Mining Assessment Work3

Index

Introduction

Regional Geology JUN ~ ·e lO\ 7.

Local Geology and Figurel GEOSCIENCE. ASSE.SSME.Ni · OFFICE.

list of Claims and Figure 2-Map

Location and Access Figure 4

Mining Conditions

Project Description Figure3

Appendix A- Sample Numbers and Disposition

B- Results of Analysis

C- District Geologist Notes

D- Photos 1,2,3,4.

E- Assessment Work Performed

Mining Assessment Work

Introduction:

Robert A Brunette and Eric Y Boudreau carried out traditional

prospecting, examined outcrops, investigated favourable rock types,

structures and contact zones. Identified mineralized areas and sampled

promising locations .Surface stripping with power saw, axe and grub

hoe was completed and sampling using rock hammers and cold chisel

was done. Samples were submitted for analysis by labs or competent

geologists. In addition Mr. Brunette hosted Peter LeBaron District

Geologist MNDM for a field visit on April19, 2012 where nine sites

were visited and samples, pictures and GPS readings were taken.

Peter's notes are attached as Appendix C.

Bedrock Geology Brunette Claim Group Clara and Maria Townships

The Brunette Claims in Clara and Maria townships are located within the Central Gneiss Belt in the Grenville Province in southeastern Ontario. There is little known about the bedrock geology in this part of the CGB.

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Excerpt CLAIM Map Clara and Maria Townships showing location of Brunette Claim group

Excerpt Preliminary Map P.1197 Showing Bedrock Geology of Brunette Claim Group

There is no detailed bedrock geological mapping available for either Clara or Maria townships. There is no docmnented previous exploration or assessment work completed in the area of the claim group. In the mid 1970's, the Ontario Geological Survey compiled a geological map for the Mattawa-Nipissing Area based largely on airborne magnetic surveys completed in the 1950's.

Ontario Department of Mines, Annual Report for 1925 reports on a past producing feldspar producer located to the southwest of the claim group near Waterloo Lake. This is the only documented Mineral Occurrence in Clara Township. The report of that operation is as follows:

"Duncan Dewar and W H. Gibson of Pembroke opened a feldspar quarry three miles from Aylen siding, on the C.P.R., jive miles east of Deux Rivieres in March, I925. Ten men were employed, and a 35-ton car was shipped to the New York Feldspar Company, and operations for the summer ceased as there was no wagon road to the property. The quarry is located on E. 0. I, I 00, north half lot 28, concession VL Clara Township, and is said to be in a 30-foot pegmatite dike uncovered for 300 feet."

There is no modern airborne geophysical data available for the area. As shown in the attached excerpt from Map 1197, the claim area is thought to be underlain by migmatitic biotite gneiss (Unit la). The map also indicates that massive granitic pegmatite dikes may also occur in the claim area. The compilation map shows a pronounced northwest gneissosity.

Bedrock samples examined by the staff of the Southern Ontario Resident Geologist's office in December 2011 confirm that in very general terms this interpretation is accurate.

Detailed mapping and sampling of the property will be necessary to provide a more complete picture of the bedrock geology.

References:

MAP P.1197 GEOLOGICAL MAP MATTAWA-DEEP RIVER AREA (EASTERN HALF) DISTRICT OF NIPISSING AND COUNTY OF RENFREW Scale: 1:63,360 NTS Reference: 31 K/3W, 4; 31 L/1E, SE

ODM-GSC Aeromagnetic Maps: 1437G, 1447G, 1457G, 145BG, ODM 1976

Exploration was focused on the potential for industrial grade garnets located within the gneissic host rocks; however, graphite and pegrnatites were also of interest.

1.2. REGIONAL GEOLOGY

The NRM claims are located within the Central Gneiss Belt of Ontario. The region

. has undergone metamorphism to the upper Figure 2 Mixed conifers in the NRM claims area. amphibolite facies (600- 700 °C). The most

recent mapping of the area was conducted in 1976 by the Ontario Division of Mines (ODM) at a scale of 1:63,360. The entire region of interest was described by the ODM as

"Medium-grained, impure sandstone (biotite- K-feldspar- quartz- plagioclase gneiss) veined by ten percent or more of quartzo-feldspathic material; minor to locally abundant intercalated arkose; biotite-rich argillite (dark grey, fine-grained, garnetiferous, biotite­feldspar- quartz gneiss and feldspar".

The ODM also reported massive granitic dikes in the northern claims region and glacial-alluvial quaternary overburden in the southern claims region. The structure was reported to be a generat NW to SE strike with the compositional layering dipping to the northeast (ODM, 1976).

Historic mineral occurrences include a small artisanal K-feldspar mine in a pegmatite dike located to the southeast of the claims region in Clara Township. Current mineral occurrences include the Bisset Creek Mine, which is mined for graphite in a metamorphosed graywacke, 30 km to the southeast (Bisset Creek Graphite Technical Report, 2010).

The most recent geophysical survey conducted in the region was an aeromagnetic survey conducted in 1959- 1960 by the Geological Survey of Canada at a scale of 1 :63,360 (GSC, 1960). Only one major anomaly is observed in the NMR claims. It is a circular, magnetic low in the northern region in which the majority of the anomaly was encompassed by claim 1500219.

1.3. LOCAL GEOLOGY

1.3.1. Geologic Map

See Appendix A 1.3.2. Rock Units

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Unit 1 (light green) is found in the southwest comer of the mapping area and provided the stratigraphy is upright, the lowest unit in the mapped stratigraphic sequence. Unit 1 is a quartzo­feldspathic gneiss containing quartz, potassium feldspar (K-feldspar), black amphiboles and biotite. The crystals of all the minerals are 1-3 mm in size and demonstrate good gneissosity. The unit weathers to a gray-pink.

Unit 2 (blue line) is hosted within Unit 1 and has sharp contacts with Unit 1. It consists of a metasedimentary greywacke dominated by quartz with minor amounts of muscovite, biotite, and flaky graphite (up to 15%). This unit ranges in thickness from 10 em to over 1 m. Unit 2 is friable, breaking apart easily. It weathers tan to buff and weathers readily compared to the surrounding gneisses.

Unit 3 (pink) lies above Unit 1 and is gametiferous quartzo-feldspathic gneiss composed of quartz, K-feldspar, amphibole, biotite, and garnet. The minerals are predominantly 1-3 mm in size; however, the garnets range in size from 3-5 mm and make up about 10% ofthe rock unit by volume. Smallleucosomes dominated by K-feldspar crystal about 10 mm in size were observed. Unit 3 weathers grey.

Unit 4 (blue-gray) sits on top of Unit 3. It is a quartzo-feldspathic gneiss very similar to Unit 1 with respect to crystal size and composition. It also contains minor garnets (1-3%) about 2 mm in diameter that were observed in the more mafic layers of the gneiss. This unit weathers gray to pink.

Unit 5 (orange) is a well-indurated, black and white gneiss (Fig. 3). It is composed mainly of

Figure 3 Black gneiss containing amphiboles and minor amounts of biotite. Red unit is composed almost entirely of garnet.

3

quartz, amphibole, plagioclase, and biotite. The crystal size is fairly homogenous throughout the unit at about 1 mm in size. Localized migmatites contained quartz and minor white feldspar crystals up to 15 mm in size. Unit 5 contains more mafic minerals (amphiboles, biotite,± plagioclase) than the other units in the NRM claims area. Garnets were observed in Unit 5 in a few localized zones only a meter long and 15 em wide (Fig. 3). The zones were dominated by garnets 1-3 mm in size. Unit 5 weathers grey to black.

Unit 6 (red; Fig. 4) is a white plagioclase-rich garnet gneiss. The feldspars and quartz crystals range in size from 0.1 to 1 mm. Biotite and amphibole are found in Unit 6 as well, ranging in size from 0.1 to 0.5 mm. Unit 6 contains an average of 10- 15 % garnets with sizes typically ranging from 3 to 10 mm in diameter. Small joints and fractures were observed striking 050 NE and dipping 90°. The amount of garnets in this unit drops to roughly 5% as towards the southeast along strike. A small, possible quartz pegmatite may be present in Unit 6; however the unit was not mapable for more than a few meters indicating that it may be a leucosome. Unit 6 weathers white to gray, and it has an irregular contact with Unit 7 (Fig. 5).

Figure 4 Garnet-bearing, plagioclase-rich gneiss (Unit 6).

Figure 5 Contact between Unit 6 and Unit ·7.

4

Unit 7 (yellow; Fig. 6) is a quartzo-feldspathic gneiss composed of quartz, K-feldspar, amphiboles, biotite, and garnet. The rock-forming minerals range from 0.5 to 7 mm in size. Local zones ofK-feldspar migmatites, approximately 10 em thick, were observed. The garnets in Unit 7 make up 1-3% ofthe rock by volume, but can be 5-10 mm in diameter. Zones composed predominantly of biotite and amphibole, roughly 2m thick were also observed (Fig. 7). Unit 7 extends to the northeast of the mapping area to the north of the Township Line Lake and tends to weather pink.

Unit 8 (blue) is a garnet amphibolite hosted within Unit 7. The rock contains up to 30% garnets; however, this decreases to 10% on the northeastern side ofthe unit. The garnets are 3 to 5 mm in diameter on average. Unit 8 is very friable and weathers to a brown, garnet-bearing soi I in low areas. A small quartz­biotite pegmatite, less than 1 m wide (Fig. 8), cross-cuts the garnet amphibolite and contains an

Figure 6 Quartzo-feldspathic gneiss (Unit 7) with K-feldspar leucosome. unknown acicular, black mineral that

is 2 em wide and over 5 em long. This quartz pegmatite may be related to the quartz leucosome found in Unit 6. The unknown black mineral has a greenish-gray streak, good cleavage, and a resinous to vitreous luster.

1.3.3. Strncture and Geophysics Analysis

Based on field observations, the geologic map, and the A- A' cross-section (Appendix B), the overall structure ofNorthem Resource Measurement's claims consists of a regional strike of290 to 320 and a dip of20° to 40° NE. These observations are in agreement with those observed by the ODM. On local scale, one synform, trending NW- SE was observed in the northwest comer ofUnit 5. A synform­antiform- synform complex was observed in the

5

-Figure 7 Quartz pegmatite with unknown acicular, black mineral.

D. List Of Claims

Clara Township 3003234 Ground Staked 4 units

1192289 Ground Staked 8 units

Maria Township 1500216 Map Staked 2 units

1500219 Map staked 2 units

1500220 Map Staked 2 units

1500230 Map Staked 2 units

1500231 Map Staked 2 units

1500353 Map Staked 2 units

1500354 Map Staked 2 units

1500355 Map Staked 2 units

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The above claims were staked in the fall of 2011 and spring 2012 by

Claimholders:

Robert A. Brunette Licence# C38830 Client# 392757

Eric Y Boudreau Licence# 1005160 Client# 404908

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A. Project Location Clara/Maria Townships

Renfrew Registry Division

Southern Ontario Mining Division

MNR Pembroke District

Clara and Maria Claim Maps

UTM 4612 38 N 0781008 W

B.Location Maps rEi!--Ciaim maps OGS "Claim Mapsn F.Z(;ul(.e ~,

~a" 2 Pr~posed""Strtpping and mg

Ma~ -location map FI~fi~e '!-Note: See resident Geologist comments re geological mapping section F.

C. Property Access The property is located approximately 25 km west of Stonecliffe, Ontario

south of highway 17.

The property is accessed by taking the Bissett Creek road south for 5 km

then turning west on the Waterloo lake road for 7.3 km. Then north West

on the Rattail Lake road 4 km to the Gardner lake road then north 5 km

where you will see to the east Post #3 for claim# 3003234 and Post# 2 for

claim# 1192289. Proceed another 1 km north to the proposed stripping/

sampling area.

Copyuptlt R.1rwt tkN.111y Canada Inc.

testing to determine quality is under way. We have a verbal opinion

from Bob Komarechka, Sudbury (Geologist) that we have inclusions in

some of our garnets. (On Line photo interpretation.)

Mining conditions: Both access to the area and its' proximity to

markets are good. (To North Bay to Sudbury to Toronto) There is all

weather road access right into the claim group. As well, a rail line and

siding are within 25 km by existing bush road and highway 17. If

desirable and funding available a new road of 1.5 km to the north

would access the rail line, hydro line and natural gas line. The claim

area has no parks or special cautions or liens. A waterway park around

Rattail and Waterloo lakes follows the Bissett creek to Highway 17 but

does not impact the claim group or access. The northern boundary of

Algonquin Park lies approximately 12 km south of the claim group and

will not be a factor.

The Algonquin Nation is in land claim negotiations with the Provincial

and Federal Governments. The claim area is part of the land claim but

no mining exclusions are in place. As a member of the Algonquins of

Greater Golden Lake community it is my intention to involve the band

and the greater nation in this project to the extent possible. Definite

benefits from royalties and employment opportunities can accrue to

my nation as this process moves forward.

Mining and Milling: Some parts of the garnet bearing host rock will be

readily mined on the surface using tracked front end loaders (see

picture A original submission) Other parts will require more traditional

open pit hard rock mining methods i.e. drill and blast. The extent to

which either will apply can only be determined as we move forwa .

The garnets are found in~ varying host rock conditions. Some are in

Mining Assessment work 2

Project Description:

During the fall of 2011 and winter/spring of 2012 Mr. Brunette and Mr.

Boudreau carried out traditional prospecting and sampling on their

claims in Maria and Clara townships. A total of 24 man days were spent

prospecting, sampling, doing sample review and preparation and

mapping. In addition Aboriginal consultation with the Algonquins of

Ontario at their Pembroke consultation office, took two man days with

preparation counting for another (not claimed at this time). The report

preparation added two man days.

Twenty three samples were collected with some being analysed and

others merely identified and retained. Location of samples is shown on

attached map figure 3.

Two trucks, two four wheelers, chainsaw and camp facilities were used

repeatedly as well as two snowmobiles on two occasions. Sample

numbers and disposition are attached as Appendix A and sample

analysis results are attached as Appendix B. We have included a series

of photographs showing mineralization of garnets and graphite on the

claim group Appendix D.

It should be noted that an OEC project was applied for and approved

for the claim group. It is well under way and will be reported for .

assessment work upon completion. The prospecting carried out above

allowed us to target areas in the OEC project for stripping and further

sampling as well as identifying a need for better geological mapping of

the area. It also put us in a position to ppen discussions with two

industrial mineral companies.

. Further work will be suggested as a result of the completion of the OEC

project and acted upon accordingly. The above prospecting I consulting

work was carried out, October 30,31, November 16, December 2,6,8

· 2011 and February 3, March 9, April12,13,14,15,16,17,18, 19,and

30.May land 5, and Junel, 2012.

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Bell Mail Print Message e. Page 1 of2

Mineral identification

-From: Johanne Robin (JRobin@mus-nature.ca)

Sent: Thu 1/19/12 3:53 PM To: andrea.brunette2@sympatico.ca (andrea.brunette2@sympatico.ca) RECEtVED

Hello Mr. Brunette, JU\ ·~ ·, tif r~ ·~ z

GEOSCIENCE ASSEStMF..NT OF~ i CE

Your specimen have been identified by Mr. Michel Picard our specialist of our mineral collection at the

museum.

1 piece is a biotite garnet gneiss,

and 3 pieces are amphibole garnet gneiss.

1 pr~ces have less than 1% almandine garnet, lpi-ece has about 10%almandine garnets and 1 piece has about 20% almandine garnets.

I would like to know how you would like to have your specimens back:

If you have a membership ,I can leave them in the discovery zone with the public inquiries and you can come to pick them up from Tuesday to Friday from lpm to 4:30pm,and during the weekend from 9:30 am to 4:30pm.

OR

I can leave the specimens at the front desk, but I need to know a few days in advance a date on which you would come to pick It up. I will leave an envelope under your name.

OR

I can mail them to you: (verify the information and I would need your postal code)

Mr. Robert Brunette

2 Bon Echo Cr.

Kanata, On

Have a nice day, and I hope to read you soon .

http://bll60w.blu160.mail.live.com/mail/PrintMessages.aspx?cpids=b2dd2129-42b5-11 e... 20/01/2012

To :

Robert Brunette and Matthew Boudreau

Your specimens were sent to Mr. Michel Picard, our Museums' Mineral Collection Manager.

And this is the information he sent me:

Only presence of:

-Black mica (probably biotite)

-Smoky quartz

-Pink feldspar (Microcline)

There is no albite, no beryl and no corundum .

This is indeed a pegmatite .

There was a pegmatite quarried for feldspar in the Kanata area that operated from 1919 to 1921.1twas

called the South March Qua rry. It is now in a housing development in Kanata . It was probably located

close to the intersection of Kanata ave. E. Goulbourn forced road. Other minerals you could expect to

see would be : black tourmaline, hematite, magnetite, minor uraninite, calcite fluorite .

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EXPLORING HEAVY MINERALS

October 17,2011

Mr. Bob Brunette Tel: 613 220 3265

Dear: Mr. Bob Brunette

Re: Rock Sample Number 76553

As requested we examined the garnet bearing rock sample you submitted earlier this month. The rock is a gneiss containing an estimated 10% coarse (2 to 8 mm) garnet phenocryst. The garnet grains are very fractured thus have no gem value.

We confirmed by SEM that the garnet grains are almandine.

Please call me if you have any questions.

$\d:~ Remy Huneault, Laboratory Manager

Overburden Drilling Management Limited 1 07-15 Capella Court

Ottawa, ON Canada K2E 7X1 Tel. 613-226-1771 Fax. 613-226-8753

odm@storm.ca

EXPLORING HEAVY MINERALS

January 31st ,2012

Mr. Bob Brunette 2 Bon Echo Cres. Kanata, ON K2M 2W5 Tel: 613 254 8534 Cell: 613 220 3265

Dear: Mr. Bob Brunette

Re: Rock Sample Number 76561

As requested we examined the hornblende/garnet bearing rock sample you submitted earlier this month. The rock is a coarse grain (grain size up to 8 mm) hornblende gneiss containing an estimated 20% almandine garnet (0.5 to 2 mm) and 5% chlorite. We did not see any graphite in the sample.

We confirmed by SEM that the garnet grains are almandine.

Please call me if you have any questions.

Remy Huneault, Laboratory Manager

Overburden Drilling Management Limited 107-15 Capella Court

Ottawa, ON Canada K2E 7X1 Tel. 613-226-1771 Fax. 613-226-87 53

odm@storm.ca

EXPLORING HEAVY MINERALS

April 51h ,2012

Mr. Bob Brunette 2 Bon Echo Cres. Kanata , ON K2M 2W5 Tel: 613 254 8534 Cell: 613 220 3265

Dear: Mr. Bob Brunette

Re: Rock Samples Number 76571

As requested we examined the two rock samples and two pea size grains you submitted earlier this month . The two rocks are migmatite. Migmatite is a heterogeneous silicate rock consisting of alternating light-coloured minerals (quartz and feldspar) and dark-coloured minerals (amphibole and biotite) . The heterogeneous nature of migmatites occurs on a wide range of scales thus may not be observable in a single outcrop.

The black hand size piece consist mainly of biotite, quartz with minor plagioclase. The large (up to 1 em ) glassy crystals you can see in the rock are all quartz (SEM confirmed) .

The pale pinkish piece consist mainly of K-spar and quartz. The pale pink grains are k-spar (SEM confirmed) and the pink orange grains are K-spar stained with iron oxide (SEM confirmed) . We did not see any rare earth minerals.

The two gray green pea size grains consist of a mixture of k-spar, sericite and iron oxide.

Please call me if you have any questions.

Yours sincerely,

%.yH~~ Laboratory Manager

Overburden Drilling Management Limited 107-15 Capella Court

Ottawa, ON Canada K2E 7X1 Tel. 613-226-1771 Fax. 613-226-8753

odm@storm.ca

EXPLORING HEA W MINERALS

May 141h ,2012

Mr. Bob Brunette 2 Bon Echo Cres. Kanata, ON K2M 2W5 Tel: 613 254 8534 Cell: 613 220 3265

Dear: Mr. Bob Brunette

---------

Re: Two Rock Samples (0716807/5120570 and 0718374/5121114)

As requested we examined the two rocks you submitted last week.

The pegmatitic rock you identified as qtz pegmatite contains coarse (up to 1 em) wide hornblende crystals (SEM confirmed). The rock also contains patches of coarse biotite. The big crystals present in this samples are not allanite nor tourmaline.

The fine to medium grain rock you identified as graphite gneiss is indeed a graphite bearing metamorphose rock. The original rock was likely a siltstone. The graphite (SEM confirmed) is present as disseminated flakes which can be found up to 2 rnm in size. Breakage of the rock preferentially occurs along the fabric of the rock where the graphite is most obvious giving the impression the rock contains a lot more graphite than it really does. The actual total graphite in the rock is estimated to be only 1 to 3 %.

Please call me if you have any questions.

Yours sincerely,

~L~ Remy Huneault, Laboratory Manager

Overburden Drilling Management Limited 107-15 Capella Court

Ottawa, ON Canada K2E 7X1 Tel. 613-226-1771 Fax. 613-226-8753

odm@storm.ca

Semi-Quantitative X-Ray Diffraction

Report Prepared for: Opta Minerals

Project Number/ LIMS No. M/5060-DEC11

Reporting Date:

Instrument:

Test Conditions:

Interpretations :

Detection Limit:

Contents:

February 17, 2012

BRUKER AXS D8 Advance Diffractometer

Co radiation, 40 kV, 35 mA Regular Scanning: Step: 0.02°, Step time:0.2s, 28 range 3-70°

PDF2/PDF4 powder diffraction databases issued by the International Center for Diffraction Data (ICDD). DiffracPius Eva software.

0.5-2%. Strongly dependent on crystallinity.

1) Method Summary 2) Summary of Mineral Asemblages 3) Semi-Quantitative XRD Results 4) Chemical Balance(s) 5) XRD Pattern(s)

Senior Mineralogist

SGS Minerals P 0 Box 4300, 185 Concession Street, Lakefield, Ontario, Canada KOL 2HO

a division of SGS Canada Inc. Tel 705) 652-2000 Fax: (705) 652-6365

Method Summary

Mineral Identification and Interpretation:

Mineral identification and interpretation involve matching the diffraction pattern of a test sample material to patterns of single-phase reference materials. The reference patterns are compiled by the Joint Committee on Powder Diffraction Standards - International Center for Diffraction Data (JCPDS-ICDD) and released on software as a database of Powder Diffraction Files (PDF)

Interpretations do not reflect the presence of non-crystalline and/or amorphous compounds. Mineral proportions are based on relative peak heights and may be strongly influenced by crystallinity, structural group or preferred orientations. Interpretations and relative proportions should be accompanied by supporting petrographic and geochemical data (Whole Rock Analysis, Inductively Coupled Plasma - Optical Emission Spectroscopy, etc.).

Semi-Quantitative Analysis:

The Semi-Quantitative analysis (RIR method) is performed based on each mineral's relative peak heights and of their respective 1/lcor values, which are available from the PDF database. Mineral abundances for the bulk sample (in weight%) are generated by Bruker-EVA Software. These data are reconciled with a bulk chemistry (e.g. whole rock analysis including Si02 , Al20 3 , Na20, K20, CaO, MgO, Fe20 3 , Cr20 3 , MnO, Ti0 2 , P20 5 , V20 5

or other chemical data). A chemical balance table shows the difference between the assay results and elemental concentrations determined by XRD.

SGS Minerals P.O. Box 4300, 185 Concession Street. Lakefield, Ontario. Canada KOL 2HO

a division of SGS Canada Inc. Tel: (705) 652-2000 Fax: (705) 652-6365

Member of the SGS Group (SGS SA)

Summary of Semi-Quantitative X-ray Diffraction Results

Crystalline Mineral Assemblaqe (relative pro Jortions based on peak heiqht) Sample Major Moderate Minor

(>30% Wt) (10% -30% Wt) (2% -10%Wt)

65901 plagioclase, quartz, topaz, pyroxene,

potassium--feldspar mica, gamet,

amphibole

• tenta!Jve JdenllficatJon due to low concentrahons, diffraction !me overlap or poor crystai!Jmty

Mineral Composition

Amphibole (Na,K)Ca2(Fe,Mg)5(AI,Si)80 22(0H)2

Pyroxene (Ca,Na)(Mg,Fe,AJ,Ti)(Si,Ai)206

Garnet (Ca,Mg,Mn2'h(V.Ai, Fe3')2(Si04h

Ilmenite FeTi03

Mica K(Mg, Fe )AI2Si3AI01 0(0Hh

Plagioclase (NaSi,CaAI)AISi20 8

Potassium-Feldspar KAISi30 8

Quartz Si02

Topaz AI2Si04(F,0Hh

Client Name 12XXX-001/MIXXXX-JAN09

05/08/2009

Trace

(<2% Wt)

*ilmenite

The Qualitaove XRO method (METH # 8-8-1) used by SGS Minerals Services, P 0. Box 4300, 185 Concession Street, Lakefield, Ontatio, Canada KOL 2HO Tel. (705) 652-2000 Fax: (705) 652-6365 Mini-method available upon request

Semi-Quantitative X-ray Diffraction Results

Mineral 65901

(wt%)

Quartz 25.5

Grossular 0.5

Spessartine 3.3

Almandine 0.9

Muscovite 4.5

Biotite 5.0

Ilmenite 1.2

Topaz 6.7

Esseneite 6.5

Albite 26.6

Orthoclase 16.1

Actinolite 3.2

TOTAL 100.0

Client Name 12XXX-001/MIXXXX-JAN09

05/08/2009

The Qualitative XRD method (METH # 8-8-1) used by SGS Minerals Services, P 0. Box 4300, 185 Concession Street, Lakefield. Ontario, Canada KOL 2HO. Tel. (705) 652-2000 Fax : (705) 652-6365 Mini-method available upon request.

2000

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Client Name 12XXX-001/M IXXXX-JAN09

0510812009

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2-Theta - Scale ~65901 -File Dec5060-1.raw- Type 2Th/Th locked- Start: 6.034 "-End· 70.034"- Step: 0.

0001 -079-1910 (C)- Quartz- S102

000 1-087-1718 (C)- Grossular, syn- Ca3AI2(S104)3

~01-074-1554 (C)- Spessarttne- (MnFe)3(AI199Fe.01)Si3012

01-074-1553 (C)- Almandine- (Fe2 59Mg.27Ca 13Mn.01)A11 98(Si04)3

§ 01-084-1304 (C)- Muscovite- KAI3SI3010(0H)2

00 01-080-1108 (C)- B10t1te- KFeMg2(AISi3010)(0H)2

[ill o 1-075-1208 (C)- llmen<te, syn- FeTi03

lEoo-012-0765 (•)- Topaz- AI2Si04(F,OH)2

C!J oo-025-0143 (I)- Essene1te, syn- Ca(Fe1.4AI0.6)Si06

(!]o 1-084-0752 (C)- Albite low- Na0.9Ca0.1AI(Si308)

~01-086-0437 (C)- Orthoclase- K(AISi308)

~00-025-0157 (D)- Actinolite- Ca2(Mg,Fe+2)5S<8022(0H)2

The Qualitative XRD method (METH # 8-8-1) used by SGS Minerals Services, P.O. Box 4300, 185 Concession Street, Lakefield, Ontario, Canada KOL 2HO. Tel: (705) 652-2000 Fax. (705) 652-6365 Mini-method available upon request.

70

SG$ SGS Canada Inc. P.O. Box 4300- 185 Concession St. Lakefield - Ontario - KOL 2HO Phone: 705-652-2000 FAX: 705-652-6365

LR Internal Dept 14 Attn : Bernie Yeung

Phone: Fax:---

January 6, 2012

Date Rec.: LR Report: Project: Client Ref:

04 January 2012 CA021 03-JAN 12 Custom Mineralogy M15060-dec11

CERTIFICATE OF ANALYSIS

Final Report

Sample ID Si02 Al203 Fe203 MgO CaO Na20 K20 Ti02 P205 MnO Cr203 V205 %

LOI %

Sum % % % % % % % % % % % %

1:65901 64.6 14.5 7.63 1.03 3.14 3.06 4.33 0.99 0.37 0.14 < 0.01 < 0.01 0.28 100.1

oL~ G9zd Tom Watt Project Coordinator

Page 1 of 1 This document IS ISSued by the Company under Its General Cond1t 1005 of Service accessible at http ://www.sgs.com/rerms_.md condit1ons.htm . Attention is drawn to the lim itation of !\ability, Indemnifica tion and jurisdiction 1ssues defined thcrctn. WARNING : TIH! sample(s ) w which the findings recorded herein (the 'Rndings' ) relate was (were ) drawn and 1 or pro vided by the Client or by a third party acting at t he Client's dt rcalon. The Flndlngs

constit ute no warranty o f the sample's re prescntat!vlty or the goods and strictly relate to [ he sam p le{s). The Company accepts no liability wit·h regard to the ongin or source from which the samplc(s ) Is/are sa id t o be e xtracted . The Find ings report on the sam ples provided by the client and arc not Intended fo r commercial or contractual settlement purposes. Any unauthorized alteration, forgery or falsification of th e content or appea\'1\ncc

of this docurnent 1s unlawful and orr enders may be prosecuted to the fullest extent of the taw. f csl method "'!ormation avtf1lablc upon reQuest .

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Ministry of · Northern Development and Mines

Date: 2012-AUG-08

Mln!stere du Developpement du Nord et des Mines

ROBERT ANTHOI\IY BRUNETTE 2 BON ECHO CRES

OTI AWA, ONTARIO IPiRffiiiilli~~~~--. K2M 2W5 CANADI PROVINCIAL RECORDING

ROFFICE- SUDBURY ECEIVED

AUG 2 0 £011.

Dear Sir or Madam A.M. - P.M.

Subject: 45-Day Notice

®Ontario GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 3rd FLOOR SUDBURY, ONTARIO P3E 6B5

Tel: (888) 415-9845 Fax:(877) 670-1555

Submission Number: 2.52183 Transaction Number(s): W1290.01653

Please respond to this notice by: 2012-SEP-22

We have reviewed your Assessment Work Submission with the above noted Transaction Number(s). The summary below outlines the reasons for this notice and, if possible, steps you can take to address this notice. If deficiencies are not corrected within this 45-day period, assessment work credit may be rejected or reduced.

Required revisions must be submitted to our office by 2012-Sep-22. If a verification of expenses is requested, only one copy of the documentation is required.

Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 day period, otherwise the credit will be distributed as outlined in Section #7 of the Declaration of Assessment Work form accompanying the submission.

Transaction Number

W1290.01653

First Claim Number

1500216

First Claim's Township

MARIA

Regulation:the work report is not accompanied by adequate technical support data as required by this Regulation;

This prospecting submission requires some revisions. Field notes are useful, however a detailed daily log is required for this work program. Also, traverse maps at a scale within the regulation (no more than 1 :5000),

indicating the date and location of all traverses and samples are needed.

If you have any question regarding this correspondence, please contact SOPHIE FORTIN by email at sophie.fortin@ontario.ca or by phone at (705) 670-5858.

"--~""Y'fJenomme

----5enior Manager, Mining Lands Section

Cc:

Robert Anthony Brunette (Claim Holder)

Robert Anthony Brunette (Assessment Office)

Visit our webstte at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:33899

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