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GEOLOGICA GROUPE-CONSEIL
ROGUE RESOURCES INC.
2016 FIELD WORK REPORT ON THE
SILICON RIDGE
SILICA PROPERTY
Charlevoix Regional County Municipality Quebec, Canada
NTS. 21M/15 UTM Z19 381350E — 5294350mN
Val-d'Or, Québec Alain-Jean Beauregard, P.Geo., OGQ (#227), FGAC March 31st, 2016 Daniel Gaudreault, Eng., OIQ (# 39834) Géologica Groupe-Conseil Inc.
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Suite 202, 450, 3e Avenue, Val-d'or (Québec) C.P. 1891, Canada J9P 6C5 Tél. : (819) 825-8643 fax : 824-4266 [email protected] www.geologica.qc.ca
1579591 G]ÉO]LOGtCA GROUPE-CONSEIL
SIGNATURE
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY
Prepared for
ROGUE RESOURCES INC. Suite 2270, 1055 West Georgia Street Royal Centre, P.O. Box 11144 Vancouver, BC Canada V6E 3P3
Signed in Val-d'Or, March 31st, 2016
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Alain-Jean Beauregard, P.Geo., OGQ (#227), FGAC
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Daniel Gaudreault, Eng., 010 (# 39834)
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page 2 G]ÉO]LOGICA G O1J]P]EeCONS]E11.
Certificate of Qualification (Alain-Jean Beauregard)
I, Alain Jean Beauregard, P. Geo., do hereby certify that:
1. I am a geologist and the President of: Geologica Groupe-Conseil Inc. 3rd 450, Avenue, Suite 202, P.O. Box 1891, Val-d'Or (Québec), J9P 6C5 2. I am a qualified geologist, having received my academic training at Concordia University, in Montréal, Québec (B.Sc. Geology and Mining —1978) with an attestation in Business Administration (Val-d'Or— 1988). 3. This certificate applies to the Technical Report entitled "2016 Field Work Report on the Silicon Ridge Silica Property" (the "Technical Report"). This report was written for Rogue Resources Inc. and dated March 31ST, 2016. 4. I am a Fellow of the Geological Association of Canada #F4951 (FGAC) and also a member of the Order of Geologists and Geophysicists of Québec #227 (OGQ), of the Québec Mining Exploration Association (AEMQ), of the Canadian Institute of Mining and Metallurgy (CIMM) and the Prospectors and Developers Association of Canada (PDAC). 5. I have field experience mapping, prospecting, sampling and compiling data in the highly metamorphic terrain of the Grenville Province for iron, titanium, uranium, rare earth minerals, graphite, precious and base metals. I have worked as a geologist for a total of 37 years since my graduation from University with the production of more than one thousand and five hundred (>1500) technical and financial evaluation reports in English or French for government authorities, private and public companies including numerous market value assessments of mining properties from grassroots projects to developed mines, and several companies' entire portfolio of properties. I have also organized and managed many exploration campaigns for gold, base metals and industrial metals, especially in remote areas of Abitibi, but also in other parts of Québec (Labrador Trough, Gaspé Peninsula, James Bay, St-Lawrence River, North Shore, Ungava, etc.), in eastern Canada, Europe, Africa and the Americas. 6. I have read the definition of "qualified person" set out in National Instrument 43-101 ("NI 43-101") and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of NI 43-101. 7. I am responsible for the technical parts of Items 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 23, 24, 25, 26 and 27 of the Technical Report. I have visited the subject property from June 9 to July 5, 2015. 8. I am not aware of any material fact or material change with respect to the subject matter of the Technical Report that is not reflected in the Technical Report, the omission to disclose which makes the Technical Report misleading. 9. I had no prior involvement with the property that is subject of the Technical Report. 10. I am independent of the issuers (Rogue Resources Inc.) applying all of the tests in section 1.5 of National Instrument 43-101. 11. I consent to the filing of the Technical Report with any stock exchange and other regulatory authorities and any publication by them, including electronic publication in the public company files on their websites accessible by the public, of the Technical Report. I confirm to have read 43-101 F1 form and related appendices and that the Technical Report has been prepared in compliance with the National Instrument 43-101. I consent to the use of extracts from, or a summary of, the technical report in the document. I confirm to have read the document and that it accurately represents the information in the technical report.
Dated this 31ST day of March, 2016
Alain-Jean Beauregard, P.Geo., OGQ (#227), FGAC
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Curriculum Vitae (Alain-Jean Beauregard)
KEY EXPERIENCE
Sound knowledge of geological sciences associated with extended experience in property management.
Involvement with the evaluation, management and realization of several mining exploration and development properties. Production of nearly 1,500 technical and financial evaluation reports in English or French for government authorities and private companies including numerous market value assessments of mining properties from grassroots properties to developed mines, and several companies' entire portfolio of properties.
Organization and management of many exploration campaigns for gold, base metals and industrial minerals, especially in remote areas of Abitibi, but also in other parts of Québec (Gaspé Peninsula, Gatineau, St-Lawrence River ("Lowlands"), North Shore, James Bay, etc.), in eastern Canada, Europe, Africa and the Americas.
Very good knowledge of Latin American and African countries. Excellent communication and mediation skills as well as sound administration practice.
INTERNATIONAL MANDATES
South America - Peru - 2000-2016 - Property Evaluation for Dynacor Gold Mines.
Europe —2002 to 2003 — Drill Program Supervision and Property Evaluation for C2C in Spain and Portugal.
East Africa - September 1994 - Evaluation of mining properties in Tanzania, Kenya, Ethiopia and Erythrea for Pangea Goldfields and Ressources KWG Inc., EAG Inc.
United Arab Emirates - June 1994 - Off-shore and on-shore oil and gaz property evaluations. Geoscientific compilations in order to define potential prospective areas for chromite within the ophiolite belt of Semail.
West Africa (Based out of London, U.K.) - 1994 - Evaluation of mining properties in Mauritania, Niger, Mali, Burkina Faso, Ivory Coast and Ghana for Placer International Exploration and Placer Outokumpu Exploration Ltd.
Morocco - November 1992 to April 1993 - Compilation of the Anti-Atlas in Morocco, in north-western Africa (180 km2) at the scale of 1:100 000. A detailed report of the Guemassa area (Douar El Ajar VMS deposit) was also completed. Ref. Mr. Garth Wilson, Placer Outokumpu Ltd., London.
Argentina - April-May 1991- Mission in the WNW Andes to evaluate properties for potential gold and base metal deposits: the Cerro Castillo Gold deposit, the Baja de Alumbrera Porphyry Copper deposit, the Farallon Negro Epithermal Gold-Manganese deposit.
Republic of Guyana - March 1991 - Evaluation of an alluvial diamond and gold deposit located on the Mazaruni River in the Roraima Formation, 300 km south of Georgetown.
CANADIAN EXPERIENCE
-Founder, shareholder, director and administrator of Geologica Groupe-Conseil Inc., Val d'Or, (Québec) since 1985 - Management, property supervision, property evaluations, geoscientific compilations at the national and international level.
-Mining Geologist, Les Mines Sigma of Placer Dome Inc., Val d'Or (Québec), 1981-1985 - Property geologist, geological and geochemical surveys, drilling supervision, grade verification and reserve estimates.
-Project Director and Geologist, Serem Ltée, Val d'Or (Québec), 1977-1981 - Geological and geochemical surveys, supervision of geophysical surveys (Mag, EMH and IP), drill program supervision.
-Assistant Geologist, Serem Ltée, Val d'Or (Québec), 1975, under the supervision of Mr. Paul Girard Ph.D and Mr. Ray Goldie Ph.D and for Hollinger North Shore and Labrador Exploration, Eastern Townships and Gaspesia, 1974 -Exploration for base metals and uranium.
-Over the past 36 years, Geologica was the key lead and instrumental geological consulting group in the discovery of significant precious and base metals occurrences, mineralized zones and deposits of Abitibi : 2008-2016: Integra Gold Corp Lamaque South Property - Triangle Deposit Discovery (drill definition program and resources calculation), 1981-1993: Nyrstar Mine Langlois VMS Deposit Discovery (drill program supervision and resources calculation), West Africa, Central and South America. Assisted and advised the founding members of SEMAFO on strategic gold property in West Africa between 1993- 1996.
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Certificate of Qualification (Daniel Gaudreault)
I, Daniel Gaudreault, Eng., do hereby certify that:
1. I am currently employed as a geological engineer by: Geologica Groupe-Conseil Inc. 3rd 450, Avenue, Suite 202, P.O. Box 1891, Val-d'Or (Québec), J9P 6C5 2. I graduated with a degree in Geological Engineering ("Eng.") from the University of Québec in Chicoutimi in 1983. 3. This certificate applies to the Technical Report entitled "2016 Field Work Report on the Silicon Ridge Silica Property" (the "Technical Report"). This report was written for Rogue Resources inc. and dated March 3e, 2016. 4. I am a member of the "Ordre des ingénieurs du Québec (OIQ)", #39834, of the Québec Mining Exploration Association (AEMQ) and the Prospectors and Developers Association of Canada (PDAC). 5. I have field experience mapping, prospecting, sampling and compiling data in the highly metamorphic terrane of the Grenville Province for iron, titanium, uranium, rare earth minerals, graphite, precious and base metals. I have worked as a geologist for a total of 32 years since my graduation from university. As an engineer specializing in geology and mining, I have been involved with all aspects of planning, organization and supervision of mineral exploration projects, especially in remote areas of Abitibi, Québec. I have been in charge of teams of professionals and technicians on geological projects in the most severe conditions. I have also completed several geoscientific compilations and technical reports on areas of interest in Québec, Ontario, USA (California & Nevada) and South America (mainly Peru). 6. I have read the definition of "qualified person" set out in National Instrument 43-101 ("NI 43-101") and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of NI 43-101. 7. I am responsible for the technical parts of Items 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, 14, 23, 24, 25, 26 and 27 of the Technical Report. I have not visited the subject property. 8. I am not aware of any material fact or material change with respect to the subject matter of the Technical Report that is not reflected in the Technical Report, the omission to disclose which makes the Technical Report misleading. 9. I had no prior involvement with the property that is subject of the Technical Report. 10. I am independent of the issuer (Rogue Resources Inc.) applying all of the tests in section 1.5 of National Instrument 43-101. 11. I consent to the filing of the Technical Report with any stock exchange and other regulatory authorities and any publication by them, including electronic publication in the public company files on their websites accessible by the public, of the Technical Report. I confirm to have read 43-101 F1 form and related appendices and that the Technical Report has been prepared in compliance with the National Instrument 43-101. I consent to the use of extracts from, or a summary of, the technical report in the document. I confirm to have read the document and that it accurately represents the information in the technical report.
Dated this 31St day of March, 2016 ,~~ fn ~a ii~roc• ~~ +~i~ ~ `~Fo %
, ` DUiIf.L CJlDDREAUL .~ T $ / f C ~ 39é13.1 ~ a-~CLGL~~~u~ .~t~ c t_/ ~~QU(gEC ~yf~ 4/~imrr.yriill
Daniel Gaudreault, P.Eng (01Q #39834)
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Curriculum Vitae (Daniel Gaudreault)
KEY EXPERIENCE
An engineer specialized in geology and mining, I have been involved with all aspects of planning, organization and supervision of mineral exploration properties especially in remote areas of Abitibi, Québec. I have been in charge of teams of professionals and technicians on geological properties in the most severe conditions. I have also completed several geoscientific compilations on areas of interest in Québec and Ontario, have written several technical reports in the USA (Nevada and California) and also written geological surveys in Labrador (Newfoundland).
I have produced a great number of technical reports in both English and French for government authorities and private companies, such as property evaluations, exploration and environmental reports. I have also completed numerous market value assessments of mining properties from grassroots properties to developed mines.
WORK EXPERIENCE
2010-2016: Participated in the resources definition of the Triangle Deposit and fifteen (15) other mineralized zones of Integra Gold Corp Lamaque South property in Val-d'Or, Quebec, Canada.
Project Director, Geologica Groupe-Conseil Inc., Val d'Or (Québec), since 1985 - Project manager, planning, mapping, drilling supervision, due diligence, property evaluations, market value assessments, environmental reports, NI 43-101 Technical Reports, fieldwork reports.
Property Geologist, Boileau and Gauthier (Kiwatin) Val d'Or (Québec), 1985 — Project Supervision, Planning, mapping and sampling.
Property Geologist, Campbell Resources Ltd., Chibougamau (Québec), 1984-1985 - Project geologist, planning, drilling supervision, mapping.
Property Geologist, Boileau and Gauthier (Kiwatin) Val d'Or (Québec), 1983-1984 -Drilling program supervision, reports.
Property Geologist, Lac Minerals Ltd., Malartic (Québec), 1983 - Exploration campaign supervision, drilling program, mapping and reports.
Assistant Geologist, Lac Minerals Ltd., Val d'Or (Québec), 1982 and Ministry of Energy and Resources of Québec, Desmaraisville (Québec), 1981.
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TABLE OF CONTENTS SIGNATURE 2
CERTIFICATE OF QUALIFICATION (ALAIN-JEAN BEAUREGARD) 3 CURRICULUM VITAE (ALAIN-JEAN BEAUREGARD) 4 CERTIFICATE OF QUALIFICATION (DANIEL GAUDREAULT) 5 CURRICULUM VITAE (DANIEL GAUDREAULT) 6 1.0 SUMMARY 9 2.0 INTRODUCTION AND TERMS OF REFERENCE 11 3.0 RELIANCE ON OTHER EXPERTS 11 4.0 PROPERTY DESCRIPTION AND LOCATION 12
4.1 LOCATION AND CLAIMS 12 4.2 PROPERTY PURCHASE AGREEMENT 13 4.2 ENVIRONMENTAL OBLIGATION, PERMITS AND OTHER RELEVANT FACTORS 18 5.0 ACCESSIBILITY, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHYI8 6.0 PREVIOUS WORK 19 7.0 GEOLOGICAL SETTING AND MINERALIZATION 23
7.1 REGIONAL AND LOCAL GEOLOGY 23 7.2 LOCAL AND PROPERTY GEOLOGY 29 7.3 MINERALIZATION 30 8.0 DEPOSIT TYPES 33 9.0 EXPLORATION WORK 33
9.1 RECONNAISSANCE AND GEOLOGICAL MAPPING 33 10.0 DIAMOND DRILLING 37 11.0 PREPARATION, ANALYSIS AND SECURITY 37 12.0 MINERAL PROCESSING AND METALLURGICAL TESTING 37 13.0 MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES 37 14.0 ADJACENT PROPERTIES 37 15.0 OTHER RELEVANT DATA AND INFORMATION 40 16.0 INTERPRETATION, CONCEPT AND CONCLUSIONS 40 17.0 RECOMMENDATIONS 41 18.0 REFERENCES 42
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LIST OF FIGURES
Figure 1 - Silicon Ridge Silica Property Regional Setting 14 Figure 2 - Detailed Location 15 Figure 3 - Property Access 16 Figure 4 - Claim Map 17 Figure 5 - Regional Geology 26 Figure 6 - Local Geology 27 Figure 7 - Schematic Section 28 Figure 8 - La Galette Geological Formation 31 Figure 9 - Property Geology and Mineralized Zones ("D", "G", and "H" Quartzites) 32 Figure 10 - Heliborne Magnetic Survey— First Vertical Derivative 36 Figure 11- Adjacent Properties 39
LIST OF TABLES
Table 1 - Rogue Resources Inc. — Silicon Ridge Mining Title List 12 Table 2 - Historical work in the vicinity of the Property 20 Table 3 - Summary of Lithological units 23 Table 4 - Section type of the La Galette Formation 24 Table 5 - Samples collected during the 2014 Prospection Workings 35 Table 6 - Samples collected during the 2015 Reconnaissance Mapping Program 35
LIST OF APPENDICES
Appendix I - Statutory Works Appendix II — Laboratory Assay Sheets IV Appendix III — Photos XVI Appendix IV - Reconnaissance Mapping Program XXIV
LIST OF MAPS
Map 1— Geological Map, Reconnaissance Mapping and Field Sample Locations XXVII
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1.0 SUMMARY
During the months of May, June and July 2015, line cutting was followed by prospecting, reconnaissance mapping and sampling. The field work was mainly focused on the recognition of the extensions of silica rich quartzite outcrops and ridges with respect to surrounding host rock units such as paragneiss, granite orthogneiss, migmatite, amphibolite and local diabase. A total of fifty (-50) kilometers of a 200 meter spaced lines oriented 330° azimuth was covered using gridded cut lines, forestry gravel roads, GPS traverses and trails. The entire property has been conscientiously prospected, pictures were taken and the most accessible well outcropping silica rich ridges were then trenched, cleaned and channel sampled prior to future diamond drilling under the diligent supervision of Mr. Eddy Canova, V.P. Exploration of Rogue Resources Inc. A total of seventy (70) outcrops, forty nine (49) boulders were localized, identified and briefly described. Twenty- two (22) grab and chip samples were collected in 2014, fifteen (15) in 2015 and results obtained are shown in tables 5 and 6 later in this report.
The main purpose of the reconnaissance and mapping survey was to to identify and precisely localize the silica rich quartzite outcrops and ridges with respect to surrounding host rock units such as paragneiss, migmatite, amphibolite and local diabase. During the course of our survey, some recognized, identified, localized and most accessible well outcropping silica rich ridges were then trenched, cleaned and channel sampled prior to future diamond drilling. A total of seventy (70) outcrops and forty nine (49) boulders were localized, identified, briefly described and photographed outcropping quartzites. The present reconnaissance mapping survey resulted in the recognition of the quartzite "H" determining its thickness and strike extension.
The difficult terrain on the property, high relief, steep pitches and gradients, canyons, dense shrubs and small trees mixed with old rotten fallen timber, resulted in the tie-lines not being cut leaving part of the reconnaissance mapping to be completed by using compass and Global Positionning System (GPS). The lumber roads and trails were also covered by foot and ATV (4X4). With tremendous efforts using grubhoes, axes, picks and geological hammers, more than a dozen massive quartzite outcrops were localized, stripped and cleaned for future channel sampling as well as following up the quartzite with diamond drilling.
The field work was supported with a truck (4X4 Pickups) travelling from the town of Les Eboulements to the property and then on site travelling by all terrain vehicle (ATV) on the logging roads. The crew consisted of two (2) geologists (Mr. Alain-Jean Beauregard and Mr. Guy Gbaguidi) and the work was planned and supervised by Eddy Canova, P. Geo. Exploration Manager and Vice President Exploration for Rogue Resources Inc.
Approximately twenty-five (25) working days of fieldwork and reconnaissance mapping was completed on the property. The scope of this report was to prepare a detailed comprehensive geological surface surface report and map to then be used for the planning of the drilling. The compilation of this field mapping is then to be filed at the Ministry of Natural Resources of Quebec submitting all the relevant and justified expenses for statutory work in order to maintain Rogue's claims in good standing. The main purpose of the reconnaissance prospecting and mapping survey was to identify and precisely locate the silica rich quartzites and adjacent host rock units such as paragneisses, migmatite, pyroxenite, amphibolite and local diabase. The succession that includes the quartzites in the area is dominantly quartz-biotite-garnet paragneiss or metasedimentary stratigraphic units, largely derived from quartz-rich sediments interlayered with thick-bedded pure quartz sands, possibly some mafic volcanic units, and pyroxenites/amphibolites. Further more, it is possible that felsic volcanic units occur in the basal part of dominantly siliceous white or light grey quartz-biotite-garnet
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paragneiss; now a massive homogeneous leucocratic gneiss. The quartzite is interpreted to be deposited in a fluvial or prograding delta complex with the Quartzite "G" having cross laminations indicating tops to the north.
The Silicon Ridge area is intensely deformed into a series of tight to isoclinal folds trending east- northeast as synclinal and anticlinal folds. A set of late, steeply dipping north-northwest, trending joints, with occasional minor displacements are prominent in the competent quartzite units and a number of northeast trending faults are recognized. Bedding is generally parallel to the prominent gneissic or schistose structures in the less competent paragneisses (typical trending 240° azimuth and steeply dipping —60-70° to the north- northwest). A prominent north to northeast trending, steeply plunging mineral lineation is locally well-develop in the quartzites. Gneissosity is well displayed in the paragneiss units and parallels the lithologic units and layering in the quartzites. The property area is dominated by two (2) isoclinal folds: the North Syncline and the Lac de la Grosse Femelle anticline to the south and these repeat the paragneiss succession and the quartzite unit.
A major anticlinal structure (the Silicon Ridge anticline) cuts through the central part of the property. The central quartzite is exposed on its north limb and a small exposure of the quartzite is recognized on its south limb just south of the lake. Four (4) northeast trending faults are recognized to occur on the property and can well be interpreted fom the offsets observed on the magnetic survey map. These are late structures cutting stratigraphic units and later folding and penetrative schistosity. Recognition of these faults and their inferred projections may be important in trying to trace the trends of the quartzite units. Geological mapping in the Silicon Ridge silica project area permitted a better understanding of the structure of the area to outline the extent of the quartzite units and predict prospective extensions. A better understanding of the structure and local stratigraphy of the area permitted to outline in more detail the extent of the quartzite units and predict prospective extensions.
Future exploration work should be oriented towards the definition of the extentions of the quartzite in the north limb of the syncline which appears to be confined or laterally displaced by a late northeast trending fault at both its west and east ends. Also, quartzite "F" located on the south part of the Silicon Ridge will require further work. This includes the evaluation of the extent of the quartzite, by mapping, trenching, channel sampling and drilling. The quartzite represents a single layer that has been repeated by a tight isoclinal syncline and anticline fold structure.
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2.0 INTRODUCTION AND TERMS OF REFERENCE
At the request of Rogue Resources Inc. ("Rogue"), Géologica Groupe-Conseil Inc. ("Geologica") was given the mandate to complete a Technical Field Work Report on the Silicon Ridge Silica Property ("Property") in compliance with the Regulation NI 43-101. The issuer, Rogue, is a Canadian mineral exploration company, trading publicy on the TSX Venture Exchange in Canada. Geologica is an independent mining exploration consulting firm based in Val-d'Or (Quebec).
M. Alain-Jean Beauregard and Daniel Gaudreault of Geologica Groupe-Conseil Inc. are Qualified Persons under the National Instrument 43-101. In June and July 2015, Mr. Beauregard, accompanied by Mr. Eddy Canova, P Geo and Senior Vice-President of Rogue Resources, supervised the works carried out on the Property.
The authors recognize the geological potential for hosting high value silica within the quartzite. These favourable metamorphosed quartzites were mapped and sampled in the past. Thes quartzites have proven to contain high silica content up to 99.54% Si02. These silica rich quartzite units are on strike with similar quartzite units presently being mined on the Sitec Quartz property, 4 km southwest of the property.
Our combined related work experience of more than 60 years as geological consultants does support the recommendations and proposed budget on this report. If future work does demonstrate the property has potential for silica resources, then the silica economic evaluation of the property will be carried out by specialized metallurgists and mining engineers.
Geologica reviewed and evaluated the information used to prepare the report and formulated its conclusions and recommendations. Geologica believes that such information is valid and appropriate considering the status of the project and the purpose for which the report is being prepared. To the best of their knowedge, the authors fully researched and documented the conclusions and recommendations made in the report. All the documents were reviewed between September 2 and 30, 2014
The authors relied on public documents filed at the Ministry of Natural Resources of the Province of Quebec (MRNQ) and information provided by Rogue for the descriptions of title and claim status. Moreover, some parts of this report were taken from reports prepared by previous property owners as well as from federal and provincial government studies.
Geologica is pleased to acknowledge the helpful cooperation of Rogue management and exploration personnel, all of whom made any and all data requested available and responded openly and helpfully to all questions, queries and requests for material.
All currency amounts are stated in Canadian dollars. Quantities are stated in both imperial and SI units (Canadian and international practice), including metric tonnes (tonnes, t) and kilograms (kg) for weight, kilometres (km) or metres (m) for distance, hectares (ha) for area, grams (g) and grams per metric tonne (g/t) for gold grades; and grams per metric tonne (g/t) for silver, platinum and palladium grades; percentage (%) for nickel and copper grades. Precious metals quantities may also be reported in troy ounces (ounces), a common practice in the gold mining industry.
3.0 RELIANCE ON OTHER EXPERTS
The authors have relied on public documents and statutory works filed at the Ministry of Natural Resources of Quebec (MRNQ) and information provided by Rogue Resources. Some parts of the report such as regional geology, property geology and Mineralization are taken from Jean Rondot's report (DPV-682, 1979)
There are no known environmental concerns or land claim issues pending with respect to the Property
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(Quebec Natural Resources Ministry - Public Mining Titles Management, 'GESTIM' Website). It is understood and agreed that the Property was received by Rogue "as is" and that Rogue shall ensure that all exploration programs on the Property are conducted in an environmentally sound manner.
It is important to acknowledge the precious assistance and contributions in the form of numerous discussions and field visits with Mr. Eddy Canova, Pascal Labarbarie, Guy Gbaguidi, Émile Beauregard and Mr. Trygve Hoy, P.Eng., Ph D. (verbal communications) which have helped understanding the geology of the area and most of the conclusions in this report are based on these discussions.
4.0 PROPERTY DESCRIPTION AND LOCATION
4.1 LOCATION AND CLAIMS The Property is located approximately 40 km north of the City of Baie-Saint-Paul, which borders the north shore of the Saint Lawrence River in central Quebec, Canada. Baie-Saint-Paul is about 100 km northeast of Quebec City and approximately 350 km northeast of Montreal (Figures 1 to 3).
The Property is located within the area covered by National Topographic System (NTS) map sheet 21M/15. The centre of the Property is approximately at UTM coordinates 381350 mE, 5294350 mN, NAD83, Zone 19N.
The Property comprises eight (8) contiguous map designated mineral claims ("CDC claims"), which form a rectangular block covering a total area of 462.6 ha (Figure 4).
All claims are currently active, have been renewed (Table 1) and have an expiry date of April 21, 2018. Rogue Resources Inc. is the registered titleholder of all the 8 claims and holds a 100% interest in the claims. The status of the claims was verified using "GESTIM", the Quebec government system for mining titles management, available on the Quebec Natural Resources Ministry Website: www. gestim.mines.gouv.gc.ca. There are no surface rights associated to the land holdings.
Table 1 - Rogue Resources Inc. - Silicon Ridge Mining Title List
Rogue Resources Inc. (88331) 100 % (responsible)
Title No NTS Sheet Expiry Date Area (Ha) Required Work Required Fees 1 2402787 NTS 21M15 2018-04-21 23:59 57.83 780.00 $ 59.67 $ 2 2402788 NTS 21M15 2018-04-21 23:59 57.83 780.00 $ 59.67 $ 3 2402789 NTS 21M15 2018-04-21 23:59 57.83 780.00 $ 59.67 $ 4 2402790 NTS 21M15 2018-04-21 23:59 57.83 780.00 $ 59.67 $ 5 2402791 NTS 21M15 2018-04-21 23:59 57.82 780.00 $ 59.67 $ 6 2402792 NTS 21M15 2018-04-21 23:59 57.82 780.00 $ 59.67 $ 7 2402793 NTS 21M15 2018-04-21 23:59 57.82 780.00 $ 59.67 $ 8 2402794 NTS 21M15 2018-04-21 23:59 57.82 780.00 $ 59.67 $
Total: 462.6 6 240.00 $ 477.36 $
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4.2 PROPERTY PURCHASE AGREEMENT
The Company announced a Property Purchase Agreement dated August 15, 2014, where 8.5 million shares were issued to Fiducie Ananke to complete the purchase of the Lac la de Grosse Femelle Silica Project ("Femelle Silica Project"), this had undergone final regulatory approval. The acquisition was subject to the issuance of 20 million shares of the Company at the closing of the private placement and the granting of a 2% net smelter return royalty (NSR) to the property vendor, Fiducie Ananke. One-half of the NSR may be re- purchased for $500,000 and the remaining one-half (1%) may be re-purchased for a further $1,000,000. No finder's fees are payable on this transaction, and the party is at arm's length to the Company. Closing is subject to the completion of a minimum $2.0 million of the Offering, TSX Venture Exchange approval and certain other customary closing conditions (extract from the Press release August 26, 2014).
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80°0'0"W 75°0'0"W 70°0'0"W • National Park Segt-iles -- ~ 0 u~ Hydrography rbibnugamau Matagami• • I Baie-Comeau I • 1 Lebel-sur-Quévillon La Sarre • s Timmins Amos SIP Saguenay Rimouski • 11 • • • • Senneterre Rouyn-Noranda • 1 •-- Val-d'Or • Québec Rogue Resources Inc. Silicon Ridge Silica Property • Edmundston Ville-Marie Baie-Saint-Paul Québec New Brunswick Témiscaming OP • Ontario Mont-Laurier North Bay • Trois-Rivières Sudbury •
Montréal Ottawa • Sherbrooke Maine
Michigan j 100 0 100 200 Vermont I New York New Hampshire I Nova Scotia From ES RI ArcGIS Data & Maps 2013 Kilometers
80°0'0"W 75°0 0"W 70°0'0"W Figure 1 - Silicon Ridge Silica Property Regional Setting
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300000 325000 350000 375000 400000 • •
-- Rogue Resources Inc. Silicon Ridge Silica Property
Sitec
Parc natiônâl'de Grands-Jardins Exploration prohibited ~ ~ 1 ~ Malbaie ~ National Park (QC) 381 i V~ithdrawn from mining activities
_Baie St-Paul
10 0 10 20 138
Nad 83 Utrfi Zone 19 j ~OLGGICA ; , Kilometers our E• c O Wai 8 7 i. > NTS`21N1 • • 300000 325000 ,.-0000 37.;000 400000
Figure 2 - Detailed Location
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370000 372500 375000 377500 380000 382500
Barley Secondary Reception Post (Zec des Martres)
8889295 Canada Inc. ~ àc_ICôte.l 8te U 0 ` iii - ' (~ ~ Nin ,~.. r• pe (Lrra Ctfta(~~ LE13Garrb emé lle
Uragold Bay Resources Inc o o te) N ~ ~`~ ~ ~ ~~ 1. as V Sitec Quartz inc. Siliclu Québeé Société en Coalman ite
Wil r 8889295 Canada inc. tlùr inc. ~ , Société d'Exploration Minière I MN ~ ~ r~ Property access (gravel road) (] 89295 Canada in~ - 9 0 9
~-~ ' ' WA. Nad 831Utm Zone 19 1g N GEOLOGICA ®. f—`-1 —~ ,: Kilometers 8889295 Can da► inc. NTS~21 M ~ CIO QPL•C ON>tLII. _ 1~ ~ I ~-- ~ Croche ~ J 1 I 1 I 370000 372500 375000 377500 380000 382500 Figure 3 - Property Access
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379 000 380 000 381 000 382 000 383 000
U`EQLaGICA qp0 ❑ t^ O ► 8 - C O N 9 6 l I.
Lac Long Lac Côte Côte
a Lac Gugy
l
~
Lac de la Grosse Femelle ----_r...1 CO CO "s". o) O - 00 00 CS) N- r--• N- N ▪ 'NS ~ (N C N ~,O NS. O O O N ~\ `N CV N L ~
~ \ 500 0 Î 500 1 000 ~ ► tv, — _Nad $3 Utrri Zone .19N Property Access N.T.S. Meters
379 000 380 000 381 000 382 000 383 000 Figure 4 - Claim Map
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4.2 ENVIRONMENTAL OBLIGATION, PERMITS AND OTHER RELEVANT FACTORS The authors are unaware of any environmental liabilities associated with the claims of the Property. However, the authors have not conducted a thorough inspection of these claims.
The exploration activities were planned to have a minimum impact on the environment. Garbage was brought out on a daily basis. No mechanical instruments were used other than the portable diamond saws (2) and small water pumps. Hand shovels, grub hoes, hammers and cisels were used to manually clean and sample the observed quartzite outcrops and their extensions.
Rogue has obtained, from the MRNQ, a Forest Intervention Permit and undertakes to comply with the standards in order to ease the drilling activities.
The Property is located within the ZEC des Martres. ZECs (Zones d'Exploitation Contrôlée) are hunting, fishing and outdoor territories found in Quebec. They are usually located on state land and are administered by agencies and non-profit organizations. These are responsible for the development, exploitation and conservation of wildlife, in addition to facilitating access to land for outdoor users (www.reseauzec.com ).
Moreover, the Property is located within the area covered by the Mining Restriction 16862, a protected wildlife habitat for the cariboo; south of the 52nd parallel (National Park Des Grands-Jardins). Exploration within this area of the mining restriction will be subject to certain conditions and exploration period restrictions. Work programs are presented to the Ministry of Natural Resources and to the MDDEP (Ministère du Développement Durable, de l'Environment de la Faune et des Parc).
It should be noted that a fully operational silica mine is located in the restricted area in close proximity to the aforementioned Silicon Ridge silica property. The Sitec Quartz Mine employs up to 75 employees during the summer of which a great number are local residents, has been in operation for the past fifty years. This area, including the Silicon Ridge property, has been logged in recent years, resulting in a number of logging roads crossing the property and providing easy access.
5.0 ACCESSIBILITY, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY
The Property area can easily be reached from Baie St. Paul by first driving northeast along the Route 138 and at the junction with the Route 381, south of Saint-Urbain, and driving north along the Route 381 to reach two turnoff points to the property, at kilometerage 35 and kilometerage 43.
One access point, kilometerage 35 on Route 381, is the road entrance to the quartzite open-pit mine currently operated by Sitec Quartz Inc. and Silicium Québec Société en Commandite. The road entrance is located off Route 381, 44.6 km north of Baie-Saint-Paul. The centre of the open-pit mine is 6.2 km northeastward from Route 381. The Property can be reached by forestry roads and trails another 9.2 km northeastward from the open-pit mine. The current status of these forestry roads and trails is uncertain and a 4x4 ATV (all-terrain vehicle) is essential to mobilize personnel on these trails.
The second access point is the Accueil Barley, kilometerage 43 on Route 381, the entrance point to the ZEC des Martres. This entrance is located off Route 381, some 52.8 km north from Baie-Saint-Paul. From this point, the property can be reached by driving about 16.8 km, eastward and then southeast, along forestry roads and trails. The status of this access is good as it is used by the ZEC des Martres. Within the property, there are excellent access trails to nearly all the claims.
Road access to the Sitec Quartz Inc. quartzite open-pit mine is year round. Access along these forestry roads is seasonal unless opened by snow removal machines.
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The Property is situated within a vast territory with no permanent residents and with two main vocations: forestry and recreational use. It is composed mainly of lands belonging to the state including the Réserve Faunique des Laurentides, the Parc National des Grands-Jardins and the ZEC des Martres (www.mrccharlevoix.ca ).
Baie-Saint-Paul, with a population of approximately 7,300, is the largest urban centre and office for the MRC de Charlevoix. Saint-Urbain, with a population of approximately 1,350, is located 14.5 km north of Baie- Saint-Paul and is the closest town to the project area.
The topography on the property is very rough with northeast trending ridges and deeply incised river valleys. Elevations within the Property vary from about 870 to 1005 meters, above mean sea level. The area is covered by tightly growing evergreens and stunted evergreens dominated by Spruce, Balsam, Fir, Birch and Alders with old fallen trees particularly in previously forested areas and/or burnt areas with conifer regrowth. The overburden on the property is thin in positive relief areas and mountainous areas, and subcropping rocks are generally covered by caribou moss, Labrador tea, bushes, lichen and tall trees are more abundant on slopes and valleys. Caribou and moose trails as well as foot prints are frequently observed, as well as bear droppings. Partridges and hares are also very commonly seen on and close to lakes and rivers.
There is a former power line right of way located approximately 100 m from the southeast corner of the property and has been abandoned. A new electrification project by Hydro Quebec and Sitec Quartz Inc. will be bringing in an electrical power line to the Sitec Quartz Inc plant approximately 9.2 km from the quartzite "G". Another major and active power line corridor is located 5.4 km east-southeast of the southeast corner of the property.
Based on Environment Canada statistics, available average temperatures in the Baie-Saint-Paul area vary from a low of -12°C in January to a high of 19°C in July. Total monthly precipitation varies from a low of 70 mm in March to a high of 147 mm in July. Water is easily accessible from Lake de la Grosse Femelle. Average snowfall is highest in December and January, 65 cm and 67 cm, respectively. Hwy roads in the area are normally open year round. Relevant to the mineral project, the length of the operating season is year round except for during hunting season, which stretches from September to mid-October and during the period caribou migrate south of the 52nd parallel.
6.0 PREVIOUS WORK
Previous field work on the Property
The Property was the subject of some previous exploration work with preliminary geological reconnaissance conducted by the Ministry in 1971 (RP-601A), GEX Silicium Limited in 1976 (GM 32263), SOQUEM in 1980 (GM 36592) and the prospector Tremblay in 1999 (GM 58264). The best sampling carried out by GEX Silicium in 1976 returned results of 0.195% A1203, 0.034% Fe203, 0.035% TiO2 and 99.6% Si02 with grab samples on the Quartzite unit.
These assay results revealed the high value silica of the "G" Quartzite with 97.6% to 99.5% Si02, 0.28% to 0.69% A1203, 0.07% to 0.21% Fe203 and 0.02% to 0.13% Ti02.
Previous Work outside the Property
In 1946, the discovery of a quartzite occurrence by prospectors ("LM" quartzite) located 2 km east of Lac de la Galette, approximately 10 km southwest of the Property triggered follow up work in the region.
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In 1965, the Leeds Metals Company carried out drilling on the "LM" quartzite occurrence and established a resource estimate (GM 17602). Additional quartzite occurrences were discovered by Rondot during mapping of the Lac des Martres area from 1969 to 1971. Further work by Rondot to 1984 revealed at least ten (10) quartzite occurrences named "A" to "I": referred to as deposits by Rondot (Map in Appendix IV, DPV 682 and MB 89-21). The terminology for the various quartzite occurrences or deposits diverges somewhat according to sources: the terminology according to Rondot's report DPV 682, published in 1979, is used in this report.
Following this period, several companies have completed exploration work in this area and today Sitec Quartzlnc. and Silicium Québec Société en Commandite operate quartzite deposits ("A" and "B"). The table below (Table 2) presents the statutory work that has been carried out in the area.
Table 2 - Historical work in the vicinity of the Property Date Company Work description Results Reference 2015 GPR Geophysics International Inc. Report on the processing and More detailed geological data should be Internal interpretation of a Helicopter-Borne obtained in order to have a Magnetic Survey completed on the betterunderstanding of the geophysical Grosse Femelle Silica Project results. 2014 GPR Geophysics International Inc. Helicopter-Borne Magnetic Data Acquisition Report. Internal Geophysical Survey on Silicon Ridge The products consist of final databases, Silica Project maps, metadata files and final grid files. 2013 Quebec Natural Resources Ministry Report on mineral activities in Quebec This annual report summarizes mining DV 2013-02 Publication activities in Quebec in 2013. 2012 Gevry Claims, St-Urbain Property, Audiomagnetotelluric Survey. The results obtained shows that it is GM 66544 Silica Deposit possible to map the quartzite unit with the help of the audiomagnetotelluric method. 2012 Sitec S.E.C. Ground prospecting. The field work shows that the claim GM 66670 Claim #1099896. contains high purity quartzite in the same general trend as the Petit Lac Malbaie silica mine. 2012 Sitec S.E.C. Ground prospecting. Two new outcrops of rose, white and GM 66790 Claims #1099897, #1099898 & grey (coloured) quartz were located and #1099899. grab sampled. Detailed mapping was difficult to carry out due to thick overburden. 2011 Sitec S.E.C. Prospecting and rock sampling The southern belt of the Petit Lac GM 66041 Hydro Zone Area activities. Malbaie Formation does not appear to have any thickened zones of white quartz as seen at Malbaie Zone B, Bec Scie and Bec Scie North. 2010 Sitec S.E.C. Geological survey, drilling & ground Several outcrops were examined and GM 65022 Bec Scie North Project prospecting. trenches were carried out in order to map the extent of previously recognized white quartz. No samples for chemical analysis were carried out. 2010 Gevry Claims, St-Urbain Property, Resistivity Survey The Promis-10 type survey permitted to GM 65085 Silica Deposit Promis-10 & GEM2 Surveys. localize a resistive rock band similar to the known massive white quartzite unit. 2008 Gevry Claims, St-Urbain Property, Quartzite fluorescence and nirs Nirs spectroscopy analysis permitted GM 63535 Silica Deposit spectroscopy analysis. identification of the presence of certain mineral traces as hematite & muscovite in quartzite. 2006 Sitec S.E.C. Ground prospecting, overburden & Presence of quartzite ranging from white GM 62596 South part of Mine Carriere Petit Lac outcrop trenching. to medium grey and pink to locally red. Malbaie Quarry Chemical analysis was carried out but no results have been made available. 2006 Sitec S.E.C. Surface trenching and prospecting The presence of the 32 year old quartzite GM 62645 Portion of BEX 0000236 & claim 3 program mining site at Petit Lac Malbaie gives a 2006 high priority to exploration, development and employment in the Charlevoix area.
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2006 Sitec S.E.C. Prospecting, overburden trenching, With the emplacement of disposition GM 62651 Bec Scie Silica Showing stripping & bulk sampling BEX 450, Sitec has shown its willingness to sustain its presence as a major employer and consumer of Charlevoix region. 2006 Gevry Claims & Groupe Gethe Inc. Infrared Reflectance Spectroscopy Numerical relationship exists between GM 62236 St-Urbain Silica Deposit Analysis iron levels and spectral signatures of silica-hematite mixtures, which allows the quantification of the proportion of iron in the mixtures without chemical analysis. 2004 Gevry Claims Petrographic & geochemical Two types of quartzite were observed GM 60892 St-Urbain Silica Deposit characterization of quartzites (white and red). Only the white quartzite could likely be exploited for several industrial applications. 2003 Sitec S.E.C. Prospecting, geological & sampling Only low grade quartz was observed in GM 60851 activities the prospecting area & no further work was warranted. 2002 Sitec S.E.C. Geological mapping and prospecting No significant results were observed. GM 59793 Lac de Petit Malbaie Area 2001 Quebec Natural Resources Ministry Report on mining exploration The report summarizes mining DV 2001-01 Publication activities in Quebec exploration activities in Quebec and highlights the mineral potential of all geological provinces. 2000 Quebec Natural Resources Ministry Silica Quebec Resources The study exposed an inventory of the ET 99-04 Publication silica resources in Quebec including a general description of the main known sources and a detailed description of the main known deposits. 2000 Gevry Claims & Groupe Gethe Inc. Magnetometric Survey The geological survey permitted the GM 58218 St-Urbain Project characterization of the quartzite zone. 2000 Sitec S.E.C. Ground prospecting, mapping Two significant bands were revealed. GM 58313 South extension of Malbaie Quarry 1999 Tremblay Claims Ground prospecting, rock analysis and Assay results pending. GM 58264 Silicon Ridge technical evaluation 1995 SOQUEM Drillhole Program Three drillholes were carried out : DDH GM 53288 Silica Project 10-743, Gisement 'C' 95-33, 95-34 and 95-35 : 8.3m, 26m and 21m of high quality quartzite. 1993 SOQUEM Summary study of the silica market The profitability study indicates that the GM 52345 La Galette Silica Deposit project is clearly marginal. 1990 Baskatong Quartz Inc. Ground prospecting, geological survey Evaluation of the quartz extension from GM 50836 Lease 674 and rock analysis lease 674 confirmed the presence of a medium grade of quartz zone (rose coloured, low aluminum). Results of the sampling indicate the existence of quality quartzite. 1989 Quebec Natural Resources Ministry Charlevoix geology General geology of Tadoussac Complex. MB 89-21 1986 Pro-Mine Enr. Quartzite deposit sampling Determined the boron content of the GM 43656 Deposit. 1985 Quebec Natural Resources Ministry Mineral deposits evaluated tonnage Compilation of mineral concentration DV 85-08 Publication and Quebec mineral prodution quantified on the Quebec territory (evaluated tonnage and/or production). 1985 Université du Quebec, Chicoutimi Deformation study of de la Galette Non mineral relation. TH 1211 Thesis Metaquartzite 1983 Gagnon Claims Sampling results and analysis The sampling results indicate the utility GM 40982 of the white-pink type quartzite in the ferro-silicium industry. 1982 SOQUEM Drillhole Program 0.09% Fe203v / 23.1 & GM 38855 Silica Project, Gisement 'C' 0.28% A1203 / 23.1 1981 SOQUEM Prospecting, geological survey & Reserves calculation by sections for 'C' GM 37749 Silica Project 10-743 diamond drilling and 'l' Deposits. 1980 SOQUEM Rock analysis, geological survey, soil Synthesis of all previously collected data GM 36592 Silica-Charlevoix Project 10-743 magnetic survey and drilling and qualitative and quantitative quartzite reserve evaluation. 1979 SOQUEM Geological survey Few visible outcrops. GM 35010 Silica-Charlevoix Project 10-743 South block 2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page 21 GEOLOGICA GROUPE-CONSEIL
1979 Baskatong Quartz Products Ltd, Ground prospecting The results are only available on multiple GM 35038 SOQUEM drawings.
1979 Baskatong Quartz Products Ltd Rock analysis, geological survey This report describes quartzites in the GM 35675 area of Lac de la Galette regarding their regional distribution and suitability for economic exploitation. 1979 Quebec Natural Resources Ministry Geological reconnaissance in The report summarizes the field data DPV 682 Publication Charlevoix and Saguenay region collected between 1975 and 1978 to better recognized the Canadian Shield stratigraphy and summarize the recent knowledge of St-Urbain Anorthosite. 1978 Baskatong Quartz Products Ltd Rock analysis, geological survey The contact between the quartzite and GM 33619 Petit Lac Malbaie Property the garnet-silliminte gneiss was established and all outcrops southwest of the contact were examined and located. 1976 Gagnon Claims, GEX Silicium Ltd Rock analysis, profitability study, 0.195% A1203, 0.034% Fe203, GM 32263 geological survey 0.035% Ti02, 99.6% Si02 1976 Quebec Natural Resources Ministry Report of resident geologists for 1975 The report provides an overview of the DPV 346 Publication activities of producing mines, prospects and mining exploration work for each district. 1975 Baskatong Quartz Products Ltd Rock analysis, geological survey Geological mapping indicated that the GM 30708 Petit Lac Malbaie Property quartzite bands were of greater extent than had previously been reported. Two main bands are exposed to the north and south of the Lac de la Baie and can be traced for several miles to the northeast. 1975 Quebec Natural Resources Ministry Silica report in Quebec The report describe the main utility of DP 323 Publication silica, briefly describes the known actual or past deposits and the most interesting geological formation to be considered for silica. 1974 Quebec Natural Resources Ministry Economic geology The economic evaluation revealed two DP 258 Publication Petit Lac Malbaie quartzite types of quartzite sufficiently pure to be considered for exploitation. 1971 Quebec Natural Resources Ministry Geology of the Martres Lake Area The geochemical survey data in this RP 601(A) Publication Preliminary Report report are available on Sigeom website. 1965 Leeds Metals Co Ltd Technical evaluation The average grades of silica in the white GM 17602 quartz are 99.04% accompanied by an average iron content of 0.059% iron as Fe203.
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7.0 GEOLOGICAL SETTING AND MINERALIZATION
7.1 REGIONAL AND LOCAL GEOLOGY
The lithological units are well described in geological reports on this area, especially that of Rondot, J. and Tremblay, G. of the Ministry of Natural Resources of Quebec (DPV-682, 1979). These reports helped to orient our geological mapping survey and gave us an excellent insight into understanding the structures in the area and provided a better understanding of the protolith of the local stratigraphic succession.
The regional geology consists of the Grenville Province of the Canadian Shield. This area shows a series of lithological units from Proterozoic intrusives and Metamorphic rocks to Quaternary deposits (see Table 3 and Figure 5).
Table 3 - Summary of Lithological units (Ref.: Rondot, DPV-682)
QUATERNAIRE P1Sistocène et Holocène Terrasses marines et alluvions Complexe morainique de Saint-Narcisse Complexes morainiques anciens DEVONIEN SUPERIEUR Astroblème de Charlevoix Impactite Mylolisthénite ORDOVICIEN MOYEN Dépôts de plate-forme et de zone instable Formation du Cap Martin Formation de Saint-Irénée Groupe de Trenton Formation de Cap-d-l'Aigle Formation de Cap-aux-Oies CAMBRIEN Prisme gëoclinal Microgrès de Saint-Bernard Flysch de l'Isle-aux-Coudres HADRYNIEN Rift du Saint-Laurent Diabase Péridotite PROTEROZOIQUE Roches intrusives et mëtamorphiques Anorthosite de Saint-Urbain Complexe du Parc des Laurentides Complexe de Tadoussac Groupe des Martres Groupe de Saint-Siméon Groupe de La Malbaie Groupe de Saint-Tite-des-Caps
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The Property is underlain by quartz, biotite and garnet gneisses and pure quartzite enclaves and/or stratigraphic units of the De La Galette Formation (quartzite, paragneiss, local pyroxenite, amphibolite, magmatite and granitic orthogneiss) which is part of the Des Martres Group within the Tadoussac Complex as presented on the Lac des Martres NTS Quadrangle Sheet 21M/15 SE.
The La Galette Formation is subdivided into three (3) members which are the Inferior Garnet Gneiss, the Quartzite and the Superior Garnet Gneiss of varied composition (Rondot, 1979). The Quartzite is exceptionally homogeneous and very pure over wide thicknesses (between 100 and 260 meters in the cross section orientation). The Superior member is characterized by garnet quartzite gneisses with the local presence of sillimanite. In places and particularly at the Lac de la Grosse Femelle Syncline, irregular stratifications corresponds to observed in channel filling areas. Table 4 below illustrates sections typical of the La Galette Formation metasedimentary sequences which are presented from top to bottom (base). The ten (10) quartzites identified by Rondot are named and are part of the Petit Lac Malbaie Quartzites.
Table 4 - Section type of the La Galette Formation (Ref.: Rondot, DPV-682)
UNITES (du sammet â la basa) ÉPAISSEUR
FORMATION DE LA GALETTE (870 m) Membre supérieur (410m) - gneiss quartzeux; niveaux de quart- zite à grenat et feldspath potassi- que 50 m - gneiss à grenat et sillimanite 150 - gneiss à grenat, sillimanite et gra- phite 10 - gneiss â grenat 50 - gneiss a hornblende et pyroxènes; grain grossier 20 - gneiss quartzeux, stratification oblique 20 - gneiss à grenat, sillimanite (gneiss quartzeux) 100 Quartzite du ,Petit lac Malbaie (2GO m) - quartzite pure (gisement C. épais- seur maximum) 260 Membréinfari.eur (500 m) - gneiss quartzeux â sillimanite; gra- phite au sommet 80 - gneiss à scapolite, diopside, spi-gè- ne, carbonate 20 - gneiss A sillimanite, biotite, cor- diérite, spinelle 10 - amphibolite, gneiss à hornblende 20 - gneiss à sillimanite, grenat, gneiss rouillé 70
UNITE INFERIEURE (plus de 500 m) - amphibolite (pyribolite) massive 250 - migmatites roses à grenat et amphi- bolite envahies par les roches char- nockitiques du complexe du Parc des Laurentides 250 - conglomérat, non en place, à galets de compositions variées (gneiss et roches intrusives) à 1 km au SW du Petit lac Malbaie
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Quartzite enclaves and garnet gneisses are observed in the charnockite rocks of Baie-St-Paul up to the Saguenay over 100 km further north.
The La Galette Formation is folded and faulted with high grade metamorphism of the amphibolite to granulite facies. The stratigraphic units are NE trending and characterized by an overturned synform near the northwestern boundrary of the Saint-Urbain Anorthosite. The Quartzite units which are located in the Petit Lac Malbaie area, are oriented N55°E. These were identified as zones "A", "B", "C", "D", "E" and "G". Three (3) Quartzite lenses or lithostratigraphic units (Zones "F", "H" and "I") were observed being oriented E-W (approximately N80°E). The Petit Lac Malbaie, nine (9) Quartzite Deposits ("A" to "I"), are described to be:
Coarse grained, massive, locally fractured and schistose. Composed of 98% to 99% quartz with trace to 1% biotite ± traces of muscovite, hematite, fuschite, rutile and ilmenite commonly associated with red quartzite. Local clusters of sillimanite with pyrite can also be observed. The maximum thickness is 260 meters with average thicknesses of 150 m. The quartzite zones or deposits are classified as: white and grey stratigraphic units; red and pink when altered with iron and near contact zones where the reddish coloration is caused by iron oxides along fine fractures and contact zones.
The Property is underlain by geological units consisting of quartzite paragneisses, amphibolites, charnockites, migmatites, opdalites and anorthosites as mapped by Rondot between 1964 and 1971 in the Charlevoix area for the Quebec Ministry of the Natural Resources. Quartzite units occur along zones identified as Zones D and G and continue along a northeast strike, toward the Silicon Ridge property. Just north of the quartzite "G" (approximately 300 meters) is the quartzite "H" identified during the summer field reconnaissance mapping survey.
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250000 350 C0 - 450000
G1of~,yly dn Qnebtc Grenville Province Geology G13: Paragneiss, gneiss, marble, quartzite & iron formation o G20: Gabbro, sorite, diorite, pyroxenite S ô o o G21: Anorthosite, Leucogabbro, leuconorite o ~ In G22: Gneiss (unsubdivided) M ~ O7 G23: Tonalitic gneiss & trondhjemite, tonalite G24: Charnocktic & mixed gneiss G25: Granitoid gneiss 026: Migmatite G27: Granitoid (unsubdivided) G28: Orthopyroxene granitoid: charnockite, mangerite, jotunite 029: Syenite. monzonite. monzodiorite G30: Granite. quartziferous monzonite & syenite, pegmatite
o o o o m l ~Y
Appalaches Province
;,4 50
Kilometers G22 From:' DV 2012-06 (Géologie du Québec) MRNQ. GEOLOGICA • Qûébéc Nad 83 Utm Zone 19 O R O O ► 9. • C O N 8 8 t I. Sept. 2014
250000 350000 450000 Figure 5 - Regional Geology
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GEOLOGICA G OU]P]E-CONSEIL
GEOLOGICA N GROUPE-CONSEIL A 381000 382000 383000 384000 I I I
A~ z = . / ~. rHe Geology: Silicon Ridge Silica Property o ✓ % Rogue Resources Inc. ô <-,_--, in i Eastern Legend9 quartzite ia as ~rlit.''a ~Gr ~^' ~ extension ~•i• ~ a Ott hcgness: granitic grrebs,fdia6edrrmrorae, syena.e. /~~~ - ~ 3 Paragr'.cn : ISarM1kYt0lal.leucocreti° Warti~fCldspr~Pprn¢td ~ f ~ !\ 9 ~ blotrcec~+Bnekt tut sslthconsklashk rua lswgrlrks)bcalNary y-~ ô 'H' OF Za ~y~ ' ~ '/ / .~ miaenu5sn! ils !evercd)sequence; same qurnsneats- N y~ /•~ /~ - lb ~rartzitecOMactinterlayered qua rtzite and feMSFothe / yr-~ G ~ •...• surrtand ffireial ~ / .f yT, i`-` ta i ' X`~,5.[~ • ~r / aL•~ '~I Za prartzltcmasm,recryslalliadmwell-layered. pure wthuidy ~¢• r .,.*.•,___,--.4 1111 t7 mina hematite stain nt: rare scours and croa-bed5 ~ ?~~ * .: ...•^~,~Cr @. - ~j ./~,..~. ' r -lb Pyroiaenrtelamphibolile: nva iw,caarxirainaR,fdiatedto J; 'H'~ ..••' i~ . i buided with more paggclasa-rkh layers r ^ i~ ~.•^~•~ . ~ ~ . - la Paragro quartz-feldspar-garnet p.re~neiss.minor m.ecrnae, (/ 1a - ~~- -~ __ ...... /,:' ~~ beater may include thin lrrpurequartzite lave, and °sergeveiled gzmet•gwrtz+yhitefaldtpag nvgmadte. 4111F, 94000
I ~ ~ ~f • Symbols 52 ~ , Fault defiled, approx., assumed MI claim border/ 1G, ~8 ._ . .1'.myennglbd0n81 O Claims' samplelocality v'' ~'L C S~ Gne igspsl[v,schistfalty, v * anlldine,euerturrasl ' `MF. e v i ~✓ MlrcrellineMlon „RV)" 5•Irg:llne.o.ertvned ~4► 1~ F ' - . . ... Contact: ~l> ~'' ~ '
0 500 1000 1500 Nad 83 Utm Zone 19N l N.T.S. 21M 15 Meters
Figure 6 - Local Geology
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GFO]LOGICA G OlU]P]E-CONSEIL
Z \ z z Orthogneiss; granitic gneiss, foliated monzanite, syenite ?, o \ o o up ~\ o in r 3 Paragneiss: (similar to la): leucocratic quartz-feldspar-garnet co f \•— -4- biotite paragneiss, but with considerable rust (sulphides) locally and rn N \ N more massive (less layered) sequences: some quartz sweats. up \ I\ '\ Quartzite contact: interlayered quartzite and feldspathic rj \\\ \\ 0 250 500 2b \ \ Y\ schist and gneiss.
- \ \ , \ \ Meters ?a Quartzite: massive, recrystallized to well-layered, pure, with only , \ \J -- ✓' minor hematite staining; rare scours and cross-beds. rJ \' 1 \ \ \ `r \\\ Pyroxenite/amphibolite: massive, coarse grained; foliated to ` \ \ \ banded with more plagioclase-rich layers. •P; l \ , Paragneiss: quartz-felsdpar-gamet paragneiss, minor muscovite, ,L\` \` \`' biotite; may include thin impure quartzite layers and coarse grained S Ç~~• Ç‘. ..\\r, Tx `\ \ + ¢ ,\ ‘\CA `, ~\ ~ garnet-quartz-white feldspar migmatite. \*P ~\ \ ,`~ \ \ \ \~ \G,\\~ \e `\ N \ ` Lake d ``~= \`
2b \ 3
4 GEOLOGICA G R O U P I- C O N S Z I L
Figure 7 - Schematic Section
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7.2 LOCAL AND PROPERTY GEOLOGY
The "Silicon Ridge Property" is essentially underlain by quartz-biotite-garnet paragneisses and pure silica quartzites enclaves and/or stratigraphic units of the "La Galette Formation" which is part of the "Des Martres Group" within the Tadoussac Complex. The "Pure Silica" Quartzite is essentially homogeneous and high purity over wide thicknesses (between 100 and 260 meters in a cross section orientation). The Superior member of the "La Galette Formation" is characterized by garnet-biotie-quartz quartzite gneisses with the local presence of sillimanite. On the property, quartz-biotite-garnet paragneiss and quartz-biotite paragneisses are the commonly observed host rocks to the quartzites. The stratigraphic units are northeast trending and characterized by an overturned synform near the northwestern boundary of the Saint-Urbain Anorthosite. The quartzite units (D, E, G and H) are N 55-60°E orientation. Near the western property boundary, quartzites (F and H) are East-West oriented. The quartzites are described to be: - Coarse grained, locally fractured and schistosed. - Composed of 98 to 99% quartz with trace to 1% biotite ± traces of muscovite, hematite, fuschite, rutile and ilmenite commonly associated with the red quartzite. Local clusters of sillimanite with pyrite can also be observed. - The maximum thickness is 260 meters with average thicknesses of 150 meters. - The quartzite zones or deposits are classified as: white and grey stratigraphic units; red and pink when altered with iron and near contact zones where the reddish coloration is caused by iron oxydizing along fine fractures and contact zones.
On the property, four (4) main geological units were recognized and identified:
1) Siliceous quartz-biotite-garnet paragneisses with occasionally thin quartzite layers are dominant. This paragneiss consists of some mafic minerals with occasional biotite and amphiboles. Thin migmatite layers and/or lenses are commonly present with coarse grained, massive quartz- feldspar and variable garnet concentrations. These migmatite layers are parallel to sub-parallel and locally cross-cut the gneissosity. The paragneiss is exposed in the core of the Lac de la Grosse Femelle anticline and in the northern part of the property along the north overturned limb of the North Syncline. Two amphibolite/pyroxenite units (see appendix Ill) were observed to be repeating on both limbs of the anticline. 2) Massive recrystallized quartziteds show well defined sedimentary structures such as cross beds and scours indicating tops directions to the north and suggesting deposition in a shallow fluvial environment. The quartzite grades upward through several tens of meters (decimetric) of interlayered, thin bedded less pure quartzite and siliceous paragneiss. 3) Siliceous white or light grey quartz-biotite-garnet paragneisses includes layers of massive schist, and orthogneisses containing more mafic minerals. It is well exposed in along the north access road where it cuts across the core of the syncline (Figure 5). Quartzite units in the hinge zone are often heavily rusted due to an increase in iron content in the protolith sediments or due to alteration related to deformation. 4) Massive to locally foliated granulite gneiss intrusions in origin are well exposed to the north and south of the paragneiss succession. The orthogneisses or granitic gneisses underly the paragneisses and quartzite sucessions (Figures 6, 7 & map 1). The road exposures to the south of the Lake are pink coloured, foliated granite gneisses and syenites. Farther north, at the contact with the
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siliceous quartz-biotite-garnet paragneiss, a white quartz-plagioclase orthogneiss of quartz monzonite composition are observed on an outcrop exposure. Pink granitic gneisses are also observed in outcrops located along the northern edge of the property claims.
7.3 MINERALIZATION The Property hosts at least two (2) known mineralized zones that correspond to silica rich quartzite units ("D", "G" and "H") of the Petit Lac Malbaie Segment of the La Galette Formation which are the main mineralizations of interest (Figures 8 and 9). Work by Rondot (DPV682) identifies the quartzite zones "D" and "E"/"G" that extend onto the property. Sitec Quartz Inc. has operated on their property in the quartzite zone "E" in the past (GM58264) and in 2015. Quartzite "G" was the subject of limited exploration work in the past; it is easily accessible by secondary logging roads and 4X4 vehicles. It is located in the central southwest part of the Property, extends SW and NE (N50E-N60°E) along strike, dips subvertically (-60° to -70°NW) and reaches widths of approximately 250 meters in places. White quartzite bands of silica have in the past (GM 36592) revealed analysis of low Fe203 (0.04%) and A1203 (0.37%). The "G" Quartzite unit was resampled for silica purity later (GM 58264) and assay results returned 99.52% Si02; 0.39% Fe203; 0.46% A1203 and 0.04% TiO2 from sample No. 37529 and 98.72% Si02; 0.43% Fe203; 0.70% A1203 and 0.06% TiO2 from sample No. 37554.
On September 2014, one of the authors visited and sampled the "G" Quartzite with the following oxide assay results: 97.6% to 99.5% Si02, 0.28% to 0.69% A1203, 0.07% to 0.21% Fe203 and 0.02% to 0.13% Ti02.
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Pure quartzite as defined by Rondot (1979) DPV 682 La Galette Geological Formation
Stratigraphy / Geology Quaternary (sand, gravel, silt, till) tl• Undifferentiated charnockitic (anorth., gabbro) Charlevoix chamockitic complex (migmatite) ▪ Sainte-Arme du Nord Opdalite Saint-Urbain anorthosite 9 Undifferentiated paragneiss tIMM Gar., paragneiss, quartz, gneiss Quartzite Sil. gar. paragneiss tttti Gar. migmatite
From: SIGEOM, MRNQ,ISept. 2014 Nad 83 Utm Zone 19
Figure 8 - La Galette Geological Formation
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G]EO][.OG[CA G OU]P]E-CONSEIL
379000 380000 381000 382000 383000
rz3 Pure quartzite as defined by Rondot (1979) DPV 682 N
/ Charnockitic migmatite Pink migmatite & associated rocks (garnet)
--_ -- ~ ` __ -- / Amphibolite ~.~,~~ .•• _ . ~ .~ iOi O•' . ~ •~•i•• •~.•~.vO~v..~.`~i~ L?' ~~'+ ~t:> ~'' '~~~~..~~•. ~ ~0ii% ~ ------..____-----__\N_,___._.---- O•••••11;.*.• .•.• ••• ••••~•••~•. ~j r~•~•~'~• :-~ 4 ►.• fr4 Quartzite = ~ '' ~i•~i~ i~Oiii%' !/ /'i~ / . ';•~•~' .< ~AA%~ ~;~ i~• ~.~•~•~-•A~AP:•:.~a --- ' .00 /ttC/ ,.• G ~•`!+s = ~• ,•~••,~•~ _~ / •• -~ • ~~ - - rf~ Q~ i' • ~~.'~ i' _ Paragneiss /a/°-• .I: • . • ~ ' / ~' ç~♦ / i~ (sillimanite, garnet, quartzite) ....• • .- • .c:.7 i~ . ~ • •• -;:.•,•.• T ~ . Quartzite ~ ~••~ .~••i••••~•o at• • v.. .0.-Amphibolitehibolite %• ~/ ~• •.•e _.••••••. .~' ,,•••••.y...... • / ►•. •••-•• •. .: . Quartzite Pink migmatite __- •~•~ ''••, ~~,~~~..y 'O'. ~ ' •,••~~,• y - •••„•!~-• 44-"— ~~ +„el,V~/ Paragneiss ••• ,.- -(garnet) e .- (garnet & quartzeous gneiss),', • D IV".- - - •,'•• , •'c•`'O '•4 / •~'O~ , /~•'••• ' ••'•• . ~ ''~ •.~~~. ~: ' Charnockitic migmatite •,•• '''• ,,•••••.• ••y.• & associated rocks ,O' '~~ ' •'~,''\ c ~ !-' ,•~~, ~,;;;;~~,; . o!, 0 soo L 4 From: SIGEOM, MRNQ, Sept. 2014 5GEO OGICA >kQU*E,CUh88r,,W Am hi® bô /lite .' ', Meters Nad
379000 380000 381000 382000 383000 Figure 9 - Property Geology and Mineralized Zones ("D", "G", and "H" Quartzites)
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8.0 DEPOSIT TYPES
On the Silicon Ridge Silica Property, quartzite lithological units or sequences are silica rich. Generally, the difficulty lies principally in identifying a horizon that is pure and thick enough for mining. However, on this Property, this is not an issue, because at least three (3) quartzite units ("G", "D" and "H") of significant length trending across the Property in a NE orientation where the "G" quartzite is known to reach up to 275 meters. The other silica deposit types are silica sand deposits and natural quartz crystal deposits or veins as well as some silica deposits in British Columbia and Ontario.
In British Columbia, the significant quartzite occurences exist at Mount Wilson, in the Parsnip Forest area, at Longworth and at Shuswap Lake. The SiO2 varies from 97.94% to 98.85% in Mount Wilson; 99.43% at Parsnip Forest; from 99.02% to 99.68% at Longworth; and from 97.28% to 98.9% at Shuswap Lake (ref.: CIMM Special Volume 29, p.286).
In Ontario, the main deposit is located in Georgian Bay and consists of the Bargeley Island quartzite deposit. A typical chemical analysis of this quartzite is 98.45% Si02, 0.60% A1203, 0.04% Fe203 and 0.03% TiO2 (ref.: CIMM Special Volume 29, p. 134-136).
9.0 EXPLORATION WORK
9.1 RECONNAISSANCE AND GEOLOGICAL MAPPING
During the months of May, June and July 2015, line cutting followed by prospecting, reconnaissance mapping and sampling were completed. The field work was focused on the recognition of the extensions of silica rich quartzite outcrops and ridges with respect to surrounding host rock units such as paragneiss, granite orthogneiss, migmatite, amphibolite and local diabase. A total of fifty ("'50) kilometers of a 200 meter spaced lines oriented 330° azimuth was covered using gridded cut lines, forestry gravel roads, GPS traverses and trails. The entire property has been conscientiously prospected, pictures were taken and the most accessible outcropping silica rich ridges were then trenched, cleaned and channel sampled prior to the diamond drilling under the diligent supervision of Mr. Eddy Canova, V.P. Exploration of Rogue Resources Inc. A total of seventy (70) outcrops, forty nine (49) boulders were localized, identified and described. Twenty-two (22) grab and chip samples were collected in 2014, fifteen (15) in 2015 and results obtained are shown in Tables 5 and 6 in this report.
The main purpose of the reconnaissance and mapping survey was to identify and precisely localize the silica rich quartzite outcrops and ridges with respect to surrounding host rock units such as paragneiss, migmatite, amphibolite and local diabase. During the course of our survey, some recognized, identified, localized and most accessible outcropping silica rich ridges were then trenched, cleaned and channel sampled prior to future diamond drilling. A total of seventy (70) outcrops and forty nine (49) boulders were localized, identified, described and photographed where quartzites were visible. The present reconnaissance mapping survey permitted to recognize the quartzite "H", identifying its thickness and extensions.
Due to the difficult terrain, high relief, steep pitches, canyons, very dense forest and shrubs, and small trees intermixed with old rotten fallen trees, the tie-lines were not cut leaving part of the reconnaissance mapping to be completed by using compass and Global Positionning System (GPS). The lumber roads and trails were also covered by foot and ATV (4X4) where accessible. Prospecting by using grub hoes and geological picks helped find more than a dozen massive quartzite outcrops found, identified and localized for future trenching, cleaning and channel sampling for future follow up by diamond drilling.
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The work was supported by truck transportation (4X4 Pickups) from the town of Les Eboulements and the property and then on the property were accessed by all terrain vehicle (ATV) on logging roads. The crew consisted mainly of two (2) geologists (Mr. Alain-Jean Beauregard and Mr. Guy Gbaguidi) and the work was planned and supervised by Eddy Canova, P. Geo. Exploration Manager and Vice President Exploration for Rogue Resources Inc.
Approximately twenty-five (25) working days of fieldwork and reconnaissance mapping were completed on the property. The scope of this report was to integrate and compile all of the information for filing at the Ministry of Natural Resources of Quebec with qualified and justified expenses for statutory work in order to maintain Rogue's property and claims in good standing. The main purpose of the reconnaissance prospecting and mapping survey was to identify and precisely localize the silica rich quartzites with respect to surrounding host rock units such as paragneiss, migmatite, pyroxenite, amphibolite and local diabase. The succession that includes the quartzites in the area is dominantly garnet paragneiss or metasedimentary stratigraphic units, largely derived from quartz-rich sediments interlayered with thick-bedded pure quartz sands and possibly some mafic volcanic units and pyroxene/amphibolite. Further more, it is possible that felsic volcanic units may occur in the basal part of dominantly siliceous white or light grey quartz-feldspar-garnet paragneisses and now a massive homogeneous leucocratic gneiss. The quartzite is interpreted to be deposited in a fluvial or prograding deltaic complex.
The Silicon Ridge area is intensely deformed into a series of tight isoclinal east-northeast trending synclinal and anticlinal folds. A set of late, steeply dipping north-northwest, trending joints, with occasional minor displacements are prominent in the competent quartzite units and a number of northeast trending faults are recognized. Bedding is generally parallel to the prominent gneissic or schistose structures in the less competent paragneisses (typical trending 240° azimuth and steeply dipping ^'600-70° to the north). A prominent north to northeast trending, steeply plunging mineral lineation is locally well-developed in the quartzites. Gneissosity is well displayed in the paragneiss units and parallels the lithologic units and layering in quartzites. The property area is dominated by two (2) isoclinal folds: the North Syncline and the Silicon Ridge anticline to the south and these repeat the paragneiss succession and the quartzite layer.
A major anticlinal structure (the Silicon Ridge anticline) cuts through the central part of the property. The central quartzite is exposed on its north limb and a small exposure of quartzite is recognized on its south limb just south of the lake. Four (4) northeast trending faults are recognized to occurring on the property and can be interpreted fom the offsets observed on the magnetic survey map. These are late structures cutting stratigraphic units and later folding and penetrative schistosity. Recognition of these faults and their inferred projections may be important in trying to trace the trends of the quartzite units. Geological mapping in the Silicon Ridge silica project area permitted a better understanding of the structure of the area to outline the extent of the quartzite units and predict prospect for extensions. A better understanding of the structure and local stratigraphy of the area permitted to outline in greater detail the extent of the quartzite units and predict prospective area for extensions.
Future exploration work should be oriented towards the definition of the extent of the quartzite in the north limb of the syncline which appears to be confined or displaced (shifted) by a late northeast trending fault at both its west and east ends. Also, quartzite "F" located on the south part of the Silicon Ridge will require immediate further work including evaluation of the extent of the quartzite, trenching, channel sampling and drilling. The quartzite represents a single layer that has been repeated by a tight to isoclinal synclinal-anticlinal fold structure.
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Table 5 - Samples collected during the 2014 Prospection Workings
Sample UTM-EST UTM-NORD Si02% A1203% Fe203% Ti02% 1 1210604 380673 5293976 97.91 0.69 0.10 0.11 2 1210605 380675 5293978 98.99 0.33 0.10 0.03 3 1210606 380680 5293975 97.97 0.47 0.08 0.13 4 1210607 380679 5293975 99.18 0.40 0.07 0.12 5 1210608 380711 5293954 98.24 0.32 0.07 0.03 6 1210609 380711 5293954 99.54 0.28 0.07 0.02 7 1210610 380746 5293952 99.13 0.59 0.11 0.03 8 J210611 380770 5293950 98.74 0.38 0.09 0.02 9 J210612 380790 5293947 99.36 0.32 0.08 0.02 10 J210613 380783 5293943 98.98 0.17 0.08 0.04 11 J210614 380799 5293937 99.17 0.58 0.10 0.03 12 J210615 380822 5293943 98.39 0.35 0.11 0.05 13 J210616 380822 5293943 98.94 0.75 0.09 0.05 14 J210617 380833 5293943 99.09 0.43 0.12 0.06 15 J210618 380845 5293945 97.86 0.68 0.18 0.07 16 1210619 380850 5293950 98.32 0.59 0.21 0.07 17 J210620 381444 5294625 98.56 0.61 0.11 0.04 18 J210621 381444 5294625 98.33 0.34 0.16 0.07 19 1210622 381563 5294416 98.66 0.90 0.20 0.06 20 1210623 381561 5294425 97.61 0.76 0.31 0.05 21 1210624 380668 5293971 97.68 1.26 0.27 0.06 22 1210625 380663 5293966 92.83 4.20 0.68 0.29
Table 6 - Samples collected during the 2015 Reconnaissance Mapping Program
5102 Outcrop Id Sample Id Comments
1 EC015 R649051 Qzite white cristalline coarse and massive. Little or no staining. 99.08 Qzite white pinkish. Med to coarse grain massive. Cristalling Qzite. Pink staining + some Fe 2 EC017 R649052 99.10 oxide grains along fractures joints. Red staining some hematite grains grey metallic -0.5% 3 ECO21 R649053 Sample on o/c ECO20 SE 98.56 4 ECO22 R649054 Qzite white o/c massive little or no pink 98.88 5 ECO23 R649055 Qzite white coarse cristal massive 98.79 6 EC037 R649056 Qzite white to grey with minor oxidation. North oxidized unit. Not a high quality of Qzite 99.10
Qzite colorless and slightly pinkish with patches. Lower quality it appears. Traces of hematite grain and 7 EC055 R649057 red stained point. Also red stain in fractures. Weathered and oxidized hematite causing stainy of the 98.35 Qzite.
8 EC059 R649058 Qzite white with pink Qzite. Coarse massive crystalline hard. Channel sample planned. 98.16 Qzite white + colorless. Massive coarse crystalline with white bands. Note some pink coloring along the 9 EC062 R649059 98.30 fractures. Weak. Qzite massive. White. Little banding. Coarse crystalline. Minor pink. Weakly to no pink. Traces of 10 EC065 R649060 98.86 Muscovite. 11 EC069 R649061 Qzite white crystalline. Coarse grains. Very minor oxidation and no pink staining. 98.78 12 EC072 R649062 Qzite colorless to white. Crystalline coarse massive. 99.18 Qzite pinkish with white bands. Not good quality. Meta beds? More staining than previous o/c. 13 EC075 R649063 97.85 crystalline coarse banded and massive 14 EC077 R649064 Qzite white. Coarse crystalline massive. Minor pink patches 98.29 15 Qtz-W R649065 Quartzites off the road to Grosse Femelle and on Sitec property, white, coarse fol 53/70NW. 98.83
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SILICON RIDGE SILICA PROPERTY N Heliborne Magnetic Survey, First Vertical Derivative _
A40.3.0. -ï0'3580" ~ lU'3+ f'./ -70'39Z0" se0000 _ ~ x~ano 081.500, Iwo 3~Do ~oD
~ f . . . .
•
g „~ . •. • vy R ~ .(N > O .-II I ~ -4~ Q^~ ~ . •< . 1 f ~- ._ ,ï — ~~r. • • . 11 -- ...... ~ ' -~• .~G. ^•~ . . ~ • ~ ^~ . . .~s.44y~t . . . s, ~ ip s~~ ~-~ ~.•'r ~ • . ~ ii .F' ~°` P.' .' ' . . ~ . r ~ a ~ay _ . •G~ y}~ . V . ~ ., . . 8 ~. • ~ ~ i~Cbl~ • • ~ Legend ~ . cces trail/road: -- • ~+' ~ Exploration access trail: - - - - • _ Power line: -_,...----w-
§,- — -_ N ' ' ' ' ' ' Quartzite (MRNF Sigeom):` ::"-1 : : ~ F, : . Grab sample P 98 09b SiO2): • 1 aeoo0o Nalco 361000 ~ *400 9e10oo 98taÔD `I 983000 aeasoo .70•95xr -WINO' •r0•70•3410*•34'ro' -70'3320- 250 Vertical Derivative r~~ nTlm •22 •2.0 •1.6 •l.e •1.1 -1.2 -t.0 o.a -o.a ~a.. 0.0 0.2 0.4 o.a 1.2 t 111 ~ (meters) t ~ •0.2 o.a .a ~ROGUE NAOO.kGWSI•Up/tpiel ~J ~ ® lfftlVllt51NC.
Figure 10 - Heliborne Magnetic Survey — First Vertical Derivative
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10.0 DIAMOND DRILLING
No diamond drilling has yet been carried out on the Property by Rogue at the moment of the reconnaissance mapping survey.
11.0 PREPARATION, ANALYSIS AND SECURITY
No sampling has yet been completed by Rogue on the Property, except those taken by Geologica for this Technical Report.
1) Each sample was collected using a sledge hammer with a chisel, and quartzite samples that were sampled were the least altered rocks;
2) The sample was placed in a plastic bag and tied with a tie wrap. A numbered sample tag was also placed in the plastic bag with the sample. Each sample number is unique and entered in the database;
3) A lab requisition form was completed with the instructions for assay procedure. The samples requisition forms were delivered by Geologica to the accredited laboratory, ALS Chemex in Val- d'Or, Quebec and a requisition form was signed;
4) At the lab, the samples underwent customary crushing and pulverizing techniques. The entire sample was passed through a primary crusher to a fine crushed product where greater than 70% passed through a minus 2 mm (-10 mesh) screen. Samples were then riffle split to obtain a one kg sample. The one kg crushed sample was then pulverized in a tungsten carbide ring mill pulverizer. All samples were pulverized greater than 75% of the ground material passing through a minus 75- micron screen. Samples were analyzed by ALS Chemex in Vancouver, B.C. for whole rock and trace elements (ME-XRF and ME-XRF06).
12.0 MINERAL PROCESSING AND METALLURGICAL TESTING
No Mineral Processing and Metallurgical testing has yet been undertaken on the Property at the moment of the reconnaissance geological mapping survey.
13.0 MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES
No Mineral Resource and Mineral Reserve Estimates have yet been undertaken on the Property.
14.0 ADJACENT PROPERTIES
A number of companies' have properties adjacent to or next to the Property and have interesting geological and mineralized settings (Figure 11). All references are from the Ministry of Natural Resources Quebec, Gestim.
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To the southwest, Sitec Quartz Inc. and Silicium Québec Société en Commandite have a large property where two (2) deposits (A and B) are presently being mined by open pit method with an annual production of 200,000 to 250,000 tons per year (DV 2013-02; Le Charlevoisien: July 27, 2012).
Other adjacent properties are owned by Fiducie Ananke, Eddy Canova, Pierre Gevry ("I" quartzite deposit), Ian Turner, Uragold Bay Resources, 8889295 Canada Inc., Société d'Exploration Minière Vior Inc., and Entreprises Minières Globex Inc. Other small blocks of mining claims are pending, awaiting MNRQ approval and confirmation.
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350000 370000 390000 4 1 II X)O
Eddy Canova Rogue Resources Inc. Silicon Ridge Silica Property Fiducie Ananke
8889295 Canada inc t \\ % J Eddy Canova
Uragold Bay Resources inc. i f lef Synergy Acquisition Corp.
Silicium Québec Société en Commandite ô ô Sitec Quartz inc. ~ 8889295 Canada inc. f Pierre Geary Parc national des Grands-Jardins 9295 Canada inc. Exploration prohibited National Park (QC) La Malbaie Withdrawn from mining activities Raymond Bédard N. ~I Entreprises Minières Globex Inc
Société d'Exploration Minière Vior inc h
20 From: GESTIM, MRNQ, Oct. 2014 ËOLOGICÂ Nad 83 Utm Zone 19 oaee.COxla~~. Kilometers
350000 370000 390000 410000
Figure 11- Adjacent Properties
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15.0 OTHER RELEVANT DATA AND INFORMATION
Sources and Markets (Ref.: www.sidex.ca)
Silica (Sî02) consists of silicon (Si) and oxygen (0), occuring commonly in igneous, metamorphic, sedimentary rocks as well as in quart veins and altered metasomatic rocks.
Silica is also found in unconsolidated sands and in consolidated rocks such as sandstone, quartzite, quartz veins and quartz-rich pegmatite. The most important market for silica is for glass production, comprising the largest part of the silica market demand. The world silica demand is forecasted to rise by 4.8% annually through 2016 with World Silica Sand Demand of 280 million metric tons in 2016 (Industry Study Freedonia publication, October 2012, page 4).
Other uses for silica include landscaping, filtration, refractory brick, foundry, hydraulic fracturing, abrasive sand blasting, smelter flux, golf course sand traps, silicon carbide, ferro silicon, container glass, float glass, fiber glass, borosilicate glass, solar glass, engineered stone, quartz powder, flux, fused silica, etc.
The demand for high purity silica and high value silica is increasing within industries such as technology, electronics, fiber optics, semiconductors, computer chips, etc. Industrial uses also include high temperature ceramics, thickeners, filters, chemical uses, paints, rubbers, catalysts, adhesives, inks, batteries, cosmetics, pharmaceutical, solar panels, metallurgy, kitchen counter tops and ferro silica metal (Industry Study Freedonia publication, October 2012, page 4).
High purity SiO2 with low contaiminant contents of Fe203, A1203, TiO2 and certain trace elements must respond to high industrial standards and generally correspond to higher market prices.
To the best of the author's knowledge there is no other relevant data or information available that pertains to this report on the Property.
16.0 INTERPRETATION, CONCEPT AND CONCLUSIONS
The information in this section is not necessarily indicative of the mineralization on the property that is the subject of this technical report. The reference to the Production is of a historical nature and is non-compliant with the new version of NI 43-101.
The Silicon Ridge Silica Property hosts three (3) significant northeast trending quartzite units that run across the property and are partly identified and explored. The balance of the Property is largely under- explored and will require prospecting, mapping and sampling to determine extensions of the two (2) known quartzite units as well as the identification of other prospective and favourable silica rich quartzite lithological units. The "D" "G" and "H" east-northeast striking quartzites are also observed on the neighbouring Sitec and contiguous property to the southwest where silica open pit mining is presently taking place. These quartzites can form massive lenses or beds of silica which occurred as sedimentary sequences with locally very high silica contents with limited impurities (<_ 1%).
These quartzite lithological units produce large outcrops with positive topographic relief where trenching and outcrop stripping is necessary. Visual inspection followed by petrography and geochemistry are usually the best approaches to locate high purity silica zones. Promising analysis and assay results will lead to bulk sampling in order to determine the appropriate processing procedures so that the product will meet the desired physical and chemical specifications (specifications vary according to the application for the product).
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page 40 +GÉO][.©GtCA GROUPE-CONSEIL
Decrepitation tests are mandatory for silicon metal or ferrosilicon. Finally, diamond drilling will help define grade continuity and deposit size.
In conclusion, the Silicon Ridge Silica Property of Rogue Resources Inc. consists of eight (8) mining claims (462.6 hectares) located 42 km north of the Town of Baie-Saint-Paul which is on the north shore of the St-Lawrence River in Central Quebec, Canada. The mining claim titles are active and registered to Rogue Resources Inc. and have an expiry date of April 21, 2018.
The property geology consists of folded highly metamorphosed metasedimentary units of the Middle Segment of the La Galette Formation. The silica-rich quartzite lithological units are part of the Petit Lac Malbaie quartzite deposits hosted within amphibole-sillimanite-garnet paragneiss and surrounded by migmatites and charnockites intrusives located in the northwest and southeast corners of the Property.
Quartzites were first discovered in 1946 by prospectors near Lac de la Galette (GM01263, GM35010, GM35675). Other silica rich quartzite occurences were mapped and discovered in the 1970s by the Quebec Ministry of Natural Resources' geologists (RP601A, Rondot 1971) (DPV682, Rondot 1979) and stimulated the interest of prospectors and mining companies in the general area. Ten (10) quartzite lithological units were identified within the Petit Lac Malbaie Group. They were named "A" to "I" and "LM".
The neighbouring Sitec Property, contiguous to the SW corner of the Rogue Property, has the "A" and "B" quartzite silica deposits, at approximately 5 km southwest of the Rogue property, are presently being mined by open pit method with annual production of 200,000 to 250,000 tons per year.
Several studies and resource calculations on the most significant quartzite occurences were completed and recognized the potential of the quartzites of the Petit Lac Malbaie for their rich pure silica and high value silica potential and its specific uses in the industry.
The significant risks and uncertainties in dealing with the exploration information supplied are the continuity of the silica rich quartzite units (variability) due to the structural complexities in the Grenville Province and the potential variability of the silica product. This is where the exploration program of mapping, drilling, sampling and assaying will be utilized to verify the silica oxide contents and the impurities in the quartzites. The purity of the silica product (Si02 content) and limited impurity contents in the product may define the different utilizations. The product will require a characterization to better understand the final uses of the product.
17.0 RECOMMENDATIONS
Future exploration work should be oriented towards collecting bulk samples in the quartzite and carrying out characterization of the silica to better identify the quality and uses of the product.
Futher exploration on the north limb, on the quartzite "H" on the edge of a syncline, is to better define the extent of the quartzite which appears to be limited by a late northeast trending fault at both the west and east ends. Also, quartzite "F" located on the south part of the Silicon Ridge will require further work including evaluation of the extent of the quartzite, trenching, channel sampling and drilling. The quartzite represents a single layer that has been repeated by a tight to isoclinal syncline-anticline fold structure.
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page 41 +GEOLOCICA GROUPE-CONSEIL
18.0 REFERENCES
DP 258 QUARTZITES DU PETIT LAC MALBAIE, COMTE DE CHARLEVOIX. 1974, Par RONDOT, J. 3 pages. 1 microfiche.
DP 323 RAPPORT SUR LA SILICE AU QUEBEC. 1975, Par TIPHANE, M. 72 pages. 5 CARTES / 4F (ECHELLES 1X 1/15 840, 3X 1/63 360, 1X 1/50 000). 3 microfiches.
DPV 346 RAPPORTS DES GEOLOGUES RESIDENTS POUR L'ANNEE 1975. 1976, Par CIMON, J, DUQUETTE, G, LAMARCHE, R Y, LATULIPPE, M, MacINTOSH, J A. 200 pages. 5 microfiches.
DPV 682 RECONNAISSANCES GEOLOGIQUES DANS CHARLEVOIX-SAGUENAY. 1979, Par RONDOT, J. 48 pages. 2 CARTES (ECHELLE 1/250 000). 2 microfiches.
DV 85-08 GITES MINERAUX A TONNAGE EVALUE ET PRODUCTION MINERALE DU QUEBEC. 1985, Par LAVERGNE, C. 84 pages. 2 microfiches.
DV 2001-01 RAPPORT SUR LES ACTIVITES D'EXPLORATION MINIERE AU QUEBEC 2000. 2001, Par GAUDREAU, R, HOULE, P, DOUCET, P, STE-CROIX, L, PERREAULT, S, LACHANCE, S, BELLEMARE, Y, BUTEAU, P, JACOB, H L, MARCOUX, P, CHOINIERE, J. 107 pages. 2 microfiches.
DV 2013-02 REPORT ON MINERAL ACTIVITIES IN QUEBEC - 2012. 2013, Par BERNATCHEZ, M, BLACKBURN, D, CARANGE, V, COTE, S, COUTURIER-DUBE, A, CYR, J, DIONNE, J, DJEMAL, D, DOUCET, P, DUFOUR, M, FRAGASSO, D, GAUDREAU, R, GIRARD, G, KHARIS, A, LABRECQUE, M, LACROIX, R, LAFRANCE, P A, LAMOTHE, J, LESAGE, D, MADORE, L, MARCOUX, P, MAURICE, C, MOORHEAD, J, MOUKHSIL, A, OUELLET, S, PAQUET, J, PROULX, S, RAYMOND, D, ROY, P, TOGOLA, N, ZETCHI, M. 138 pages.
ET 99-04 LES RESSOURCES QUEBECOISES EN SILICE. 2000, Par JACOB, H L. 38 pages. 1 microfiche.
MB 89-21 GEOLOGIE DE CHARLEVOIX. 1989, Par RONDOT, J. 606 pages. 2 CARTES / 19F (ECHELLES 1/250 000 ET 1/20 000). 14 microfiches.
RP 601(A) PRELIMINARY REPORT, GEOLOGY OF THE MARTRES LAKE AREA. 1971, Par RONDOT, J. 13 pages. CARTE 1729 (ECHELLE 1/63 360). 1 microfiche.
TH 1211 ETUDE DES DEFORMATIONS DU METAQUARTZITE DE LA GALETTE, DU COMTE CHARLEVOIX. 1985, Par TREMBLAY, G. 128 pages.
Deposit Files from MRNQ: 21M15-0001, 21M15-0002, 21M10-0001, 21M10-1000
SIDEX Exploring for Silica in Québec, 2002 (www.sidex.com)
HORA, Z.D. Silica in British Columbia. Extract from: "The Geology of Industrial Minerals in Canada", Special Volume 29, The CIMM, p.286.
RONDOT, J. Quartzites purs du Quebecia. Extract from: "The Geology of Industrial Minerals in Canada", Special Volume 29, The CIMM, p.81-87.
TUREK, V. and MacGREGOR, D. Badgeley Island Quartzite deposit. Extract from: "The Geology of Industrial Minerals in Canada", Special Volume 29, The CIMM, p.134-136.
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Appendix I - Statutory Works
GM 01263 REPORT ON CHARLEVOIX GENERAL MINING COMPANY. 1939, Par MALOUF, P M. 11 pages. 1 microfiche.
GM 17602 REPORT. 1965, Par COPELAND, J G. 4 pages. 1 microfiche.
GM 30708 REPORT ON PETIT LAC MALBAIE PROPERTY. 1975, Par HOGAN, H R. 6 pages. 1 carte. 1 microfiche.
GM 32263 RAPPORT GEOLOGIQUE SUR LA PROPRIETE DU CANTON DE CHARLEVOIX-3. 1976, Par MARLEAU, R A. 29 pages. 1 carte. 1 microfiche.
GM 33619 GEOLOGICAL SURVEY, PETIT LAC MALBAIE. 1978, Par HOGAN, H R. 4 pages. 2 cartes. 1 microfiche.
GM 35010 RAPPORT GEOLOGIQUE, PROJET 10-743, SILICE CHARLEVOIX BLOC SUD. 1979, Par GILBERT, J, SAVOIE, A. 7 pages. 1 carte. 1 microfiche.
GM 35038 RELEVES TOPOGRAPHIQUES & PLANS, SILICES DE CHARLEVOIX. 1979, Par CHATEL, P, POIRIER, G. 6 pages. 72 cartes. 27 microfiches.
GM 35675 REPORT OF GEOLOGICAL SURVEY. 1979, Par VELDHUYZEN, H. 34 pages. 2 cartes. 2 microfiches.
GM 36592 RAPPORT, PROJET 10-743, SILICE-CHARLEVOIX. 1980, Par GILBERT, J, MARCOTTE, C, QUINTIN, P, SAVOIE, A. 249 pages. 55 cartes. 16 microfiches.
GM 37749 RAPPORT DES TRAVAUX DE TERRAIN, 1980-81, PROJET 10-743 SILICE. 1981, Par GILBERT, J. 286 pages. 38 cartes. 14 microfiches.
GM 38855 RAPPORT DE SONDAGE, PROJET SILICE, GISEMENT C. 1982, Par GILBERT, J. 22 pages. 2 cartes. 1 microfiche.
GM 39387 ORE RESERVES-PIT OUTLINE-SILICA DEPOSIT, LAFLECHE TWP. 1982, Par ROBERT, J L, MARCHAND, J, HALDE, J. 16 pages. 5 cartes. 2 microfiches.
GM 40982 RESULTATS D'ECHANTILLONNAGES ET ANALYSES. 1983, Par PICHETTE, M. 5 pages. 1 carte. 2 microfiches.
GM 43656 ECHANTILLONNAGE DU DEPOT DE QUARTZITE. 1986, Par GAGNON, A. 5 pages. 1 carte. 1 microfiche.
GM 50836 REPORT ON THE EVALUATION OF QUARTZ EXTENSIONS FROM LEASE 674. 1990, Par TURNER, I. 12 pages. 2 cartes. 1 microfiche.
GM 52345 ETUDE SOMMAIRE DU MARCHE DE LA SILICE. 1993, Par MCCANN, A J. 95 pages. 2 microfiches.
GM 52346 ETUDE DE PRE-FAISABILITE - ALIMENTATION DE L'USINE DE VERRE PLAT DE GLAVERBEC A SAINT-AUGUSTIN, GISEMENT LA GALETTE. 1990, Par GROUPE CONSEIL ROCHE LTEE. 221 pages. 4 microfiches.
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page I G1ÉO]LOGICA G Is OtJ]P]E-CONSEIL,
GM 52347 RAPPORT GEOLOGIQUE DU GISEMENT C, PROJET SILICE 10-743. 1982, Par GILBERT, J. 191 pages. 17 cartes. 7 microfiches.
GM 53288 RAPPORT DE SONDAGE 1995, PROJET SILICE 100743, GISEMENT "C". 1995, Par McCANN, A J. 29 pages. 1 carte. 1 microfiche.
GM 58218 LEVE DE MAGNETOMETRIE ET LEVE AU RDTGPS SUR LE PROJET SAINT-URBAIN. 2000, Par GRANGER, B. 6 pages. 3 cartes. 1 microfiche.
GM 58264 RAPPORT DE PROSPECTION, PROJET 1999-A2-206, SILICON RIDGE. 1999, Par TREMBLAY, F, LAPOINTE, B. 34 pages. 5 cartes. 3 microfiches.
GM 58313 MAPPING EXTENSION SOUTH OF THE MALBAIE QUARRY. 2000, Par VELDHUYZEN, H, TURNER, I. 3 pages. 1 microfiche.
GM 59793 REPORT ON GEOLOGICAL MAPPING AND PROSPECTING ON LAC DE PETIT MALBAIE AREA. 2002, Par TURNER, R W. 6 pages. 1 carte. 1 microfiche.
GM 60851 ASSESSMENT REPORT DESCRIBING PROSPECTING, GEOLOGICAL AND SAMPLING ACTIVITIES. 2003, Par TURNER, R W, YORIO, D. 10 pages. 1 microfiche.
GM 60892 CARACTERISATION PETROGRAPHIQUE ET GEOCHIMIQUE DES QUARTZITES DU GITE DE SILICE DE ST-URBAIN, CHARLEVOIX. 2004, Par CAMIRE, G. 68 pages. 1 microfiche.
GM 62236 ANALYSE PAR SPECTROSCOPIE DE REFLECTANCE PROCHE, INFRAROUGE SUR DES ECHANTILLONS PROVENANT DU GITE DE SILICE DE ST-URBAIN. 2006, Par CAMIRE, G, RICHER- LAFLECHE, M. 40 pages.
GM 62596 EXPLORATION ASSESSMENT REPORT COVERING OVERBURDEN AND OUTCROP TRENCHING. 2006, Par TURNER, R W, YORIO, D. 13 pages. 2 cartes.
GM 62645 EXPLORATION ASSESSMENT REPORT FOR THE SURFACE TRENCHING AND PROSPECTING PROGRAMME ON A PORTION OF BEX 0000236 AND CLAIM 3 2006. 2006, Par TURNER, R W, YORIO, D. 12 pages. 3 cartes.
GM 62651 ASSESSMENT REPORT OF EXPLORATION INCLUDING PROSPECTING, OVERBURDEN TRENCHING, STRIPPING AND BULK SAMPLING OF THE BEC SCIE SILICA SHOWING CLAIM NO 1100286. 2006, Par TURNER, R W. 15 pages. 2 cartes.
GM 63535 ANALYSES PAR SPECTROSCOPIE NIRS ET FLUORESCENCE -X D'ECHANTILLONS DE QUARTZITE PROVENANT DU GITE DE SILICE DE ST-URBAIN. 2008, Par CAMIRE, G, RICHER-LAFLECHE, M. 22 pages.
GM 65022 ASSESSMENT REPORT ON THE EXPLORATION ACTIVITIES, PROJECT BEC SCIE NORTH. 2010, Par TURNER, R W, YORIO, D. 11 pages. 2 cartes.
GM 65085 LEVES D'INDUCTION ELECTROMAGNETIQUE PROMIS-10 ET GEM-2, GITE DE SILICE DE LA PROPRIETE ST-URBAIN. 2010, Par CAMIRE, G, RICHER-LAFLECHE, M. 66 pages.
GM 66041 ASSESSMENT REPORT OF THE PROSPECTING AND ROCK SAMPLING ACTIVITIES IN THE HYDRO ZONE AREA. 2011, Par TURNER, R W. 15 pages. 3 cartes.
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GM 66544 LEVE AUDIOMAGNETOTELLURIQUE A SOURCE NATURELLE (NSAMT), GITE DE SILICE, PROPRIETE ST-URBAIN. 2012, Par RICHER, M, CAMIRE, G. 55 pages.
GM 66670 EXPLORATION ASSESSMENT REPORT COVERING GROUND PROSPECTING WITHIN CELLULE CDC 1099896. 2012, Par TURNER, R W, POULIN, R. 12 pages. 3 cartes.
GM 66790 EXPLORATION ASSESSMENT REPORT COVERING GROUND PROSPECTING WITHIN CDC'S 1099897, 1099898, AND 1099899. 2012, Par TURNER, R W. 11 pages. 3 cartes.
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Appendix II — Laboratory Assay Sheets
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page IV
ALS Canada Ltd. À: ROGUE RESOURCES Page: 1 2103 Dollarton Hwy P.O. BOX 1444, ROYAL CENTRE Nombre total de pages: 2 (A - B) North Vancouver BC V7H 0A7 1055 WEST GEORGIA ST. SUITE 2270 plus les pages d'annexe Téléphone: 604 984 0221 Télécopieur: 604 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 23- SEPT- 2014 ALS www.alsglobal.com Compte: ROGRES minerals CERTIFICAT V014134277 PRÉPARATION ÉCHANTILLONS CODE ALS DESCRIPTION Projet: GRANDE FEMELLE WEI- 21 Poids échantillon reçu CRU- 31 Granulation - 70 % <2 mm PUL- 33 Pulvériser en carbure de tungstène Ce rapport s'applique aux 22 échantillons de autre soumis à notre laboratoire de Val d'Or, QC, Canada le 10- SEPT- 2014. SPL- 21 Echant. fractionné - div. riffles LOG- 22 Entrée échantillon - Reçu sans code barre Les résultats sont transmis à: ALAIN BEAUREGARD PROCÉDURES ANALYTIQUES CODE ALS DESCRIPTION INSTRUMENT ME- XRFO6 Roche totale - XRF XRF OA- GRA06 Perte par calcination pour ME- XRFO6 WST- SIM
À: ROGUE RESOURCES ATTN: ALAIN BEAUREGARD P.O. BOX 1444, ROYAL CENTRE 1055 WEST GEORGIA ST. SUITE 2270 VANCOUVER BC V6E 3P3
Ce rapport est final et remplace tout autre rapport préliminaire portant ce numéro de certificat. Les résultats s'appliquent aux échantillons soumis. Toutes les pages de ce rapport ont été vérifiées et approuvées avant publication. r ~,- Signature: ***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** Colin Ramshaw, Vancouver Laboratory Manager ALS Canada Ltd. À: ROGUE RESOURCES Page: 2 - A 2103 Dollarton Hwy P.O. BOX 1444, ROYAL CENTRE Nombre total de pages: 2 (A - B) North Vancouver BC V7H 0A7 1055 WEST GEORGIA ST. SUITE 2270 plus les pages d'annexe Téléphone: 604 984 0221 Télécopieur: 604 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 23- SEPT- 2014 www.alsglobal.com Compte: ROGRES Projet: GRANDE FEMELLE 11111111111111111111=11 IIMIII.MIR CERTIFICAT D'ANALYSE V014134277
Méthode WEI-21 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 ME XRFO6 élément Poids reçu Si02 A1203 Fe203 Ca0 Mg0 Na20 K20 Cr203 TiO2 Mn0 P205 Sr() BaO LOI unités kg % % % % % % % % % % % % % % Description échantillon L.D. 0.02 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.001 0.01 0.01 0.01
J210604 1.24 97.91 0.69 0.10 0.01 0.02 0.01 0.05 0.01 0.11 <0.01 0.013 <0.01 0.03 0.30 J210605 1.43 98.99 0.33 0.10 0.08 0.02 0.01 0.05 0.01 0.03 <0.01 0.075 <0.01 0.01 0.14 J210606 1.97 97.97 0.47 0.08 <0.01 0.02 <0.01 0.07 0.01 0.13 <0.01 0.007 <0.01 0.02 0.17 J210607 1.52 99.18 0.40 0.07 <0.01 0.02 0.01 0.06 0.01 0.12 <0.01 0.005 <0.01 0.01 0.11 J210608 2.45 98.24 0.32 0.07 <0.01 0.02 <0.01 0.03 0.01 0.03 <0.01 0.009 <0.01 0.01 0.17 J210609 1.82 99.54 0.28 0.07 <0.01 0.02 0.01 0.02 0.01 0.02 <0.01 0.007 <0.01 0.01 0.14 J210610 1.90 99.13 0.59 0.11 0.01 0.02 0.01 0.09 0.01 0.03 <0.01 0.007 <0.01 0.01 0.16 J21 061 1 2.22 98.74 0.38 0.09 <0.01 0.02 0.01 0.08 0.01 0.02 <0.01 0.006 <0.01 0.01 0.09 J21 061 2 2.34 99.36 0.32 0.08 <0.01 0.02 <0.01 0.06 0.01 0.02 <0.01 0.007 <0.01 0.01 0.11 J21 061 3 2.26 98.98 0.17 0.08 <0.01 0.02 0.01 0.03 0.01 0.04 <0.01 0.002 <0.01 0.01 0.06 J210614 1.72 99.17 0.58 0.10 <0.01 0.02 0.01 0.05 0.01 0.03 <0.01 0.004 <0.01 0.01 0.15 J21 061 5 1.63 98.39 0.35 0.11 <0.01 0.02 <0.01 0.06 0.01 0.05 <0.01 0.006 <0.01 0.01 0.11 J210616 2.21 98.94 0.75 0.09 0.02 0.02 0.01 0.09 0.01 0.05 <0.01 0.006 <0.01 0.01 0.11 J21 061 7 2.30 99.09 0.43 0.12 0.01 0.02 0.01 0.05 0.01 0.06 <0.01 0.009 <0.01 0.01 0.11 J21 061 8 2.47 97.86 0.68 0.18 <0.01 0.02 0.01 0.04 0.01 0.07 <0.01 0.015 <0.01 0.01 0.20 J21 061 9 1.69 98.32 0.59 0.21 <0.01 0.05 <0.01 0.11 0.01 0.07 <0.01 0.007 <0.01 0.01 0.18 J210620 2.13 98.56 0.61 0.11 <0.01 0.03 0.02 0.24 0.01 0.04 <0.01 0.006 <0.01 0.03 0.12 J210621 1.71 98.33 0.34 0.16 <0.01 0.03 <0.01 0.05 0.02 0.07 <0.01 0.004 <0.01 0.01 0.14 J21 062 2 2.10 98.66 0.90 0.20 0.01 0.06 0.04 0.13 0.01 0.06 <0.01 0.007 <0.01 0.01 0.25 J21 062 3 1.16 97.61 0.76 0.31 0.01 0.06 0.03 0.11 0.01 0.05 <0.01 0.005 <0.01 0.01 0.26 J210624 1.17 97.68 1.26 0.27 0.02 0.07 0.13 0.60 0.01 0.06 <0.01 0.017 <0.01 0.04 0.16 J21 062 5 2.28 92.83 4.20 0.68 <0.01 0.22 0.03 0.53 0.01 0.29 0.01 0.012 <0.01 0.05 0.69
***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** ALS Canada Ltd. À: ROGUE RESOURCES Page: 2 - B 2103 Dollarton Hwy P.O. BOX 1444, ROYAL CENTRE Nombre total de pages: 2 (A - B) North Vancouver BC V7H 0A7 1055 WEST GEORGIA ST. SUITE 2270 plus les pages d'annexe Téléphone: 604 984 0221 Télécopieur: 604 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 23- SEPT- 2014 www.alsglobal.com Compte: ROGRES Projet: GRANDE FEMELLE 1111111111111111=11 CERTIFICAT D'ANALYSE V014134277
Méthode ME-XRF06 élément Total unités % Description échantillon L.D. 0.01
J210604 99.24 J210605 99.85 J210606 98.93 J210607 99.99 J210608 98.89 J210609 100.15 J210610 100.15 J21 061 1 99.45 J21 061 2 99.99 J21 061 3 99.41 J210614 100.15 J21 061 5 99.10 J210616 100.10 J21 061 7 99.92 J21 061 8 99.09 J21 061 9 99.53 J210620 99.77 J210621 99.14 J210622 100.35 J210623 99.21 J210624 100.30 J21 062 5 99.53
***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** ALS Canada Ltd. À: ROGUE RESOURCES Page: Annexe 1 2103 Dollarton Hwy P.O. BOX 1444, ROYAL CENTRE Total # les pages d'annexe: 1 North Vancouver BC V7H 0A7 1055 WEST GEORGIA ST. SUITE 2270 Finalisée date: 23- SEPT- 2014 Téléphone: 604 984 0221 Télécopieur: 604 984 0218 VANCOUVER BC V6E 3P3 Compte: ROGRES www.alsglobal.com
Projet: GRANDE FEMELLE CERTIFICAT D'ANALYSE V014134277
COMMENTAIRE DE CERTIFICAT
ADRESSE DE LABORATOIRE Traité à ALS Val d'Or, 1 324 Rue Turcotte, Val d'Or, QC, Canada. Applique à la Méthode: CRU- 31 LOG- 22 SPL- 21 WEI- 21
Traité à ALS Vancouver, 2103 Dollarton Hwy, North Vancouver, BC, Canada. Applique à la Méthode: ME- XRFO6 OA- GRA06 PUL- 33
ALS Canada Ltd. À: ROGUE RESOURCES Page: 1 2103 Dollarton Hwy 2270 - 1055 WEST GEORGIA STREET Nombre total de pages: 2 (A - D) North Vancouver BC V7H 0A7 PO BOX 11144 plus les pages d'annexe Téléphone: +1 (604) 984 0221 Télécopieur: +1 (604) 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 9-JUIL-2015 www.alsglobal.com Compte: ROGRES ALS Minerals CERTIFICAT SD15091853 PRÉPARATION ÉCHANTILLONS CODE ALS DESCRIPTION
Projet: Silica WEI-21 Poids échantillon reçu LOG-22 Entrée échantillon - Reçu sans code barre CRU-QC Test concassage QC Ce rapport s'applique aux 14 échantillons de roche soumis à notre laboratoire de Val PUL-QC Test concassage QC d'Or, QC, Canada le 22-JUIN-2015. CRU-31 Granulation - 70 % <2 mm Les résultats sont transmis à: SPL-22Y EDDY CANOVA PUL-33 Pulvériser en carbure de tungstène LOG-24 Entrée pulpe - Reçu sans code barre
PROCÉDURES ANALYTIQUES CODE ALS DESCRIPTION INSTRUMENT ME-ICP61 33 éléments, quatre acides ICP-AES ICP-AES ME-XRF26 XRF OA-GRA05x LOI pour XRF WST-SEQ
À: ROGUE RESOURCES ATTN: EDDY CANOVA 905 PLYMOUTH AVE. SUITE 311 MONTRÉAL QC H4P 164
Ce rapport est final et remplace tout autre rapport préliminaire portant ce numéro de certificat. Les résultats s'appliquent aux échantillons soumis. Toutes les pages de ce rapport ont été vérifiées et approuvées avant publication. Signature: ***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** Colin Ramshaw, Vancouver Laboratory Manager ALS Canada Ltd. A: ROGUE RESOURCES Page: 2 - A 2103 Dollarton Hwy 2270 - 1055 WEST GEORGIA STREET Nombre total de pages: 2 (A - D) North Vancouver BC V7H 0A7 PO BOX 11144 plus les pages d'annexe Téléphone: +1 (604) 984 0221 Télécopieur: +1 (604) 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 9-JUIL-2015 www.alsglobal.com Compte: ROGRES Projet: Silica ■•••■ ■ C■ coi.m. CERTIFICAT D'ANALYSE SD15091853
Méthode wEI-21 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 ME-XRF26 élément Poids reçu Al2O3 BaO Ca0 Cr203 Fe203 K20 Mg0 MnO Na20 P205 S03 Si02 SKI) TiO2 unités kg % % % % % % % % % % % % % % Description échantillon LD. 0.02 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.01
R649051 0.68 0.29 0.01 0.01 0.01 0.03 0.02 <0.01 <0.01 <0.01 <0.01 <0.01 99.08 <0.01 0.05 R649052 0.77 0.37 0.01 0.01 0.01 0.05 0.05 0.01 <0.01 0.01 <0.01 <0.01 99.10 0.01 0.07 R649053 1.43 0.33 0.01 0.01 0.01 0.04 0.04 <0.01 <0.01 <0.01 <0.01 <0.01 98.56 0.01 0.04 R649054 0.99 0.19 0.02 <0.01 0.01 0.03 0.02 <0.01 <0.01 <0.01 <0.01 0.01 98.88 0.01 0.05 R649055 1.34 0.47 0.01 0.01 0.01 0.05 0.10 <0.01 <0.01 0.01 <0.01 <0.01 98.79 <0.01 0.05 R649056 1.36 0.15 <0.01 0.01 0.01 0.08 0.02 <0.01 <0.01 <0.01 <0.01 0.01 99.10 <0.01 0.06 R649057 1.50 0.31 0.01 0.01 0.02 0.13 0.06 <0.01 <0.01 <0.01 <0.01 0.02 98.35 0.01 0.09 R649058 0.34 0.52 0.01 0.06 0.01 0.09 0.05 0.02 <0.01 0.05 0.01 0.02 98.16 0.01 0.05 R649059 1.00 0.59 0.01 0.01 0.01 0.07 0.02 <0.01 <0.01 0.02 <0.01 0.01 98.30 <0.01 0.08 R649060 1.63 0.31 0.01 0.01 0.01 0.05 0.03 <0.01 <0.01 0.01 <0.01 0.01 98.86 <0.01 0.05 R649061 0.93 0.27 0.01 0.01 0.01 0.05 0.02 <0.01 <0.01 <0.01 <0.01 0.01 98.78 0.01 0.06 R649062 0.44 0.33 0.01 0.02 0.01 0.06 0.02 <0.01 <0.01 0.01 <0.01 0.01 99.18 0.01 0.05 R649063 2.33 0.53 0.01 0.01 0.02 0.07 0.04 <0.01 <0.01 0.01 0.01 0.01 97.85 0.01 0.08 R649064 0.52 0.39 0.01 0.01 0.01 0.06 0.12 <0.01 <0.01 <0.01 <0.01 0.08 98.29 0.01 0.07
***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** ALS Canada Ltd. A: ROGUE RESOURCES Page: 2 - B 2103 Dollarton Hwy 2270 - 1055 WEST GEORGIA STREET Nombre total de pages: 2 (A - D) North Vancouver BC V7H 0A7 PO BOX 11144 plus les pages d'annexe Téléphone: +1 (604) 984 0221 Télécopieur: +1 (604) 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 9-JUIL-2015 www.alsglobal.com Compte: ROGRES Projet: Silica ■•••■ ■ C■ coi.m, CERTIFICAT D'ANALYSE SD15091853
Méthode ME-XRF26 0A-GRA05x ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 élément Total LOI 1000 Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe Ga unités % % ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm Description échantillon L D. 0.01 0.01 0.5 0.01 5 10 0.5 2 0.01 0.5 1 1 1 0.01 10
R649051 99.66 0.05 <0.5 0.15 <5 10 <0.5 <2 <0.01 <0.5 782 27 2 0.02 <10 R649052 99.87 0.08 <0.5 0.18 <5 30 <0.5 <2 <0.01 <0.5 577 45 <1 0.03 <10 R649053 99.25 0.11 <0.5 0.16 <5 10 <0.5 3 <0.01 <0.5 598 30 <1 0.02 <10 R649054 99.39 0.05 <0.5 0.10 <5 <10 <0.5 2 <0.01 <0.5 810 29 <1 0.01 <10 R649055 99.68 0.08 <0.5 0.24 <5 20 <0.5 <2 <0.01 <0.5 687 27 <1 0.02 <10 R649056 99.57 0.02 <0.5 0.07 <5 10 <0.5 3 0.01 <0.5 778 46 <1 0.04 <10 R649057 99.16 0.06 <0.5 0.16 <5 <10 <0.5 <2 0.01 <0.5 650 57 3 0.08 <10 R649058 99.32 0.17 <0.5 0.26 <5 10 <0.5 <2 0.04 <0.5 656 36 1 0.05 <10 R649059 99.32 0.09 <0.5 0.27 <5 <10 <0.5 2 <0.01 <0.5 688 59 1 0.05 <10 R649060 99.63 0.18 <0.5 0.15 <5 10 <0.5 2 <0.01 <0.5 726 59 <1 0.03 <10 R649061 99.40 0.07 <0.5 0.13 <5 <10 <0.5 <2 <0.01 <0.5 696 51 1 0.03 <10 R649062 99.89 0.09 <0.5 0.17 <5 <10 <0.5 <2 0.01 <0.5 663 41 <1 0.03 <10 R649063 98.97 0.23 <0.5 0.28 <5 20 <0.5 2 <0.01 <0.5 689 54 <1 0.04 <10 R649064 99.25 0.11 <0.5 0.19 <5 <10 <0.5 <2 <0.01 <0.5 686 34 <1 0.03 <10
***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** ALS Canada Ltd. A: ROGUE RESOURCES Page: 2 - C 2103 Dollarton Hwy 2270 - 1055 WEST GEORGIA STREET Nombre total de pages: 2 (A - D) North Vancouver BC V7H 0A7 PO BOX 11144 plus les pages d'annexe Téléphone: +1 (604) 984 0221 Télécopieur: +1 (604) 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 9-JUIL-2015 www.alsglobal.com Compte: ROGRES Projet: Silica ■i.i■ iC■ i7i,m, CERTIFICAT D'ANALYSE SD15091853
Méthode ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 élément K La Mg Mn Mo Na Ni P Pb S Sb Sc Sr Th Ti unités % ppm % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm % Description échantillon LD. 0.01 10 0.01 5 1 0.01 1 10 2 0.01 5 1 1 20 0.01
R649051 0.02 10 <0.01 <5 2 <0.01 4 30 2 <0.01 <5 <1 2 <20 0.01 R649052 0.04 10 <0.01 <5 3 0.01 <1 20 <2 <0.01 <5 <1 3 <20 0.01 R649053 0.03 10 <0.01 <5 3 <0.01 2 20 <2 <0.01 <5 <1 2 <20 0.01 R649054 0.01 10 <0.01 <5 2 <0.01 2 20 <2 <0.01 6 <1 2 <20 0.01 R649055 0.09 10 <0.01 <5 2 <0.01 <1 20 <2 <0.01 <5 <1 4 <20 0.01 R649056 0.01 <10 0.01 <5 2 <0.01 <1 10 <2 <0.01 <5 <1 2 <20 0.03 R649057 0.04 10 <0.01 <5 3 <0.01 1 20 <2 <0.01 <5 <1 4 <20 0.03 R649058 0.03 10 0.02 7 2 0.04 2 20 <2 0.01 <5 <1 7 <20 0.01 R649059 0.01 10 <0.01 <5 3 0.01 2 20 <2 <0.01 <5 <1 2 <20 0.02 R649060 0.02 10 <0.01 <5 3 <0.01 1 30 <2 <0.01 <5 <1 3 <20 0.01 R649061 0.01 10 <0.01 <5 3 <0.01 2 20 <2 <0.01 <5 <1 2 <20 0.02 R649062 0.01 10 <0.01 <5 2 0.01 1 20 <2 <0.01 <5 <1 4 <20 0.01 R649063 0.04 10 <0.01 <5 2 0.01 1 30 <2 <0.01 <5 <1 4 <20 0.03 R649064 0.02 10 <0.01 <5 2 <0.01 1 20 <2 <0.01 <5 <1 3 <20 0.03
***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** ALS Canada Ltd. À: ROGUE RESOURCES Page: 2 - D
2103 Dollarton Hwy 2270 - 1055 WEST GEORGIA STREET Nombre total de pages: 2 (A - D) North Vancouver BC V7H 0A7 PO BOX 11144 plus les pages d'annexe Téléphone: +1 (604) 984 0221 Télécopieur: +1 (604) 984 0218 VANCOUVER BC V6E 3P3 Finalisée date: 9-JUIL-2015 www.alsglobal.com Compte: ROGRES ■...■ ■ v■ vi.mo Projet: Silica CERTIFICAT D'ANALYSE SD15091853
Méthode ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 ME-ICP61 élément TI U V w Zn unités ppm ppm ppm ppm ppm Description échantillon L.D. 10 10 1 10 2
R649051 <10 <10 1 360 2 R649052 <10 <10 1 420 <2 R649053 <10 <10 2 510 <2 R649054 <10 <10 1 450 <2 R649055 <10 10 1 500 <2
R649056 <10 <10 1 510 <2 R649057 <10 <10 3 460 <2 R649058 <10 <10 1 420 <2 R649059 <10 <10 2 390 <2 R649060 <10 <10 1 370 <2
R649061 <10 <10 2 430 <2 R649062 <10 <10 1 360 <2 R649063 <10 <10 2 400 <2 R649064 <10 <10 4 490 <2
***** Voir la page d'annexe pour les commentaires en ce qui concerne ce certificat ***** ALS Canada Ltd. À: ROGUE RESOURCES Page: Annexe 1
2103 Dollarton Hwy 2270 - 1055 WEST GEORGIA STREET Total # les pages d'annexe: 1 North Vancouver BC V7H 0A7 PO BOX 11144 Finalisée date: 9-JUIL-2015 Téléphone: +1 (604) 984 0221 Télécopieur: +1 (604) 984 0218 VANCOUVER BC V6E 3P3 Compte: ROGRES www.alsglobal.com
Projet: Silica MOM iC■ 1=111.M0 CERTIFICAT D'ANALYSE SD15091853
COMMENTAIRE DE CERTIFICAT
ADRESSE DE LABORATOIRE Traité à ALS Sudbury, 1351-B Kelly Lake Road, Unit #1, Sudbury, ON, Canada. Applique à la Méthode: CRU-31 CRU-QC LOG-22 LOG-24 SPL-22Y WEI-21
Traité à ALS Vancouver, 2103 Dollarton Hwy, North Vancouver, BC, Canada. Applique à la Méthode: ME-ICP61 ME-XRF26 OA-GRA05x PUL-33 PUL-QC GEOLOGICA GROUPE-CONSEIL
Appendix Ill — Photos
Silicon Ridge, viewed to the southwest
Exposure of quartzite immediately south of Silicon Ridge
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XVI +GEOLOCIECA GROUPE-CONSEIL
Quartz-feldspar garnet paragneiss in the basal part of Unit 3 (Station DT-50)
Details of garnets in paragneis (Station DT-09)
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XVII +GEOLOCIECA GROUPE-CONSEIL
Granitic orthogneiss immediately west of the Lake Fault (Station DT-23)
Tight to isoclinal rootless minor folds in felsic paragneiss of Unit la (Station DT-01)
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XVIII +GEOLOCICA +GROUP&CONS EII.,
Isoclinal minor folds in layered pyroxenite/amphibolite unit showing (Station DT-52)
Foliated pyroxenite/amphibolite (unit 1B); note feldspar rich layers (Station DT-04)
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XIX GÉO]LOGICA GROUPE-CONSEII.,
Siliceous paragneiss of Unit la with irregular coarser grained migmatite layers (Station DT-02)
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XX +G]ÉO]LOGICA GROUPE-CONSEIL
Sampling of the "G" Quartzite in the SW part of the Property
White and light pink quartz of the "G" Quartzite of the Petit Lac Malbaie
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XXI +G]ÉO]LOGICA GROUPE-CONSEIL
Sampling of "G" Quartzite in SW of the Property
Sampling an other Quartzite in the north part of the Property
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XXII +G]ÉO]LOGICA GROUPE-CONSEIL
Sampling of "G" Quartzite in north central part of the Property
Idem
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XXIII +G]ÉO]LOGICA GROUPE-CONSEIL
Appendix IV - Reconnaissance Mapping Program
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XXIV La Grosse Femelle Silica Property Mapping - Boulder and Outcrop Descriptions
Point ID Utm-Est Utm-Nord Type Descriptions 1 EC084 380298.00 5294567.00 Boulder Rounded granite boulders 2 EC087 380187.00 5294748.00 Boulder Gneiss or charnockite boulders, end of line 6 W to 9+25N 3 GG001 380291.00 5293739.00 Boulder Tonalite boulder (magmatite) pinkish white, granular, massive, feldspar 4 GG009 380351.00 5293555.00 Boulder Boulder 2x3m, paragneiss, massive, tonalitic 5 GG017 381364.00 5293496.00 Boulder Paragneiss boulder 6 GG022 381253.00 5293698.00 Boulder Beige to black charnockite boulder, grained rock, migmatite with charnockitic bands. ATV path 7 GG030 380421.00 5294785.00 Boulder Rounded beige granular and massive tonalite boulder 8 GG031 380404.00 5294808.00 Boulder Banded tonalite, granulite boulder 3x2m. 9 GG032 380381.00 5294851.00 Boulder 2 Boulders (1X1m et 2X3m) massive rounded tonalite, beige to pale pink 10 GG042 380777.00 5294551.00 Boulder Tonalite charnockite rounded boulder (1X1m) 11 GG043 380819.00 5294477.00 Boulder Pink grey granulite boulder, granular (3X4m) 12 GG044 380842.00 5294433.00 Boulder Pink grey granulite boulder, granular 13 GG046 380944.00 5294262.00 Boulder Beige grey charnockite granulite boulder, granular, porphyric 14 GG047 380990.00 5294177.00 Boulder Rounded granulite boulder 15 GG048 380999.00 5294160.00 Boulder Boulder (1X1m) granulite, tonalite, base Line, road 16 GG049 381037.00 5294094.00 Boulder Beige granulite boulder (1X1m) 17 GG050 381056.00 5294061.00 Boulder Granitic gneiss boulder 18 GG051 381074.00 5294029.00 Boulder Paragneiss and granulite boulders > 1m 19 GG070 380726.00 5295069.00 Boulder Locally porphyric rounded granulite boulders, secondary road, azimut 75 deg. 20 GG072 380626.00 5295245.00 Boulder Rounded granulite boulders, beige to pale grey granular intrusive rocks 21 GG074 380603.00 5295298.00 Boulder Granulite boulders, slope to the north 22 GG076 380810.00 5295250.00 Boulder Beige to pale grey rounded granulite, tonalite, charnockite, migmatite, granular porphyric boulders, slope beginning to the south, glacial till + massive intrusive rocks boulders 23 GG077 380836.00 5295210.00 Boulder Rounded beige granulite boulder (7X8m), middle of steep slope to the south, dense forest. 24 GG078 380932.00 5295041.00 Boulder Tonalite boulder (1X1m) quartzite, former skidder trail 25 GG080 381115.00 5294736.00 Boulder Rounded beige tonalite, downward slope to the south, end of the top of the plateau. 26 GG084 381333.00 5294380.00 Boulder Boulders, top of the slope to the south ridge 27 GG112 381302.00 5294856.00 Boulder Granulite boulder with quartzite fragments 28 GG113 381206.00 5295015.00 Boulder Paragneiss boulder, granulite. massive, granular, pink beige (2-3 X 4-5m) 29 GG114 381120.00 5295175.00 Boulder Numerous paragneiss boulders, rounded granulite, massive, granular, pink beige 30 GG116 381337.00 5294788.00 Boulder Granulite boulders, upward slope to the south 31 GG125 381607.00 5294312.00 Boulder Locally tonalite boulders, granulite, migmatite, paragneiss garnets, high summit plateau, downhill to the lake 32 GG146 382418.00 5293754.00 Boulder Quartzite boulder 33 GG151 382153.00 5294142.00 Boulder Tonalite boulder (1X1m), south border of the lake, EW trail junction 34 GG153 382037.00 5294359.00 Boulder Paragneiss boulder, garnets (3X4m) 35 GG158 381610.00 5293417.00 Boulder Tonalite boulder, quartzite, paragneiss (1-3m) creek, azimut 320 deg 36 GG159 381544.00 5293559.00 Boulder Paragneiss boulders, garnets, top of the hill 37 GG162 381707.00 5293679.00 Boulder Migmatite boulders (1X3m), erratic fragments, granulite and/or paragneiss garnets (almandin, pyrope) top of the hill 38 GG165 381968.00 5293640.00 Boulder Rounded corners granulite boulders, porphyric tonalite (1-2m X 3-4m) 39 GG166 381873.00 5293823.00 Boulder Dispersed granulite-tonalite boulders, downward slope towards the lake, caribou path junction 40 GG168 381995.00 5294008.00 Boulder Quartzite boulder, south limit of the lake 41 GG169 382038.00 5293934.00 Boulder Rounded pink beige granulite boulder, upward slope to the south 42 GG218 382404.00 5294537.00 Boulder Granulite boulders, few tonalites, glacial till soil 43 GG220 382337.00 5294652.00 Boulder Angular quartzite boulder (1x1m) 44 GG226 382588.00 5294208.00 Boulder Dispersed boulders, mistakes on tags (line cutters) Line 12 E 7+75 not 8, 25 m error 45 GG227 382635.00 5294123.00 Boulder Paragneiss and granulite boulders 46 GG235 381951.00 5294938.00 Boulder Locally subangular to rounded boulders, granulite, paragneiss, low topo (1-2m X 2-3m) 47 GG236 381896.00 5295043.00 Boulder White granulie block, high topo, summit 48 GG239 381827.00 5295176.00 Boulder Granulite erratic blocks 49 GG240 381646.00 5295075.00 Boulder White beige and pink tonalite-granulite block
1 EC093 380595.00 5294088.00 Outcrop Quartz feldspar paragneiss with garnet (5-8%) 2 EC093B 380603.00 5294069.00 Outcrop Paragneiss oxyde 3 EC093C 380604.00 5294066.00 Outcrop Quartz feldspar biotite paragneiss 4 EC094A 380625.00 5294038.00 Outcrop Paragneiss, end of plateau, cliff 5 EC094B 380628.00 5294028.00 Outcrop Paragneiss 6 EC095 380636.00 5294023.00 Outcrop Paragneiss, end of the cliff 7 EC096 380647.00 5294008.00 Outcrop Paragneiss 8 EC097 380672.00 5293991.00 Outcrop Quartzite and paragneiss contact, L6W 0+15N 9 GG002 380230.00 5293699.00 Outcrop Paragneiss 4x6m, foliation, Az. 300/75 Subvertical SE
Page 1 de 2 Point ID Utm-Est Utm-Nord Type Descriptions 10 GG003 380208.00 5293688.00 Outcrop Paragneiss with garnets 11 GG013 381046.00 5293615.00 Outcrop Paragneiss (2x3m) downward slope to the south 12 GG052 381091.00 5294000.00 Outcrop Beige paragneiss cliff, feldspar and garnets (10%) quartz veimlets 1- 2 cm or felsic banded (mobilized, recristallized quartz cumulate) 13 GG053 381103.00 5293971.00 Outcrop Paragneiss, steep slope cliff, banded, siliceous 10 - 50 cm, saccharoide texture, end of cut line 2+355 14 GG055 380874.00 5293968.00 Outcrop Already sampled white quartzite, probable contact to the south 15 GG056 380864.00 5293984.00 Outcrop Quartzite 16 GG057 380851.00 5294000.00 Outcrop White-pink quartzite, paragneiss block 17 GG058 380849.00 5294010.00 Outcrop Pinkish white quartzite (1X2m) 18 GG079 380969.00 5294968.00 Outcrop Brown-beige banded paragneiss (3x2m) top of hill, high plateau 19 GG086 381373.00 5294302.00 Outcrop Massive paragneiss (cliff) between 0+50N and BL. 20 GG087 381429.00 5294216.00 Outcrop Paragneiss, bottom of cliff, clear zone, former skidder path 21 GG094 381057.00 5294467.00 Outcrop Paragneiss - migmatite 22 GG100 381116.00 5294559.00 Outcrop Quartzite (10x15m outcrop). Massive, slightly altered and rose, locally brecciated, to sampled with a saw. 23 GG101 381341.00 5294591.00 Outcrop Gneissic migmatite (5x30m) white-beige-brown, locally oxyded, granular, locally brecciated and banded, feldspar rich + qtz + almandins garnets (10-15%) 24 GG102 381444.00 5294630.00 Outcrop Locally transparent white quartzite (5x10m) 25 GG103 381489.00 5294616.00 Outcrop White to beige migmatite with garnets (15-20%) 26 GG104 381548.00 5294612.00 Outcrop White to beige migmatite (10x35m) 27 GG105 381569.00 5294581.00 Outcrop Whitish migmatite with garnets (5x20m) 28 GG106 381568.00 5294528.00 Outcrop Migmatite (10x40m), locally gossan, pyrite (1%) and biotite 29 GG107 381681.00 5294420.00 Outcrop Banded migmatite (10x20m) 30 GG109 381797.00 5294387.00 Outcrop Paragneiss garnets or migmatite, cliff, view of the lake 31 GG110 381693.00 5294557.00 Outcrop Paragneiss or migmatite (20x75m) 32 GG117 381448.00 5294589.00 Outcrop Beige to grey migmatite with more siliceous horizons, upslope 33 GG122 381789.00 5294448.00 Outcrop Pink and black banded granitic gneiss, (7x30m) E-W road 34 GG123 381910.00 5294504.00 Outcrop Rose and black banded granitic gneiss (20x30m) side of road 35 378772.00 5293766.00 Outcrop White quartzite (10X20) sample collected out of the west limit of the property (sample no. R649065) 36 GG126 381626.00 5294280.00 Outcrop Paragneiss (10x20m) 37 GG131 381834.00 5294313.00 Outcrop Siliceous paragneiss (top of the hill) 38 GG132 381811.00 5294353.00 Outcrop Siliceous paragneiss (bottom of the hill) 39 GG133 381805.00 5294378.00 Outcrop Paragneiss, pink garnets (tonalite - granulites?) beginning of cliff 40 GG141 382421.00 5294018.00 Outcrop Quartzite 41 GG145 382516.00 5293787.00 Outcrop Siliceous quartzite and paragneiss contact, quartzite enclave on paragneiss 42 GG154 381954.00 5294509.00 Outcrop Paragneiss garnets (4x6m) banded 5-15cm 43 GG170 382049.00 5293903.00 Outcrop Beige to pink quartzite (locally hematized) (10x50m) 44 GG171 382060.00 5293891.00 Outcrop Milky white quartzite, red hematized, locally fractured (10x30m) 45 GG172 382068.00 5293865.00 Outcrop Beige paragneiss garnets, medium grain 46 GG175 382135.00 5293738.00 Outcrop White massive granulite (10x30m) 47 GG182 382368.00 5293505.00 Outcrop Banded paragneiss, outcrop and boulder (3x4m) 48 GG183 381914.00 5293610.00 Outcrop White-beige granite-granulite, massive, coarse grain, porphyric with feldspars, outcrop on ATV path 49 GG212 382060.00 5294569.00 Outcrop Paragneiss (3x15m) on ATV path 50 GG213 382330.00 5294553.00 Outcrop Black amphibolite (20x40m), massive, grenular, coarse grain, Labradorite 51 GG214 382326.00 5294573.00 Outcrop Non magnetique glacial striation, only magnetic on oxyded parts 52 GG221 382415.00 5294686.00 Outcrop Banded paragneiss quartite contact, enclaves? 53 GG228 382432.00 5294697.00 Outcrop Paragneiss (5x10m) 54 GG229 382282.00 5294645.00 Outcrop Banded Paragneiss 55 GG230 382255.00 5294667.00 Outcrop Banded Paragneiss 56 GG233 382048.00 5294743.00 Outcrop White Quartzite 57 GG234 382036.00 5294762.00 Outcrop White Quartzite, top of outcrop 58 GG242 381782.00 5294822.00 Outcrop Banded paragneiss, cliff 59 GG243 381784.00 5294818.00 Outcrop Milky white massive quartzite, looks pure, 10-15m thickness 60 GG245 381802.00 5294782.00 Outcrop Paragneiss 61 GG248 381903.00 5294604.00 Outcrop paragneiss 62 GG249 381912.00 5294581.00 Outcrop Massive white quartzite, cliff (15x20m) 63 GG250 381924.00 5294558.00 Outcrop Paragneiss, at the top (2x3m) 64 GG251 381936.00 5294517.00 Outcrop Paragneiss (5x7m) 65 GG252 382053.00 5294577.00 Outcrop Banded paragneiss 66 GG253 381629.00 5294380.00 Outcrop Banded paragneiss 67 GG254 381715.00 5294434.00 Outcrop Banded paragneiss 68 GG255 381765.00 5294449.00 Outcrop Paragneiss, ATV path junction 69 GG257 381693.00 5294566.00 Outcrop Paragneiss, top of the hill 70 GG259 380885.00 5294436.00 Outcrop Massive intrusive Rocks, beige-grey to pink, medium grain, non banded
Page 2 de 2 +G]ÉO]LOGICA GROUPE-CONSEIL
Map 1— Geological Map, Reconnaissance Mapping and Field Sample Locations
2016 FIELD WORK REPORT ON THE SILICON RIDGE SILICA PROPERTY Page XXVII Carte 4. Localisation des Decapage R1, R2, R3, R4, R5, R12, R13, et R14.
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Legend Trace de Decapage
R6 No de Decapage 'i4' BL ----Contact Qtzite I. Point d'Affleurement • M4 QzBoGrtGneiss " M4b MtQzBoGneiss M12 WhPkQtzite PkRdDefQtzite CDC-2402792 Claim 25 lo 75 100m Dessin par E.Canova I I 'Scale 30 Avril, 2016 Carte 3. Localisation des Decapage R6, R7, et R8
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M4 M1L Ml r ~ Chemin N1ED N4o 5,294,000N Legend , Trace de Decapage R6 No de Decapage -'Contact Qtzite ' Point d'Affleurement • M4 QzBoGrtGneiss ▪ M4b MtQzBoGneiss M12 WhPkQtzite M12D PkRdDefQtzite 25 q0 75 100m CDC-2402787 Claim Dessin par E.Canova Scale 380,750E 30 Avril, 2016 Legend Carte 5. Localisation des Descapages R9, R19 et R11. *1', Trace de Decapage
R6 No de Decapage L1oE' ., ----Contact Qtzite • Point d'Affleurement • M4 QzBoGrtGneiss • M4b MtQzBoGneiss M12 WhPkQtzite M12D PkRdDefQtzite CDC-2402787 Claim Dessin par E.Canova 30 Avril, 2016 V
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382,000E
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