2015 slocan white eagle gold silver slocan british columbia mls mining

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Eagle 1023615 Claim Group John Nick Bakus Event 5538445

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April 14, 2015 Sookochoff Consultants Inc. of 30

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JOHN NICK BAKUS

(Owner & Operator)

GEOLOGICAL ASSESSMENT REPORT (Event 5538445)

on a

STRUCTURAL ANALYSIS

on Tenures

1023615,1023616,1029331,1033413,1032039,1033412,1033414,1032035,1033411

of the nine claim

Eagle 1023615 Claim Group Slocan Mining Division

BCGS Maps 082K.025/.035

Centre of Work

UTM 5,537,363N 488,388E (NAD 83 Zone 11U)

work done from

December 5, 2014 to December8, 2014

Author & Consultant

Laurence Sookochoff, PEng Sookochoff Consultants Inc.

Submitted

May 6, 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 ------------------------------------ 6.

Water and Power ---------------------------------------------------------------- 7.

History: Property Area --------------------------------------------------------- 7.

082KSW059 – ISLE -------------------------------------------------------- 8.

082KSW084 – UPPER COMSTOCK ------------------------------------ 9.

082KSW088 – SWEDE ---------------------------------------------------- 9.

082KSW089 – MOTHER LODE ----------------------------------------- 9.

082KSW125 – JUNO ------------------------------------------------------- 9.

082KSW127 – NOONDAY ----------------------------------------------- 9.

082KSW149 – NORTH STAR AMBER -------------------------------- 10.

082KSW164 – MAGGIE --------------------------------------------------- 10.

History: Property ---------------------------------------------------------------- 10.

082KSW086 – SNOWSTORM ------------------------------------------- 10.

082KSW126 – WHITE EAGLE ------------------------------------------ 10.

082KSW143 – SILVER SPARROW ------------------------------------- 11.

082KSW197 – WEST RIDGE -------------------------------------------- 11.

082KSW198 – LAKEVIEW ----------------------------------------------- 11.

Geology: Regional -------------------------------------------------------------- 12.

Geology: Property Area -------------------------------------------------------- 13.

082KSW059 – ISLE -------------------------------------------------------- 13.


082KSW088 – SWEDE ---------------------------------------------------- 15.

082KSW089 – MOTHER LODE ----------------------------------------- 15.

082KSW125 – JUNO ------------------------------------------------------- 16.

082KSW127 – NOONDAY ----------------------------------------------- 16.


082KSW164 – MAGGIE --------------------------------------------------- 17.

Geology: Property --------------------------------------------------------------- 17.

082KSW086 – SNOWSTORM ------------------------------------------- 17.

082KSW126 – WHITE EAGLE ------------------------------------------ 18.


082KSW197 – WEST RIDGE -------------------------------------------- 18.

082KSW198 – LAKEVIEW ----------------------------------------------- 19.

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Table of Contents (cont’d)

Mineralization: Property Area ------------------------------------------------- 19.

082KSW059 – ISLE -------------------------------------------------------- 19.


082KSW088 – SWEDE ---------------------------------------------------- 20.

082KSW089 – MOTHER LODE ----------------------------------------- 20.

082KSW125 – JUNO ------------------------------------------------------- 20.

082KSW127 – NOONDAY ----------------------------------------------- 20.


082KSW164 – MAGGIE --------------------------------------------------- 21.

Mineralization: Property ------------------------------------------------------- 21.

082KSW086 – SNOWSTORM ------------------------------------------- 21.

082KSW126 – WHITE EAGLE ------------------------------------------ 21.


082KSW197 – WEST RIDGE -------------------------------------------- 22.

082KSW198 – LAKEVIEW ----------------------------------------------- 22.

Structural Analysis -------------------------------------------------------------- 23.

Interpretation and Conclusions ------------------------------------------------- 26.

Selected References ------------------------------------------------------------- 28.

Statement of Costs -------------------------------------------------------------- 29.

Certificate ------------------------------------------------------------------------ 30.

TABLES

Table I Eagle 1023615 Claim Group Tenure --------------------------- 6.

Table II Approximate UTM Location of Figures 5 & 7

Cross-Structures & Minfiles ------------------------------------ 25.

ILLUSTRATIONS

Figure 1. Location Map ---------------------------------------------------- 5.

Figure 2. Property Location from Castlegar ---------------------------- 6.

Figure 2a Property Location from Kaslo --------------------------------- 6.

Figure 3. Claim Map ------------------------------------------------------- 7.

Figure 4. Geology, Claim, Minfile & Index Map ---------------------- 14.

Figure 5. Lineaments as Indicated Structures on

Eagle 1023615 Claim Group --------------------------------- 23.

Figure 6. Rose Diagram from Lineaments of

Eagle 1023615 Claim Group --------------------------------- 24.

Figure 7. Locations of Structural Intersections and Minfiles --------- 25.

Figure 8. Eagle Property Vein Location in a porphyry-

Epithermal geological model -------------------------------- 26.

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SUMMARY

The nine claim Eagle 1023615 Claim Group (“Property”) is located within the covering an area of 227

hectares, is located 440 kilometres east-northeast of Vancouver and 114 kilometres north-northeast of

Castlegar.

The Property is also located within 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. Thirteen mines have produced more than one million grams

of silver.

An indication of the potential mineral zones to be located in the Property area is from the Rambler Mine

32 kilometres south which is reported as a polymetallic vein deposit hosting silver-lead-zinc with or

without gold deposit type (Minfile 082KSW018) The Rambler mine was one of the largest past

producers in the area where three ore shoots were explored by 14 levels to an approximate depth of 400

metres below the surface and developed by workings over a horizontal distance of 610 metres. During

its mine life a total of 189,421 tonnes of ore was mined from which 108,959,934 grams (3,503,143

ounces) silver, 839 grams (27 ounces) gold, and significant quantities of cadmium, lead, and zinc were

recovered.

The Rambler ore reportedly appears closely related to nearly east-west dilation jogs and cross fractures.

The structural analysis of the Eagle 1023615 Claim Group resulted in the delineation of three cross-

structures on an indicated major northwesterly trending structure extending the entire three kilometre

length of the Property with three of the five Minfile deposits, Snowstorm, Lakeview, and Silver

Sparrow, directly correlating with the structure or an en echelon structure. The Snowstorm and the

Lakeview having a near direct correlation with cross-structures A and C where there should be greater

indication of a resource potential. However, the weaker mineralization at these cross structural/deposit

locations may indicate less than optimum surficial geological features, such as fracture density, for a

resource development.

Nevertheless, the White Eagle past producer, where 42 channel samples from the main vein yielded 298

grams silver per tonne and 6.5 grams per tonne gold, and located some 200 metres from cross-structure

B, may be indicative of significant geological features at cross-structure B that would enhance mineral

resource development and provide valuable geological information as to the proximity of a potential

depth related porphyry mineral resource (Figure 8).

Thus, the White Eagle/cross-structure B location is the prime area to explore for surficial geological

indicators of a potential polymetallic vein or a depth related porphyry mineral resource. These

geological indicators could be indicated as primary or secondary minerals or alteration patterns which

would be subject to interpretation as to follow-up exploration.

Excluding other variable geological conditions, the structures are essential as mineral controls to both

deposit types and the cross-structures of greater importance to enhance the mineralogical and economic

aspects of the mineral deposit.

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INTRODUCTION

In December 2014 a structural analysis was completed on the nine claims of the Eagle 1023615 Claim

Group. The purpose of the structural analysis was to delineate potential structures which may be integral

in geological controls to potentially economic mineral zones on the Eagle 1023615 Claim Group.

Information for this report was obtained from sources as cited under Selected References, and from

previous work the writer has done in the general area.

PROPERTY LOCATION and DESCRIPTION

Location

The Eagle 1023615 Claim Group is located in the Slocan Range of the Selkirk Mountains in

southeastern British Columbia 475 kilometres east-northeast of Vancouver. 113 kilometres north-

northeast of Castlegar, 47 kilometres of Nakusp, and 47 kilometres north-northwest of Kaslo, within

BCGS Maps 082K.025 and 082K.035 of the Slocan Mining Division.

Figure 1. Location Map (Base Map from MapPlace)

Description

The Eagle 1023615 Claim Group is comprised of nine contiguous claims covering an area of 227.07

hectares. Particulars are as follows:

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Table I. Tenures of the Eagle 1023615 Claim Group D

Tenure Number

Type Claim Name Good Until Area (ha)

1023615 Mineral White Eagle 1 20220113 20.6426

1023616 Mineral White Eagle 3 20220113 20.6462

1029331 Mineral W EAGLE W RIDGE 1540 GTAG 20220101 20.6462

1032035 Mineral WHITE EAGLE LAKEVIEW N 20161105 20.6444

1032039 Mineral

20171101 20.6443

1033411 Mineral Slocan WEagle Snowstorm 20220101 20.639

1033412 Mineral Slocan Snowstorm E 20150702 41.2798

1033413 Mineral Slocan WEagle Sparrow 20220101 41.2832

1033414 Mineral Slocan WEagle SparrowS 20150717 20.6443

Total Area: 227.07 ha

*Upon the approval of the assessment work filing Event Number 5538445.

ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY

Road access to the Eagle 1023615 Claim Group from the Castlegar airport is as follows:

From To km Direction via

Castlegar Junction with Hwy 3A

and 6 14 N Hwy 3A

Junction Nelson 21 ENE Hwy 3A

Nelson Kaslo 87 N Hwy 31

Kaslo Property 45 NNW Helicopter

Climate

The climate of the area is of relatively warm summers and moderately cold winters with heavy snowfall.

Snowfall within the lower elevations of the Property by mid-November and snow free by May.

Local Resources

Sufficient accommodation and supplies for a preliminary exploration program would be available at

Castlegar or Kaslo.. Contracts for required technical exploration and development programs would

probably be made with companies based in Vancouver with some supporting personnel from local

communities.

Infrastructure

Provisions for all telecommunication and public transportation services are available at Kaslo. Castlegar,

where helicopter services are available, is also serviced daily by a commercial airline from Vancouver

and Calgary. An airport for small aircraft is located at Kaslo.

Physiography

The Property covers an area of forested steep slopes in the southwestern portions with an elevation of

1,800 metres near a creek valley rising to a barren mountainous alpine area in the northwest where

elevations reach 2,577 metres on a mountain ridge.

https://www.mtonline.gov.bc.ca/mtov/tenureDetail.do?tenureNumberIDParam=1023615









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Figure 2. Property Location from Castlegar (Base Map from MapPlace & Google)

Figure 2a. Property Location from Kaslo (Base Map from MapPlace & Google)

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Figure 3. Claim Map (Base Map from MapPlace)

WATER AND POWER

Sufficient water for a summer diamond drill program should be available from water courses or lakes on

or adjacent to the Eagle 1023615 Claim Group

Property generated power would be required in the initial pre-production stages of a exploration and

development program.

HISTORY: PROPERTY AREA

The history on some MINFILE reported showings, prospects, and past producers peripheral to the Eagle

1023615 Claim Group as blocked out on Figure 4 is reported as follows. The descriptions are copied

from Minfile.

The distance is relative to the Eagle 1023615 Claim Group.

ISLE past producer (Polymetallic veins Ag-Pb-Zn+/-Au; Stibnite veins and disseminations)

Minfile 082KSW059

Four kilometres south-southeast

The Isle occurrence is located on the west side of Meadow Mountain at 2256 metres elevation above sea level, near the headwaters of John Creek in the Slocan Mining Division.

A short adit was excavated to evaluate a quartz vein within the shear zone

In 1970, two tonnes were mined form the vein to produce 31 grams of silver, 12 kilograms of lead and 8 kilograms of zinc.

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History: Property Area (cont’d)

UPPER COMSTOCK prospect (Polymetallic veins Ag-Pb-Zn+/-Au)

Minfile 082KSW084

Three kilometres northeast

The Upper Comstock occurrence is located at the head of Cascade Creek at 2635 metres elevation above sea level in the Slocan Mining Division. The property is on the ridge between Cascade and Mat creeks.

SWEDE past producer (Polymetallic veins Ag-Pb-Zn+/-Au; Au quartz veins)

Minfile 082KSW088

Eleven kilometres north

The Swede property is situated at 1160 metres elevation above sea level on the south bank of Poplar Creek in the Slocan Mining Division. The property consists of two Reverted Crown grants (Lots 4738 and 4739).

In 1904, Great Northern Mines mined 8 tonnes of high-grade ore from the occurrence to produce 778 grams of gold.

MOTHER LODE past producer (Polymetallic veins Ag-Pb-Zn+/-Au;

Polymetallic manto Ag-Pb-Zn)

Minfile 082KSW089

Ten kilometres north

The Mother Lode prospect is located at 1035 metres elevation above sea level between Poplar and Cascade creeks, in the Slocan Mining Division.

One tonne of ore was mined from the adits in 1924 to produce 1649 grams of silver and 396 kilograms of lead.

JUNO prospect (Polymetallic veins Ag-Pb-Zn+/-Au)

Minfile 082KSW125

Two kilometres north

The Juno occurrence is located at the head of Cascade Creek at 1524 metres elevation above sea level in the Slocan Mining Division.

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the Juno showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the Juno, West Ridge (082KSW197), and White Eagle (082KSW126) showing areas (Assessment Report 23669).

NOONDAY prospect (Polymetallic veins Ag-Pb-Zn+/-Au)

Minfile 082KSW127

Three kilometres north

The Noonday occurrence is located at the head of Cascade Creek at 2200 metres elevation above sea level in the Slocan Mining Division. The prospect is on the ridge between Cascade and Mat creeks on the old Comstock claims.

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History: Property Area (cont’d)

NORTH STAR AMBER prospect (Polymetallic veins Ag-Pb-Zn+/-Au; Stibnite veins)

and disseminations)

Minfile 082KSW149

Three kilometres south-southeast

The North Star Amber occurrence is located at the head of Meadow Creek at 2360 metres elevation above sea level in the Slocan Mining Division.

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the North Star showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the Juno (082KSW125), West Ridge (082KSW197), and White Eagle (082KSW126) showing areas (Assessment Report 23669).

MAGGIE showing (Type: unknown)

Minfile 082KSW164

Four kilometres northeast

The Maggie occurrence is located at the head of Mat Creek at 2375 metres elevation above sea level in the Slocan Mining Division.

HISTORY: PROPERTY

The history on some MINFILE reported showings, prospects, and past producers on the Property as

blocked out on Figure 4 is reported as follows. The descriptions are copied from Minfile.

SNOWSTORM prospect (Polymetallic veins Ag-Pb-Zn+/-Au)

Minfile 082KSW086

Within Tenure 1033411

The Snowstorm occurrence is located at the head of Cascade Creek at 2255 metres elevation above sea level in the Slocan Mining Division.

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the Snowstorm showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the Juno, West Ridge (082KSW197), and White Eagle (082KSW126) showing areas (Assessment Report 23669).

WHITE EAGLE past producer (Polymetallic veins Ag-Pb-Zn+/-Au;

Sedimentary exhalative Zn-Pb-Ag)

Minfile 082KSW126


The White Eagle occurrence is located at the head of Cascade Creek at 2175 metres elevation above sea level in the Slocan Mining Division. The occurrence is about 500 metres north of Blue Lake.

In 1928, eight tonnes of ore were mined from the property to produce 6158 grams of silver, 2667 kilograms of lead, 1809 kilograms of zinc and 93 grams of gold.

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History: Property (cont’d)

White Eagle (cont’d)

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the White Eagle showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the White Eagle, West Ridge (082KSW197), and Juno (082KSW125) showing areas (Assessment Report 23669).

SILVER SPARROW prospect (Polymetallic veins Ag-Pb-Zn+/-Au)

Minfile 082KSW143


The Silver Sparrow occurrence is located at the head of Cascade Creek at 2285 metres elevation above sea level in the Slocan Mining Division.

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the Silver Sparrow showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the Juno (082KSW125), West Ridge (082KSW197), and White Eagle (082KSW126) showing areas (Assessment Report 23669).

WEST RIDGE showing (Polymetallic veins Ag-Pb-Zn+/-Au)

Minfile 082KSW197


The West Ridge occurrence is located at the head of Cascade Creek at 2225 metres elevation above sea level in the Slocan Mining Division.

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the West Ridge showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the West Ridge, Juno (082KSW125), and White Eagle (082KSW126) showing areas (Assessment Report 23669).

LAKEVIEW showing (Polymetallic veins Ag-Pb-Zn+/-Au; Irish-type carbonate-hosted Zn-Pb)

Minfile 082KSW198


The Lakeview occurrence is located at the head of Cascade Creek at 2100 metres elevation above sea level in the Slocan Mining Division.

During 1987 and 1988 Ambergate Explorations conducted an exploration program which consisted of 1:10000 scale mapping, a soil survey, and trenching on their Amber 1-4 claims in which the Lakeview showing is located. A follow-up to the 87-88 exploration program was done in 1994 by Lumby Resources Corporation, an optionee of Kenrich Mining Corporation, formerly Ambergate Explorations. This program extended the soil survey in the Juno, West Ridge (082KSW197), and White Eagle (082KSW126) showing areas (Assessment Report 23669).

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GEOLOGY: REGIONAL (from Ostler, 1994)

The area around Cascade Creek and the Amber Property is underlain by rocks that range in age from Early Palaeozoic to Jurassic. These rocks can be divided into two provenancal groups: the Lardeau Group, a eugeosynclinal assemblage and the Milford Group, a miogeosynclinal assemblage. Both assemblages are intruded by Mesozoic-age granitic rocks.

This stratigraphy forms part of the Kootenay Arc, which extends in southwestern British ' Columbia from the U.S. border to northeast of Revelstoke (Douglas et al; 1970).

Kootenay Arc sediments and volcanics were deposited at the western margin of proto-North America in the Cordilleran Geosyncline. Kootenay Arc deposition from Late Proterozoic until Middle Palaeozoic time was in a large eugeosyncline that segregated into smaller sub-basins during the Late Palaeozoic Era. The rocks underlying the Amber Property were deposited in one of those eugeosynclinal sub-basins. Mesozoic deposition was mostly miogeosynclinal.

Lithological mapping conducted by Read (1973) around the Amber Property reveals that this region is underlain by a succession of rocks that record the gradual filling of a basin (Figure 3). He later interpreted that stratigraphy within a regional context (Figure 4) (Read and Wheeler, 1976).

Northeast of the claims is a thick sequence of mafic to intermediate volcanics comprising the Index Formation (Figures 3 and 4). In the Cascade Creek area, these volcanics are accompanied by a minor amount of shale and phyllite. Farther north near Trout Lake, the Index Formation volcanics are accompanied by far more sediments. There, the volcanics are interpreted to have been deposited from basin-floor vents in deep water (Fyles and Eastwood, 1962).

Read (1973) mapped a contact between the Index Formation volcanics and the overlying sediments of

the Broadview Formation northeast of the Comstock showings about 2 km north of the Amber claims (Ostler, 1988) (Figure 6). This location is about 1 km southwest of where Read (1973) mapped the contact (Figure 3).

Northeast of the Comstock showings, Ostler (1988) interpreted the contact between Index Formation volcanics and Broadview Formation sediments to have been originally conformable and gradational, defined by a facies change on the flank and top of a basin-floor volcanic pile. The main mass of the Index Formation volcanics then seems to have been decoupled from the overlying Broadview Formation sediments. Both thrusting and transverse movement probably took place along the Index- Broadview boundary fault.

The Milford Group-Broadview Formation contact was also mapped by Read (1973) southwest of the Amber Property (Figure 3).

Read (1973) mapped across the Broadview Formation northwest of Cascade Creek; about 10 km northwest of the Amber Property. There, he found the Broadview Formation clastics to be overlain by a thin sequence of phyllites and phyllitic carbonates.

Two reconnaissance traverses into the Amber Property-area from the north and west (Figure 3) hinted that the area of distal basin sedimentation represented by phyllites and phyllitic carbonates increased significantly southeastward. This was confirmed by the writer's mapping (Spearing and Ostler, 1987). Later mapping revealed that the Broadview Formation was represented in the Cascade Creek area by a fining-upward sequence of turbidites beneath phyllitic carbonates and phyllites (Spearing and Ostler, 1988) (Figure 6).

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Geology: Regional (cont’d)

The Broadview Formation clastics lie in fault contact with the sandstones of the Milford Group about 700 m southwest of the Amber 3 claim (Figures 3 and 4).

The Milford Group comprises a series of micaceous sandstones, phyllite and calcite-bearing quartzite that form a miogeosynclinal sequence above the Broadview Formation sediments (Read, 1973; Read and Wheeler, 1976) (Figures 3 and 4).

Rocks of the Milford Group and Broadview Formation were intruded during the Early Jurassic Period by leucoquartz monzonite and syenite of the Kuskanax Batholith. Batholithic intrusion was succeeded by the intrusion of small parasitic stocks of massive leucoquartz monzonite and syenite along the northeastern margin of the batholith (Read, 1973; Read and Wheeler, 1976). Some of these parasitic intrusions are exposed along the southwestern margin of the Amber 3 claim (Figures 3 and 4).

Read (1973) recorded three generations of coaxial folding in the rocks northwest of the Amber Property; and locally near intrusions, a fourth generation.

Regionally, the most important structures are second-generation folds that form northwest-southeast trending structures. First-generation folds are most commonly seen as isoclines within second-generation structures. Third-generation structures are most commonly large open warps or minor folds.

The area around Cascade Creek is regionally metamorphosed to the upper greenschist and lower amphibolite grades of metamorphism. Locally, near intrusive contacts, upper amphibolite and granulite grade metamorphism occurs.

The region is crossed by several long northwest-southeasterly trending faults. The Mount Emnens Fault southwest of the Amber Property and the Mobbs Fault which crosses the property are notable examples (Figures 3, 4 and 6).

GEOLOGY: PROPERTY AREA

The geology on some MINFILE reported showings, prospects, and past producers peripheral to the

Eagle 1023615 Claim Group as blocked out on Figure 4 is reported as follows. The descriptions are

copied from Minfile. The distance is relative to the Eagle 1023615 Claim Group.


Minfile 082KSW059


Regionally, the area lies within the Selkirk Mountains of southeastern British Columbia. The occurrence is within the Kootenay Arc, a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Upper Proterozoic to Lower Cambrian Hamill Group, the Lower Cambrian Badshot Formation, and the Paleozoic Lardeau and Milford groups. The volcano-sedimentary sequence is intruded by numerous Paleozoic to Mesozoic granitoid plutons and has been metamorphosed to at least middle greenschist facies.

Rocks on the Isle property include phyllite, sandstone and grey limestone of the Broadview Formation (Lardeau Group). The strata strike northwest and dip east between 60 to 80 degrees. Mineralization is hosted within a 20 metre wide shear zone that strikes north and dips subparallel to bedding.

A short adit was excavated to evaluate a quartz vein within the shear zone. The rocks within the shear are altered to sericite schist.

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Figure 4. Geology, Claim, Minfile, & Index Map (Base Map from MapPlace)

MJSe

Middle Jurassic

Selkirk Stocks

granodioritic intrusive rocks

MJKx

Middle Jurassic

Kuskanex batholith

monzonitic intrusive rocks

TrSlc

Triassic

Slocan Group

limestone, slate, siltstone, argillite

uMPm

upper Mississippian to Permean

Milford Group


CmDLB

Carboniferous to Permean

Lardeau Group-Broadview Formation


CmDLJ

Carboniferous to Permean

Jewett Formation

basaltic volcanic rocks

lCmB

Lower Cambrian

Badshot Formation

limestone, marble, calcareous sedimentary rocks

uPrVmH

Upper Proterozoic to Lower Cambrian

Hamill Group

quartzite, quartz arenite sedimentary rocks

uPrHsc

Upper Proterozoic

Horsethief Creek Group

clastic sedimentary rocks

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Geology: Property Area (cont’d)


Minfile 082KSW084


Regionally, the area lies within the Selkirk Mountains of southeastern British Columbia. The occurrence is within the Kootenay Arc, a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Upper Proterozoic to Lower Cambrian Hamill Group, the Lower Cambrian Badshot Formation, and the Paleozoic Lardeau and Milford groups. The volcano-sedimentary sequence is intruded by numerous Paleozoic to Mesozoic granitoid plutons and has been metamorphosed to at least middle greenschist facies before the emplacement of the mineralization.

The oldest rocks on the Comstock property are andesitic tuffs and flows of the Index Formation of the Lardeau Group. A northwest- trending fault which passes through the centre of the Comstock property separates the volcanic rocks of the Index Formation from sandstone, siltstone and phyllite of the Broadview Formation to the west. The rocks are deformed in a series of northwest-trending folds that are cut at oblique angles by faults.


Minfile 082KSW088


Regionally, the area lies within the Selkirk Mountains of southeastern British Columbia. The occurrence is within the Kootenay Arc, a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Upper Proterozoic to Lower Cambrian Hamill Group, the Lower Cambrian Badshot Formation, and the Paleozoic Lardeau and Milford groups. The volcano-sedimentary sequence is intruded by numerous Paleozoic to Mesozoic granitoid plutons.

The Lardeau River area of the Selkirk Mountains is mainly underlain by massive pillow lavas, volcanic breccia and green phyllitic rocks of the Index Formation and by grey-green mica schist of the Broadview Formation. Grey phyllitic rocks and marble of the Milford Group are exposed near the edges of the Mesozoic Mobbs Creek, Rapid Creek and Poplar Creek stocks. All rocks have undergone regional metamorphism to middle or upper greenschist facies. Rocks of the Milford Group have also been affected by thermal metamorphism (Geological Survey of Canada Bulletin 193).

MOTHER LODE past producer (Polymetallic veins Ag-Pb-Zn+/-Au;


Minfile 082KSW089



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Mother Lode past producer (cont’d)

The Lardeau River area of the Selkirk Mountains is mainly underlain by massive pillow lavas, volcanic breccia and green phyllitic rocks of the Index Formation and by grey-green mica schist of the Broadview Formation. Grey phyllitic rocks and marble of the Milford Group are exposed near the edges of the Mesozoic Mobbs Creek, Rapid Creek and Poplar Creek stocks. All rocks have undergone regional metamorphism to middle or upper greenschist facies. Rocks of the Milford Group have also been affected by thermal metamorphism (Geological Survey of Canada Bulletin 193).


Minfile 082KSW125



The Juno property is underlain by andesite, sandstone, siltstone and phyllite which forms the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been folded in a series of northwest-trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).


Minfile 082KSW127



The oldest rocks on the Comstock property are tuffaceous andesite and flows of the Index Formation of the Lardeau Group. A northwest-trending fault which passes through the centre of the Comstock property separates the volcanic rocks of the Index Formation from sandstone, siltstone and phyllite of the Broadview Formation to the west. The rocks are deformed in a series of northwest-trending folds that are cut at oblique angles by faults.

NORTH STAR AMBER prospect (Polymetallic veins Ag-Pb-Zn+/-Au; Stibnite veins

and disseminations)

Minfile 082KSW149


Regionally, the area lies within the Selkirk Mountains of southeastern British Columbia.

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North Star Amber prospect (cont’d)

The occurrence is within the Kootenay Arc, a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Upper Proterozoic to Lower Cambrian Hamill Group, the Lower Cambrian Badshot Formation, and the Paleozoic Lardeau and Milford groups. The volcano-sedimentary sequence is intruded by numerous Paleozoic to Mesozoic granitoid plutons and has been metamorphosed to at least greenschist facies.

The North Star Amber property is underlain by andesite, sandstone, siltstone and phyllite which forms the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been deformed in a series of northwest-trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).


Minfile 082KSW164



No geological description could be located for this occurrence; however, it is situated west of a northwest-trending fault that separates sandstone, siltstone and phyllite of the Broadview Formation from andesitic tuffs and flows of the Index Formation to the east. The rocks are deformed in a series of northwest-trending folds (Assessment Report 18136).

GEOLOGY: PROPERTY

The geology of the MINFILE reported showings, prospects, and past producers within the Eagle

1023615 Claim Group as blocked out on Figure 4 is reported as follows. The descriptions herein are

copied from Minfile.


Minfile 082KSW086


Regionally, the area lies within the Selkirk Mountains of southeastern British Columbia. The occurrence is within the Kootenay Arc, a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Upper Proterozoic to Lower Cambrian Hamill Group, the Lower Cambrian Badshot Formation, and the Paleozoic Lardeau and Milford groups. The volcano-sedimentary sequence is intruded by numerous Paleozoic to Mesozoic granitoid plutons and has been metamorphosed to at least middle greenschist facies before the emplacement of the mineralization. The property is underlain by andesite, sandstone, siltstone and phyllite which forms the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been folded in a series of northwest-trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).

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Geology: Property (cont’d)

WHITE EAGLE past producer (Polymetallic veins Ag-Pb-Zn+/-Au)


Minfile 082KSW126



The White Eagle property is underlain by andesite, sandstone, siltstone and phyllite which forms the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been folded in a series of northwest-trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).

The White Eagle occurrence consists of quartz veins containing massive sulphide pods 0.6 metre wide and 5 metres long. The quartz veins have been exposed in two adits, an incline shaft and a winze in the upper adit.


Minfile 082KSW143



The property is underlain by andesite, sandstone, siltstone and phyllite which forms the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been folded in a series of northwest-trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).


Minfile 082KSW197



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Geology: Property (cont’d)

West Ridge showing (cont’d) The West Ridge property is underlain by andesite, sandstone, siltstone and phyllite which forms the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been folded in a series of northwest-trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).


Minfile 082KSW198



The area is underlain by andesite, sandstone, siltstone and phyllite of the lower portion of the Broadview Formation of the Lardeau Group. The rocks have been folded in a series of northwest- trending folds that were subsequently thrusted in a northeasterly direction along local faults (Geological Survey of Canada Bulletin 193).

MINERALIZATION: PROPERTY AREA

The mineralization on some MINFILE reported showings, prospects, and past producers peripheral to

the Eagle 1023615 Claim Group as blocked out on Figure 4 is reported as follows. The descriptions

herein are copied from Minfile.

The distance is relative to the Eagle 1023615 Claim Group.


Minfile 082KSW059


High silver, lead and antimony values occur with massive sulphides on the apex of drag folds within the shear. Mineralization consists of galena and tetrahedrite within quartz-calcite veins. A chip sample across 0.6 metre of vein material assayed 2358 grams per tonne silver, 29.9 per cent lead, 10.4 per cent antimony and 9.7 grams per tonne gold (Assessment Report 8532).


Minfile 082KSW084


The Upper Comstock occurrence consists of two vertically dipping quartz veins striking 275 and 295 degrees respectively. The veins consist of white milky quartz sparsely mineralized with disseminated to massive galena with traces of sphalerite. The veins are exposed in a series of surface trenches. A selected grab sample from the mineralized portion of the vein assayed 800 grams per tonne silver and 26.7 per cent lead (Assessment Report 18149).

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Mineralization: Property Area (cont’d)


Minfile 082KSW088


On the Swede property carbonaceous phyllitic rocks of the Index Formation are cut by Mesozoic meta-andesite and metadiorite dikes. The dikes are fine grained, massive and usually contain disseminated pyrite. Quartz veins carrying pyrite, arsenopyrite and ankerite cut black carbonaceous phyllite. Some of the arsenopyrite is very coarse grained. A massive sulphide vein, 10 centimetre wide, is hosted within a meta-andesite dike. The vein consists of galena, sphalerite, chalcopyrite and pyrite. Free gold occurs in the vein with lead sulphate and carbonate where the sulphides have been leached (Geological Survey of Canada Memoir 161).

MOTHER LODE past producer (Polymetallic veins Ag-Pb-Zn+/-Au)


Minfile 082KSW089


The main showing consists of quartz with coarse-grained pyrite, galena and sphalerite as replacement of calcareous schist of the Index Formation. The mineralization has been exposed in two short adits driven 15 metres apart for a total length of 45 metres. Replacement has taken place parallel to the foliation for at least 12 metres along strike. The mineralization has an average thickness less than 45 centimetres. A grab sample of the replacement vein assayed 5.5 grams per tonne gold, 1190 grams per tonne silver, 15 per cent lead and 10 per cent zinc (Minister of Mines Annual Report 1919).


Minfile 082KSW125


The occurrence consists of a well-defined quartz vein 30 to 60 centimetres in width mineralized with pyrite, galena and sphalerite. The vein strikes east and dips 45 degrees north. A 60 centimetre chip sample from the vein assayed 1.4 grams per tonne gold, 600 grams per tonne silver, 29 per cent lead and 29.8 per cent zinc (Minister of Mines Annual Report 1925). The vein has been explored with several surface trenches and a 12-metre long adit.


Minfile 082KSW127


The Noonday occurrence consists of a quartz vein 1.5 metres wide that strikes 342 degrees and dips 25 degrees northeast. The vein is emplaced in fine-grained arenites of the Broadview Formation just below an aplite dike. The vein is composed of white milky quartz with smoky grey bands. Subhedral galena grains, 2 millimetres wide, are disseminated and concentrated in small patches with minor sphalerite crystals. Selected grab samples from the vein assayed up to 663 grams per tonne silver and 33.1 per cent lead (Assessment Report 18149). The vein has been explored by several surface trenches and at least two adits driven for a total length of 105 metres.

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Mineralization: Property Area (cont’d)

NORTH STAR AMBER prospect (Polymetallic veins Ag-Pb-Zn+/-Au; Stibnite veins

and disseminations)

Minfile 082KSW149


The occurrence consists of a 10-centimetre wide brecciated quartz vein emplaced along a thrust plane that separates metasiltstone and carbonate rocks. The vein, which strikes 155 degrees and dips 60 degrees northeast, consists mainly of broken white quartz mixed in a black sulphide-rich gouge. A channel sample of the gouge material assayed 1978 grams per tonne silver, 1.17 per cent copper, 2.74 per cent lead and 1.14 per cent antimony (Assessment Report 18136). Narrow stringers of pyrite also extend through the metasiltstone. The vein is exposed in two trenches and a short, 9-metre long adit.


Minfile 082KSW164


The occurrence is reported to contain gold and copper values (Assessment Report 18136).

MINERALIZATION: PROPERTY

The mineralization of the MINFILE reported showings, prospects, and past producers included in the

Eagle 1023615 Claim Group as blocked out on Figure 4 is reported as follows. The descriptions herein

are copied from Minfile.


Minfile 082KSW086


The occurrence consists of quartz veins containing minor galena, sphalerite, and pyrite mineralization hosted within siltstone of the Broadview Formation. The veins are exposed in 26 trenches covering an area of about 7.5 hectares. The largest vein is about 1 metre wide, strikes 313 degrees and dips 39 degrees to the east. Grab samples have assayed 572 grams per tonne silver, 2.81 grams per tonne gold, 22.4 per cent lead, and 0.06 per cent zinc (Assessment Report 16433; 23669).

WHITE EAGLE past producer (Polymetallic veins Ag-Pb-Zn+/-Au)


Minfile 082KSW126


A weighted average of 42 channel samples taken from the main vein in the upper adit yielded 14.88 per cent lead, 7.58 per cent zinc, 298 grams per tonne silver and 6.5 grams per tonne gold. The main vein within the upper adit has an average width of 40 centimetres and dips 48 degrees northeast which is subparallel to the enclosing carbonaceous siltstone of the Broadview Formation. Mineralization is unevenly distributed throughout the vein with the higher grades being associated with pods of massive sulphides that appear to plunge to the north. Silver values are highest within the galena-sphalerite rich portions of the massive sulphide while gold is associated with pyrite in the lower portion of the massive sulphide ore shoot (see Noonday, 082KSW127 - Prospectus, Ambergate Exploration Inc., 1988).

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Mineralization: Property (cont’d)


Minfile 082KSW143


The occurrence consists of two separate quartz veins some 90 metres apart. The Silver Sparrow vein consists of iron-stained quartz containing stringers of auriferous pyrite, argentiferous galena and minor sphalerite. The vein strikes 120 degrees, dips 30 degrees northeast and is about 1 metre thick where it is exposed in the trenches. The vein has also been exposed in a 6-metre deep inclined shaft. The best grab sample from the vein assayed 27.5 grams per tonne gold, 1083 grams per tonne silver, 56.2 per cent lead and 0.55 per cent zinc (Assessment Report 18136). The Pine Tree vein is situated 90 metres west of the Silver Sparrow and has similar mineralogy. The vein is exposed for about 20 metres in three trenches. The vein strikes 071 degrees, dips 30 degrees northwest and ranges in width from 7 to 50 centimetres. Both veins are hosted within siltstone of the Broadview Formation.


Minfile 082KSW197


The occurrence consists of a 30 centimetre wide milky quartz vein striking 119 degrees and dipping 45 degrees southwest. The vein is mineralized with disseminations and pods of argentiferous galena, tetrahedrite and stibnite. A selected grab sample of the mineralized vein assayed 1540 grams per tonne silver, 41.1 per cent lead, 16.1 per cent antimony and 1.58 per cent copper (Assessment Report 18136).

The vein has been explored with several trenches and a 15-metre deep shaft. Boulders of massive galena-stibnite mineralization up to 1 metre across are reported from a dispersion train below the workings for a distance of 137 metres (see Noonday, 082KSW127 - Prospectus, Ambergate Exploration Inc., 1988)


Minfile 082KSW198


At the Lakeview showing two trenches expose sparsely mineralized metasandstone between two quartz veins. The quartz veins are mineralized with disseminated and massive galena, pyrite and sphalerite. Some of the mineralization resembles the massive mineralization at the White Eagle (082KSW126). The No. 1 vein strikes 128 degrees and dips steeply southwest. It is 20 centimetres wide in the trenches. A composite chip sample of about 10 blocks of vein material taken from the soil at the western end of the trench assayed 144 grams per tonne gold, 158 grams per tonne silver, 6.04 per cent lead and 3.47 per cent zinc (Assessment Report 18136). The No. 2 vein is exposed in a trench 4.6 metres above the No. 1 vein. This vein strikes 281 degrees and dips 81 degrees north. Mineralization in the sandstone between the veins comprises thin sheets of pyrite and minor galena with sphalerite along cleavage planes.

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STRUCTURAL ANALYSIS

The Structural Analysis was accomplished marking the observed lineaments of all nine claims of the

Eagle 1023615 Claim Group on a DEM Hillside Shade Map downloaded from MapPlace. A total of 66

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 66 lineaments into an individual 8 °class sector angle

interval as shown on Figure 6.

Figure 5. Lineaments as Indicated Structures on the Eagle 1023615 Claim Group

(Base Map from MapPlace)

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Structural Analysis (cont’d)

Figure 6. Rose Diagram from lineaments on the Eagle 1023615 Claim Group

Rose Diagram Statistics

(Usage Reference: Holcombe, 2009)

Axial (non-polar) data

No. of Data = 66

Sector angle = 8°

Scale: tick interval = 2% [1.3 data]

Maximum = 16.7% [11 data]

Mean Resultant dir'n = 121-301

[Approx. 95% Confidence interval = ±58.2°]

(valid only for unimodal data)

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Mean Resultant dir'n = 120.8 - 300.8

Circ.Median = 115.0 - 295.0

Circ.Mean Dev.about median = 39.3°

Circ. Variance = 0.35

Circular Std.Dev. = 52.72°

Circ. Dispersion = 12.40

Circ.Std Error = 0.4335

Circ.Skewness = 0.50

Circ.Kurtosis = -2.60

kappa = 0.37

(von Mises concentration param. estimate)

Resultant length = 12.14

Mean Resultant length = 0.1839

'Mean' Moments: Cbar = -0.0876; Sbar = -0.1617

'Full' trig. sums: SumCos = -5.7791; Sbar = -

10.6709

Mean resultant of doubled angles = 0.1613

Mean direction of doubled angles = 132

(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. Locations of structural intersections and Minfiles

Table II. Approximate UTM locations of Figure 5 & 7 cross-structures & Minfiles

(UTM-11 NAD 83)

Cross

Structures UTM East UTM North Elevation (m)

A 488,238 5,571,985 2,277

B 488,576 5,571,255 2,299

C 489,091 5,570,431 2,167

Minfiles

Lakeview 489,017 5,570,454 2,100

Silver Sparrow 488,366 5,571,475 2,285

Snowstorm 488,229 5,572,031 2,255

West Ridge 488,533 5,570,362 2,225

White Eagle 488,622 5,571,134 2,175

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Figure 8. Eagle property polymetallic vein location in the porphyry-epithermal geological model showing potential for a deep-seated

porphyry Cu-Au resource (Map from Bisson, 2014)

INTERPRETATION & CONCLUSIONS

Three cross-structural locations have been mapped on all the nine claims of the Eagle 1023615 Claim

Group (“Property”). The significance of the structures within the Property Area are in the major

structures, and/or brecciation zones, shearing and cross fractures that provide a preferred conduit for the

transport and ultimate deposition of metals from rising volatiles.

Virtually all the herein reported five Minfile deposit types within the Property and the nine peripheral

are polymetallic veins hosting silver-lead-zinc with or without gold. These quartz hosting mineral types

commonly occur within structures peripheral to a mineralized intrusive (Figure 8) and more often than

not, mineralization within the veins is unevenly distributed with the “heavier” mineralization occurring

as pods or pockets of massive sulphides. These “heavier” pockets of mineralization were probably hand

sorted and shipped giving the “Past Productive” designation to many properties. Although the maximum

production from any one of the four Minfile past producers reported herein was only eight tonnes, the

reported assay values from the past productive properties (Isle) were as high as 2,358 grams per tonne

silver.

The mineral controls to the mineralization are structurally related with the “better” locations for

mineralization with volume occurring as extensive mineralized zones or “shoots” at cross-structures or

at warps in structures where open spaces were created for the quartz/mineral deposition.

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Interpretation & Conclusions (cont’d)

An indication of the potential mineral zones to be located in the area is from the Rambler Mine which is

reported as a polymetallic veins hosting silver-lead-zinc with or without gold deposit type (Minfile

082KSW018) and was one of the largest past producers in the area. Three ore shoots were explored and

developed by workings over a horizontal distance of 610 metres and by 14 levels to an approximate

depth of 400 metres below the surface. During its mine life a total of 189,421 tonnes of ore was mined

from which 108,959,934 grams (3,503,143 ounces) silver, 839 grams (27 ounces) gold, and significant

quantities of cadmium, lead, and zinc recovered.

The Rambler ore reportedly appears closely related to nearly east-west dilation jogs and cross fractures.

On the Eagle Property, the northwesterly trending structure, AC, as indicated from the structure analysis,

appears as a major structure extending the entire three kilometre length of the Property with three of the

five Minfile deposits, Snowstorm, Lakeview, and Silver Sparrow, directly correlating with the structure

or an en echelon structure, with the Snowstorm and the Lakeview having a near direct correlation with

cross-structures A and C. The weaker mineralization at these cross structural/deposit locations may

indicate less than optimum surficial geological features, such as fracture density, for the development of

a mineral resource.

However, the White Eagle past producer, where 42 channel samples from the main vein yielded 298

grams silver per tonne and 6.5 grams per tonne gold, and located some 200 metres from cross-structure

B, may be indicative of significant geological features at cross-structure B that would enhance mineral

resource development and provide valuable geological information as to the proximity of a potential

depth related porphyry mineral resource (Figure 8).

Thus, the White Eagle/cross-structure B location is the prime area to explore for surficial geological

indicators of a potential polymetallic vein or a depth related porphyry mineral resource. These

geological indicators could be indicated as primary or secondary minerals or alteration patterns which

would be subject to interpretation as to follow-up exploration.

Excluding other variable geological conditions, the structures are essential as mineral controls to both

deposit types and the cross-structures of greater importance to enhance the mineralogical and economic

aspects of the mineral deposit.

Respectfully submitted

Sookochoff Consultants Inc.

Laurence Sookochoff, PEng

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SELECTED REFERENCES

Church, B.N. – Metallogeny of the Slocan City Mining Camp. B.C.Geological Survey, Geological

Fieldwork 1997, Paper 1998-1.

Holcombe, R. – 2009: GEOrient, ver 9.4.4. Stereographic Projections and Rose Diagram Plots.

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. University of Calgary Thesis, Department of Geoscience, Calgary, Alberta. May, 2012.

MtOnline - MINFILE downloads.

082KSW059 – ISLE

082KSW084 – UPPER COMSTOCK

082KSW086 – SNOWSTORM

082KSW088 – SWEDE

082KSW089 – MOTHER LODE

082KSW125 – JUNO

082KSW126 – WHITE EAGLE

082KSW127 – NOONDAY

082KSW143 – SILVER SPARROW

082KSW149 – NORTH STAR AMBER

082KSW164 – MAGGIE

082KSW197 – WEST RIDGE

082KSW198 – LAKEVIEW

Ostler, J. – Extension of Soil-Geochemical Survey on the Amber Property for Lumby Resources

Corporation. December 17, 1994. AR 23,669.

Ostler, J., Spearing, C. G. – Geological and Geochemical Report on the Amber Property for

Ambergate Explorations Inc. October 15, 1987 AR 16,433.

Ostler, J., Spearing, C. G. – Report on Geological and Geochemical Conducted on the Amber Property

for Ambergate Explorations Inc. November 1, 1988. AR 18,136.

Paradis, S. – Carbonate-hosted Zn-Pb deposits in southern British Columbia-Potential for Irish-type

deposits. Current Research 2007-A10. Geological Survey of Canada. 2007

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STATEMENT OF COSTS

The Structural Analysis on the nine claim Eagle 1023615 Claim Group was done from December 5,

2014 to December 8, 2014 to the value as follows:

Laurence Sookochoff, PEng.

3 days @ $ 1,000.00 per day --------------------------------------------- $ 3,000.00

Maps ---------------------------------------------------------------------------- 1,000.00

Report --------------------------------------------------------------------------- 3,500.00

$ 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 the nine claim Eagle 1023615 Claim Group.

5) I have no interest in the Eagle 1023615 Claim Group as described herein.

Laurence Sookochoff, P. Eng.

AUTHOR(S): SIGNATURE(S):

STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S):

NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): YEAR OF WORK:

PROPERTY NAME:

CLAIM NAME(S) (on which the work was done):

COMMODITIES SOUGHT:

MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN:

NTS/BCGS:MINING DIVISION:

LATITUDE: o ' " LONGITUDE: o ' "

OWNER(S):1) 2)

OPERATOR(S) [who paid for the work]:1) 2)

MAILING ADDRESS:

TYPE OF REPORT [type of survey(s)]: TOTAL COST:

PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude):

REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS:

Ministry of Energy, Mines & Petroleum ResourcesMining & Minerals DivisionBC Geological Survey

Assessment ReportTitle Page and Summary

(at centre of work)

MAILING ADDRESS:

Next Page

GEOLOGICAL (scale, area)

Ground, mapping

Photo interpretation

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)

(scale, area)

Legal surveys (scale, area)

Road, local access (kilometres)/trail

Topographic/Photogrammetric

Trench (metres)

Underground dev. (metres)

Other

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EXTENT OF WORK(IN METRIC UNITS)

ON WHICH CLAIMS PROJECT COSTSAPPORTIONED

(incl. support)

TOTAL COST:

(scale, area)

Line/grid (kilometres)

PROSPECTING (scale, area)

Metallurgic

Mineralographic

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Sampling/assaying

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Rock

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