NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): 103H H.016

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1 Ministry of Energy, Mines & Petroleum Resources Mining & Minerals Division BC Geological Survey Assessment Report Title Page and Summary TYPE OF REPORT [type of survey(s)]: Geological TOTAL COST: $ 7, AUTHOR(S): Laurence Sookochoff, PEng SIGNATURE(S): NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): YEAR OF WORK: 2014 STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): October 15, 2014 PROPERTY NAME: Surf CLAIM NAME(S) (on which the work was done): COMMODITIES SOUGHT: Gold MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN: 103H H H H H H049 MINING DIVISION: Skeena NTS/BCGS: 103H H.016 LATITUDE: o ' " o LONGITUDE: ' 21 " (at centre of work) OWNER(S): 1) Rupert Resources Ltd. 2) MAILING ADDRESS: Suite Toronto Street Toronto ON M5C 2C5 OPERATOR(S) [who paid for the work]: 1) John Bakus 2) MAILING ADDRESS: Lorne Street East Kamloops BC V2C 1X8 PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude): Mid Cretaceous Ecstall Plutonic Suite. Regional north trending complex fault zone with several shear zones up to nine metres thick. Major northerly, northwesterly, and northeasterly structures and two cross-structures on Tenure At the Surf Inlet (103H 027) up to 12 metre wide quartz veins contain mainly auriferous pyrite with minor chalcopyrite, silver, chalcocite, bornite, and molybdenite. Drill core assays include 0.15 metres of grams per tonne gold and 3.33 per cent copper. REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: Next Page

2 TYPE OF WORK IN THIS REPORT EXTENT OF WORK (IN METRIC UNITS) ON WHICH CLAIMS PROJECT COSTS APPORTIONED (incl. support) GEOLOGICAL (scale, area) Ground, mapping Photo interpretation 465 hectares $ 7, GEOPHYSICAL (line-kilometres) Ground Magnetic Electromagnetic Induced Polarization Radiometric Seismic Other Airborne GEOCHEMICAL (number of samples analysed for...) Soil Silt Rock Other DRILLING (total metres; number of holes, size) Core Non-core RELATED TECHNICAL Sampling/assaying Petrographic Mineralographic Metallurgic PROSPECTING (scale, area) PREPARATORY / PHYSICAL Line/grid (kilometres) Topographic/Photogrammetric (scale, area) Legal surveys (scale, area) Road, local access (kilometres)/trail Trench (metres) Underground dev. (metres) Other TOTAL COST: $ 7,500.00

3 Rupert Resources Ltd Surf Claim Group Event RUPERT RESOURCES LTD. (Owner JOHN BAKUS (Operator) GEOLOGICAL ASSESSMENT REPORT (Event ) on a STRUCTURAL ANALYSIS Work done on Tenure of the eight claim Surf Claim Group Skeena Mining Division BCGS Maps 093H.006/.016 Centre of Work 5,882,930N 587,782 E (Zone 9 NAD 83) Author & Consultant Laurence Sookochoff, PEng Sookochoff Consultants Inc. Submitted December 14, 2014 (Amended September 12, 2015) Sookochoff Consultants Inc. November 10, 2014 page 1 of 22

4 Rupert Resources Ltd Surf Claim Group Event TABLE OF CONTENTS page Summary Introduction Property Description and Location Accessibility, Climate, Local Resources, Infrastructure and Physiography History: Property Area H 026 WELLS History: Property H 027 SURF INLET H 045 INDEPENDENCE H 046 DIABASE H 047 BONANZA H 048 SUMMIT H 049 CASSIE Geology: Regional Geology: Property Area H 026 WELLS Geology: Property H 027 SURF INLET H 045 INDEPENDENCE H 046 DIABASE H 047 BONANZA H 048 SUMMIT H 049 CASSIE Mineralization: Property Area H 026 WELLS Mineralization: Property H 027 SURF INLET H 045 INDEPENDENCE H 046 DIABASE H 047 BONANZA H 048 SUMMIT H 049 CASSIE Structural Analysis Interpretation and Conclusions Recommendations Selected References Statement of Costs Certificate Sookochoff Consultants Inc. November 10, 2014 page 2 of 22

5 Rupert Resources Ltd Surf Claim Group Event Table of Contents (cont d) ILLUSTRATIONS Figure 1. Location Map Figure 2. Claim Location Figure 3. Claim & Index Map Figure 4 Property Geology (MapPlace) Figure 5. Indicated Structures on Tenure Figure 6. Rose Diagram from Lineaments of Tenure Figure 7. Cross-Structure Locations on Google Earth Figure 8. Map showing access to Surf and Pugsley Mines Regional Fault Structure Figure 9. Map showing Surf Mine and Pugsley Mine Workings TABLES Table 1. Mineral Tenures of the Surf Claim Group Table 2. Approximate UTM locations of Figure 5 cross-structures and Minfile Sookochoff Consultants Inc. November 10, 2014 page 3 of 22

6 Rupert Resources Ltd Surf Claim Group Event SUMMARY The eight claim, 873 hectare Surf Claim Group ( Property ) is located near the head of Surf Inlet on Princess Royal Island, 650 km north-northwest of Vancouver and 168 kilometres south of Prince Rupert. The property includes the Surf Inlet ( Surf ) mine from which past production was 921,245 tons averaging 13.5 g/t gold (0.42 opt. A large, complex fault zone, traced for about 4.5 kilometres in a north-south direction, hosts the ore zones of the Surf and Pugsley mines. In the mine area the fault zone is convex toward the west and consists of several shear zones up to nine metres thick and 45 to 60 metres apart with average dips of 45 degrees west. Mineralized quartz veins parallel or subparallel the shear zones. The veins, 30 to 50 metres apart and up to 12 metres wide, contain mainly auriferous pyrite with minor chalcopyrite, silver, chalcocite, bornite, covellite and molybdenite. The structural analysis of Tenure of the Surf Claim Group identified two crossstructures that are on a northeasterly trending structure within 300 metres north of the Surf Mine. The significance of the cross-structures is in the resultant extensive area of brecciation and thus the potential for a more extensive mineralized zone that might be exploited by open-pit and/or underground blockcaving methods. Should the cross-structural location A zone, which is at an elevation of 493 metres, manifest positive surficial geological indications to any peripheral mineralized zone, the zone could possibly be tested at depth by diamond drilling from the Surf Mine 900 portal (?) level which is at an elevation of 300 metres. With a vertical AB structure, the horizontal distance to location A from the 250 metre mark of the 900 level is 250 metres. The dips of the drill hole and the AB structure would determine the distance to the structural intersection. In the drilling to target the location A structure, other gold-bearing structures may be intersected. Thus, the potential for the development of new gold reserves at the formerly productive Surf Mine could stem from locations A & B. An exploration program recommended to explore for additional gold reserves on the Surf Claim Group would be to explore location A for any surficial geological indicators of a potential gold resource at depth and if warranted, test the cross-structure to depth by a diamond drill hole from level 900 of the Surf mine workings. INTRODUCTION In October 2014 a Structural Analysis was completed on Tenure of the eight claim, 873 hectare, Surf Claim Group ( Property ). The purpose of the program was to delineate crossstructures which may be integral in geological controls to potentially economic mineral zones that may occur on Tenure or other claims of the Property. For additional information on the Property, the reader is referred to the pertinent publications as cited in the Reference section. Sookochoff Consultants Inc. November 10, 2014 page 4 of 22

7 Rupert Resources Ltd Surf Claim Group Event Figure 1. Location Map PROPERTY LOCATION AND DESCRIPTION Location The Surf Claim Group is located within BCGS Maps 103H.006/.016 of the Skeena Mining Division, 13 km from tidewater on Princess Royal Island, 650 km north-northwest of Vancouver, and 168 kilometres south of Prince Rupert. Description The Property is comprised of eight claims covering an area of hectares. Particulars are as follows. Table 1. Mineral Tenures of the Surf Claim Group Tenure Number Type Claim Name Good Until Area (ha) Mineral SURF FR Mineral Mineral Mineral Mineral SURF EXT Mineral SURF S SURFPILE Mineral Mineral Total Area: ha Sookochoff Consultants Inc. November 10, 2014 page 5 of 22

8 Rupert Resources Ltd Surf Claim Group Event ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY Access Access is by float equipped aircraft either from Prince Rupert or Port Hardy to either the head of Surf Inlet or to the east shore of Bear Lake where a road leads to the mine workings on the Property. Climate The climate is moderate with limited snowfall in winter. It is possible to work on the property on a year round basis however, winter weather conditions can limit both marine and float plane transport. Local Resources and Infrastructure The closest commercial supply and accommodation location is at Prince Rupert or Port Hardy which are both served daily by a commercial airline from Vancouver and where float plane service can be arranged to the Surf Property Physiography The topography on Tenure , the subject claim of structural analysis, is of forested lower and barren rugged alpine slopes. Elevations are from 50 metres within Paradise Creek valley to 949 metres on a mountain peak in the northwest. HISTORY: PROPERTY AREA The history on the more significant mineral MINFILE reported showing peripheral to the Surf Claim Group is reported (Minfile records) as follows. The distance is relative to the Surf Claim Group. WELLS showing (Au quartz veins) MINFILE 103H 026 One hundred metres west The property is located on the steep side of the precipitous mountain which stands just north of the point where Paradise Creek enters Bear Lake, at about 610 metres elevation. The property was originally staked by Mr. Wells in During the years 1920 and 1921, work by Mr. Wells mainly involved the driving of a drift adit for over 90 metres, just below the surface showing. He also did some surface stripping. HISTORY: PROPERTY The history on some of the more significant mineral MINFILE reported showings, prospects, and past producers on the Surf Claim Group are reported as follows. SURF INLET Past Producer (Au quartz veins) MINFILE 103H 027 Within Tenure The Surf Inlet mine is located on Princess Royal Island near the head of Surf Inlet southeast of Prince Rupert. The property straddles a deeply entrenched creek; the Surf Inlet group (D.L.S. group and La Cuivre group) of claims lying to the north, and the Pugsley group (Princess Royal and Homestake groups) of claims lying to the south. Exploration and development work began in about The Princess Royal group of 3 claims was owned by Messrs. Wilson, Irving, & Rithet; the Homestake group of 5 claims, adjoining and south of the Princess Royal group was owned by Messrs. McMillan, Howden, Cliff, and Nowell; the D.L.S. group was owned by Messrs. Cleveland and Kelly Sookochoff Consultants Inc. November 10, 2014 page 6 of 22

9 Rupert Resources Ltd Surf Claim Group Event History: Property (cont d) Surf Inlet past producer (cont d) Additional claims in the Bluff group were staked in 1901 adjoining the D.L.S. group and were subsequently included in it. The Princess Royal and Homestake groups were bonded to Mr. J. Findlay and Associates in 1902; the Princess Royal claim (Lot 7, R 4) was Crown-granted to Messrs. Wilson and Rithet in All groups were apparently idle from about 1903 until Figure 2. Claim Location (base map from MapPlace & Google Earth) Figure 3. Claim Map (from MapPlace) Sookochoff Consultants Inc. November 10, 2014 page 7 of 22

10 Rupert Resources Ltd Surf Claim Group Event History: Property (cont d) Surf Inlet past producer (cont d) Surf Inlet Gold Mines Limited was formed in 1910 to develop the D.L.S. group of 9 claims; however, very little work was done by the company. The Tonopah-Belmont Development Company optioned the property in 1915 and Belmont Canadian Mines Limited was formed to carry on development work. The following year the Princess Royal group was optioned from Princess Royal Gold Mines Limited; this group had previously been held by Princess Royal Island Mining Company Limited, which was incorporated in June Belmont Canadian Mines Limited was reorganized under the name Belmont-Surf Inlet Mines Limited in 1917 with Surf Inlet Mines Limited retaining a 20 per cent interest in the new company. A 270 tonne mill was put into operation in Development of the Princess Royal group under the option agreement continued until 1921 when the purchase of the property was completed. The company operated continuously until June 1926 when operations were suspended. Princess Royal Gold Mines Limited, incorporated in May 1933, acquired the Surf Inlet and Pugsley groups and exploration and development work was begun. The old mill was reconditioned to handle 63 tonnes per day. The company name was changed in 1935 to Surf Inlet Consolidated Gold Mines Limited. Operations were continuous until November 1942 when the mine closed for the duration of the war. Work was resumed in April 1946 and suspended again the following December. During the year some 152 metres of underground development work was completed and 2320 metres of diamond drilling was done from the surface. Underground development work totals some 15,240 metres of drifts, cross-cuts, and raises. During the period some 20,420 metres of diamond drilling were completed. The company name was changed to Surf Inlet Consolidated lines Limited in 1955 and to Western Surf Inlet Mines Limited in Matachewan Consolidated Mines, Limited acquired the assets of the company in Reserves on the Pugsley group were estimated in 1961 at tonnes. In 1981, the occurrence was optioned by Cominco Limited and Placer Development Limited. They diamond drilled 10 holes totalling 1526 metres along a shear zone strike length of 1950 metres; results ruled out a large tonnage low-grade potential. The option was terminated in June 1984 with Matchewan retaining 100 per cent interest in 21 patented Crown leases. Surf Inlet Mines Limited began work on the property in Sampling programs, surveys and metallurgical test work were done to evaluate the tonnage and grade of the stockpiles and tailings on the Surf Inlet property. During 1988 work was begun on rehabilitation of the 900 level of the Surf Mine, in preparation for drill testing. During 1991 the company contracted Rem Exploration to carry out a sampling program of the Surf and Pugsley Mine dumps. In 1997, Rupert Resources Limited drilled the downdip extension of the Surf orebody. This extension occurs on the former Wells property (103H 026). In 2010, two drill holes were performed on the same sites as the 1997 drilling program. INDEPENDENCE showing (Au quartz veins) MINFILE 103H 045 Within Tenure The Independence showings are located in the southern part of the north-south trending shear system, about 1800 metres south of the Surf Inlet Mine (103H 027) and just east of the Pugsley Mine. DIABASE showing (Au quartz veins) MINFILE 103H 046 Within Tenure Sookochoff Consultants Inc. November 10, 2014 page 8 of 22

11 Rupert Resources Ltd Surf Claim Group Event History: Property (cont d) Diabase showing (cont d) An extensive, complex shear system occurs in intrusive and gneissic volcanics and metasediments of the Coast Plutonic Complex. Gold associated with pyrite occurs in quartz-ankerite-sericite- sulphide veins within the shear zone. BONANZA showing (Au quartz veins) MINFILE 103H 047 Within Tenure The Bonanza showing is located in the southern part of the north-south trending shear system, about 2700 metres south of the Surf Inlet Mine (103H 027). SUMMIT showing (Au quartz veins) MINFILE 103H 048 Within Tenure The Summit showing is located in the southern end of the north- south trending shear system, about 3400 metres south of the Surf Inlet Mine (103H 027). CASSIE showing (Au quartz veins) MINFILE 103H 049 Within Tenure The Cassie showing is located in the southern part of the north- south trending shear system, about 3700 metres south of the Surf Inlet Mine (103H 027). GEOLOGY: REGIONAL The Surf Inlet Project is situated within the Coast Belt Tectonic province in western British Columbia. Gold mineralization is localized along an extensive shear system that cuts predominantly intrusive and lesser mixed inclusions of gneissic volcanics and sediments of the extensive Coast Range Batholith. The gneiss unit consists of coarse grained moderately well bonded, quark biotite feldspar gneiss and plagioclase, hornblende, biotite gneiss. Accessory minerals include apatite and augite. Complex folding is common. The contact between the gneiss unit and diorite is rarely a well-defined, sharp boundary. Instead, a type of an assimilation zone from 5 to 100 metres wide exists. This unit is characterized by variably oriented gneiss fragments in diorite and irregular diorite dykes or injections in the bordering gneisses. GEOLOGY: PROPERTY AREA The major unit on the property is diorite with minor associated quartz diorite. In the unaltered state, this unit is medium to coarse grained, granular to weakly foliated. Major constituents include plagioclase, hornblende, biotite with lessor quartz, and accessory augite, sphene and magnesite. The geology on the more significant mineral MINFILE reported showing peripheral to the Surf Claim Group is reported (Minfile records) as follows. The distance is relative to the Surf Claim Group. WELLS showing (Au quartz veins) MINFILE 103H 026 One hundred metres west The area is underlain by hornblende-biotite quartz diorite with diorite gneiss bands of the Tertiary-Jurassic Coast Plutonic Complex. A large, complex fault zone, traced for about 4.5 kilometres in a north-south direction, hosts the ore zones of the Surf Inlet and Pugsley mines. Sookochoff Consultants Inc. November 10, 2014 page 9 of 22

12 Rupert Resources Ltd Surf Claim Group Event Geology (cont d) Wells showing (cont d) In the mine area the fault zone is convex toward the west and consists of several shear zones up to 9 metres thick and 45 to 60 metres apart with average dips of 45 degrees west. Locally, a quartz vein containing auriferous pyrite occurs in sheared quartz diorite of the Coast Plutonic Complex. The vein is 1.2 to 1.5 metres wide for 18.2 metres. GEOLOGY: PROPERTY The geology on some mineral MINFILE reported showings, prospects, and past producers on the Surf Claim Group is reported as follows (from Minfile records). The distance is relative to the Surf Claim Group. SURF INLET Past Producer (Au quartz veins) MINFILE 103H 027 Within Tenure The area is underlain by hornblende-biotite quartz diorite with diorite gneiss bands of the Tertiary-Jurassic Coast Plutonic Complex. A large, complex fault zone, traced for about 4.5 kilometres in a north-south direction, hosts the ore zones of the Surf Inlet and Pugsley mines. In the mine area the fault zone is convex toward the west and consists of several shear zones up to 9 metres thick and 45 to 60 metres apart with average dips of 45 degrees west. INDEPENDENCE showing (Au quartz veins) MINFILE 103H 045 Within Tenure An extensive complex shear system occurs in intrusive and gneissic volcanics and metasediments of the Coast Plutonic Complex. Gold associated with pyrite occurs in quartz-ankerite-sericite- sulphide veins within the shear zone. DIABASE showing (Au quartz veins) MINFILE 103H 046 Within Tenure An extensive, complex shear system occurs in intrusive and gneissic volcanics and metasediments of the Coast Plutonic Complex. Gold associated with pyrite occurs in quartz-ankerite-sericite- sulphide veins within the shear zone. BONANZA showing (Au quartz veins) MINFILE 103H 047 Within Tenure Two parallel north-northwest trending quartz veins occur along the contact between diorite and quartzfeldspar-biotite-hornblende gneiss. The contact zone is altered with chlorite, sericite, ankerite and quartz. SUMMIT showing (Au quartz veins) MINFILE 103H 048 Within Tenure A narrow northeast trending quartz vein occurs along the contact between diorite and quartz-feldspar-biotitehornblende gneiss. The contact zone is altered with chlorite, sericite, ankerite and quartz. Sookochoff Consultants Inc. November 10, 2014 page 10 of 22

13 Rupert Resources Ltd Surf Claim Group Event Figure 4. Property Geology (Base map from MapPlace GEOLOGY MAP LEGEND Early Cretaceous EKMqd McCauley Island Plutonic Suite Quartz diorite intrusive rocks Early Cretaceous EKMEog McCauley Island Plutonic Suite Orthogneiss metamorphic rocks Mid Cretaceous MKEq ad Ecstall plutonic suite Quartz diorite intrusive rocks Mid Cretaceous MKEgd Ecstall plutonic suite gronodioritic intrusive rocks Geology: Property (cont d) CASSIE showing (Au quartz veins) MINFILE 103H 049 Within Tenure Two parallel northwest trending quartz veins occur along the contact between diorite and quartz-feldsparbiotite- hornblende gneiss. The contact zone is altered with chlorite, sericite, ankerite and quartz. MINERALIZATION: PROPERTY AREA The mineralization of the more significant mineral MINFILE reported showing peripheral to the Surf Claim Group is reported (Minfile records) as follows. The distance is relative to the Surf Claim Group. Sookochoff Consultants Inc. November 10, 2014 page 11 of 22

14 Rupert Resources Ltd. Surf Claim Group Event WELLS showing (Au quartz veins) MINFILE 103H 026 One hundred metres west In 1942, drilling near the Wells property intersected 3 metres of 6.5 grams per tonne gold, and one metre of 21.6 grams per tonne gold (George Cross Newsletter Number 108). In 1997 Rupert Resources drilled the down dip extension of the Surf orebody (103H 027). This extension occurs on the Wells property. In 2010, two drill holes were performed on the same sites as the 1997 drilling program. Drill hole intersected a 2.5 metre wide mineralized zone including a 1.1 metre interval grading 0.60 gram per tonne gold, 0.8 gram per tonne silver and 138 parts per million copper. Two additional mineralized stringers were intersected further down hole at to metres and to metres. The first mineralized stringer returned 0.4 metres grading 4.9 grams per tonne gold, 158 grams per tonne silver and 9.32 per cent copper. The second mineralized ringer returned 0.15 metres grading grams per tonne gold, 16.0 grams per tonne silver and 3.33 per cent copper. Drill hole intersected a 7.1 metre wide zone on quartz and brecciated metasediments including a 1.1 metre section which assayed 1.1 grams per tonne gold, 2.2 grams per tonne silver and 814 parts per million copper (Assessment Report 26704). MINERALIZATION: PROPERTY The mineralization on some of the more significant mineral MINFILE reported showings, prospects, and past producers on the Surf Claim Group are reported as follows (from Minfile records). SURF INLET Past Producer (Au quartz veins) MINFILE 103H 027 Within Tenure Mineralized quartz veins parallel or subparallel the shear zones. The veins, 30 to 50 metres apart and up to 12 metres wide, contain mainly auriferous pyrite with minor chalcopyrite, silver, chalcocite, bornite, covellite and molybdenite. Gangue minerals include quartz, ankerite and minor calcite. Sericite and chlorite alteration are common near the veins. Distribution of ore shoots within the veins depends on late-stage fault adjustments and flexures during which veins along certain shear surfaces and zones were fractured and mineralized (Assessment Report 15377). Drill hole intersected a 2.5 metre wide mineralized zone including a 1.1 metre interval grading 0.60 grams per tonne gold, 0.8 grams per tonne silver and 138 parts per million copper. Two additional mineralized stringers were intersected further down hole at to metres and to metres. The first mineralized stringer returned 0.4 metres grading 4.9 grams per tonne gold, 158 grams per tonne silver and 9.32 per cent copper. The second mineralized stringer returned 0.15 metres grading grams per tonne gold, 16.0 grams per tonne silver and 3.33 per cent copper. Drill hole intersected a 7.1 metre wide zone on quartz and brecciated metasediments including a 1.1 metre section which assayed 1.1 grams per tonne gold, 2.2 grams per tonne silver and 814 parts per million copper (Assessment Report 26704). Drilling near the Wells property in 1942 intersected 3 metres of 6.5 grams per tonne gold and 1 metre of 21.6 grams per tonne gold (George Cross Newsletter #108, June 5, 1997). Sookochoff Consultants Inc. November 10, 2014 Page 12 of 22

15 Rupert Resources Ltd. Surf Claim Group Event Mineralization: Property (cont d) INDEPENDENCE showing (Au quartz veins) MINFILE 103H 045 Within Tenure A north trending quartz vein, with chalcopyrite, occurs in sheared and altered diorite. A 30 centimetre sample across the vein assayed per cent copper, 0.46 grams per tonne gold, and 3.6 grams per tonne silver (Assessment Report 15377). DIABASE showing (Au quartz veins) MINFILE 103H 046 Within Tenure A 1 metre wide quartz vein, occurring within sheared and altered diorite, is cut by a 3 metre wide diabase dyke. A 70 centimetre sample across the vein assayed 4.4 grams per tonne gold, 24.4 grams per tonne silver and per cent tellurium (Assessment Report 15377). BONANZA showing (Au quartz veins) MINFILE 103H 047 Within Tenure A 1.2 metre sample across a quartz vein assayed 12.8 grams per tonne gold, 86.0 grams per tonne silver, 1.72 per cent copper and grams per tonne tellurium (Assessment Report 15377). SUMMIT showing (Au quartz veins) MINFILE 103H 048 Within Tenure A 90 centimetre sample across the quartz vein assayed 6.67 grams per tonne gold, 14.5 grams per tonne silver, per cent copper and per cent tellurium (Assessment Report 15377). CASSIE showing (Au quartz veins) MINFILE 103H 049 Within Tenure Grab samples from an ore dump assayed 63.0 grams per tonne gold, 93.2 grams per tonne silver and per cent tellurium (Assessment Report 15377). STRUCTURAL ANALYSIS The Structural Analysis of Tenure was accomplished marking the observed lineaments on a DEM Image hillshade map downloaded from MapPlace. A total of 55 lineaments were indicated as shown on Figure 5. A Georient 32v9 software program was used to create a Rose Diagram reflecting the grouping of the lineaments into an individual 10 class sector angle interval as shown on Figure 6. Sookochoff Consultants Inc. November 10, 2014 Page 13 of 22

16 Rupert Resources Ltd. Surf Claim Group Event Structural Analysis (cont d) Figure 5 Indicated Structures on Tenure (Base map: MapPlace & Google) Sookochoff Consultants Inc. November 10, 2014 Page 14 of 22

17 Rupert Resources Ltd. Surf Claim Group Event Structural Analysis (cont d) Figure 6. Rose Diagram from Lineaments of Tenure STATISTICS (for Figure 5) Axial (non-polar) data No. of Data = 55 Sector angle = 8 Scale: tick interval = 2% [1.1 data] Maximum = 14.5% [8 data] Mean Resultant dir'n = [Approx. 95% Confidence interval = ±26.8 ] (valid only for unimodal data) Mean Resultant dir'n = Circ.Median = Circ.Mean Dev.about median = 30.5 Circ. Variance = 0.21 Circular Std.Dev. = Circ. Dispersion = 2.91 Circ.Std Error = Circ.Skewness = Circ.Kurtosis = kappa = 0.83 (von Mises concentration param. estimate) Resultant length = Mean Resultant length = 'Mean' Moments: Cbar = ; Sbar = 'Full' trig. sums: SumCos = ; Sbar = Mean resultant of doubled angles = Mean direction of doubled angles = 000 (Usage references: Mardia & Jupp, 'Directional Statistics', 1999, Wiley; Fisher, 'Statistical Analysis of Circular Data', 1993, Cambridge University Press) Note: The 95% confidence calculation uses Fisher's (1993) 'large-sample method' Sookochoff Consultants Inc. November 10, 2014 Page 15 of 22

18 Rupert Resources Ltd. Surf Claim Group Event Structural Analysis (cont d) Figure 7. Cross-structure locations on Google Earth (Base map from MapPlace & Google Earth) Table 2. Approximate UTM locations of Figure 5 cross-structures and Minfile (UTM-NAD 83 Zone 9) Area UTM East UTM North Elevation (metres) A 507,797 5,882, B 508,091 5,883, Surf Adit 507,887 5,882, Sookochoff Consultants Inc. November 10, 2014 Page 16 of 22

19 Rupert Resources Ltd. Surf Claim Group Event Figure 7. Map Showing Access to Surf Mine and Pugsley Mines and Regional Fault Structure (Map from AR 26,704) Sookochoff Consultants Inc. November 10, 2014 Page 17 of 22

20 Rupert Resources Ltd. Surf Claim Group Event Figure 7. Map Showing Surf Mine and Pugsley Mine Workings (Map from AR 26,704) INTERPRETATION and CONCLUSIONS Based on the geological controls to the mineral zones of the past productive Surf Inlet and other mineralized zones on a convex fault zone as shown on Figure 7, the two cross as determined from the structural analysis appear to be on a common separate northeasterly trending structure. However, if the Surf structural 023 trend is projected northward from the Surf Inlet Mine (Figure 6), location B could be on the same structure as the Surf Mine. If so, then location B would be at the intersection of three major structures. Location A is indicated at 300 metres north-northwest of the Surf Mine portal and is at the intersection of three prime structures. The significance of the cross-structures is in the resultant extensive area of brecciation and thus the potential for a more extensive mineralized zone that might be exploited by open-pit and/or underground block-caving methods. The Surf structure had been previously tested for a potential bulk tonnage resource with discouraging results, however, with the increase in gold prices and the ideal location, the cross-structural locations would be prime areas to explore for that potential. Sookochoff Consultants Inc. November 10, 2014 Page 18 of 22

21 Rupert Resources Ltd. Surf Claim Group Event Interpretation and Conclusions (cont d) Should the cross-structural location A zone, which is at an elevation of 493 metres, zone manifest positive surficial geological indications to any peripheral mineralized zone, the zone could possibly be tested at depth by diamond drilling from the Surf Mine 900 portal (?) level which is at an elevation of 300 metres. If the AB structure is vertical, the horizontal distance to Location A from the 250 metre mark of the 900 level is approximately 250 metres. The dips of the drill hole and the AB structure would determine the distance to the structural intersection. Thus, the potential for the development of new gold reserves at the formerly productive Surf Mine could stem from locations A & B. RECOMMENDATIONS Initially explore location A for any surficial geological indicators of a potential gold resource at depth; Should the geological indicators warrant follow-up exploration, a diamond drill hole from the 900 level of the Surf Mine workings should be completed to test the A structural zone at depth. Should the geological indicators at location B warrant follow-up exploration, an exploration program would have to be designed to test the structural zone at depth. Respectfully submitted Sookochoff Consultants Inc. Laurence Sookochoff, PEng Sookochoff Consultants Inc. November 10, 2014 Page 19 of 22

22 Rupert Resources Ltd. Surf Claim Group Event SELECTED REFERENCES Beck, R., Ledwon, A Technical Assessment Report for the Surf Property for Richard Billingsley. January, AR 34,037. Burton, R.K., Gardiner, S.L. Report on Volume Surveys and Testing of Tailings for Matachewan Consolidated Mines, Limited and Surf Inlet Mines Ltd. January, AR 17,275 Capps, R.C., Moore, J.A. Castle Mountains Geology and Gold Mineralization. Nevada Bureau of Mines Daughtry, K.L. Prospecting and Geochemical Assessment Report on the Winfield Creek Property for D.A. Davidson and Partners. January 21, AR 22,077. Gardiner, S.L., Harris, J.F. Summary Report on the Lithogeochemical and Mineralogical Study of the Surf Inlet Property for Matachewan Consolidated Mines, Limited. December 16, AR 15,377. MapPlace Downloads Marshak, S., Mitra, G. Basic Methods of Structural Geology. pp , 264*.Prentice-Hall Inc MtOnline - MINFILE downloads. 103H 026 WELLS 103H 027 SURF INLET 103H 045 INDEPENDENCE 103H 046 DIABASE 103H 047 BONANZA 103H 048 SUMMIT Von Einsiedel, C. Geological Report on the Surf and Pugsley Mine Dumps for Ram Exploration Ltd. February 24,1992. AR 22, H 049 CASSIE Von Einsiedel, C. Underground Drilling Report Surf Mine 900 Level Surf Inlet Property for Kermode Resources Ltd. March 01, AR 26,704. Sookochoff Consultants Inc. November 10, 2014 Page 20 of 22

23 Rupert Resources Ltd. Surf Claim Group Event STATEMENT OF COSTS Work on Tenure of the Surf Claim Group was done from October 10, 2014 to October 14, 2014 to the value as follows: Structural Analysis Laurence Sookochoff, $ 1,000.00/day $ 2, Maps , Report , $ 7, ======== Sookochoff Consultants Inc. November 10, 2014 Page 21 of 22

24 Rupert Resources Ltd. Surf Claim Group Event CERTIFICATE I, Laurence Sookochoff, of the City of Vancouver, in the Province of British Columbia, do hereby certify: That I am a Consulting Geologist and principal of Sookochoff Consultants Inc. with an address at Suite A-1030 Denman Street, Vancouver, BC V6G 2M6. I, Laurence Sookochoff, further certify that: 1) I am a graduate of the University of British Columbia (1966) and hold a B.Sc. degree in Geology. 2) I have been practicing on profession for the past forty-eight years. 3) I am registered and in good standing with the Association of Professional Engineers and Geoscientists of British Columbia. 4) The information for this report is based on information as itemized in the Selected Reference section of this report. 5) I have no interest in the Property as described herein. Laurence Sookochoff, P. Eng. Sookochoff Consultants Inc. November 10, 2014 Page 22 of 22