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1

REPORT

ON THE

DIENT IP SURVEY

MELBA SOUTH CLAIM GROUP

MELBA AND BERNHARDT TOWNSHIPS

DISTRICTS OF COCHRANE AND TIMISKAMING

·ONTARIO

FOR

JONAT·HAN CAMILLERI !

.. .

L o. s. Winter

BASc, MSc App March 15, 2019

TABLE of CONTENTS

1. . Introduction

2. Property

3. · Location and Access

4. Regional and Property Geology

5. Previous work. in the Area

6. Gradient IP Survey'Program and Results

7. Summarry and Recommendations

8. Expenditure

9. References

10. Certificate of Qualification ·

11. Appendices

i !

/

UST of TABLES

Table 1 Camilleri Melba South Property = MLAS Claims/cells

Table 2 Table of Lithologic Units

Figure 1

Figure 2

Figure 3

Figure 4

Figure 5

Figure 6

Figure 7

Figure 8

Figure 9

LIST of FIGURES

Property Location

Camilleri Melba South Property - MLAS Claims/cells

Location and Access

Airborne Residual Magnetic Field Survey Map

Gradient IP Survey Lines - Location Map

Gradient IP Survey Line 65 E

Gradient IP Survey Line 66 E ', .

Gradient IP Survdy Line 67 E

Gradient IP Survey Line 68 E

1. k1troduction

The Camilleri Melba South Claim Group ( the Property ) was acquired over a period of time for its potential to host gold and copper mine_ralization of economic interest. The Claim Group is located in the south to southwestern part of Melba township and the adjacent part of Berrifiardt fownshfp to the souffi;-approximately 15 km north of Kirkland Lake;)Bfstr.ict of Timiskaming, Larder Lake Mining Division, Ontario. Between ·November 17 and 20, 2018, 4 lines of Gradient Induced Polarization (lP) surveying totalling 8.65 km were completed on the Property by Dan Patrie Exploration Ltd., an experienced geophysical contractor.

The following report presents a brief review of the regional and property geology as well as a summary of previous work in the area and a description of the work done and the results obtained.

2. Property

The Claim Group being reported on consists of 67 active MLAS mining claims/cells as shown in Figure 2 and as listed in Table 1. They cover an area of approxirnately:1000 ha.

3. Location and Access

The Claim Group is loc?ted in the southerp to southwestern part of Melba· township and the adja,cent northern to northwestern part of Bernhardt township at UTM ·co-brdinates, NAO 83, Zone 17, 566750mE,5347600mN. The Property is approximately 15 km north of Kirkland Lake and can be acc?ssed by gr�yel roads as_ shown in Figure 3.

FIGURE 1

MELBA SOUTH CLAIM GROUP

kilometres PROPERTY LOCATION MAP

Scale: as shown Mar 2019

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FIGURE 2

MELBA SOUTH CLAIM GROUP

CLAIM MAP

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B 1)1·1 ais - ' -, 0 5-00 -too

B L I �

1)3.1 � Metres

1 07485 2019-06-23 .

1 07486 2019-06-23

109465 2019-06-23

1 09466 2019-06-23

1 1 1400 201 9-06-23 .

1 1 1401 2019-06-23

1 1 1416 2019-06-23

11 1417 2019-06-23

1 1 1432 2019-06-23.

1 1 3316 2019-06-23- ·

120718 2019-06-23· '

120719 2019-06-23"

1221 68 2019-06-23··

122855 2019-06-23:

122856 2019-06-23·'

122857 2019-06-23··

122858 2019-06-23

1241 91 2019-06-23 128092 2019-06-23

128734 2019-06-23

1 33804 2019-06-23

1 36588 2019-06-23

139631 2019-06-23

140269 2019-06-23

140270 2019-06-23

141041 2019-06-23

146230 2019-06-23

146231 201 9-06-23

149880 2019-06-23

1 50392 2019-06-23

150403 2019-06-23

1 50404 2019-06-23 .

153365 2019-06-23 ,

156636 2019-06-23

156637 2019-06-23 "/

1 68531 2019-06-23' ..

1 68532 2019-06-23

1 68533 2019-06-23 .

1 71 301 2019-06-23

171302 2019-06-23 .

1 74179 2019-06-23 .

MLAS Claims/CeUs

42799f4

4279919

427991 6

427991 8

427991 5

4279915 4279917

4279917 427991 7

427991 3

4281809

4281809

427991 9

4279.91 8

. . ,,4is1�91 8 427991 8 427991 8

4279919 427991 5

4279916

427991 7

427991 3 4279914

427991 6

4279��8

427991 8

427�916

427991 8

427991 5

427991 7

4279917

427991 7

427991 5

427991 3

427991 3

4279915

4279915

427991 5 427991 3

427991 3

4279914

MELBA BERNHARDT,MELBA MELBA BERNHARDT MELBA MELBA BERNHARDT BERNHARDT BERNHARDT MELBA MELBA MEl.,\3A BERNHARDT BERNHARDT

I' ' . . '

BE�J}{v!ARDT B��NbfARDT BERNHARDT BERNHARDT MELBA MELBA BERNHARDT,MELBA MELBA MELBA BERNHARDT,MELBA BERNHARDT BERNHARDT BERNHARDT,MELBA BERNHARDT -

MELBA BERNHARDT BERNHARDT BERNHARDT MELBA MELBA MELBA MELBA MELBA MELBA

·- MELBA MELBA MELBA

107485 1 07486

1 09465

1 09466

1 11400

1 11401

1 1 141 6

1 11417 1 1143� 11331Q 1 2071 8.· .

1 20719

122168

122855

122856

, 122857 122858

124191 �--� �.·- -

128092 128734

1 33804

1 36588 1 39631

140269

140270

141041

146230

146231

149880

1 50392

150403

1 50404

153365

156636

1 56637

1 68531

1 68532

168533

1 71 301·

1 71 302·

1 7417S

Single- CeWMining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Boundary Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Boundary Cell Mining Claim Single Cell Mining Claim Single Cell Minirig Claim . ____ Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Boundary Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell_ Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining Claim Single Cell Mining .,Olaimn

174816 201 9-06-23 4279916 BERNHARDT 174816 Single Cell Mining Claim I 1 86222 2019-06-23 427991 8 BERNHARDT 1 86222 Single Cell Mining Glaim

1 86223 2019-06-23 4279918 BERNHARDT 1 86223 Single Cell Mining Claim 192 152 2019-06-23 4279914 MELBA 192152 Single Cell Mining Claim 19431 3 2019-06-23 427991 6 MELBA 194313 Single Cell Mining Claim 194314 2019-06-23 . 427991 8 BERNHARDT,MELBA 194314 Single Cell Mining Claim 19431 5 2019-06-23 4279916 BERNHARDT 19431 5 Single Cell Mining Claim 198537 20.19�06-23 427991 7 BERNHARDT 198537 Single Cell Mining Claim 204246 201 9-06-23 4279914 MELBA 204246 Single Cell Mining Claim 204247 2019-06-23 427991 7 BERNHARDT,MELBA 204247 Single Cell Mining Claim 205728 2019-06-23 . 4279918 BERNHARDT 205728 Single Cell Mining Claim 205729 201 9-06-23 , 427991 8 BERNHARDT 205729 Single Cell Mining Claim 205968 201 9-06-23 4279915 MELBA 205968 Single Cell Mining Claim 205984 201 9-06-23 427991 7 BERNHARDT,MELBA 205984 Single Cell Mining Claim 205996 2019-06-23 427991 7 BERNHARDT 205996 Single Cell Mining Claim 210400 2019-06-23 . 427991,4 MELBA 210400 Single Cell Mining Claim 211031 2019-06-23 427991 8 BERNHARDT 211031 Single Cell Mining Claim 223971 2019-06-23 4281 809 MELBA 223971 Single Cell Mining Claim 228072 2019-06-23 427991 6 BERNHARDT,MELBA 228072 Sin�le Cell Mijiing Claim 229427 2019-06-23 427991 5 MELBA 229427 Single Cell Mining Claim 229428 2019-06-23 , 4279917 BERNHARDT,MELBA 229428 Single Cell Mining Claim 240922 2019-06-23 427991 6 BERNHARDT 240922 Single Cell Mining Claim 245001 2019-06-23 427991 9 BERNHARDT 245001 Single Cell Mining Claim 248933 2019-06-23. 427991 6 MELBA 248933 Single Cell Mining Claim 253048 . 2019-06-23 427991 8 BERNHARDT 253048 Single Cell Mining Claim

____ , _ __ -4L._,. _ _ .-_ . - . ·::.. .· � ·=�---=-==-=� �- ---

253049 2019-06-23 427991 8 BERNHARDT 253049 Single Cell Mining Claim 253050 .2019-06-23 42.79918 BERNHARDT 253050 Single Cell Mining Claim 255.921 2019-06:":23 427991 3 MELBA 255921 Single Cell Mining Claim 271992 2019-06-23 4279915 . MELBA 271992 Single Cell Mining Claim 272002 2019-06-23 4279917 BERNHARDT 272002 Single Cell Mining Claim 273133 2019-06-23 427991 9 BERNHARDT,MELBA 273133 Single Cell Mining Claim 273134 2019-06-23 427991 9 BERNHARDT 2731 34 Single Cell Mining Claim 273 135 2019-06-23 4279919 BERNHARDT 273135 Single Cell Mining Claim 288072 2019-06-23 427991 8 BERNHARDT 288072 Single Cell Mining Claim 289550 2019-06-23 / 427991 8 BERNHARDT 289550 Single Cell Mining Claim

2019�06-2� 295448 4279914 MELBA 295448 Single Cell Mining Claim 295449 2019-06-23 427991 7 BERNHARDT,MELBA 295449 Single Ceil Mining Claim 296072 2019-06-23 427991 6 MELBA 296072 Single Cell Mining Claim

301 604 2019-06-23 ' 427991 8 BERNHAROT 301858 201 9-06-23 427991 7 BERNHARDT 301 871 201 9-06-23 427991 7 BERNHARDT 302961 201 9-06-23 4279919 BERNHARDT.MELBA 303605 201 9-06-23 427991 9 BERNHARDT 304577 2019-06-23 427991 3 MELBA 308165 201 9-06-23 4279914 MELBA 31 5509 201 9-06-23' 427991 6 MELBA 3191 97 201 9-06-23 427991 7 BERNHARDT 319198 201 9-06-23 427991 7 BERNHARDT 319199 201 9-06-23 427991 7 BERNHARDT 320378 2019-06-23 427991 8 BERNHARDT.MELBA 333093 201 9-06-23 4279917 BERNHARDT.MELBA 334506 201 9-06-23 4279913 MELBA 335729 201 9-06-23 427991 4 MELBA 335730 201 9-06-23 4279914 MELBA

107485, 107486, 1 09465, 1 09466, 1 11400, 1 11 401 , 1 1 1416, 1 1 1417, 1 1 1432, 1 1 3316, 12071 8, 1 2071 9, 122168, 1 22855, 122856, 122857, 122858, 12419 1 , . 128092, 128734, 133804, 1 36588, 1 39631 , 140269, 140270, 1 41 041 , 1 46230, 146231 , 149880, 150392, 1 50403, 1 50404, 1 53365, 156636, 1 56637, 1 68531 , 168532, 1 68533, 171301 , 1 71302, 1 74179, 1 7,-4816, 186222, 1 86223, 1921 52, 1 94313,194314,194315, 1 98537,204246,204247,205728,205729,205968, 205984,205996,2.10400,211031 ,223971 ,228072,229427,229428,240922, 245001,248933,253048,253049,2530�0.255921 ,271 992,272002,273133, 2731 34,2731 35,288072,289550,29�fo.�95449,296072,301 604,301858,

. . . . . • --�::.J,..,J • •

301871 ,302961 ,303605,304577,308165,31 5509,3191 97,31 91 98,3191 99, 320378,333093,334506,33572!i335730

301604 Single Cell Mining Claim 301 858 Single Cell Mining Claim 301 871 Boundary Cell Mining Claim 302961 Single Cell Mining Claim 303605- Single Cell Mining Claim 304577 · Single Cell Mining Claim 3081 65 Single Cell Mining Claim 31 5509 Single Cell Mining Claim 319197 Single Cell Mining Claim 31 9198 Single Cell Mining Claim 31 9199 Single Cell Mining Claim 320378 Single Cell Mining Claim 333093 Single Cell Mining Claim 334506 Single Cell Mining Claim 335729 Single Cell Mining Claim 335730 Single Cell Mining Claim

BENOIT

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011713 \''

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Claim Group and Work Area

LEE

BOMPAS

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SISLEY

FIGURE 3

MELBA SOUTH CLAIM G ROUP

LOCATION and ACCESS MAP

Scale: as shown Mar 2019

4. Regional and Property Geology

The Melba township area is underlainby Archean-age metavolcanic rocks of the Blake river Group which ?xtends from the Timmins area in the west to and beyond, Noranda, Quebec in the east in the form of a large sync!inorium. The geological sequence is summarized in Table 2, Table of Lithologic Units. The Archean assemblage is a volcanic sequence with interbedded metasediments in th -e upper part. The metavolcanictn!rre ptedominantly intermediate in composition, however, there are mafic metavolcanics in the upper part and felsic metavolcanics in the lower part. Regional al teration is in general of a low grade.

Late mafic intrusive rocks of Matachewan age occur in the area as part of a swarm of north-trending diabase dykes extending east from Benoit township.

Major faults in the area trend north to northwest (Ontario Geological Survey Map 2252).

Pleistocene deposits consist mainly of sand, g ravel and clay deposited on the Archean basement units during the Wisconsin glacial retreat (Jensen, 1 972).

Figure 4 is a copy of the OGS airborne residual magnetic field survey map of the Melbai�:md adjacent townships area.and shows the dominant east-southeast, regional trend. The Melba South Claim Group in the southern part of Melba township overlies an area of mafic metavolcanic units while the areas to the north and south (blue) are underlain by metavolcanics of an intermediate to felsic composition (OGS Prel. Map P.5 19,/Melba Township)

Table 2 'I'ABLE OF LI'I'HOLOGIC UNI'I'S

CENOZOIC

RECENT

Peat, alluvium PLEIS_TOCENE

Gravel, sand, silt, irarved clay

MELBA AND BISLEY TOWNSHIPS

Unconformity

PRECAMBRIAN

. ARCHEAN

LATE MAFIC INTRUSIVE ROCKS

Quartz diabase (dikes)

FELSIC INTRUSIVE ROCKS

Intrusive Contact

Hornblende diorite, monzonite porphyry

Intrusive Contact

EARLY MAFIC INTRUSIVE ROCKS

Gabbro, quartz __ gab bro, hornblende gab bro

/ Intrusive Contact

FELSIC VOLCANIC ROCKS Pillow lava, flow breccia, pyroclasticrocks

INTERMEDIATE VOLCANIC AND SEDIMENTARY ROCKS

Massive lava, pillow lava, flow breccia, J?Jroclastic rocks, argillite

MAF,tc VOLCANIC ROCKS Basalt, andesite, massive lava, pillow lava, flow brecda

FIGURE 4

MELBA SOUTH CLAIM GROUP

0 1 AIRBORN E RESIDUAL FIELD MAGN ETICS

Kilometres Scale: as shown Mar 2019

5. Previous Work in the Area .,.

Following the discovery of gold in area in 1 906 there . · �as work in the Melba area based on of old pits, , however, the first

recorded work dates from 1934. At this time in the northwestern quadrant of Melba township, north of the Black River gold mineralization was d iscovered fol lowed by extensive surface work, underground exploratio·n and diamond

. drilling. The operation was shut down due to the onset of World War I I in 1939. The next work was in 1·959 by Pitchvein Mines Limited through to 1 96a and consisted of stripping, dewatering of the shaft and workings, UG mapping and sampling and surface and UG diamond dri l l ing. The Property was shut down in 1963. This property is currently represented by the patented claims in this area. A bulk sample taken from UG returned 0.210 oz gold per ton across a vein width of 4.5 ft.

In 1 962 chalcopyrite minerali�ation was discovered i n the northeastern part of Melba township and over the next 3 years several pits were put down . . ! n 1965 Midrim Mining Company Limited optioned the property, carried out an airborne survey and dril led 7 holes for a total of 2932 ft.The main vein is 1 foot wide and 500 ft long and contains .small specks of chatcopyrite and gold .

Kinika Gold Mines Limited carried out considerable exploration work in the 1 920's in northwestern Bernhardt township approximately 2 km south of the current Melba South Pr9perty (Figure 4 - Kinika Gold Mines, after ODM Pref. Map 446, Site 10) {White quartz veins carrying epidote and less than 5% pyrite were explored with the best gold values being 0.23 and 0.58 oz gold/ton. The longest veins parall el the ESE-trending metavolcanic contacts while the widest veins are perpendicular to the contacts. (Rupert and Lovell, 1970)

_ I n the last_20 years or so'the esker trending ·south through the central part of the prope.rty has been sampled and the pr?p�rty �as been cover�9 by airborne surveys as part of the OGS Discover Abrt1b1 pro1ect.

6. Gra.dient IP Survey Program and Results

. Between November 1 7 and 20, 2018, Dan Pat�ie Exploration Ltd. at the request of Mr. Camilleri carried out a Gradient' IP Survey on the Camilleri Melba South Claim Group. The program consisted of line-

. cutting followed by the IP Survey along 4 north-south lines as shown in Figue 5, for a total of 8.65 line-km.

Commencing on the 17 November the current electrodes, wire and the generator and transmitter were moved to the survey area and the current electrodes and connecting cable were put in place in the central part of the area to be surveyed (Figures 4 and 5). The southern current electrode was located at UTM co-ordinates 567000mE, 5345400mN with the northern current electrode at 567000mE, 5349500mN, approximately 41 00 m north of the southern electrode and 500 m north of the north ends of the survey lines. The southern electrode was approximately 500 m south of the south end of Line 68E and the generator and transmitter were also at this site. The 4 lines were surveyed along pre-cut lines at the the following locations and all lines run north-south.

Line 65E, 565000mE and 5346600mN to 5349000mN, 2.35 km

Line 66E, 5661 OOmE and 5346600mN to 5349000mN, 2.35 km

Line 67E, 567400mE and 5346600mN to 5349000mN, 2.35 km

Line 68E, 568900mE and 5345900mN to 5347500mN, 1.6 km

Line 65E was read starting at the south end with one measuring electrode at 0+00 and the second measuring electrode at 0+50 mN, a = 50 m., with the balanc of the line being read in 50 m intervals for a total of 47 readings per line. The other 3 lines were surveyed in a similar fashion.

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:386 MELBA SOUTH CLAIM G ROUP

:io �. 006 (10/ ((13 oo·:i

GRADIEN T IP SURVEY LIN E LOCATIONS

:390

HO i53! 1422 0 1 1

:3 7 :? 3 ;,�3

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,"lttll'11Cl·

I

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100 0 �

M ar 20·1 9 ... ,._, ('l �f· B on 0 "':• 0:3(1 03 1 BB t):3 1 Metres Scale: as shown

,-

For each read ing taken in the field , the nPR-12 Receiver calculates the chargeability and resistivity for the site . h1 addition to the readings taken, the e lectrode array and locations are also noted by the ORerator. The current vonage at the time of the reading is also recorded. Fol!owinQI the completion.of the survey, the recorded chargeabmty and resistivity values cani be downk,ader:f from the !PR-12 Receiver to a computer with a Geosoft program and from there the chargeability and resistivity values can be plotted as maps as presented in Figures 6 and 7. Mr Gab Roy supervised the field work and did the corr1put�f work.

The !P Survey Equipment Specifications for the motor generator, transmitter and !PR-12 Receiver arre provided in Appendix L The transmitter can pulse at 1, 2 , 4, 8, 1 6 or 32 seconds and for this survey a 2 second on and off cycle was used . During the survey, readings were generally completed within a 5 minute time interval which is normal. Clhargeability readings are reported as mVN and resitivity values as ohm-metres.

The traverse on Line 65E was from south to north and at the start of the line the underlying ground is generally one of low, small to medium size knobby outcrops covered by glacial sediments varying in composition from clay to sand. At approximately 4+00 mN the line crosses a branch of the Little Black River which flows northwesterly. The area of outcrop continues to approximately 20+00 mN with low to swampy ground to the end of the line at 23+50 mN. Line 66E is very similar to Line 65E in that i t mainly traverses knobby outcrops covered by glacial sediments. Between 4+00 mN to 6+00 mN line 66 runs along the Li ttle Black River and at 7+00 mN i t crosses the southern, east-west access road (Figure 3). Line 67E from i ts south end to 16+00 mN crosses knobby, glacial sediment covered ground as for Lines 65E and 66E. From 16+00 mN to almost the end of the line i s low to swampy. From 18+00 mN to 20+00 mN the line parallels Melba Creek which flows north into the Black River. The last 300 m of the line is underlain by knobby outcrops covered by glacial $�diments. Line 68,E is 1600 m long and crosses the southern, east-west access road at approximately 3+00 mN. and contacts the north-trending access road at 16+00 mN. From here the north-south access road runs south, parallel to the line

for about 500 m then trends off to the southeast. The l ine mainly l ies on knobby outcrops, however, the covering sediments are more sandy due to a north-south-trending esker to the east.

The only cultural features in the area are the access roads and they did not appear to affect the readings.

Vegetation in the a rea consists dominantly of jackpine in the areas of sandy to gravelly soils plus spruce, poplar and birch. Several years ago the larger trees in the area were harvested. I n the areas of low ground such as along Melba Creek alders are common. No problems with electrode contact were reported by the field crews from the lines . .

The temperatures in the Kirkland Lake area at the time of the field work varied from daytime highs of =2 "C to ovemight l ows of = 16° C so the ground was in the process of freezing, however, the ground was stm soft enou{gh that there were no reported problems with electrode contact

in Figures 6, 7, 8 and 9 , the calculated chargeabilities and resistivities for the survey l ines, 65E, 66E, 67E and 68E. have been plotted. The minimum chargeability value recorded is from Line 67E at 2 mVN while the maximum value is from Line 65E and is 9.2 mVN, for a difference of only 7.2 mVN. Resistivity values for the 4 l ines surveyed range from 4190 ohm-metres to 43120 ohm-metres. For comparison purposes, another Gradient IP survey by the same contractor approximately 20 km to the east in a similar geological environment (Blake River Group metavolcanics) returned chargeability values from zero to 70 mVN and resistivity values from 200 ohm-metres. to 37260 ohm-metres. Based on this comparison and the writer's , experience with IP surveys it is considered that the chargeability values are al l in the low "background" range and would at best represent very

. low amounts of disseminated sulphides. The resistivity values appear to be typical of Archean metavolcanics in the area.

9.2

8.7

8. 3

8.1

7.9

7 .8

7 .7

7.5

7.4

7.3

7.2 7. 1

7 .0

6.9

6.9

6.8

6.7

6.7

6.6

6.6

6.5

6.4

6.3

6.2

6.1

6.0

5.8

5.7

5.6

5.5

5. 3

5.2

5. 1

5. 1

5.0

4.9

4.6

4.1

mVN

0 0 0 m "<!' (') l()

0 0 co co "<!' (') l()

0 0 co co "<!' (') l()

0 0 '<I' 00 'St (') l()

0 0 N co '<I' (') l()

0 0 0 co '<I' (') l()

0 0 co I'-­'¢ (') l!)

0 0 co l'-­'<t' (') l()

0 0 N l'-­'<t (') l()

0 0 0 l'-­'<t' (') l()

565000

565000

Scale 1 : 1 0000 1 00 0 100 .e s

(mete1s) ,'./.t..063/UiM.!OM !lN

Ol <,) .r:,.. co 0 0 0

Ol <,) .r:,.. (X) (X) 0 0

Ol <,) .r:,.. <» .r:,.. 0 0

Ol <,) .r:,.. (X) N 0 0

en <,) .r:,.. <» 0 0 0

Ol <,) .r:,..

- -...J (X) 0 0

en <,) .r:,.. -...J m 0 0

en (,.) .r:,.. -...J .r:,.. 0 0

(.,., (,) .r:,.. 'l N 0 0

en (,) .r:,..

- -...J 0 0 0

en <,) .r:,.. m (X) 0 0

JOHN CAMILLERI MELBA TWP GRADIENT IP

LINE 65E

Line 65 E

334506

1 56636

333093 1 1 1 4 16

1 50403

FIGU RE 6

43120

40900

38968

3491 1

30704 28258

26157

23585

2 1 375

1 9398

18184

1 7405

16861

16150

15629 151 13

14694

· 1 4395

13990

13601

13298

1 2956

12694

12381

12093 1 1 795

1 1456

1 0808

9810

8790

8353

8068 7824

7617

7432

7325

7090

6692

ohm*m

M ELBA SOUTH CLAIM GROUP GRADIEN T IP SU RVEY LIN E 65 E Scale: as shown Mar 2019

0 0 0 0) '<1' (') l!)

0 0 co co 'St (') l!')

0 0 (D co 'St (') l!)

0 0 'St co -.!" (') l!')

0 0 N co '<1' (') l!')

0 0 0 co 'St (') l!)

0 0 co I'-­-.;!­(') l()

0 0 (D

!;;: (') l!')

0 0 -.!" l'-­'<t' (') l!')

0 0 N I'-­'¢ (') l!)

0 0 0 l'-­'<t' (") l()

0 0 co co '<1' (") l!')

564800 565000 565200

564800 565000 565200

Scale 1 : 1 0000 100

!-ii

0

(meters)

100

NA063 I UTA< zone 17.V

(Jl <,) .r:,.. (D 0 0 0

(Jl (,.) .r:,.. (X) 00 0 0

en (;) .r:,.. <» 0) 0 0

Ol <,) .r:,.. (X) .r:,.. 0 0

en (;) .r:,.. (X) (\.) 0 0

C1l (;) .r:,.. (X) 0 0 0

en (,) .r:,.. 'l <» 0 0

Ol (,) .r:,.. -...J .r:,.. 0 0

Ol w .r:,.. 'l N 0 0

Ol (,.) .r:,.. -...J 0 0 0

Ol w .r:,.. 0) <» 0 0

(Jl w .r:,.. 0) 0) 0 0

7.6

7.3

7 . 1

7.0

6.9

6.8

6.6

6.6

6.5

6.4

6.4

6.3

6.3

6.2

6.2

6. 1

6.0

6.0

5.9

5.9

5.8

5.7

5.7

5.6

5.5

5.5

5.4

5.3

5.3

5.2

5.2

5.1

5.1

5.0

4.9

4.6

4.3

3.6

mVN

0 0 0 0) v (") r.n

0 0 co co v (") r.n

0 0 CD co v (") r.n

0 0 v co v (") r.n

0 0 N co 'Sf" (") r.n

0 0 0 co v (") r.n

0 0 CD r-­v (") r.n

0 0 v r-­v (") r.n

0 0 N r-­v C') l!')

0 0 0 r-­v (") r.n

0 0 co CD v (") r.n

0 0 CD CD v (") r.n

566000 566200

566000 566200

Scale 1 : 1 0000 1 00 0 100

Ml - • (meters)

,".JA.083/UTM :or.e 17N

()l (,.) .I>, (!) 0 0 0

()l (,.) .I>, 0:, 0:, 0 0

()l (,.) .I>, 0:, 0) 0 0

()l (,.) .I>, 0:, N 0 0

()l w .I>, 0:, 0 0 0

(Jl w .I>, --.J 0:, 0 0

()l w .I>,

� 0 0

()l w � � 0 0

()l w .I>, --.J 0 0 0

(Jl w .I>, 0) 0:, 0 0

(Jl w .I>, 0) cj) 0 0

JOHN CAMILLERI MELBA TWP GRADIENT IP

LINE 66E

Line 66 E

1 07485

1 92 1 52

295449

301 858

1 98537

FIGURE 7

41399

37986

35334

33640

32256

30527

28437

26985

25601

24337

23301

22442

21837

21 151

20531

19758

18767

1 7447

1 5995

1 4716

13679

13005

1 2367

1 1 629

10655

9785

9076

8643

8325

7976

7595

7322

7007

6604

6079

5539

4846

4068

ohm*m

MELBA SOUTH CLAIM G ROUP GRADl"EN T IP SURVEY LIN E 66 E Scale: as shown Mar 2019

0 0 0 0) 'Sf" (") l!')

0 0 co co -'Sf" (") r.n

0 0 (!) co v (") r.n

0 0 'Sf" co 'Sf" (") r.n

0 0 N co v (") LO

0 0 0 co 'Sf" (") r.n

0 0 co r-­-.;j- . (") r.n

0 0 (!) r-­v (") r.n

0 0 N r-­v (") r.n

0 0 0 r-­v C') r.n

0 0 co (!) 'Sf" C') LO

0 0 CD (!) v (") r.n

566000 566200

566000 566200

Scale 1 : 1 0000 100 0 1 00

.. - - j (meters)

,\.J'AD83/UTM zo,.,e 17.\'

()l w .I>, CD 0 0 0

(Jl (.,) .I>,

- 0:, 0:, 0 0

(Jl (,.) .I>, 0:, 0) 0 0

(Jl (,.) .I>, 0:, N 0 0

()l (.,) .I>, 0:, 0 0 0

()l w .I>, --.J 0:, 0 0

()l w .I>, --.J 0) 0 0

(Jl (.,) .I>, --.J (\.) 0 0

()l w .I>, --.J 0 0 0

()l (,.) .I>, 0) 0:, 0 0

(Jl (,.) .I>, 0) 0) 0 0

567200 567400 567600 JOHN CAMILLERI 567200 567400 567600 MELBA TWP GRADIENT IP

0 0, LINE 67E 0 0, 0 <,.) 0 <,.) 0 .:,.. 0 .!>, 0) (!) 0) (!) ""' 0 ""' 0 C'") 0 C'") 0 lO 0 I.() 0

0 0, 0 0, 0 <,.) 0 <,.) cO .:,.. cO .!>, cO 00 cO 00 ""' 00 ""' 00 C'") 0 C'") 0 I.() 0 I.() 0

0 0, 0 0, 0 <,.) 0 w (!) .:,.. (!) .:,.. cO 00 co 00 ""' 0) ""' 0) (") 0 C'") 0 I.() 0 I.() 0

8

8 0 0, 32178 0 0 <,.) 0 <,.)

8 ""' .!>, 30185 ""'

00 co 00 8

'<t .!>, 28739 ""' C'") 0 C'") 0

8 lO 0 27828 I.() 0

8 27080

7 0 0,

26384 0 0 <,.) 0 <,.)

7 N .i:,..

25693 N 00 cO OJ

7 ""' N 25134 '<!" N C'") 0 C'") 0

7 I.() 0 24556 I.() 0

7 24103

7 0 0,

23319 0 0 <,.) 0 v,)

7 0 .!>,

22520 0 co 00 co 00 7

"<!- 0 21351 '<!" 0

0 C'") 0 7

I.() 0 20143 I.() 0

7 1 9271

7 0 0,

187 1 1 0 0, 0 <,.) 0 <,.)

7 co .!>,

18182 co .i:,.. I"- ..._j

Line 67 E I"- ..._j

7 '<!" 00

1 7488 '<!" 00 C'") 0 C'") 0

7 I.() 0

16876 I.() 0

7 1 68531 16055

7 0 ()'J

15342 � 0 (}l 0 e,,

1 1 1 401 0 v,)

7 (!) .i:,..

1 4596 (!) .i:,.. I"- ..._j I"- ..._j

7 '<!" OJ 2731 33 1 3866 ""' OJ C'") 0 C'") 0

7 I.() 0 1 24 1 91 1 3183 I.() 0

6 273 1 34

1 2467

6 0 0,

1 1 916 0 0, 0 v,) 0 v,)

6 '<!" .!>,

1 1 463 '<!" .i:,.. I"- ..._j I"- - ..._j

6 "<!- .i:,..

1 1 1 64 ""' .i:,.. C'") 0 C'") 0

6 I.() 0

10696 I.() 0

6 9923

6 0 0,

9178 0 0, 0 v,) 0 <,.)

6 N .!>,

8568 N .i:,.. I"- ..._j I"- ..._j

6 ""' N

8060 '<!" N (") 0 C'") 0

5 lO 0 7657 lO 0

5 7205

4 0 0,

6689 0 ()'J 0 v,) 0 v,)

2 0 .i:,..

5473 0 .i:,.. I"- ..._j I"- ..._j "<!- 0 4190 '<!" 0

(") 0 C'") 0 mVN I.() 0 I.() 0

ohm*m 0 a, 0 0, 0 <,.) 0 v,) 00 .i:,.. co .!>, (!) 0) (!) 0) ""' 00 "<!- 00 C'") 0

C'") - 0 I.() 0 I.() 0

0 ()'J 0 a, 0 <,.) 0 v,) (!) """ (!) .i:,.. (!) 0) (!) 0) '<!" 0) '<!" 0) C'") 0 C'") 0 lD 0 lD 0

567200 567400 567600 567200 567400 567600

FIGURE 8 Scale 1 : 1 0000 Scale 1 : 1 0000 1 00 0 100 Ml;LBA SOUTH CLAIM GROUP 1 00 0 1 00 ..,.. . I '-"': -

(meters) GRADI ENT IP SURVEY LIN E 67 E (meters) NA0(}3 IUT!1,f zor.e 17N

NAD83 !UTM zone 17N

Scale: as shown Mar 2019

8

8

8

7

7

7

7

7

7

7

7

7

7

7

7

7

7

7

7

7

7

6

6

6

6

G

G G

G

6

6

6

6

6

G 6

G 6

mVN

0 0 0 l'-­'s:t C0 I.()

0 0 co (0 's:t C0 I.()

0 0 's:t (0 "q" C0 I.()

0 0 N (0 "q" C0 I.()

0 0 0 (0 's:t C0 I.()

568800 569000

568800 569000

Scale 1 : 1 0000 1 00 0 -----

(meters)

100 I

NAD83 I UTM zone 1 i.V

JOHN CAMILLERI M ELBA TWP GRADIENT IP

LIN E 68E

u, (.,.) ""' "" N 0 0

u, (.,.) ""' (J) co 0 0

u, (.,.) .p.. (J) (J) 0 0

(J1 (.,.) � (J) N 0 0

(J1 w .i:,. 0) 0 0 0

Line 68 E

288072 21 1 031

253049

253050

27004 24542 23104 22349 21678 2 1071 20588 20009 19541 19126 18642 1 8365 18145 1 7989 1 7832 17670 17507 17321 1 7078 16742 16409 16131 15940 15674 15365 15029 1 4745 1 4443 1 4089 1 3660 13 105 1 2306 1 1 652 1 0675 9268 7678 6397 541 1

ohm*m

FIGU RE 9

0 0 N "' "<:!' (") LO

0 0 0 "' 's:t C") LO

0 0 co <O "<:!' C") LO

0 0 (D <.D 's:t C") I.{)

0 0 N <.D 's:t C0 I.{)

MELBA SOUTH CLAIM GROUP GRADIEN T IP SU RVEY LIN E 68 E Scale: as shown Mar 2019

568800 569000

568800 569000

Scale 1 : 1 0000 100 0 1 00

_,..___ I (meters)

NAD83 /UTM zone 1 iN

(JI (.,.) ""' "" N 0 0

(JI <.,.) ""' "" 0 0 0

(JI (.,.) ""' 0) C):) 0 0

(.)) <.,.) � (J) (J) 0 0

()'1 (.,.) � 0) N 0 0

The work program was carried out by Dan Patrie Exploration ltd., an experienced geophysical contractor with Mr. Brent Patrie, owner/manager responsible for the overall program. The field program was carried out and supervised by Mr. Gab Roy who also did the plotting of the final maps. Field assistants were Beau Nevme, Espanola, James Henderson, Webbwood, Hunter Busch, Val Therese, Ron Bilton, Massey and Bronson Edy, Capreol. No log of the work program was kept, however, the information in this report was provided by Mr. Brent Patrie and Mr. Gab Roy.and by the writer from h is experience nn general , and the Kirkland lake area in particular.

7. Sum marry and Recommendations

Four l ines of a Gradient IP survey were completed on the Melba South Claim Group as shown in Figure 5 with the chargeability and resistivity values for each l ine plotted in Figures 6, 7, 8 and 9. The 4 l ines are paral lel , run north-south and represent a total of 8.65 l ine-km. The calculated chargeability values fal l in what would normally be considered as low "background" values. The calculated resistivity values are considered to be typical for the Archean metavolcanics in the area. To further evaluate the area of the survey for mineralization of economic interest it is recommended that a program of prospecting, sampling and geological mapping be carried out. If the results of this work are positive then soil geochemical surveying is recommended to identify areas of interest and if this work provided targets of interest then some Pole-Dipole work cou ld be considered.

8. Expenditures

The exploration expenditures for the 4 lines of Gradient . IP are as follows ( see Invoice in Appendix II )

1 . Line-cutting, 8.65 line-km @ $ 1 1 00 per km $ 9 5 1 5.00

2. Gradient IP Survey @ .$ 1 600 per km 1 3 840.00 for 8.65 line-km /

3. M ob and Demob 2 080.00

4. Data processir:tg 832.00

TOTAL $ 26 267.00

In Table 2 all the Melba South mining claims/cells are listed and they are shown in Figure 2. Of the 95 listed mining claims/cells, 91 are Single Cell Mining Claims and 4 are Boundary Cell Mining Claims. Of the 95 claims, 67, including the 4 Boundary Cell Claims are contained in Area A of Figure 2 and are to be retained. Twenty .. eight (28) Single Cell Mining Claims in Areas B and C of Figure 2

· wm· be- droppett · There is $· 26 267 of Assessment Credits available and the 63 Single Cell Mining-Claims in Area A at $ 400l)e.r .claim will require a total of $ 25 200 of Assessment Credits. The 4 Boundary Cell Claims wil l require ·$ 800 of Assessment Credits for a total of $ 26 000 which will hold the indicated 67 claims/cells in Area A for one year.

L.D.S. Winter, BASc, MSc(App)

15 March 201 9

References

1. Gordon et al, 1979

Gold Deposits of Ontario, Part 2, Ontario Geological Survey, Mineral Deposits Circular,, Melba twp

2. Jensen, LS. , 1970

Geology of Melba and Sisley Townships, District of Timiskaming, Ontario, Ontario Dept. Mines, Geological Branch, OFR 5052, 2 Maps, 41 p.

3. Jen sen, LS. , 1972 Geology of Melba and Sisley Townships, District of Timiskaming, Ontario, Ontario Division of M in es, Geological Report 103, 26p, Map 2252

4 Ontario Geological Survey,. 2003 Airborne Magnetic Survey; Residual Magnetic Field , Map 81 780, Scale 1: sot 000

5. Rupert' R. J. and lov�U, H. L. , 1970 Geology of Bernhardt and Morrisette Townships, District of Timiskaming, Ontario, Ont. Dept. Min es, GR 84, Prel. Map P 446, Scale: 1 in = 1/4 mile

L.D.S. Winter 1 849 Oriole Dr., Sudbury, Ontario -

P3E 2W5 winbourne@eastlink.ca

705 523 4597 Cell 705 507 4960

CERTIFICATE of AUTHOR

I, Lionel Donald. �tewart Winter, do hereby certify that:

1 . I am currently an independent consulting geologist, ,

2. that I graduated with a degree in Mining Engineering (BASc) from the University of Toronto in 1 957 and in addition I graduated from McGill University, Montreal in 1 961 with a Master of Science Appl ied (MSc App)

3 and that I am a Life Member of the Canadian Institute of M ining and also a Life Member of the Prospectors and Developers Association of Canada

4. I am a retired Professional Geoscientist in both British Columbia and Ontario (201 6).

Dated this t5 th day of March 201 9

L.D.S. Winter

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APPENDIX !

INDU CED POLARIZATION (IP) SURVEY

GEOPHYSICAL SURVEY EQUIPMENT SPECIFICATIONS . '

·' .

·' ·

. , J I ! ·. ' I ' . .

ELECTRICAL METHODS

A D i i l I O N O F I R S

IPR�1 2

I nd uced Polarization

.-��:·:�> . . - ,-. �· � ... .sCIN'l1lE<Lm.coM·� . -: ; · Setting the Standards

,,: . . •}.�' '.. .· . . .... . . ·:

IPR-1 2 SPECIFICATIONS

The IPR-1 2 IP receiver has been successfully used for many years a s a m ineral exploration tool, specifically for gold exploration.

Induced polarization can also be used as a method for mapping hydrocarbon plumes and geotechnical applications.

Inputs: Input Impedance: SP Bucking:

Input Voltage (Vp) Range: Chargeabil ity (M) Range: Tau Range: Reading Resolution of Vp, SP and M : Absolute Accuracy o f Vp , Sp and M: Common Mode Rejection: Vp Integration Time: IP Transient Program :

Transmitter Timing: External Circui t Test:

Filtering: Internal Test Generator: Analog Meter: Memory Capacity:

Power Supply:

Operating Temperature: Dimensions and Weights:

OPTIONS

Transmitters Software Packages Train ing Program

1 to 8 dipoles are measured simultaneously. 1 6 MO ±1 O volt range. Automatic l inear correction operating on a cycle by cycle basis . 50 µV to 14 V O to 300 mVN 60 microseconds to 2000 seconds. Vp - 1 0 µV; SP - 1 mV; M - 0.0 1 mVN Better than 1 % At input more than 1 OOdB. 1 0% to 80% of the current on t ime. Pulse selectable at 1 ,2 ,4,8, 16 or 32 seconds. Programmable windows also available. 50% duty cycle. On/off times of 1 ,2,4,8, 1 6 or 32 seconds. All dipoles measured individually in sequence. Range O to 2 MO with 0 . 1 kQ resolution. Circuit resistances d isplayed and recorded. RF filter, 10 Hz 6 pole low pass filter, statistical noise spike removal. 1 200 mV of SP; 807 mV of Vp and 30.28 mV/V of M. For monitoring input signals; switchable to any dipole via keyboard . Stores approximately 400 dipoles of information when 8 dipoles a re measured simultaneously. Rechargeable Ni-Cad D cells. More than 20 hours service at +25°C. (77°F), more than 8 hours at -30°C (-22°F) -30°C to +50°c (-22°F to 122° F) Console: 355 x 270 x 1 65 mm ( 1 4" x 1 0.6" x 6.5") Charger: 1 20 x 95 x 55 mm (4.7" x 3.7" x 2") Console: 5.8 kg ( 1 2.8 lbs. ) Batteries: 1 .3 kg (2.8 lbs . ) Charger: 1 . 1 kg (2.4 lbs.)

ISO 9001 :2000 registered com pany. All specifications are subject to change without notice.

Specification Sheet Part Number 7457 1 1 Revision O

r., ( .. ,, (' I 1-..·, J ··1 F' c:. / .J • .. , , .

CANADA Scintrex 222 Snidercroft Road Concord, Ontario L4K 2K1 Telephone: +1 905 669 2280 Fax: +1 905 669 6403 e-mail: scintrex@scintrexltd .com Website: www.sclntrex.com

/\/\ I (� f� 1 /g' I /\ ( ... ( } ' ' 'T L

USA Mlcro·g LaCoste 1 401 Horizon Avenue Lafayette, CO 80026 Telephone: +1 303 828 3499 Fax: +1 303 828 3288 e-mail: info@microqlacoste.com Website: www.microglacoste.com

Walcer Geophysics Ltd. - Motor Generators - MG-1 2A

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MG-1 2A

Output Self Excite I Regulaled

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400 Hz I 3 phase

Generator Bendix Aircraft Type

Very durable Forced Air Cooled

Engine 24 HP Honda Electric Start

Size 79cm. x 61 cm. x 48cm.

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Walcer Geophysics Ltd. - Transmitters - Walcer TX KWl O

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Voltage Input 1 25V line lo neutral 400 Hz I 3 phase

Powered by MG12, MG6 and MG12A

Output 100 - 3200V in 10 steps

0.05 - 20 Amps Tested lo 10.5 kVA

Switching 1 sec,, 2 sec., 4 sec., 8 sec.

Metering LED for line voltage and output current

Size 63cm. x 54c�- x 25cm,

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Page 1 of 1

/ /

APPENDIX II

GRADI ENT IP SURVEY INVOIC E

Ministry of Northern Development and Mines

Mineral Dev�lopment and Lands Branch

Ontario Government Complex - E Wing PO Bag 3060, 5520 Highway 101 . East South Porcupine ON PON 1 HO Tel: (705) 235-1625 Fax: (705) 235-1 660

December 1 , 201 7

Jonathan Camilleri 35 Redstone Path Etobicoke, ON M9L 1Y7

Dear Mr. Camiiieri:

Ministere du Developpement du Nord et des Mines

Direction de !'exploitation des mineraux et de la gestion des terrains miniers

Complexe du Gouvernement de !'Ontario Aile E, Sac postal 3060, 5520 Route 101 Est South Porcupine ON PON 1 HO Tel: (705) 235-1625 Te!ec: (705) 235-1660

Re: Exploration Permit Submission, PR-17-1 1 179,. Melbern South Project Melba and Bernhardt Townships; Larder Lake Mining Division

ntari

Attached is your exploration permit, PR-1 7-1 1 1 79, issued pursuant to subsection 78.3(2) of the Mining Act, R.S.O. 1 990, Chapter M . 14. This permit is subject to the requirements of the Mining Act, Ontario Regulation 308/12, the applicable Provincial Standards for Early Exploration and any additic;mal Terms and Conditions in the permit that are specific to your project

Please note that the attached exploration permjt is effective for a period of 3 years. You can apply to renew your permit, which should be dd.ne well in advance of the expiry date so there will btl i::IUtlyua[tl timtl JUI fJI Ut;tl:;Si1 1u i::II IU tu ql1uid 1:1 1 1y :;tu1-11-11:1ut::1 i 1 1 tl.1'.fJiUraliu1 1 adivititl:s. . '

If there are cl]g.ngesto any names or addresses on thE;l permit please advise the Ministry of Northern Development and Mines (MNDM) and an information amendment will be made to your

· exploration permit. If you would like to make changes to the exploration activities such as the type of activity, location of activity or scale of the work please follow.the amendment process and contact MNDM for further dire�tion.

,, ;

- 2 -

If you have any questions or need any assistance, please do not hesitate to contact Genevieve Sulatycky, Mineral Exploration and Development Consultant in the South Porcupine office, at (705) 235-1 656 or by e-mail to genevieve.sulatycky@ontario.ca.

Sincerely, "-, I . ', !'-, . Q / �}b4l{&l"/ . '

Desmond O'Connor Director of E;xplqr9tion

Enclosure: Exploration Permit

cc: Chief Alex (Sonny) Batisse, Chief, Matachewan First Nation Kayla Schram, Mineral Development Advisor, Matachewan First Nation Jason Batise, Executive Director, Wabun Tribal Council Stephanie Labelle, Mineral Development Advisor, Wabun Tribal Council Liliane Ethier, President, Temiskaming Metis Council Jacques Pictote, President, Timmins Metis Council Doug Hull, President, Northern Lights Metis Council David Hamilton, President, Chapleau Metis Council Andy Lefebvre, Mineral Development Advisor, Metis Nation of Ontario Aly N. Alibhai, Director of Lands, Resources & Consultations, Metis Nation of Ontario Chief Wayne McKenzie, Chief, Timiskaming First Nation Clifton Polson, MDA and Mining Coordinator, Tlmiskaming First Natlon Rose Thomas, Council Secretary, Timiskaming First Nation Chief Joel Babin, Chief, Wahgoshig First Nation Paul McKenzie, Mineral Development Advisor, Wahgoshig First Nation Chris Sackaney, Land and Resources Manager, Wahgoshig First Nation Brian Gelinas, Wahgoshig First Nation .

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