45

5050

607585

62 65 75

45

50

33

4545

7670

39

36

74

50

6550

69

80 65

55

83

6574

634942

7658

3441

58

6044

74

4

54 464559 53

39

40 578556

346036 12

8263

4152 69

8045 4776 68

12 55

4862

866688

626046 80

4051

4885 706967

56 726367

76 5654

62 747345

55555635 64

754086 85

5185

6175 60

45

38

453465

70

70

60 50 65

335175 80 43

536845mPA2mPA2

mPA2

mPA2

mPA2mPA2

mPA2

mPms

mPmsmPms

mPms

mPms

mPms

mPms

mPC2

mPC2

mPC2mPC2

mPC3

mPC3

mPK

mPK

mPKs

mPVC

mPNC

mPSH CC

Qal

mPA1

mPA3mPA2

mPms

mPK

mPC2

mPA2

5489000

54

90

00

05

49

10

00

54

92

00

0

54

8900

05

49

00

00

54

91

00

05

49

20

00

567000 568000 569000 570000 571000

567000 568000 569000 570000 571000

Quartz Creek Fault

Perr

y C

reek

F

ault

St. M

ary

Fau

lt

Saw

mill

C

reek

F

ault

QUATERNARY

LOWER AND (?) MIDDLE CAMBRIAN

PROTEROZOIC

CRANBROOK FORMATION

PURCELL SUPERGROUP

KITCHENER FORMATION

CRESTON FORMATION

ALDRIDGE FORMATION

MAFIC INTRUSIONS

Unconsolidated outwash, alluvium, colluvium and till.

Quartzite, limestone, calcite marble, dolomite marble, calc-silicate.

Undivided; thin-bedded, brown-weathering dolomite siltstone and green argillite.

Upper: Green siltstone; black to purple argillite and siltstone.

Middle: Light grey, mauve, thin to medium-bedded quartz arenite,quartz wacke, lesser grey siltite and argillite. White quartzite interbeds. Lenticular bedding, ripples, crossbeds and mudcracks.

Upper: Rusty brown weathering, grey to dark grey, fissile to platy,laminated silty argillite and siltite.

Middle: Grey to rusty weathering, thick- to thin-bedded, quartzo-feldspathic wacke with argillite and siltite, intercalations.

Lower: Rusty brown weathering. thin- to medium-bedded, quartzwacke, quartz arenite.

“Moyie Sills”. Dark green to black, medium- to fine-grained gabbroand hornblende quartz diorite sills and minor dikes. Zircon U-Pb dates circa 1467 Ma (Anderson and Davis, 1995).

SHEPPARD FORMATION

NICOL CREEK FORMATION

VAN CREEK FORMATION

Sandstone and conglomerate locally at base; dolomitic quartzite, sandstone, oolitic dolomite, stromatolitic dolomite at top.

Undivided volcanic rocks. Massive to amygdaloidal basalt toandesite lava flows, volcanic sandstone, siltite.

Pale green, laminated, siltite and argillaceous siltite and quartz wacke. Minor ripple marks, lenticular bedding, rare flattened mudcracks.

mPs

mPms

mPA3

mPA2

mPA3

mPC2

mPC3

mPK

mPVC

mPNC

mPSH

CC

Qal

Mafic sills, rare dikes hosted in Kitchener Formation. Olive green,massive to plagiclase porphyritic.

GEOLOGY LEGEND

STRUCTURES

SYMBOLS

Geological contact: defined, approximate, assumed

STRUCTURES, SYMBOLS AND FEATURES

Fault: defined, approximate, assumed

Outcrop

Bedding: inclined, vertical

Foliation: inclined, vertical

Joint: inclined, vertical

Vein: inclined, vertical

Lineation: intersection, mineral, slickenside

Dike: inclined, vertical

80

36

76

27

64

06 72 65

SELECTED BIBLIOGRAPHY

Anderson, D. (2008): Diamond Drilling Report for the Quartz Mountain Property; B.C. Ministry of Energy and Mines, Assessment Report 30258, 63 pages.Banting, R.T. (1988): Geological and Geochemical Report on the Morgan Property (North Block); B.C. Ministry of Energy and Mines, Assessment Report 17111, 30 pages.Brown, D.A. (1998): Geological Compilation of Grassy Mountain (East Half) and Moyie Lake (West Half) Map Areas, Southeastern British Columbia (82F/8E, 82G/5W); B.C. Ministry of Energy and Mines, Geoscience Map 1998-3, 1:50,000 scale map.Dandy, L., Troup, A.G. (1985): Geological, Geophysical and Geochemical Surveys Report on the Perry Creek Property; B.C. Ministry of Energy and Mines, Assessment Report 14211, 90 pages.Hardy, J.L. (1986): Geology and Diamond Drilling, Perry Creek Property; B.C. Ministry of Energy and Mines, Assessment Report 15649, 173 pages.Höy, T., Anderson, D., Kennedy, S., Kennedy, M. (2013): Quartz Mountain Property: Rock Sampling and Drill Core Analysis. B.C. Ministry of Energy and Mines, Assessment Report 34197, 46 pages.Höy, T. (1993): Geology of the Purcell Supergroup in the Fernie West-half Map Area, Southeastern British Columbia; B.C. Ministry of Energy, Mines and Petroleum Resources, Bulletin 84.Höy, T. and Diakow L. (1982): Geology of the Moyie Lake Area; B.C. Ministry of Energy, Mines and Petroleum Resources, Preliminary Map 49.Klewchuk, P. (1992): Assessment Report on VLF- EM Geophysics, Quartz Creek, Saw and Burn Claims; B.C. Ministry of Energy and Mines, Assessment Report 22492, 17 pages.Jackson, D.C., Schadt, W.E. (1996): Report JAN 22, 1996 Cornucopia Group Mineral Claims; B.C. Ministry of Energy and Mines, Assessment Report 24289, 23 pages.Klewchuk, P. (2004): Assessment Report on Diamond Drilling, Sawmill Property; B.C. Ministry of Energy and Mines, Assessment Report 27382, 28 pages.Klewchuk, P. (1996): Assessment Report on Diamond Drilling, Quartz Creek, RWH Properties; B.C. Ministry of Energy and Mines, Assessment Report 24680, 37 pages.Rodgers, G.M. (1995): Diamond Drilling, Geophysics and Geology Report, Quartz Creek Claim Group; B.C. Ministry of Energy and Mines, Assessment Report 23741, 41 pages.Southam, P. (2002): Prospecting Report on the QM Property; B.C. Ministry of Energy and Mines, Assessment Report 26780, 13 pages.Southam, P. (2003): Mapping and Rock Sampling Report on the QM Property; B.C. Ministry of Energy and Mines, Assessment Report 27098, 26 pages.

Year

1985

19861988

199219951996

199620022003200420082013

Dandy, L., Troup, A.G.

Hardy, J.L.Banting, D.A.

Klewchuk, P.Rodgers,G.M.Jackson, D.C., Shadt, W.E.

Klewchuk, P.Southam, P.Southam, P.Klewchuk, P.Anderson, D.Höy, T., Anderson, D., Kennedy, S.,Kennedy, M.

Author ARIS

14211

1564917111

224922374124289

246802678027098273823025834197

Work Conducted

Soil Geochemistry, Rock Geochemistry,Geophysics, Diamond Drilling, GeologyRock Geochemistry, Diamond Drilling, GeologySoil Geochemistry, Rock Geochemistry,GeologyGeophysicsSoil Geochemistry, Diamond Drilling, GeologySoil Geochemistry, Rock Geochemistry,Diamond DrillingDiamond DrillingGeologyRock Geochemistry, Diamond Drilling, GeologyDiamond Drilling, GeologyDiamond DrillingRock Geochemistry, Drill Assays

COMPILATION TABLE

Quartz Mountain PropertyKIMBERLEY GOLD TREND

Fort Steele Mining DivisionKootenay District

550000 600000

550000 600000

5450000

5500000

5550000

5450000

5500000

5550000

Quartz Mtn.Quartz Mtn.

KIMBERLEY

CRESTON

CRANBROOK

KIMBERLEY

CRESTON

CRANBROOK

Suggested reference: Seabrook, M. and Hoy, T. (2015): Quartz Mountain Property, Kimberley Gold Trend; Geoscience BC Map 2015-13-02, 1:20,000 scale.

May 2015

Geoscience BC Map 2015-13-02

KIMBERLEY GOLD TREND

Note: Some historical data locations and values have been inferred from the historical map.

The Quartz Mountain property is currently owned and operated by Klondike Gold Corp. The property straddles the St. Mary fault, the approximate north-west boundary of the Kimberley Gold Trend. A locally intense penetrative structural fabric parallels the St. Mary fault and is intersected by east south-east trending faults and structural breaks. The intersections of a prominent east south-east fault and the St. Mary fault is correlative with the presence of gold mineralization in the Golden Egg (Rice) deposit (Minfile: 082FNE055).

The Price’s Pit (Anderson) deposit (Minfile: 082FNE056) lies to the southeast of the Golden Egg and is hosted in poorly exposed Creston and Kitchener formation rocks covered by alluvium. The Price’s Pit deposit is thought to occur at the intersection of he Perry Creek Thrust and an unnamed east trending fault that has not been recognized in the field.

Small occurrences of copper sulphides have been found proximal to the trace of the Quartz Creek at the intersection of the Sawmill Creek fault, but are not well understood at this time.

MINERAL OCCURANCES

NTS Map Sheet: 082F56300 56500 56700 56900

56600

56600

56600

56600

56600

56600

5660

0

56600

56600

56850

56850

80

65

55

83

74

6349

4276

58

34

4158 60

44

74

4

544645

59

533940

5785

56 34

6036 12

82

4152

69 8045

47

68

12

4862 8666 88

60

46 8040

51

85 6967

56 72 6367

76

5654

6274

73

45

55

55

56357540

8685

5185

6175 60

45

38

mPA2

mPA2

mPms

mPms

mPC2

54

90

50

05

49

10

00

54

91

50

0

54

90

50

05

49

10

00

54

91

50

0

567500 568000 568500 569000 569500

567500 568000 568500 569000 569500

SURVEY SPECIFICATIONS:

AIRBORNE GEOPHYSICS (TMI)

TMI(nT)

Geometrics G-823AOptically pumped caesium vapour sensorSensitivity: 0.001nTSampling Interval: 0.1s

MAGNETOMETER:

Survey Date: April 19 - 21, 2006Survey Base: Castlegar, British ColumbiaAircraft: Eurocopter Aerospatiale (A-Star) 350 B2 C-FPTGNominal Survey Line Spacing: 100 mNominal Survey Line Direction: N 0° E / N 180° ENominal Tie Line Spacing: 1000 mNominal Tie Line Direction: N 90° E / N 270° ENominal Terrain Clearance: 68 mEM Loop: Towed at a mean distance of 38 mMagnetic Sensor: Towed at a mean distance of 17 m

Airborne geophysical data was commisioned in2006 by Klondike Gold Corporation and was provided for this project upon request.

l

l

Price’s Pit

Golden Egg

7.1

1.6

3.4

25.5

0.9

21.5

2.6

187.3

16.4

11.8

18

173.8

28.72.6

4.3

33.4

7.4

3

6.6

33

5.2

2

1.9

2.8

0.6

12.3

0.8

99.6

33.3 419.2

21.3

36.1

8.5

0.9

1

13.8

1.9

39.5

42.2

8.6

10

19

3.8

16.8

4.73.8

27.8

2.987

4.2

41.94.223.3

1.9

30.30.7

24.5

21.5

5940

59.428.312.4

3.7

0.9

1.7 4.8

1.5 4.7

7.9

7.2

11.4

6.7

2.4

25.6

2.34.9

2.13.6

4.6 13.5

3.91.9

1.8

20.5

154.77.2

2.1

2.511.4

79.74.22.61.6

0.91.6

0.72.712.6

2.9 2.3

788.4

929.643

224.14.2

3.3

53

843.8

5

6.9

8.31.69.5

1239.92.92.10.4

1.1

1

0.4

33.8

5.7

174.3

8.6

5.1

2.63.9

4.4

9.27.8

80.6

7.5

11.3

34.7

6.9

1.1 1.637

5.432.65.1

46.9

61

5.8

87.347132

70.1

12.54.3

10.5

96.3

101163

133

63.478.5

5.5

6.3

3.5

5.25.5

4.1

1

2.7

8.70.5

35.1

25.7

1

1.10.9

87.8

5

10

540

5

5

5

5

5

5

5

5

44062.5

427501625

187.5

83125

1312.5

187.52187.5

312.51625

107250

115156.25

mPA2

mPA2

mPms

mPms

mPC2

5490500

54

91

00

05

49

15

00

54

9050

05

49

10

00

54

91

50

0

567500 568000 568500 569000 569500

567500 568000 568500 569000 569500

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1 0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.1

0.10.1

0.1

0.1

0.1

0.1

0.1

0.10.10.1 1

11

1

1

1

1

1

1

1

1

1

1

1

1

1

1 1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

11 10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

1010

1010

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

10

1010

100

100

100

100

100

100

100

100

100

100

100

100

100

100

100

1000

1000

1000

1000

1000

1000

1000

788.4

929.6

43

224.1

4.2

3.3

53

843.8

5

6.9

8.3

9.5

1239.9

9.2 7.8

80.67.5

11.3 34.7

6.9

1.11.6 37

5.432.6

5.1

46.961

5.8

87.3

47

132

70.1

12.54.3

10.5

96.3

10

1163

13363.4

78.5

187.8

287562.5

250

437.5

125437.5

62.5

3125

125

16250

1250

1000

562.5

62.5125

62.5

125

125

250125

437.5

875

1937.5

62.5

312.5812.5

15000

312.5250

1251252375

187.5

187.5312.5

44062.5

427501625

187.5

83125

1312.5

187.5 2187.5312.5

1625

107250

115156.25

567400 567500 567600 567700 567800

567400 567500 567600 567700 567800

54916

00

5491700

54

9160

0549

1700

<10

10 to 25

25 to 100

100 to 200

200 to 400

400 to 1000

1000 to 5000

5000 to 50000

>50000

ROCK GEOCHEMISTRY

Gold in ppb

0 25 50 75 100

number of samples

SOIL GEOCHEMISTRY

0

50

Log10 ScaleAu (ppb)

Co

un

t 40

30

20

10

0.1 1 10 100 1000 10000 100000

5ppb lower limit

125

# of valuesminmaxmedianmean var std.dev coef.var

Summary Stats265

510000

5314.8

2150545.21466.5

4.7

# of valuesminmax

Summary Stats266

<0.5115156.3

ST. MARY FAULT ZONE

A widespread fol iat ion occurs in a broad zone in both the hanging wall(northwest) and footwall (southeast) of the St. Mary fault. In manycases, the fol iat ion is the dominant structural trend and bedding isdiff icult to determine. The fol iat ion is accompanied by sl ickensides,minor folds and shear sense indicators similar to the feature in the photoabove. Foliation parallel veining is rare on the Quartz Mountain propertyand has not been sampled enough to make an association between gold mineralization and the structural trend.

ALTERATION

Sericite, carbonate, +/- chlorite, +/- pyrite, +/- pyrolusite

Albite, specularite, chlorite

Albite-hematite breccia within Aldridge medium bedded quartzites.The hematite breccia is associated with the south-east trendingQuartz Creek fault. The breccia is locally distr ibuted along thefault and grades to a chlorite-albite breccia distal from the fault.Several zones were observed along the fault trend with chlorite andalbite mineralogy. Rock geochemistry sampling of the zones did notcontain consistent anomalous concentrations of gold.

1cm

10cm

Location of veining with approximate trend

VEINING

ALTERATION AND MINERALIZATION

Sericite and carbonate alteration associated with composite quartzveins and breccias. The veins are sporadically mineralized with pyrite blebs and are haloed by disseminated pyrite weathered to jarosite. The sericite alteration zones are regionally associated with north-east trending shears however, sericite zones on the Quartz Mountain property do not have a consistent association to a structural trend.Gold concentrations among sericite zones is not consistent though mult iple samples from a zone are either consistently anomalous in gold, or consistently absent of elevated gold concentrations. This maysuggest sericite zones are produced in more than one structural eventand gold emplacement is l imited to a select few of those events.

Geology map of the Quartz Mountain property from mapping in 2014 and compiled historical data

see detail map

see detail map

Rock geochemistry historical data and alteration

Total Magnetic Induction (TMI) geophysics from Klondike Gold Corp. internal report

Detail of Golden Egg deposit with surrounding contoured soil geochemistry from historical data

1000m

SCALE: 1:10,000

0m 500m

200m

SCALE: 1:2,000

0m 100m

1000m

SCALE: 1:10,000

0m 500m