2015 Slocan Dayton gold MLS Mining

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Ruby 773182 Claim Group John Nick Bakus Event 5543468
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July 5, 2015 Sookochoff Consultants Inc. Page 1 of 33
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GEOLOGICAL ASSESSMENT REPORT
(Event 5543468)
for
JOHN NICK BAKUS
(Owner & Operator)
on a
STRUCTURAL ANALYSIS
Work done on Tenures
1034221, 1034222, 773182, and 773162
of the 20 claim
Ruby 773182 Claim Group
Slocan Mining Division
BCGS Maps 082F.063/.073/.074/.083/.084
Centre of Work
5,517,706N, 468,181E
(Zone 11U NAD 83)
work done from
February 11, 2015 to February 14, 2015
Author & Consultant
Laurence Sookochoff, PEng
Sookochoff Consultants Inc.
Report Submitted
July 20, 2015

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TABLE OF CONTENTS
page
Summary ------------------------------------------------------------------------- 4.
Introduction ---------------------------------------------------------------------- 5.
Property Location and Description ------------------------------------------- 5.
Accessibility, Climate, Local Resources,
Infrastructure and Physiography ------------------------------------ 7.
Water and Power ---------------------------------------------------------------- 8.
History: Ruby 773182 Claim Group Area ----------------------------------- 9.
082FNW129 – HOPE--------------------------------------------------------- 9.
082FNW155 – OTTAWA -------------------------------------------------- 11.
082FNW168 – REPUBLIC ------------------------------------------------ 12.
082FNW169– CLUB ------------------------------------------------------- 12.
082FNW172 – LAKEVIEW ----------------------------------------------- 12.
082FNW174 – EXCHANGE ---------------------------------------------- 12.
History: Ruby 773182 Claim Group ----------------------------------------- 12.
082FNW165 – WHITE HOPE -------------------------------------------- 13.
082FNW167 – NORTHERN LIGHT ------------------------------------ 13.
082FNW173 – DAYTON -------------------------------------------------- 13.
082FNW216– MORNING STAR ----------------------------------------- 14.
082FNW224 – KIMBERLY ----------------------------------------------- 14.
082FNW243 – SPRINGER CREEK ------------------------------------- 14.
Geology: Ruby 773182 Claim Group Area --------------------------------- 14.
082FNW129 – HOPE--------------------------------------------------------- 16.
082FNW155 – OTTAWA -------------------------------------------------- 16.
082FNW168 – REPUBLIC ------------------------------------------------ 17.
082FNW169– CLUB ------------------------------------------------------- 18.
082FNW172 – LAKEVIEW ----------------------------------------------- 18.
082FNW174 – EXCHANGE ---------------------------------------------- 18.
Geology: Ruby 773182 Claim Group ---------------------------------------- 19.
082FNW165 – WHITE HOPE -------------------------------------------- 19.
082FNW167 – NORTHERN LIGHT ------------------------------------ 19.
082FNW173 – DAYTON -------------------------------------------------- 19.
082FNW216– MORNING STAR ----------------------------------------- 19.
082FNW224 – KIMBERLY ----------------------------------------------- 20.
Mineralization: Ruby 773182 Claim Group Area -------------------------- 20.
082FNW129 – HOPE--------------------------------------------------------- 21.
082FNW155 – OTTAWA -------------------------------------------------- 21.
082FNW168 – REPUBLIC ------------------------------------------------ 21.
082FNW169– CLUB ------------------------------------------------------- 21.
082FNW172 – LAKEVIEW ----------------------------------------------- 21.
082FNW174 – EXCHANGE ---------------------------------------------- 22.

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Table of Contents (cont’d)
Mineralization: Ruby 773182 Claim Group --------------------------------- 22.
082FNW165 – WHITE HOPE -------------------------------------------- 22.
082FNW173 – DAYTON -------------------------------------------------- 22.
082FNW216– MORNING STAR ----------------------------------------- 23.
082FNW224 – KIMBERLY ----------------------------------------------- 23.
Structural Analysis: ------------------------------------------------------------ 25.
Interpretation and Conclusions ------------------------------------------------- 28.
Selected References ------------------------------------------------------------- 31.
Statement of Costs -------------------------------------------------------------- 32.
Certificate ------------------------------------------------------------------------ 33.
TABLES
Table I Tenure of the Ruby 773182 Claim Group ---------------------- 6.
Table II Ruby 773182 Claim Group Minfile Summary -------------- 23.
Table II Approximate UTM Location of Figures 5 & 7
Cross-Structures & Minfiles ------------------------------------- 27.
ILLUSTRATIONS
Figure 1. Ruby 773182 Claim Group: Location Map ----------------- 5.
Figure 2. Ruby 773182 Claim Group: Claim Location --------------- 8.
Figure 3. Ruby 773182 Claim Group: Claim Map ------------------- 9.
Figure 4. Ruby 773182 Claim Group North: Geology, Claim
, & Minfile ------------------------------------------------------ 15.
Figure 4a . Ruby 773182 Claim Group South: Geology, Claim
, & Minfile ------------------------------------------------------ 15.
Figure 5. Lineaments as Indicated Structures -------------------------- 25.
Figure 6. Rose Diagram from Lineaments of Figure 5 --------------- 26.
Figure 7. Structural Intersections and Minfile locations -------------- 27.
Figure 8 Conceptual Model of a Porphyry-Polymetallic
Vein Association ----------------------------------------------- 28.

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SUMMARY
The 20 claim Ruby 773182 Claim Group (“Property”) is located within the historic Slocan
mining camp area 445 kilometres east-northeast of Vancouver and adjacent and east of
Slocan Lake and the village of Slocan City. The Property covers an area of 3,714 hectares
with dimensions of 14 kilometres north-south and up to five kilometres east-west. Most
resources and infrastructure requirements for a preliminary exploration and
development program could be found at Slocan City or Castlegar some 65 kilometers
distant.
The Property is entirely underlain by the Nelson Batholith which occupies the central
portion of the Kootenay Arc, a 400 kilometre long curving belt of early Palaeozoic to
Mesozoic sedimentary, volcanic, and crystalline metamorphic rocks trending northeast
for 160 kilometres across Washington State into British Columbia, thence north along
Kootenay Lake and northwest into the Revelstoke area.
The historic Slocan Mining Camp, where active exploration began around 1865, became
one of the most productive mining camps in the province, and achieved peak
production in 1918. The camp and surrounding areas includes 175 documented mineral
deposits of which more than half are mineral producers; 13 mines have produced more
than one million grams of silver. The Property includes four of these mineral producers;
the most being the 91 tonnes from the White Hope property.
Four indicated primary structures and four structural intersections were delineated in
the structure analysis of four claims of the Property. Both the primary structures and
the cross-structures are significant as mineral controls in this geological environment
based on the Nelson intrusive. The mineral controls may be for a potential polymetallic
vein hosted or for a potential porphyry resource. Both types are indicated on the
Property with the vein type predominant as polymetallic veins of silver, lead, zinc and at
times gold.
Cross-structure “A” is the most significant as it is near the White Hope past producer
(Minfile 082FNW165); one of the most developed and productive properties of the five
past producers included in the Property (Table II). Cross-structure “B” is also located
near a known mineral zone; the Northern Light showing (Minfile 082F167).
Thus, the cross-structures should be explored for a potential depth related mineral
feeder zone where most pertinent geological information would be available to
locations of a potential porphyry mineral resource. The potential being indicated in the
polymetallic veins typically peripheral to a porphyry (Figure 8) and the several veins and
stockworks at the Springer Creek showing (Minfile 082FNW224).

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INTRODUCTION
In February 2015 a Structural Analysis was completed on Tenures 1034221, 1034222,
773182, and 773162 of the 20 claim Ruby 773182 Claim Group. The purpose of the
program was to locate any cross-structures which may be integral in geological controls
to potentially economic mineral zones comparable to other productive mineral zones in
the immediate area.
Information for this report was obtained from sources as cited under Selected
References, from previous work the writer has done in the general area, and from the
information gained from the completion of the structural analysis.
Figure 1. Ruby 773182 Claim Group: Location Map
(Base Map from MapPlace)
PROPERTY LOCATION & DESCRIPTION
Location
The Ruby 773182 Claim Group is located 445 kilometres east-northeast of Vancouver
British Columbia, in the Slocan Mining Division, within BCGS Maps
082F.063/.073/.074/.083/.084. The northern portion of the Property borders Slocan
Lake to the east with the village of Slocan City at the south end of the Lake.
Description
The Ruby 773182 Claim Group is comprised of 20 contiguous claims covering an area of
3714.9867 hectares. Particulars are as follows:

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Table I Tenures of the Ruby 773182 Claim Group
Tenure Number Type Claim Name Good Until Area (ha)
607060 Mineral RUBY STEEL 20150802 479.6776
705871 Mineral RUBY STEELE 2 20150802 500.7562
774262 Mineral RUBY SOUTH 2 20150801 438.4704
855179 Mineral 20150802 125.1248
944429 Mineral LILY B 20160801 62.5854
1027826 Mineral Slocan Kim 57OTAG 25GTAU 20160801 41.7237
1030338 Mineral 20170701 104.3074
1030341 Mineral SLOCAN KIMBERLY SOUTH 20170701 104.3215
1034177 Mineral Slocan Exchange SW 20150802 83.4879
1034178 Mineral RUBY SOUTH1 20150801 333.9789
1034179 Mineral RUBY SOUTH PrL CONNECT 20150801 20.8707
1034221 Mineral Slocan White Hope AU RL 20150802 41.6926
1034222 Mineral Slocan White Hope N PL 20150802 20.8445
Total Area: 3714.9867 ha
*Upon the approval of the assessment work filing Event Number 5543468.

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ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND
PHYSIOGRAPHY
Access
Road access to the Ruby 773182 Claim Group from Castlegar is as follows:
From via Direction To
Kilo-
metres
Castlegar Hwy 6 North South Slocan 20
South Slocan Hwy 6 NNW Passmore 20
Passmore Hwy 6 NNE
Lemon Creek. S end
of claim group two k
east
24
Lemon Creek Hwy 6 N
N end of claim group
To Tenure 1034222
15
Forestry roads provide access across the southern and northern portions of the claim,
Climate
The climate of the area is of relatively warm summers and moderately cool winters.
Exploration would probably be restricted to about eight months due to snow cover
Local Resources
Sufficient accommodation and supplies, for a preliminary exploration program would be
available at the village of Slocan City and to a much greater extent at Castlegar, some 65
kilometres south of Slocan City. Contracts for technical exploration and development
programs would probably be made with companies based in Vancouver with some
supporting personnel from surrounding communities.
Infrastructure
Castlegar is linked to Vancouver through commercial flights and by road. Vancouver is a
port city on the southwest corner of, and the largest city in the Province of British
Columbia.

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Accessibility, Climate, Local Resources, Infrastructure and Physiography (cont’d)
Physiography
The Property covers an area of gradual to moderate forested slopes with selectively
logged areas.
Elevations range from 542 metres in the north at Slocan Lake which the claims
encroach, to 2,060 metres along a mountain ridge in the mid-east portion of the
Property.
WATER AND POWER
Sufficient water for a summer diamond drill program should be available on or adjacent
to the Golden Crown Claim
The nearest commercial power source is at Slocan City. Diesel-electric generated power
would be required in the initial pre-production stages of a mineral resource
development.
Figure 2. Ruby 773182 Claim Group: Claim Location
(Base Map from MapPlace & Google)

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Figure 3. Ruby 773182 Claim Group: Claim Map
(Base map from MapPlace)
HISTORY: RUBY 773182 CLAIM GROUP AREA
The history on some of the more significant mineral MINFILE reported prospects and
past producers on the Ruby 773182 Claim Group or areas as blocked out on Figures 4 &
4a are reported as follows. The descriptions herein are copied from Minfile.
The distance from the Ruby 773182 Claim Group is relative to the Ruby 773182 Claim
Group
HOPE past producer (Pb-Zn skarn, Au skarn)
Minfile 082FNW129
400 metres east
The earliest reported activity in this vicinity was on the Cameronian claim (Lot 5976), located about
0.5 kilometre north of the Hope No. 2 claim. The Cameronian workings in 1897 included a 24-
metre shaft; some ore was reportedly soaked for shipment. The claim was Crown-granted in 1903
to the Cameronian Gold and Silver Mining Company, Limited Liability. The adjacent Sligo claim (Lot
5975) was probably also held by the company.

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History: Ruby 773182 Claim Group Area (cont’d)
Hope past producer (cont’d)
The Quebec claim (Lot 2885), located about 0.5 kilometre southwest of the Hope No. 2 and lying
across Cameronian creek, was Crown-granted to Wm. Harrison in 1899.
The Hope No. 2 claim (Lot 2884) was Crown-granted in 1899 to R. Cooper and H. Sheran.
Development work from 1898 or earlier included open cuts and a 15-metre adit. No further work
was reported until 1922 when owner R. Cooper resumed explorations. Regina interests acquired
the property and in May 1927 incorporated Piedmont Mines Limited to put the property into
production. A 1676-metre long tramway was installed and some 435 tonnes of ore were shipped.
A new adit exposed only limited mineralization and work ceased in 1928.
A claim group owned in 1927 by F. and J. Binnish, of Slocan City, and comprising the First Thought
FR, Success, Motherlode FR and Diamond Jubilee FR, was located below the Hope No. 2 claim on
the Cameronian creek slope. Surface work was reported on lead-zinc showings located about 305
metres lower than the Hope showings.
By 1948 the Hope No. 2 claim was owned by R.D. Kennedy of South Slocan. That year a lessee
shipped 23 tonnes of mineralized dump rock. In 1951 lessee W. Foster shipped 11 tonnes of ore.
The showings were reportedly examined and sampled for Cominco Ltd. in 1949 by E.H. Caldwell,
who estimated a potential of about 129,730 tonnes at 263.9 grams per tonne silver, 7.9 per cent
lead and 17.4 per cent zinc (D.G. Allen, 28/11/84, in Chapleau Resources Ltd Prospectus,
17/05/85).
When examined by A.B. Irwin for the Geological Survey of Canada in 1950, the workings included 4
adits totalling about 177 metres of crosscuts and drifts, and a raise to a 10 metre diameter glory
hole which was the source of most of the ore shipments.
Chapleau Resources Ltd. in October 1984, optioned the Hope No. 2 from Lena Kennedy of South
Slocan, the Hope 3-7 located claims, and the overlying Hope 8 and 9 (40 units) from R.D. Kennedy,
of Cranbrook; the company also acquired the Quebec claim; prospecting and sampling was
reported in the fall of 1984.
Noranda Exploration Company optioned the property from Chapleau in October 1986. Chapleau
in January 1987, obtained an option on the Cameronian claim from D. Cameron, of Vancouver.
Work 1986-87 included geochemical soil, silt and rock surveys, mag, EM and HLEM surveys.
Trench of anomalous targets located narrow beds of low grade zinc.
Drilling in 1988 intersected stratiform massive sulphide zones of zinc (Assessment Report 17323).
In 1991, Kokanee Explorations Ltd. drilled 9 holes, totalling 255.5 metres.
They indicated a reserve of 13,600 tonnes grading 59.3 grams per tonne silver, 1.3 per cent lead
and 3.6 per cent zinc is readily available to open pit mining with 1.7:1.0 waste to ore ratio
(Assessment Report 21324).
A sample from the dump taken in 1987, assayed 320 grams per tonne silver, 0.03 grams per tonne
gold, 0.0563 per cent copper, 7.8 per cent lead and 21.4 per cent zinc (Open File 1988-11). A
sample taken 500 metres to the southwest assayed 0.32 per cent molybdenum, 0.024 per cent
lead and 0.029 per cent zinc (Open File 1988-11).

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OTTAWA past producer (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW155
One kilometre east
The history of the Ottawa mine dates back to 1896 when the Ottawa claim (Lot 4968) was located,
however, it was not until 1902 that major development work by a Pittsburg syndicate was
attempted. By 1904 the property was developed by 1067 metres of tunnel on 4 levels. It was
operated intermittently by the owners until 1908 and then by leasers until 1913. In 1913 the
group of over 20 claims was acquired by the Consolidated Mining & Smelting Co. Ltd. and
extensive development work was carried on until 1918 when the mine was closed and the
equipment removed.
The workings at this time consisted of 5 adits at vertical intervals of 30.4 metres and a 6th level
driven from a shaft. In 1920 a 50-ton per day mill was constructed. Leasers continued to operate
the mine until 1935. In 1935 the group, consisting of 31 claims, was acquired by the Ottawa Silver
Mining & Milling syndicate of Spokane, who, in 1937, built a 100-ton per day flotation plant which
burned shortly after. They drove an 8th level as a crosscut for 366 metres and then drifted on the
vein. Leasers worked the property intermittently from 1941 to 1950. An option on the property
was given to Violamac Mines (B.C.) Ltd. in 1950.
The following year Harrison Drilling and Exploration Co. Ltd. of Vancouver held operating control
under an agreement with Violamac Mines. Harrison Drilling and Exploration Co. Ltd. was
reorganized in 1953 under the name of Hardex Mines Ltd. and a diamond drilling program was
carried out. In 1956 the owners resumed operations. An option on the property was given to the
Yukon Western Mining & Prospecting Co. Ltd. of Slocan City in 1958. In 1960 the name of this
company was changed to Skylane Mines Ltd. Most of the work done at this time was confined to
stoping in the West vein on No. 8 level. In 1960 Ottawa Silver Mines Ltd. bought the option from
Skylane Vines Ltd. Later in the year an option was given to the Silver Buckle Mining Co. of Wallace,
Idaho. This option was dropped in December after a geological examination of the property had
been made. A 9th level was started at this time. In 1962 a ventilation raise was driven from No. 8
level to No. 6 level, a distance of approximately 143 metres, following the dip of the vein. In
driving the raise, several lenses of very high-grade ore were opened up and subsequently stoped
out.
The No. 9 level drift was extended to a length of 152 metres. During 1963 and 1964 exploration
and development work was carried out on No. 9 level. A 75-ton mill was built in 1963 and put into
part time operation in 1964. In 1963 the company was reorganized under the name Slocan
Ottawa Mines Ltd. In 1980 the mine was owned by the Slocan Development Corporation Limited
and leased to C. Thickett and Memphis Mines Ltd. between 1976 and 1982.
Total recorded production between 1903 and 1984 amounts to 26,476 tonnes mined, yielding
55,940,682 grams of silver, 982 grams of gold, 360,085 kilograms of lead, 12,774 kilograms of zinc
and 793 kilograms of copper.

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REPUBLIC showing (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW168
One kilometre west
The Republic group of claims is located about 5 kilometres by gravel road northeast of Slocan City.
The claims were first staked in 1895 and worked intermittently until 1952. Tandem Resources Ltd.
held the property, including the Club (082FNW169) in 1972. In 1979, they conducted an IP survey
and sampling.
R.B. Stewart prospected the Evening No. 9 claims in 1987.
CLUB past producer (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW169
50 metres west
The Club claim is situated towards the head of Scorpion Creek, 3.5 kilometres northeast of Slocan.
Access is from the Slocan highway via a switchback road that crosses Scorpion Creek below the
property. See also Republic (082FNW168).
The Club property was first prospected in 1904. The target of exploration was two quartz veins in
crushed granitic rocks that appear to be related to the Nelson batholith.
The property was covered by the Ross claims, held in 1972 by Tandem Resources Ltd.
LAKEVIEW past producer (Polymetallic veins Ag-Pb-Zn+/-Au; Au-quartz veins)
Minfile 082FNW172
200 metres west
The Lakeview property is situated east of Springer Creek, at the elevation of 900 metres, and 1.5
kilometres due east of Slocan. Access is directly from Slocan via the Springer Creek gravel road
EXCHANGE past producer (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW172
200 metres east
The Exchange property is at 1600 metres elevation on the ridge southwest of Dayton Creek, 3
kilometres due east of Slocan. Access to the property is from a switchback mountain road that
joins the Springer Creek road just east of the Slocan highway.
HISTORY: RUBY 773182 CLAIM GROUP
The history on some of the MINFILE reported occurrences, prospects, and past
producers within the Ruby 773182 Claim Group as blocked out on Figure 4 are reported
as follows. The descriptions herein are copied from Minfile.

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History: Ruby 773182 Claim Group (cont’d)
WHITE HOPE past producer (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW165
Within Tenure 1034221
The history of the property prior to 1928 is obscure. Cairnes (Memoir 184) reports that it was
formerly known as the Paystreak, however the only Paystreak mentioned in the Annual Reports of
the Minister of Mines (1897 and 1902) is reported to be on Twelvemile Creek. Maps of the area
show Twelvemile and Tenmile creeks as tributaries of Kaslo creek. However, according to the
1906 zinc commission report on the Enterprise mine, Tenmile creek empties into Slocan Lake
about 16 kilometres south of New Denver. On maps of the area this creek is called Enterprise
creek. The 1897 report listed the Paystreak property on Twelvemile creek under the heading
"Tenmile creek". Due to these changes in names, the location of the Paystreak property is not
clear.
In 1928 the White Hope group, consisting of 6 claims and a fraction, was owned by Peter Strand
and C.W. Tipping of Slocan. During the year a 46-metre tunnel was driven in limestone by leasers
C. Hansen and associates of Idaho. The mine was closed in 1929 and remained so except in 1935
and 1942 when it was operated by C.W. Tipping.
In 1947 the Spokane Slocan Co. acquired the White Hope group along with the Homestake
(082FNW213), Senator (082FNW164), Get-There-Eli (082FNW191) and V & M (082FNW191)
claims. During 1950 and 1951 J.J. McDonell worked the property.
In 1957 the Dolores-Dorothy Exploration and Mining Co. Ltd. of Nelson acquired the White Hope,
White Hope No. 1, Homestake and Senator Crown-granted claims and 6 recorded claims.
NORTHERN LIGHT showing (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW167
This property is located at the extreme headwater area of Scorpion Creek, at an elevation of 1300
metres, 4.5 kilometres northeast of Slocan. Access to the property is from the Slocan highway via
a switchbacked logging road on the northwest slope of Ottawa Hill. The Republic (082FNW168)
lies to the southwest. Adit locations are shown on Geological Survey of Canada Map 272A.
The Northern Light was located in 1902 and Crown granted (Lot 11130) in 1916.
The only development work is two short adits from which there is no known ore production.
International Cherokee Development and Manny Consultants conducted geochemical and
geophysical surveys over the S and R claims between 1983 and 1986.
DAYTON past producer (Polymetallic veins Ag-Pb-Zn+/-Au; Au-quartz veins)
Minfile 082FNW173

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History: Ruby 773182 Claim Group (cont’d)
Dayton past producer (cont’d)
The Dayton property is near the mouth of Dayton Creek at the elevation of 1035 metres, 3
kilometres east-northeast of Slocan. Access is from the Slocan highway via the Springer Creek
road. OGG Corporation held the property in 1982.
MORNING STAR past producer (Polymetallic veins Ag-Pb-Zn+/-Au; Au-quartz veins)
Minfile 082FNW216
The Morning Star is located on the north side of Springer Creek, a few metres above its junction
with Dayton Creek. It may be reached by a 5-kilometre long road from Slocan City. The claim was
originally staked in 1900 and the following year about 210 metres of development work was done.
The claim has been held by record and throughout most of its history the work done on it has been
confined to yearly assessment requirements. Most of the development work was done during the
years 1901 and 1946.
OGG Mining and Investing Inc. held the property in 1914.
KIMBERLEY past producer (Polymetallic veins Ag-Pb-Zn+/-Au;
Minfile 082FNW224
In 1906, some development work was done by C. Dempster resulting in a small shipment of ore
(Minister of Mines Annual Report 1906, page H146).
SPRINGER CREEK showing (Vein, Stockwork)
Minfile 082FNW243
Several quartz veins and stockworks are located within the Nelson Intrusives lying east of Slocan
Silver Camp and south of Springer Creek. A series of logging roads provide access to prospectors
and geologists. During 2010, a prospecting effort discovered several mineralized quartz veins along
the road system and in old workings. In particular, along the new Ottawa logging road, which
heads uphill from the Springer Creek Forest Service Road, there were several sites located, grab
sampled and analyzed by Tom Kennedy. This is the Ruby Steel(e) Property of Kootenay Gold
Incorporated.
GEOLOGY: RUBY 773182 CLAIM GROUP AREA
The geology on some of the more MINFILE reported occurrences, prospects, and past
producers on the Ruby 773182 Claim Group are blocked out on Figures 4 & 4a and are
reported as follows. The descriptions herein are a copy from Minfile.
Group.

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Figure 4. Ruby 773182 Claim Group (North): Geology, Index, Claim & Minfile
Figure 4a. Ruby 773182 Claim Group (South): Geology, Index, Claim & Minfile

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Geology: Ruby 773182 Claim Group (cont’d)
GEOLOGY LEGEND
PeESTgr
Paleocene to Eocene
Sheppard, Tuzo, Creek, Shingle
Creek Intrusions
Granite, alkali feldspar, granite
intrusive rocks
Kog
Cretaceous
Unnamed
orthogneiss metamorphic rocks
MJNgd
Middle Jurassic
Nelson Batholith
granodioritic intrusive rocks
CPm
Carboniferous to Permean
Unnamed
metamorphic rocks, undivided
Minfile 082FNW129
400 metres east
The country rock is porphyritic Nelson granite enclosing a large pendant of black argillaceous
quartzite and minor limestone, largely altered to skarn. The pendant rocks are cut by small
irregular bodies of granitic rocks and pegmatite. The ore occurs in skarn that consists of garnet and
calcite. The ore minerals are pyrrhotite, sphalerite and galena forming bands and disseminations.
Minfile 082FNW155
One kilometre east
The property is developed on nine levels, 5 of which are serviced by adits driven at vertical intervals
of about 30 metres. These workings explore a broad shear/breccia zone in coarse grained,
porphyritic Nelson quartz monzonite cut by felsite and lamprophyre dikes. The zone trends nearly
north and dips easterly from 25 to 45 degrees. The zone comprises two rather well-defined lodes
known as the West or Noble and East or Ottawa veins, respectively.

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Geology: Ruby 773182 Claim Group Area (cont’d)
Ottawa past producer (cont’d)
Mining at the surface and underground indicates that these lodes are not exactly parallel, but
approach each other towards the south and may join. On the No. 5 level the lodes are about 10
metres apart Most of the work has been done on the East lode that is 0.6 to 6 metres wide,
composed of crushed and broken granite, gouge and vein material - the latter having been stoped
in places across a width of as much as 2.4 metres. The West lode is as much as 15 metres wide in
places and it is reported to have produced some good ore in the uppermost workings. On No. 8
level, the stoped vein on the West lode, strikes 025 to 040 degrees and dips 20 degrees southeast.
The vein is up to 0.3 metres wide - bounded by a sharply defined gouge- filled slip along the
footwall and an irregular hanging wall. The East lode on the No. 8 level is strong and composed of
about 1 metre of gouge and breccia cemented by quartz. It strikes 170 degrees and dips 30 to 40
degrees east.
Minfile 082FNW168
One kilometre west
Past production occurred from the Republic vein which is less than 75 centimetres thick. The
quartz vein contains pyrite, argentite, native silver and gold with minor galena and sphalerite.
Bornite are also reported. The vein is hosted in potassium-feldspar porphyritic granite. Wallrock
alteration includes quartz, sericite, chlorite, and carbonate. It extends less than 1 metre from the
quartz veins. There are at least 2 main quartz veins on the property. They strike west and dip
moderately to gently north.
The Republic vein has been developed by an inclined shaft, collared at an elevation of 1334 metres.
The incline has been sunk to a depth of some 18 metres on the vein which is approximately 1-
metre wide. The vein strikes 085 degrees and dips 30 degrees to the north and is offset slightly by
step-faults striking 025 degrees to 045 degrees with dips from 65 degrees to 85 degrees northwest.
Short irregular drifts and slopes have been driven from the incline. Another shaft, some 244 metres
west of the above shaft, has been sunk on what appears to be the extension of the Republic vein.
The vein is 0.6-metre wide, strikes 050 degrees and dips 35 degrees northwest. Further west 2
levels have been driven to crosscut the vein but neither one did before the work was stopped.
The Bell No. 2 adit, west of the Republic adits, follows a discontinuous vein which strikes 020
degrees and dips 45 degrees southeast. Beyond 18 metres from the portal the vein is complexly
faulted. The veins in the eastern portion of the property generally strike east and dip gently north
whereas the west veins strike northeasterly with a flat dip to the northwest. Ore shoots within the
veins are erratically distributed and are elongated down the dip. The Crown-granted mineral claims
have numerous showings and surface workings and a few claims which were previously worked on
and surveyed were covered by some of the Ross claims in 1922. The Slocan Bob claim was covered
by Ross No. 9 and the Ross No. 11 claims. The Club claim (082FNW169), which has two veins
reported to be at right angles to one another, were covered by Ross No. 10 and Ross No. 12 claims.

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Minfile 082FNW169
50 metres west
The Club property was first prospected in 1904. The target of exploration was two quartz veins in
crushed granitic rocks that appear to be related to the Nelson batholith. The main vein is about 0.9
metre in width, strikes northeast and dips northwest at about 30 degrees. Rich samples have
reportedly been obtained from a shallow inclined shaft sunk on this vein
The main vein is about 0.9 metre in width, strikes northeast and dips northwest at about 30
degrees. Rich samples have reportedly been obtained from a shallow inclined shaft sunk on this
vein.
Minfile 082FNW172
200 metres west
The Lakeview property comprises the Lakeview No. 8 claim (Crown granted in 1898) and located
MS claims, Selmon, Maur I and II. The property is underlain predominantly by granitic rocks of the
Nelson batholith. The focus of exploration and development is a northerly trending vein exposed
for a strike length of 100 metres at surface and 35 metres underground. The vein, consisting of
lenses and stringers of quartz, dips 70 degrees east and is hosted by highly crushed granite.
Disseminated sulphides occurring in the wall rocks and the vein system include pyrite, galena and
sphalerite, together with a minor amount of chalcopyrite and pyrrhotite. At surface chalcocite and
covellite occur associated with late carbonate gangue replacing chalcopyrite and cerussite replaces
galena.
Development on the property consists of open cuts, an adit, a shallow shaft and a small floatation
plant. The shaft, about 5 metres deep, remains from the original workings. At the south side of
the shaft, the quartz vein has a width of 0.7 metre, which narrows to 40 centimetres at a point 9
metres south, where a sample taken across cellular rusty quartz assayed 17 grams per tonne gold
and 410 grams per tonne silver. The adit is a crosscut for 15 metres on a course of 125 degrees to
the vein, then 12 metres at 155 degrees, and further drifting for 23 metres, striking 175 degrees to
the face that lies directly below the end of stripping on surface. There is an ore shoot at the second
bend in the tunnel that connects to the shaft - the best mineralization is exposed in the first 15 to
18 metres of drift section of the tunnel.
EXCHANGE past producer (Polymetallic veins Ag-Pb-Zn+/-Au)
Minfile 082FNW172
200 metres east
A quartz vein in Nelson granite has been explored by three adits, a shaft and a 30-metre winze sunk
from the lowest adit. The vein is 1.5 metres wide, banded with clear and milky white quartz and
pyrite accompanied by some galena, sphalerite and ancillary silver-bearing minerals.

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GEOLOGY: RUBY 773182 CLAIM GROUP
The property is almost wholly underlain by granodioritic rocks of the middle Jurassic
Nelson batholith (MJNgd) being fringed on the west by rocks of the Paleocene to Eocene
Sheppard, Tuzo Creek, and Shingle Creek intrusions.
The geology on the MINFILE reported occurrences, prospects, and past producers within
the Ruby 773182 Claim Group as blocked out on Figure 4 are reported as follows. The
descriptions herein are copied from Minfile.
Minfile 082FNW165
The property is underlain by banded gneiss and foliated granite on the west boundary of the
Nelson batholith. The gneiss carries abundant zenoliths of older country rocks and the banded
structures conform to the foliated structures of the intrusion.
Minfile 082FNW167
Little is known about this property other than it is underlain by coarse grained, porphyritic Nelson
granite.
Minfile 082FNW173
The Dayton claim (Lot 2419) is underlain by coarse grained, porphyritic Nelson granite. The
workings consist of a crosscut adit that intercepts two vein structures.
Drifting on the principal structure explores a fault fissure system that strikes 160 degrees and dips
35 degrees northeast. This contains lenses of quartz up to 46 centimetres wide, mineralized with
pyrite, some galena, argentite and tetrahedrite. A second quartz vein, 15 metres further on at the
face of the crosscut, strikes 025 degrees and dips 55 degrees southeast. This vein is 1.8 metres
wide and contains some coarse pyrite cubes.
Minfile 082FNW216
The Morning Star occurrence is hosted by porphyritic potassium feldspar granite and hornblende-
biotite diorite of the Middle Jurassic Nelson plutonic rocks, cut by numerous small felsic
occasionally pegmatic dykes. The vein is mainly hosted by the diorite which is strongly silicified and
locally kaolinized close to vein walls.

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Morning Star past producer (cont’d)
The vein is a fracture to brittle shear filling of quartz with some siderite and calcite with
disseminated to veinlets of sheared galena, sphalerite, and cubic pyrite with possibly some
tetrahedrite. The vein is offset by numerous small faults and its southern end is terminated by a
fault.
The workings consist of two adits. In the lower one the main vein has been traced for 116 metres
and a branch vein near the south end has been followed for 37 metres. With the other lateral
workings off from the main tunnel a total of about 180 metres of development work has been done
on this level. The upper adit, 30-metres above, is about 30 metres long.
Minfile 082FNW224
The Kimberly is located along Springer Creek and is assumed to be quartz vein-hosted
mineralization in granite of the Middle Jurassic Nelson intrusions.
Minfile 082FNW243
Several quartz veins and stockworks are located within the Nelson Intrusives lying east of Slocan
Silver Camp and south of Springer Creek. A series of logging roads provide access to prospectors
and geologists. During 2010, a prospecting effort discovered several mineralized quartz veins along
the road system and in old workings. In particular, along the new Ottawa logging road, which heads
uphill from the Springer Creek Forest Service Road, there were several sites located, grab sampled
and analyzed by Tom Kennedy. This is the Ruby Steel(e) Property of Kootenay Gold Incorporated.
The Jurassic-Cretaceous Nelson Batholith granodiorite is the host rock for these vein systems.
MINERALIZATION: RUBY 773182 CLAIM GROUP AREA
The mineralization on some of the more significant mineral MINFILE reported
occurrences, prospects, and past producers peripheral to the Ruby 773182 Claim Group
are blocked out on Figures 4 & 4a and are reported as follows. The descriptions herein
are copied from Minfile.
Group.

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Mineralization: Ruby 773182 Claim Group Area (cont’d)
Minfile 082FNW129
400 metres east
A sample from the dump taken in 1987, assayed 320 grams per tonne silver, 0.03 grams per tonne
gold, 0.0563 per cent copper, 7.8 per cent lead and 21.4 per cent zinc (Open File 19
Minfile 082FNW155
One kilometre east
The ore minerals consists mostly of mixture of galena, pyrite, sphalerite and a little chalcopyrite,
native silver, argentite and tetrahedrite disseminations in quartz gangue. In some high grade ore,
barite is reported to be predominant gangue mineral.
Minfile 082FNW167
The only development work is two short adits from which there is no known ore production.
Minfile 082FNW168
One kilometre west
From 300 tonnes mined 428,271 grams silver, 3,472 grams gold, 268 kilograms lead, and 184
kilograms zinc was recovered.
Minfile 082FNW169
50 metres west
A shipment of 4.5 tonnes of ore from this property in 1904 produced 8367 grams of silver.
Minfile 082FNW172
200 metres west
There is an ore shoot at the second bend in the tunnel that connects to the shaft - the best
mineralization is exposed in the first 15 to 18 metres of drift section of the tunnel.
Intermittent shipments of ore were made from 1937 to 1980; these totalled 4150 tonnes, yielding
132,843 grams of silver, 1504 grams of gold, 5175 kilograms of lead, 4139 kilograms of zinc, and 24
kilograms of cadmium.

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Mineralization: Ruby 773182 Claim Group Area (cont’d)
EXCHANGE past producer (Polymetallic veins Ag-Pb-Zn+/-Au; Au-quartz veins)
Minfile 082FNW174
200 metres east
The vein is 1.5 metres wide, banded with clear and milky white quartz and pyrite accompanied by
some galena, sphalerite and ancillary silver-bearing minerals.
Production from this property in 1896 amounted to 4.5 tonnes averaging 41 grams per tonne gold
and 5100 grams per tonne silver. In 1940, 12 tonnes produced 25,784 grams of silver and 156
grams of gold. Total production is estimated to be more than 50 tonnes, although records are
incomplete.
MINERALIZATION: RUBY 773182 CLAIM GROUP
The mineralization on the MINFILE reported occurrences, prospects, and past producers
within the Ruby 773182 Claim Group as blocked out on Figures 4 & 4a are reported as
follows. The descriptions herein are copied from Minfile.
Minfile 082FNW165
The target of exploration on the property is a narrow, locally pyritized quartz vein in granite,
striking 140 degrees and dipping 50 degrees southwest. The early development consists of three
main adits and several open cuts. The principal showing is on No. 2 level which has a total of 150
metres of drifts and crosscuts. The lode here is about 30 metres in length and has an average
width of 25 centimetres. Most of the original ore shipments came from the upper adit which is
about 25 metres long, with a raise to surface. The best part of the vein shows 5 to 15 centimetres
of zinc mineralization. The lower adit is 15 metres long and exposes a wider vein section but with
minor mineralization. There is another adit at the elevation of the upper adit which was driven 40
metres as a crosscut to intersect a parallel vein exposed in an open cut above, but no vein was
encountered. In 1957, a new adit site was chosen to explore the vein system from a horizon about
15 metres below the lowest workings, however no worthwhile mineralization was encountered. In
1964, the workings were reopened by Western Standard Silver Mines Ltd. In 1986, Manny
Consultants Ltd. surveyed the property as the JR claims.
In 1897 and 1902, a total of 12 tonnes was shipped from the Paystreak; recovery was 19,128 grams
of silver and 622 grams of gold. The total intermittent production from this property from 1935 to
1964 was 81 tonnes, yielding 155 grams of gold, 25,691 grams of silver, 11,424 kilograms of lead
and 11,052 kilograms of zinc.
Minfile 082FNW173

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Mineralization: Ruby 773182 Claim Group (cont’d)
Dayton past producer (cont’d)
The Dayton claim (Lot 2419) is underlain by coarse grained, porphyritic Nelson granite. The
workings consist of a crosscut adit that intercepts two vein structures. Drifting on the principal
structure explores a fault fissure system that strikes 160 degrees and dips 35 degrees northeast.
This contains lenses of quartz up to 46 centimetres wide, mineralized with pyrite, some galena,
argentite and tetrahedrite. A second quartz vein, 15 metres further on at the face of the crosscut,
strikes 025 degrees and dips 55 degrees southeast. This vein is 1.8 metres wide and contains some
coarse pyrite cubes.
Intermittent production from 1903 to 1935 totalled 17 tonnes, yielding 12,224 grams of silver, 93
grams of gold and 1006 kilograms of lead.
Minfile 082FNW216
From four tonnes milled a recovery of 6,220 grams silver, 1,991 grams gold, 35,500 kilogram of
lead, and 21,359 kilograms of zinc were recovered.
Minfile 082FNW224
… assumed to be quartz vein-hosted mineralization in granite of the Middle Jurassic Nelson
intrusions.
Recovery of 8,926 grams silver and 124 grams of gold from five tonnes mined.
Minfile 082FNW243
The Jurassic-Cretaceous Nelson Batholith granodiorite is the host rock for these vein systems.
Mineralogy includes pyrite, limonite, chalcopyrite, galena and sphalerite. A total of 42 grab samples
from both bedrock and float identify a widespread area of mineralization. Analyses include the
following selected rock samples: in parts per million for copper, lead, zinc, and silver and parts per
billion for gold.
------------------------------------------------------------------------------
Sample Type Cu (ppm) Pb (ppm) Zn (ppm) Ag (ppm) Au (ppb)
TK10-63 Quartz float >10000 >10000 >10000 >100 40567
TK10-64 Quartz vein 149.6 197.1 85 29.9 195.7
TK10-65 Quart stockwork 208.7 107.0 93 17.4 202.1
TK10-70 Quartz blocks roadbed 39.7 4124 233 >100 6020
TK10-72 Quartz stockwork 89.2 219.2 21 >100 444.1
TK10-76 Stockwork zone 67.9 684.5 113 >100 1268
TK10-86 Quartz vein 635.9 1990 78 >100 14950
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Table II. Ruby 773182 Claim Group: Minfile Summary
Minfile
82FW /Property
Location
(Tenure)
Vein strike
/dip
Major workings Production
(tonnes)
165/White Hope 1034221 140/50S 3 adits 91
167/Northern
Light
773162 ?? 2 short adits Not known
173/Dayton 705781 160/35E;
025,55SE
Crosscut adit 17
216/Morning Star 705871 170/60W 2 adits; 263m of
development
23 tonnes
mined; 4
tonnes milled
224 Kimberley 1027826 ?? ?? 5
243/Springer
Creek
705781 Several quartz
veins and
stockworks
nil nil

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STRUCTURAL ANALYSIS
The Structural Analysis was accomplished marking the observed lineaments on a Google
Earth map. A total of 66 lineaments were indicated. A Georient 32v9 software program
was used to create a Rose Diagram reflecting the grouping of the 66 lineaments into an
individual 10 °class sector angle interval.
Figure 5. Lineaments as Indicated Structures on Tenures
773162, 773182, 1034221, & 1034222
(Base Map from MapPlace)

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Structural Analysis (cont’d)
Figure 6. Rose Diagram from lineaments of Figure 5
Rose Diagram (Figure 5) Statistics
(Usage Reference: Holcombe, 2009)
Axial (non-polar) data
No. of Data = 66
Sector angle = 10°
Scale: tick interval = 3% [2.0 data]
Maximum = 22.7% [15 data]
Mean Resultant dir'n = 128-308
[Approx. 95% Confidence interval = ±22.9°]
(valid only for unimodal data)
_________________________
Mean Resultant dir'n = 128.5 - 308.5
Circ.Median = 127.5 - 307.5
Circ.Mean Dev.about median = 31.2°
Circ. Variance = 0.23
Circular Std.Dev. = 41.25°
Circ. Dispersion = 2.61
Circ.Std Error = 0.1989
Circ.Skewness = 3.15
Circ.Kurtosis = -7.17
kappa = 0.76
(von Mises concentration param. estimate)
Resultant length = 23.40
Mean Resultant length = 0.3546
'Mean' Moments: Cbar = -0.0803; Sbar = -0.3453
'Full' trig. sums: SumCos = -5.3024; Sbar = -
22.7922
Mean resultant of doubled angles = 0.3438
Mean direction of doubled angles = 124
(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'

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Structural Analysis (cont’d)
Figure 7. Structural intersection and Minfile locations
Table III. Approximate location of Figures 5 & 7 cross-structures & Minfiles
(Zone 11U NAD 83)
Cross
Structures
UTM East UTM North Elevation (m)
A 468,000 5,518,692 808
B 468,305 5,518,092 1,103
C 467,705 5,517,810 1,064
D 468,850 5,517,031 1,336
White Hope 467,928 5,518,559 900
Northern
Light
468,678 5,516,825 1,310

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Figure 8. Conceptual Model of Porphyry-Polymetallic Vein Association
(Base Map from Corbett)
INTERPRETATION & CONCLUSIONS
Four indicated primary structures and four structural intersections were delineated
from the structural analysis of the four-claim of the Ruby 773182 Claim Group
(“Property”). Both the primary structures and the cross-structures are significant as
mineral controls in this geological environment based on the Nelson intrusive. The
mineral controls may be for a potential polymetallic vein hosted or for a potential
porphyry resource. Both types are indicated on the Property with the vein type
predominant.
Although eleven of fourteen Minfile mineral properties reported on herein appear to
be related to polymetallic veins, the Springer Creek showing (Minfile 082FNW224) with
the several veins and stockworks, indicates the porphyry indication at surface with the
potential of a major porphyry at depth. This would pattern the porphyry model by the
polymetallic veins forming a halo to a porphyry (Figure 8.).

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Interpretation & Conclusions (cont’d)
In any event, the mineralized structures are important as to an interpretation to the
location of a potential porphyritic resource. The greatest information available might
be at a cross–structural location where the maximum degree of structural variance
should occur, such as brecciation and expansive stockworks. This could also provide a
conduit for pressurized hydrothermal solutions released from depth and according to
variable depositional requirements, the mineralogical and alteration features at
surface could provide the required information to additional exploration in this specific
area.
As to the four cross-structures, the location of cross-structure “A” should be the initial
are to explore. This location is near the White Hope past producer (Minfile
082FNW165); one of the most developed and productive properties (91 tonnes) of the
five past producers included in the 20 claim Ruby 773182 Claim Group (Table II). With
the three main White Hope adits exploring and developing mineral zones hosted by a
northwesterly trending structure (145/325 degrees) and the prime “AD” structure of
the structure analysis, indicated with a parallel trend some 200 metres to the east and
cross-structure “A” some 200 metres northwest along structure “AD”, cross-structure
“A” may be the main mineral feeder zone an en-echelon White Hope structure.
There are mineral properties in the Slocan area that reportedly have an increased
mineral zone or an “ore-shoot” at a cross-structure with the mineralization
proportionately decreasing with the distance along one or both structures from the
“ore-shoot”.
A comparable feature may occur at the Northern Light showing (Minfile 082F167)
where two short adits were completed to develop a mineral zone of an unreported
mineral control. The mineral showing is located 250 metres from cross-structure “D”
where a main mineral “feeder” zone may occur.
Subsequent to the exploration and evaluation of the cross-structural “A” and “D”
areas, areas “B” and “C” should be explored utilizing the geological information
acquired from the previous locations.
In the exploration of the areas, samples should be analyzed for pathfinder minerals
and all types, degrees, and environment, of alteration should be noted.

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Respectfully submitted
Sookochoff Consultants Inc.
Laurence Sookochoff, Peng

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SELECTED REFERENCES
Amedolagine, M. – Soil Geochemical Survey Report and Proton Magnetometer Survey Report for
International Cherokee Developments Ltd. February 13th
, 1985. AR 13,552.
Allen, D.G. – Geological Report on the Hope Prospect for Chapleau Resources Ltd .September 28,
1984. AR 12,980.
Arnold, R.R. – Geochemical, Geophysical, and Geological Assessment Report on the Baluga Mineral
Claim Group for Monica Resources Ltd. November 29, 1985. AR 14,473.
Church, B.N. – Metallogeny of the Slocan City Mining Camp (82F11/14). BC Geological Survey
Branch. Geological Fieldwork. Paper 1998-1.
Corbett, G. – Geological Models in Epithermal-Porphyry Exploration: Terry Leach’s Legacy.
(Undated). .greg@corbettgeology.com.
Goldsmith, L. – Prospecting Report Paterson and Orga 1-5 Claims for Monica Resources Ltd.
February, 1982. AR 10,468.
Holcombe, R. – 2009: GEOrient, ver 9.4.4. Stereographic Projections and Rose Diagram Plots.
Kennedy, T. – Assessment Report on Rock Geo-Chem Program on the Ruby Steele Claim Group. for
Kootenay Gold Incorporated. March, 2012. AR 33,025.
MapPlace – Map downloads
Marshak, S., Mitra, G. – 1988: Basic Methods of Structural Geology. pp 258-259, 264* Prentice-Hall
Inc.
Moynihan, D.P. – Metamorphism and Deformation of the Central Kootenay Arc, Southeastern British
Columbia. Department of Geoscience, Calgary, Alberta, 2012.
MtOnline - MINFILE downloads.
082FNW129 – HOPE.
082FNW155 – OTTAWA
082FNW165 – WHITE HOPE
082FNW167 – NORTHERN LIGHT
082FNW168 – REPUBLIC
082FNW169– CLUB
082FNW172 – LAKEVIEW
082FNW173 – DAYTON
082FNW174 – EXCHANGE
082FNW216– MORNING STAR
082FNW224 – KIMBERLY
082FNW243 – SPRINGER CREEK
Roberts A.F. – Geochemical Report on the Pino Claims for Varitech Resources Ltd. August 1, 1989.
AR 12,748.
Stephenson, L. – Assessment Report on Diamond Drill Holes H90-1 to H90-9 Hope Property for
Kokanee Explorations Ltd. April 1, 1991. AR 21,234.

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STATEMENT OF COSTS
The Structural Analysis on Tenures 1034221, 1034222, 773182, and 773162 of the
Ruby 773182 Claim Group was done from February 11, 2015 to February 14, 2015 to
the value as follows:
Structural Analysis (Contract) -------------------------------------------$ 4,000.00
Maps ------------------------------------------------------------------------- 500.00
Report ----------------------------------------------------------------------- 3,000.00
$ 7,500.00
=======

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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 120 125A-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 my profession for the past forty-nine 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, from exploration work done in the general area of the
Slocan Mining Camp, and from the Structural Analysis performed on Tenures 1034221,
1034222, 773182, and 773162
5) I have no interest in the Ruby 773182 Claim Group as described herein.
Laurence Sookochoff, P. Eng.

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