1

w 0 .1:>

~ 0 3 z

(J1

w 0 .1:> 0 ~ 3 z

(J1

w 0 .1:> 0 8 3 z

29

APPENDIX C: SAMPLES DESCRIPTIONS

Table C1. Sample descriptions and Assay results.

30

Trench Sample UTM83_X

UTM83_Y Description Length Au_ppm_Au-ICP21

Au_ppm_Au-GRA21

Au Check_ppm_Au-GRA21

Ag_ppm_ME-ICP41

1 I531771 597675 5303827 1-2 cm quartz vein with minimal Fe staining

Grab 0.009 <0.2

I531770 597675 5303825 Qtz veneer 1mm with patchy Fe staining on surface

Grab 3.53 3.09 3.04 0.6

2 I531763 597718 5303878 Quartz calcite vein with >1 cm calcite grains and 3-5% pyrite + trace chalcopyrite

Grab 0.037 <0.2

I531764 597717 5303879 Quartz carb vein with deep brown Iron and sulphur staining in rock, 1-3% pyrite

Grab 0.041 <0.2

I531765 597719 5303880 Quartz calcite vein (5-8cm) with 50% calcite and 3% chalcopyrite

Grab 2.07 1.7

I531766 597721 5303876 Silicified shear with Fe staining and 2% disseminated pyrite + chalcopyrite

Grab 2.14 0.5

I531767 597722 5303875 Mafic volcanic at contact with shear. Trace sulphides

Grab 0.008 <0.2

I531768 597722 5303874 Pitted quartz vein with copper staining (light green) but no visible economic minerals

Grab 0.132 0.2

I531769 597722 5303880 Host rock: mafic volcanic breccia with 1 mm to 5 cm sub rounded clasts

Grab 0.003 <0.2

3 I531756 597696 5303925 Heavily silicified volcanic with quartz Grab 0.548 3.9

I531757 597695 5303927 Silicified mafic volcanic with 1-2% disseminated euhedral pyrite

Grab 0.1 0.4

I531758 597695 5303928 2-3% chalcopyrite & trace malachite in silicified intermediate volcanic

Grab 2.18 1

I531759 597695 5303930 Silicified intermediate volcanic in shear with 5% sulphides, mainly chalcopyrite with 1% malachite

Grab 8.04 6.99 6.09 5.8

I531760 597695 5303930 1 mm quartz veinlet, 50 cm from shear, contains volcanic host rock

Grab 0.053 0.2

I531761 597695 5303932 Heavily silicified intermediate volcanic in shear with 1-2% sulphide

Grab 2.67 1

31



Au_ppm_Au-GRA21


Ag_ppm_ME-ICP41

I531762 597695 5303933 Iron stained (heavy) in silicified intermediate with 5% sulphides, minimal malachite.

Grab 4.11 4.75 2.2

4 I531601 597686 5303959 Taken from shear+mg;cg qtz+cg chalco in vug,rusted

Grab 0.903 0.9

I531602 597686 5303957 host rock+fg;aphanitic rusted(burgundy) qtz

Grab 0.19 <0.2

I531603 597686 5303957 host rock+fg;aphanitic rusted(burgundy) qtz

Grab 0.368 0.3

I531604 597686 5303955 chloritized host rock,rusted, minor silicification/carbonatization

Grab 1.905 0.9

I531605 597686 5303955 rusty host rock+vuggy qtz Grab 0.033 <0.2

I531606 597686 5303953 moderate-strongly chloritized rock in shear. weakly rusted

Grab 0.326 0.2

I531607 597686 5303953 Host rock+brownish-red stained fg;mg Qtz.

Grab 0.27 <0.2

I531608 597686 5303952 Same as I531607 except contains possible sphalerite

Grab 2.3 1

I531609 597687 5303952 Host rock with rusty spots+trace chalco. and malachite+sugary quartz

Grab 1.74 2.4

I531610 597687 5303952 Host rock with rusty spots+trace chalco. +sugary quartz, weakly chloritized

Grab 0.1 0.2

5 I531611 597681 5303973 Vuggy Qtz + country rock+ chlorite Grab 0.021 <0.2

I531612 597680 5303974 Vuggy Qtz + country rock+ chlorite Grab 0.016 <0.2

I531613 597680 5303975 Vuggy Qtz + country rock+ chlorite Grab 0.048 <0.2

I531614 597678 5303976 Massive Qtz (also carbonate)+lime-green mineral

Grab 0.02 <0.2

I531615 597679 5303976 Vuggy Quartz+Host rock+chlorite Grab 0.015 <0.2

I531616 597678 5303977 Vuggy Qtz+chlorite Grab 0.034 <0.2

I531617 597677 5303979 Vuggy Qtz+chlorite Grab 0.013 <0.2

I531618 597676 5303981 qtz+up to 3% chalc+trace malachite Grab 1.09 1.9

32



Au_ppm_Au-GRA21


Ag_ppm_ME-ICP41

I531619 597672 5303987 up to 8% chalc+trace malachite+qtz+anchorite

Grab 0.349 2.2

I531620 597672 5303987 Qtz-carb+rusty spots Grab 0.182 0.3

I531621 597672 5303988 Country rock+Fe staining Grab 0.015 <0.2

I531622 597670 5303992 silicified/carbonatized volcanic+trace Chalc.

Grab 0.789 0.6

6 I531751 597665 5304006 Silicifed intermediate volcanic in weak shear with trace sulphides

Grab 0.002 <0.2

I531752 597668 5304006 Volcanic breccia with <1mm crystalline quartz veinlet. Minimal Fe staining

Grab 1.005 0.8

I531753 597666 5304000 Silicified shear with 1-2% chalcopyrite Grab 0.457 0.6

I531754 597668 5303995 Silicified shear with 3-5% chalcopyrite with pitted quartz

Grab 4.86 4.55 5

I531755 597666 5303997 Intermediate Volcanic (host lithology) Grab 0.008 <0.2

7 I531623 597650 5304003 silicified int. tuff breccia, up to 12% Chalco.

Grab/ Float

>10.0 46.7 16

I531624 597653 5304005 Massive aphanitic Qtz+chlorite+(k-spar?) pink stained Qtz

Grab 0.012 <0.2


Grab 0.003 <0.2


Grab 0.004 <0.2

I531627 597648 5304006 Int. tuff breccia on wall adjacent to Qtz vein

Grab 0.004 <0.2

Recon I528663 597700 5303999 quartz vein with minor carbonate and trace to 1% mg pyrite in north-trending shear

grab 0.01 <0.2

Recon I528664 597700 5303999 quartz vein with minor carbonate and trace to 1% mg pyrite in north-trending shear; shear hosts 2-3% fg disseminated pyrite and trace chalcopyrite

grab 1.395 2.2

33



Au_ppm_Au-GRA21


Ag_ppm_ME-ICP41

Recon I528665 597713 5303851 quartz vein with minor carbonate and trace to 1% mg pyrite in north-trending shear; rubble from pit

grab 0.571 0.4

Recon I973567 597635 5304168 silicified, carbonatized feldspar porphyry, specular hematite on fracture surface

Grab/ Float

0.013 <0.2

Recon I973568 597635 5304168 volcaniclastic with 3% sulphides, qtz phyric

grab 0.002 <0.2

Recon I531628 597676 5303831 qtz vein hosted by int. volcanic Grab/ Float

0.067 <0.2

34

APPENDIX D: ALS ASSAY CERTIFICATES

ALS CODE DESCRIPTION

WEI- 21 Received Sample WeightLOG- 22 Sample login - Rcd w/o BarCodeCRU- 31 Fine crushing - 70% < 2mmSPL- 21 Split sample - riffle splitterPUL- 32 Pulverize 1000g to 85% < 75 um

ALS CODE DESCRIPTION INSTRUMENT

Au- ICP21 ICP- AESAu 30g FA ICP- AES FinishME- ICP41 ICP- AES35 Element Aqua Regia ICP- AES

This report is for 7 Rock samples submitted to our lab in Sudbury, ON, Canada on 12- JUL- 2011.

Project: PN- 11

P.O. No.:

The following have access to data associated with this certificate:GREG COLLINS PETER MCINTYRE SCOTT MCLEAN

To:

To:ALS Canada Ltd.

2103 Dollarton HwyNorth Vancouver BC V7H 0A7 Phone: 604 984 0221 Fax: 604 984 0218 www.alsglobal.com

This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release.

Colin Ramshaw, Vancouver Laboratory Manager

ALS Canada Ltd.


To:

Project: PN- 11

WEI- 21 Au- ICP21 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41

Recvd Wt. Au Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe

kg ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm %

0.02 0.001 0.2 0.01 2 10 10 0.5 2 0.01 0.5 1 1 1 0.01

I528663 0.48 0.010 <0.2 0.41 6 <10 <10 <0.5 2 4.74 <0.5 3 17 17 1.32I528664 1.19 1.395 2.2 0.67 5 <10 40 <0.5 15 1.83 <0.5 15 11 3400 2.13I528665 2.41 0.571 0.4 1.31 3 <10 20 <0.5 3 5.74 <0.5 13 18 1315 3.10I973566 1.00 0.002 <0.2 1.35 <2 <10 10 <0.5 2 1.06 <0.5 12 157 28 1.90I973567 0.97 0.013 <0.2 0.44 <2 <10 30 <0.5 <2 4.64 <0.5 20 104 13 2.95

I973568 1.27 0.002 <0.2 0.53 <2 <10 30 <0.5 <2 0.26 <0.5 15 129 21 2.23I973569 1.60 0.120 <0.2 0.41 <2 <10 <10 <0.5 <2 4.72 <0.5 3 21 1 1.00

ALS Canada Ltd.


To:

Project: PN- 11

ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41

Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr

ppm ppm % ppm % ppm ppm % ppm ppm ppm % ppm ppm ppm

10 1 0.01 10 0.01 5 1 0.01 1 10 2 0.01 2 1 1

I528663 <10 <1 0.03 30 0.28 549 <1 0.02 9 100 2 0.03 <2 1 111I528664 <10 <1 0.17 10 0.31 391 1 <0.01 26 680 2 0.95 <2 1 30I528665 <10 <1 0.09 10 0.99 891 3 <0.01 20 210 3 0.56 <2 2 70I973566 10 <1 0.02 10 1.32 291 <1 0.05 72 630 <2 0.02 <2 2 116I973567 <10 <1 0.03 10 2.59 1120 <1 0.07 65 1120 3 0.50 <2 8 178

I973568 <10 <1 0.10 <10 0.37 160 <1 0.03 140 250 2 0.67 <2 2 10I973569 <10 <1 0.01 <10 0.28 251 <1 <0.01 11 80 <2 0.27 <2 <1 49

ALS Canada Ltd.


To:

Project: PN- 11

ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41

Th Ti Tl U V W Zn

ppm % ppm ppm ppm ppm ppm

20 0.01 10 10 1 10 2

I528663 <20 <0.01 <10 <10 7 <10 11I528664 <20 <0.01 <10 <10 7 <10 13I528665 <20 0.02 <10 <10 25 <10 31I973566 <20 0.13 <10 <10 40 <10 35I973567 <20 0.01 <10 <10 55 <10 33

I973568 <20 0.08 <10 <10 13 <10 40I973569 <20 0.02 <10 <10 25 <10 7

ALS CODE DESCRIPTION

WEI- 21 Received Sample WeightLOG- 22 Sample login - Rcd w/o BarCodeCRU- 31 Fine crushing - 70% < 2mmSPL- 21 Split sample - riffle splitterPUL- 32 Pulverize 1000g to 85% < 75 um

ALS CODE DESCRIPTION INSTRUMENT

Au- ICP21 ICP- AESAu 30g FA ICP- AES FinishAu- GRA21 WST- SIMAu 30g FA- GRAV finishME- ICP41 ICP- AES35 Element Aqua Regia ICP- AESME- OG46 ICP- AESOre Grade Elements - AquaRegiaCu- OG46 VARIABLEOre Grade Cu - Aqua Regia

This report is for 49 Rock samples submitted to our lab in Sudbury, ON, Canada on 31- AUG- 2011.

Project: PN#11

P.O. No.:

The following have access to data associated with this certificate:GREG COLLINS THOMAS HART PETER MCINTYRESCOTT MCLEAN

To:

To:ALS Canada Ltd.


This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release.

Colin Ramshaw, Vancouver Laboratory Manager

ALS Canada Ltd.


To:

Project: PN#11

WEI- 21 Au- ICP21 Au- GRA21 Au- GRA21 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41

Recvd Wt. Au Au Au Check Ag Al As B Ba Be Bi Ca Cd Co Cr

kg ppm ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm

0.02 0.001 0.05 0.05 0.2 0.01 2 10 10 0.5 2 0.01 0.5 1 1

I531751 1.00 0.002 <0.2 2.62 4 <10 20 <0.5 <2 1.08 <0.5 15 40I531752 1.40 1.005 0.8 3.34 3 <10 60 <0.5 3 0.56 <0.5 19 77I531753 0.51 0.457 0.6 0.88 5 <10 120 <0.5 3 0.11 <0.5 17 16I531754 0.92 4.86 4.55 5.0 0.73 7 <10 220 <0.5 18 0.12 <0.5 10 11I531755 0.95 0.008 <0.2 1.87 <2 <10 40 <0.5 <2 3.41 <0.5 12 30

I531756 0.59 0.548 3.9 0.74 3 <10 30 <0.5 2 0.24 <0.5 12 9I531757 1.14 0.100 0.4 4.15 5 <10 80 <0.5 6 1.37 <0.5 40 62I531758 1.52 2.18 1.0 0.65 20 <10 60 <0.5 8 0.47 <0.5 33 6I531759 1.15 8.04 6.99 6.09 5.8 0.26 8 <10 70 <0.5 212 0.11 <0.5 24 4I531760 0.65 0.053 0.2 2.67 4 <10 150 <0.5 6 1.71 <0.5 25 51

I531761 0.70 2.67 1.0 1.01 6 <10 60 <0.5 9 0.20 <0.5 31 9I531762 1.09 4.11 4.75 2.2 0.35 24 <10 40 <0.5 17 0.19 <0.5 46 6I531763 0.96 0.037 <0.2 2.12 <2 <10 30 <0.5 <2 10.8 <0.5 16 14I531764 0.68 0.041 <0.2 1.96 2 <10 40 <0.5 <2 1.94 <0.5 22 28I531765 0.73 2.07 1.7 1.08 14 <10 60 <0.5 4 1.11 <0.5 32 15

I531766 0.85 2.14 0.5 1.18 6 <10 240 <0.5 <2 0.98 <0.5 21 17I531767 0.79 0.008 <0.2 3.15 2 <10 30 <0.5 <2 1.03 <0.5 35 76I531768 0.40 0.132 0.2 2.43 <2 <10 160 <0.5 <2 0.48 <0.5 28 43I531769 1.06 0.003 <0.2 3.17 <2 <10 20 <0.5 <2 2.34 <0.5 28 53I531770 0.29 3.53 3.09 3.04 0.6 1.20 3 <10 10 <0.5 <2 0.08 <0.5 9 11

I531771 0.33 0.009 <0.2 2.41 <2 <10 10 <0.5 <2 0.73 <0.5 13 30I531601 1.03 0.903 0.9 1.51 8 <10 290 <0.5 23 0.29 <0.5 33 24I531602 1.43 0.190 <0.2 1.13 3 <10 140 <0.5 2 0.11 <0.5 11 14I531603 0.94 0.368 0.3 1.32 2 <10 540 <0.5 17 0.11 <0.5 14 14I531604 1.30 1.905 0.9 1.08 3 <10 200 <0.5 11 0.26 <0.5 32 16

I531605 1.56 0.033 <0.2 1.61 5 <10 140 <0.5 2 3.33 <0.5 12 24I531606 0.93 0.326 0.2 1.70 2 <10 290 <0.5 3 0.44 <0.5 23 20I531607 2.10 0.270 <0.2 1.00 <2 <10 110 0.5 <2 0.20 <0.5 12 17I531608 1.97 2.30 1.0 0.39 4 <10 190 <0.5 6 0.08 <0.5 7 18I531609 1.96 1.740 2.4 0.37 4 <10 120 <0.5 23 0.06 <0.5 17 14

I531610 1.15 0.100 0.2 1.17 2 <10 840 0.5 3 1.07 <0.5 13 18I531611 0.67 0.021 <0.2 1.51 7 <10 60 <0.5 2 0.22 <0.5 20 33I531612 0.76 0.016 <0.2 0.78 4 <10 30 <0.5 <2 0.24 <0.5 13 15I531613 1.50 0.048 <0.2 1.61 <2 <10 40 <0.5 <2 2.24 <0.5 11 19I531614 0.88 0.020 <0.2 1.10 4 <10 20 <0.5 <2 0.14 <0.5 8 16

I531615 0.75 0.015 <0.2 2.65 5 <10 10 <0.5 <2 0.02 <0.5 30 10I531616 0.92 0.034 <0.2 0.81 3 <10 20 <0.5 <2 0.07 <0.5 9 17I531617 1.81 0.013 <0.2 0.84 5 <10 20 <0.5 <2 0.02 <0.5 10 24I531618 1.37 1.090 1.9 0.57 5 <10 40 <0.5 11 0.30 <0.5 10 12I531619 0.99 0.349 2.2 0.39 4 <10 80 <0.5 6 2.24 <0.5 11 15

ALS Canada Ltd.


To:

Project: PN#11


Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb

ppm % ppm ppm % ppm % ppm ppm % ppm ppm ppm % ppm

1 0.01 10 1 0.01 10 0.01 5 1 0.01 1 10 2 0.01 2

I531751 76 3.27 10 <1 0.12 10 2.12 648 <1 0.01 47 440 <2 0.01 <2I531752 340 5.05 10 <1 0.13 10 2.38 831 <1 0.02 63 820 <2 0.07 <2I531753 474 2.57 <10 <1 0.20 <10 0.31 282 7 0.01 24 440 2 0.25 <2I531754 1880 3.57 <10 <1 0.23 <10 0.20 108 5 0.01 16 730 3 0.74 <2I531755 55 2.92 <10 <1 0.24 10 0.77 920 <1 0.01 44 770 <2 0.10 <2

I531756 3460 2.20 <10 <1 0.12 <10 0.41 597 1 <0.01 13 240 2 0.72 <2I531757 429 8.15 10 <1 0.25 <10 2.23 2290 2 0.01 70 780 2 1.00 <2I531758 861 3.30 <10 <1 0.24 <10 0.29 220 2 <0.01 31 600 2 2.73 <2I531759 >10000 4.94 <10 <1 0.15 <10 0.06 68 32 <0.01 24 260 8 4.22 <2I531760 170 5.34 10 <1 0.29 10 1.43 1705 1 0.01 62 1210 4 0.58 <2

I531761 147 3.88 <10 <1 0.14 <10 0.59 582 29 <0.01 29 240 3 1.48 <2I531762 5360 4.87 <10 <1 0.20 <10 0.07 115 28 <0.01 32 480 4 3.82 <2I531763 2140 3.83 10 <1 0.16 10 1.35 2240 <1 0.02 21 890 <2 0.37 <2I531764 600 3.49 <10 <1 0.11 20 1.57 1390 1 0.01 36 290 2 0.11 <2I531765 4790 3.95 <10 <1 0.24 <10 0.53 502 5 0.01 39 440 7 2.17 <2

I531766 1035 3.02 <10 <1 0.17 10 0.68 528 5 <0.01 25 420 3 0.24 <2I531767 35 5.37 10 <1 0.16 10 2.33 876 <1 0.05 62 1050 <2 0.01 <2I531768 46 4.49 10 <1 0.23 <10 1.55 773 2 0.01 55 760 <2 0.08 <2I531769 39 5.30 10 <1 0.09 10 2.53 754 <1 0.06 42 1370 <2 0.02 <2I531770 11 3.41 <10 <1 0.01 <10 0.72 780 <1 0.01 13 110 2 0.01 <2

I531771 27 5.04 10 <1 0.06 10 1.46 1210 <1 0.04 33 750 <2 0.03 <2I531601 3700 3.39 <10 1 0.19 <10 1.00 642 3 <0.01 40 560 2 0.89 <2I531602 117 2.66 <10 <1 0.17 10 0.78 257 1 <0.01 23 410 2 0.01 <2I531603 555 2.91 <10 <1 0.20 30 0.90 265 1 <0.01 32 460 4 0.05 <2I531604 441 2.99 <10 <1 0.25 <10 0.57 272 4 <0.01 45 620 2 1.05 <2

I531605 157 2.07 <10 <1 0.21 10 1.08 1000 <1 0.01 36 560 <2 0.09 <2I531606 177 3.02 <10 <1 0.20 <10 1.11 557 1 <0.01 43 600 <2 0.27 <2I531607 84 2.38 <10 <1 0.19 10 0.60 306 <1 <0.01 30 520 <2 0.01 <2I531608 268 2.14 <10 <1 0.12 10 0.18 132 1 <0.01 11 170 3 0.05 <2I531609 >10000 2.71 <10 <1 0.08 <10 0.19 137 4 <0.01 17 100 2 1.69 <2

I531610 156 2.37 <10 <1 0.21 10 0.73 434 1 0.01 39 700 2 0.17 <2I531611 108 2.47 <10 <1 0.12 10 1.04 1955 <1 0.01 38 540 6 <0.01 <2I531612 82 1.37 <10 <1 0.04 <10 0.51 1005 <1 <0.01 21 280 2 0.01 <2I531613 59 2.01 <10 <1 0.24 10 0.91 631 <1 0.02 31 930 <2 0.01 <2I531614 40 1.85 <10 <1 0.13 10 0.66 312 <1 0.01 23 450 <2 0.01 <2

I531615 39 4.36 10 <1 0.01 <10 1.81 455 <1 <0.01 77 80 <2 0.01 <2I531616 43 1.63 <10 <1 0.05 10 0.53 467 <1 <0.01 21 290 2 0.01 <2I531617 37 2.32 <10 <1 0.02 <10 0.47 1010 1 <0.01 19 320 7 0.02 <2I531618 6580 2.15 <10 <1 0.13 <10 0.30 212 1 <0.01 13 300 <2 1.10 <2I531619 5220 1.77 <10 <1 0.11 <10 0.20 725 3 0.01 16 240 2 1.20 <2

ALS Canada Ltd.


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Project: PN#11

ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 Cu- OG46

Sc Sr Th Ti Tl U V W Zn Cu

ppm ppm ppm % ppm ppm ppm ppm ppm %

1 1 20 0.01 10 10 1 10 2 0.001

I531751 1 18 <20 0.01 <10 <10 18 <10 64I531752 3 11 <20 0.01 <10 <10 34 <10 78I531753 1 6 <20 <0.01 <10 <10 11 <10 16I531754 1 9 <20 <0.01 <10 <10 9 <10 9I531755 2 47 <20 <0.01 <10 <10 13 <10 36

I531756 1 4 <20 0.01 <10 <10 12 <10 20I531757 4 13 <20 0.06 <10 <10 39 <10 111I531758 1 6 <20 0.02 <10 <10 8 <10 16I531759 1 7 <20 0.01 <10 <10 5 <10 8 2.59I531760 3 19 <20 0.09 <10 <10 25 <10 79

I531761 1 4 <20 0.01 <10 <10 12 <10 27I531762 1 5 <20 0.01 <10 <10 5 <10 5I531763 3 186 <20 0.06 <10 <10 27 <10 44I531764 3 30 <20 0.02 <10 <10 28 <10 39I531765 1 11 <20 0.03 <10 <10 14 <10 21

I531766 1 15 <20 0.04 <10 <10 17 <10 35I531767 6 12 <20 0.12 <10 <10 66 <10 119I531768 3 10 <20 0.08 <10 <10 33 <10 94I531769 8 32 <20 0.26 <10 <10 84 <10 40I531770 <1 11 <20 0.03 <10 <10 24 <10 47

I531771 3 80 <20 0.23 <10 <10 48 <10 70I531601 1 10 <20 0.01 <10 <10 14 <10 35I531602 1 7 <20 0.01 <10 <10 12 <10 26I531603 1 15 <20 0.01 <10 <10 14 <10 33I531604 1 11 <20 <0.01 <10 <10 11 <10 21

I531605 2 33 <20 0.03 <10 <10 11 <10 38I531606 2 11 <20 0.01 <10 <10 16 <10 41I531607 1 7 <20 0.01 <10 <10 12 <10 23I531608 1 6 <20 0.01 <10 <10 22 <10 8I531609 1 4 <20 <0.01 <10 <10 13 <10 8 1.565

I531610 1 19 <20 0.01 <10 <10 12 <10 27I531611 2 11 <20 0.01 <10 <10 23 <10 45I531612 1 7 <20 <0.01 <10 <10 12 <10 25I531613 2 36 <20 <0.01 <10 <10 11 <10 37I531614 2 8 <20 <0.01 <10 <10 15 <10 24

I531615 1 3 <20 <0.01 <10 <10 30 <10 91I531616 1 9 <20 0.01 <10 <10 16 <10 20I531617 1 5 <20 0.02 <10 <10 31 <10 22I531618 1 9 <20 <0.01 <10 <10 7 <10 10I531619 1 52 <20 <0.01 <10 <10 5 <10 8

ALS Canada Ltd.


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Project: PN#11

WEI- 21 Au- ICP21 Au- GRA21 Au- GRA21 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41

Recvd Wt. Au Au Au Check Ag Al As B Ba Be Bi Ca Cd Co Cr

kg ppm ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm

0.02 0.001 0.05 0.05 0.2 0.01 2 10 10 0.5 2 0.01 0.5 1 1

I531620 1.24 0.182 0.3 1.15 4 <10 130 <0.5 2 0.19 <0.5 20 20I531621 0.99 0.015 <0.2 2.09 2 <10 70 <0.5 <2 0.84 <0.5 17 26I531622 0.56 0.789 0.6 1.50 6 <10 50 <0.5 3 0.14 <0.5 12 26I531623 1.14 >10.0 46.7 16.0 1.91 3 <10 280 <0.5 2410 3.32 <0.5 13 42I531624 1.71 0.012 <0.2 1.51 2 <10 10 <0.5 7 0.26 <0.5 9 30

I531625 1.18 0.003 <0.2 0.40 <2 <10 10 <0.5 <2 0.14 <0.5 3 18I531626 0.87 0.004 <0.2 1.25 <2 <10 10 <0.5 <2 0.57 <0.5 8 36I531627 1.71 0.004 <0.2 2.79 <2 <10 30 <0.5 <2 1.60 <0.5 16 71I531628 0.98 0.067 <0.2 1.45 4 <10 20 <0.5 <2 2.05 <0.5 11 46

ALS Canada Ltd.


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Project: PN#11


Cu Fe Ga Hg K La Mg Mn Mo Na Ni P Pb S Sb

ppm % ppm ppm % ppm % ppm ppm % ppm ppm ppm % ppm

1 0.01 10 1 0.01 10 0.01 5 1 0.01 1 10 2 0.01 2

I531620 194 2.47 <10 <1 0.25 <10 0.47 333 1 0.02 32 730 2 0.29 <2I531621 31 3.28 <10 <1 0.21 10 1.12 668 <1 0.02 46 890 <2 0.14 <2I531622 423 3.26 <10 <1 0.20 <10 0.73 317 1 0.02 26 440 <2 0.15 <2I531623 >10000 3.39 <10 <1 0.18 20 1.35 692 9 0.01 39 410 17 1.43 <2I531624 64 2.28 <10 <1 0.04 <10 1.20 405 <1 0.01 28 200 <2 0.01 <2

I531625 17 0.94 <10 <1 0.01 <10 0.31 157 1 0.01 9 40 <2 0.01 <2I531626 16 1.85 <10 <1 0.03 <10 1.00 384 <1 0.01 26 230 <2 0.01 <2I531627 23 3.41 10 <1 0.11 10 2.40 840 <1 0.01 54 910 2 0.01 <2I531628 27 2.18 <10 <1 0.05 10 0.92 558 <1 0.08 29 570 <2 0.04 <2

ALS Canada Ltd.


To:

Project: PN#11

ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 ME- ICP41 Cu- OG46

Sc Sr Th Ti Tl U V W Zn Cu

ppm ppm ppm % ppm ppm ppm ppm ppm %

1 1 20 0.01 10 10 1 10 2 0.001

I531620 1 11 <20 <0.01 <10 <10 12 <10 18I531621 2 20 <20 <0.01 <10 <10 18 <10 47I531622 2 8 <20 <0.01 <10 <10 18 <10 28I531623 2 40 <20 <0.01 <10 <10 17 <10 44 1.545I531624 1 8 <20 0.02 <10 <10 17 <10 36

I531625 <1 9 <20 0.01 <10 <10 6 <10 9I531626 1 12 <20 0.02 <10 <10 14 <10 30I531627 3 23 <20 0.04 <10 <10 34 <10 77I531628 3 62 <20 0.19 <10 <10 38 <10 40

report of physical work on the new kirkland project … · 4.0 geology 3 4.1. regional geology 3...

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