Exhibit 10.2

                                 Geology Report

                                       On

                               EMORY CREEK Claims

                     Nickel Copper Massive Sulphide Project

                               Northing 5477500 m
                                Easting 597500 m

                    Longitude 121(0)34' W Latitude 49(0)26' N

                                   UTM Zone 10

                              Map Sheets M092H0 53

                                       For

                            Deer Bay Resources Inc.,
                               1333 West Broadway,
                              Vancouver BC V6H 4C1

                                    Geologist

                             Glen Macdonald, P.Geo.
                             Date: February 10, 2010
<PAGE>
TABLE OF CONTENTS

                                                                            Page
                                                                            ----

Table Of Contents.............................................................2

List Of Figures...............................................................3

1.   Summary..................................................................4

2.   Introduction.............................................................5
       2.1 Disclaimer.........................................................5

3.   Property Description And Location........................................6

4.   Access, Climate, Local Resources, Infrastructure, And Physiography.......7

5.   History..................................................................8

6.   Recent Exploration Work.................................................10

7.   Geological Setting......................................................10
       7.1 Regional Geology..................................................10

8.   Deposit Type............................................................12
       8.1 Pacific Nickel Mine Geology (As Summarized From A. Aho, 1956).....12

9.   Property Geological Setting.............................................14
       9.1 Emory Creek Property Geology......................................14

10.  Geophysics..............................................................15
       10.1 Regional Geophysics..............................................15
       10.2 Geophysics Of Claims.............................................15

11.  Regional Geochemistry...................................................15

12.  Conclusions.............................................................16

13.  Recommended Program.....................................................17

16.  Budget..................................................................17
       Budget - Phase I......................................................18
       Budget - Phase II.....................................................18

17.  Statement Of Qualifications.............................................19

18.  References..............................................................20

Appendix 1:  Regional Showings...............................................22


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 2
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LIST OF FIGURES

         Figure 1:      Property Location Map and Claim Map....................7

         Figure 2:      Regional Geology......................................11

         Figure 2a:        Property Geology and Claim Map.....................15

         Figure 3:         Regional Geophysics................................16

         Figure 4a:        Regional Geochem Copper............................16

         Figure 4b:        Regional Geochem Nickel............................16


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 3
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1. SUMMARY

     The Pacific Nickel Mine located in Southwestern BC near Hope was a very
     significant past producer of copper and nickel from an ultramafic intrusive
     geologic environment. As one of the most significant Canadian sources of
     these metals outside of Sudbury, Ontario and Thompson, Manitoba, the lack
     of exploration in this area makes it a unique underdeveloped mineral belt
     that warrants a further exploration program that should include additional
     geological mapping; compilation of data for silt, soil and rock sample
     surveys, thin section analysis, and airborne geophysical surveys leading to
     definition of diamond drill targets.

     The Emmy Claim is located 5 kilometres north of the mine area and
     approximately 11 kilometres north of Hope B.C. on Map Sheet M092H053.

     There are similar and coincident features in the rock types and geophysical
     imprint between the geology of the Pacific Nickel Mine area and the
     ultramafic belt extending to the northwest and south west from it. It is
     evident from the public and private record that this belt has not been
     subjected to detailed recent exploration until now with numerous
     exploration companies initiating large scale programs. Research into the
     mine area has provided exploration concept s that can be used to guide
     further work in the under-explored area.

     It is recommended that a Phase I program of geological mapping, sampling
     and prospecting be undertaken to further define areas of potential
     interest. This is estimated to cost some $10,000; an additional $25,000 to
     compile all relevant existing technical data following the field
     investigation will comprise Phase II and lead to prioritize possible drill
     targets.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 4
<PAGE>
2. INTRODUCTION

     Following up on the recent exploration activity in the Hope, B.C. area, and
     after researching local potential for Ni-Cu-Pd-Pt deposits, Deer Bay
     Resources Inc. focussed on the Pacific Nickel Mine, 7 kilometres north of
     Hope, BC.

     The claims, which are the subject of this report were prospected, sampled
     and staked. Deer Bay Resources Inc. acquired a 100% interest in them.

2.1 DISCLAIMER

     This report was initiated by the President of Deer Bay Resources Inc. to
     evaluate the area of the claims and to recommend an exploration program to
     develop its mineral prospects and to be filed with the appropriate
     regulatory bodies.

     In order to write the report, old mine data and geological reports were
     reviewed and geologists and mine personnel who were present during the
     active mining operations in the region from 1958 to 1974 were interviewed
     as available.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 5
<PAGE>
3. PROPERTY DESCRIPTION AND LOCATION

     The Property is located east of Harrison Lake and northwest of Hope in
     south-western British Columbia (Figure 1) and has recently been further
     opened by logging operations which provide new access to the region.
     Permitting for initial exploration work has already been obtained.

     The entire Property consists of 1 unpatented mineral claim containing 20
     units staked and recorded online as per the new British Columbia Map
     staking regulations. The claim delineating the interests of Deer Bay
     Resources Inc. is found below and the claim is displayed on Figure 2a.

                     TABLE 1. DEER BAY RESOURCES INC. CLAIMS

    Claim Name   Units   Record #   Expiry Date   Map Sheet  Locator   Hectares:
    ----------   -----   --------   -----------   ---------  -------   ---------

       EMMY        20     705501    Feb 04 2011    092H053                418

       TOTAL       18     UNITS

     In British Columbia, each unit equals 25 hectares.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 6
<PAGE>

     All claims staked in British Columbia require $4 per hectare worth of
     assessment work to be undertaken in Year 1 through 3, followed by $8 per
     hectare per year thereafter. There are no known environmental concerns or
     parks designated for any area contained within the claims. The Fraser River
     is designated as a salmon habitat but is part of the main highway and rail
     corridor to the interior of the province. The area is used extensively for
     recreational pursuits and has no official designation. The property has no
     encumbrances. As advanced exploration proceeds there may be bonding
     requirements for reclamation.

     The claims lie north of the Pacific Nickel Mine leases (Figures 1). Deer
     Bay Resources Inc. has acquired outright, a 100% interest in the property
     for a cash payment of $7,500.

4. ACCESS, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE, AND PHYSIOGRAPHY

     Access to the Property is from well maintained logging roads on the east
     and south sides of the Property, from the TransCanada Highway that connects
     the town of Yale to Hope, British Columbia (Property Location: Figure 1).
     The area has been permitted for mining in the past and a major power line
     passes by the claims. The author had no difficulty accessing the claim
     blocks along any of the drainage road networks covered by the claims with
     4-wheel drive truck.

     Topography is rugged rising from the Fraser River at under 200 metres to
     the top of Settler Peak at over 1800 metres. The valleys are steep sided
     coastal alpine mountain type with typical rain forest vegetation of the
     coastal ranges of British Columbia. There is a mix of cedar, hemlock,
     spruce trees with alder, willow and cottonwood on old roads and poorly
     drained areas. Undergrowth brush consists of salal, devil's club and
     assorted berry bushes. Climate is also typical of the lower mainland area
     and is such that the lower and middle elevations will be workable year
     round with little difficulty. Higher ground may require snow machines or


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 7
<PAGE>
     similar track mounted vehicles. The most snow observed on roads was 2
     metres in late January 2009.

     All the major river drainages flow year round as do many subsidiary creeks.
     Harrison Lake is an active logging region with a plentiful supply of heavy
     equipment and operators available for hire. Most live in Harrison, Agassiz,
     Mission, Chilliwack or Hope. All these population centres totalling almost
     50,000 people are within a one hour drive of the project and provide all
     amenities including police, hospitals, groceries, fuel, helicopter
     services, hardware and other necessary items. Drilling companies are
     present in communities nearby while assay facilities are located in
     Vancouver.

5. HISTORY

     Gold placer mining on the Fraser River at Yale in the latter part of the
     19th century was first mining activity in this area. Yale marked the end of
     the navigable part of the Frazer River by paddle wheelers.

     The first indications of a significant ore zone in the region were
     discovered in 1923 along the Stulkawhits Creek and by 1926 the BC Nickel
     Company had been formed to develop the prospect. Subsequent exploration
     through the 1920's and 1930's discovered the main open pit Pride of Emory
     zone and led to initial mine development and bulk testing. By 1936 a 22.7
     ton sample from the 1600 level was reported carrying 2.74 grams per tonne
     Pd and Pt and 0.68 grams per tonne Au while earlier samples were reported
     3.98 grams per ton Pt and Pd and 7.89 grams per ton Au. Further work was
     curtailed by the Second World War and it was not until the 1950's that
     additional exploration and development work was completed. Reserves from
     this work were reported by A. Aho in 1954 to be 1.8 million tons. Full
     scale production was achieved in 1958/59 by Pacific Nickel Mines Ltd.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 8
<PAGE>
     From 1959 to the curtailment of operations in 1974 a total of 4.2 million
     tonnes of ore was mined and milled at the Pacific Nickel Mine with a mill
     grade of 0.77 % Ni and 0.34% Cu with "reported grades" of Pt and Pd in the
     0.6 grams per ton range. The average for the ore pods listed in government
     records were 1.19% Ni and 0.46% Cu. Only minor values of the platinum group
     minerals were "reported" from the smelter but in addition to the values
     reported above one sample from the "1500" pod reported 2.85 grams per tonne
     Pt and 4.94 grams per tonne Pd (the sample type and description is not
     available). The 0.1% Co grade was not paid for initially and payment for
     the 1% Cr is unknown.

     In 1974/75 Giant Mascot - the successor company to Pacific Nickel Mines -
     embarked on a limited exploration program of the ultramafic belt to the
     north and west of the mine area and of the intrusive Spuzzum Diorite. A
     regional contour soil, stream sediment survey was completed. Access at that
     time was limited and Giant Mascot concentrated on the stream sediment
     anomaly to the west of the mine area defining a resource of 100 million
     tonnes grading 0.22% Ni and 0.22% Cu. This resource figure is reported in
     government publications but has no technical data available and no
     parameters for its calculation. Therefore it is regarded as speculative and
     not to be relied upon .

     The area has been surveyed by a Geological Survey of Canadian airborne
     magnetic survey (1972), which highlights the mine area as a distinct
     magnetic anomaly. Various other magnetic anomalies identified by the survey
     were not investigated at that time; most have been covered by recent
     staking. No regional government geological mapping party has detailed the
     area. A government regional geochemistry survey has been completed and the
     data corresponds favourably within the staked claims and the mine site.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 9
<PAGE>
6. RECENT EXPLORATION WORK

     Since the commencement of staking of the Harrison Lake area numerous
     companies have been engaged in determining access, prospecting and
     preliminary geological inspection of the property and the old mine area.
     Although no definitive mapping has been completed, general observations and
     several rock samples were taken during the initial program on the adjacent
     properties.

     The Emmy Claim was staked by Santoy Minerals in the early part of the 21st
     century. They conducted a limited amount of geological prospecting and
     sampling but dropped the claims to pursue other areas of interest. No
     details of their work are available.

7. GEOLOGICAL SETTING

7.1 REGIONAL GEOLOGY

     The Harrison Lake area of the ultramafic belt is part of the Coastal
     Plutonic Sequence between the major suture structure along the Fraser
     River, located 8 to 15 kilometres to the east and the geological province
     of Wrangallia - which it represents as the eastern most portion - to the
     west. This terrain is highly metamorphosed as the contact zone of the
     Wrangallia geologic province where it was being rafted on to the North
     American Craton (Figure 2).

     The ultramafic belt as mapped by the Geological Survey of Canada is a
     continuous unit that extends from the Pacific Nickel Mine re-emerging from
     the Spuzzum Diorite Intrusive and swinging north through Settler Mountain
     and beyond towards Breckenridge Mountain and Glacier approximately 80
     kilometres to the north. The belt is between one to over five kilometres


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 10
<PAGE>
     wide and intrudes the very sulphide rich metasedimentary rocks equivalents
     of the Chilliwack Formation (Carboniferous or Permian age). These
     metasedimentary rocks are marked by the rusty character that is associated
     with distinctive sulphide gossan throughout the area.

     The Spuzzum Diorite borders the entire east side of the ultramafic belt as
     mapped by regional government geologists, separating the metasedimentary
     (Chilliwack) rocks located along the Fraser River to the east. The medium
     grained diorite appears to be relatively homogeneous in composition with
     finer grained and coarser grained phases. The felspar quartz hornblende
     composition was recorded and observed in outcrop and boulders with an
     anorthosite phase noted in one area. That felsic phase of the ultramafic
     belt has not been delineated to any extent or specifically traced and its
     size and relationship to both the other ultramafics and diorite remains
     unknown.

     Metasediment (Chilliwack equivalents) assemblages are recorded along the
     west side of the ultramafic belt between it and Harrison Lake. As well,
     various granitic intrusions are reported in the region, probably related to
     the Coastal Igneous plutonic rocks.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 11
<PAGE>
8. DEPOSIT TYPE

8.1 PACIFIC NICKEL MINE (as summarized from A. Aho, 1956)

     As the most comprehensive and proximal exploration model, the Pacific
     Nickel Mine is a guide to what should be looked for in the recommended
     exploration program.

     The area of the mine is hosted within ultramafic rocks with xenoliths of
     metasediments within the diorite.

     The ultramafics have hornblendite reaction zones up to 100 metres in
     contact with the diorite and appear to represent several pulses of
     intrusive. The ultramafic rocks contain minimal to no feldspar and the
     mafic mineral (olivine, bronzite, augite and hornblende) textures suggest
     recrystallization.

     The main structural trend of the ore zones is N75(Degree)W, which is
     parallel to the internal structure of the diorites, the internal
     arrangement of the ultramafics and the southwest contact of them. It
     reflects the possible presence of an older structure of weakness that could
     be responsible for the introduction of the ultramafic body.

     In 1956 Aho reported that the grade of the recovered ore averaged 1.4% Ni,
     0.5 % Cu, 1 % Cr, and 0.1% cobalt with 0.02 ounces per ton Au and 0.01 opt
     platinum metals occurring mainly with sulphides as pyrrhotite, pentlandite
     and chalcopyrite. Magnetite appears to be an integral part of the sulphide
     system and with olivine forms cores of the sulphide grains. Pyrite appears
     to be a later replacement of the pentlandite and in stringers within the
     ore.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 12
<PAGE>
     Supergene alteration minerals of limonite, chalcocite, covellite,
     violarite, melanterite and morenosite were noted in the ore zones. Their
     extent outside of the ore was not noted but possibly excludes them from
     being a significant exploration factor.

     Disseminated sulphide mineralization is found mostly in the southwestern
     half of the main ultramafic body and the smaller subsidiary ultramafic
     bodies to the south and southwest. The peridotites and olivine pyroxenites
     appear to be the best mineralized with the former being the most prolific
     especially near the margins.

     Uralitization is widespread throughout the complex represented by
     actinolitic alteration and steatitization . Serpentinization up to 50%
     accompanies the uralization in some of the peridotites and along the
     cleavages and grain boundaries in most of the peridotites and olivine
     pyroxenites, forming deeply weathered soft crumbly rocks. Hornblendization
     has also been recognized in association with structure and intrusive
     contacts.

     All the alteration features are closely related to structures (joints and
     faults) and contacts (dykes and intrusives).

     The main mineralized zone trends approximately 285(0) with a plunge or dip
     steeply to the north. Most of the visible fractures are post ore. Later
     work identified four main fault trends; 310(0)-315(0) dipping 50(0)-70(0)
     northeast; 15(0)-30(0) dipping 70(0) to either the southeast or northwest;
     350(0)-10(0) dipping 55(0) to either the east or west; and 330(0) - 30(0)
     dipping 20(0)-30(0) to either the east or west.

     The intersection of the first two fault trend sets has been concluded to be
     the control of the ore zones deposition. Tectonic and intrusive breccia was
     found to be spatially related to several of the ore pods.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 13
<PAGE>
     Twenty-six pods of massive sulphide were mined during the history of the
     operating mine ranging in size from 3,000 tons to 807, 000 tons. The shoots
     were described as steeply dipping circular to ellipsoid in shape around the
     long axis of the structure and are 100 feet or more in diameter with their
     depth extent 5 to 10 times that measure.

9. PROPERTY GEOLOGICAL SETTING

9.1 EMORY CREEK PROPERTY GEOLOGY

     The property is accessible by road up Emory Creek. The geology of the area
     of the Property is based on preliminary identification of some outcrops and
     interpreting the regional mapping completed by the government as it relates
     to the claim areas. New road cuts investigated by the author displayed a
     complex sequence of intrusives and ultramafic dykes requiring follow-up.

     Ultramafic units and the Cogburn and Settler Schist and Intrusive units
     were identified on the claims by prospecting and initial geological
     mapping. It was noted that these units are all related to the
     mineralization at the B.C. Nickel Mine. Ultramafic boulders were identified
     and the sources of these boulders are juxtaposed so that they cannot be
     related to Pacific Nickel Mine and therefore represent potentially new
     mineralized areas.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 14
<PAGE>
10. GEOPHYSICS

10.1 REGIONAL GEOPHYSICS

     The area of the claims has been covered by a Geological Survey of Canada
     airborne magnetometer survey (Figure 3), which some discreet anomalous
     magnetic features. These magnetic features appear related to that found
     associated with the ultramafic rocks that host the ore pods of the Pacific
     Nickel Mine. `Therefore, a logical initial exploration approach has been to
     follow-up in these areas with similar geophysical imprints in the area of
     the claims.

10.2 GEOPHYSICS OF CLAIMS

     No ground geophysical surveying has been reported for the Property.

11. REGIONAL GEOCHEMISTRY

     Regional government stream sediment geochemical surveying was completed
     which identifies the Property as an area of very anomalous base metal and
     indicator values. National geochemical reconnaissance surveys completed by
     the Geological Survey of Canada and the British Columbia Ministry of Energy
     Mines and Petroleum Resources on stream sediment samples have published
     values in Cu, Ni, Co, and Cr for the drainages of the Property that
     consistently identify the region in the 90th percentile of anomalous
     samples.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 15
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12. CONCLUSIONS

     The Harrison Lake ultramafic belt provides a very attractive exploration
     prospect for platinum group and Ni/Cu mineralization. The belt has not been
     subjected to exploration for at least 25 years despite hosting one of
     British Columbia's most profitable Ni/Cu/Pt/Pd mines and Canada's fourth
     largest mining area of these metals to date, following only the prolific
     Sudbury, Ontario, Thompson and Lynn Lake, Manitoba areas.

     Preliminary exploration and research to date by indicates that this
     ultramafic belt is permissive to host additional mineralization similar to
     the zones mined at the Pacific Nickel Mine. Locally, the ultramafic rocks
     underlying the Emmy claim are very similar to those present at the Pacific
     Nickel Mine and exhibit similar geophysical and geological signatures.

     It is concluded that detailed exploration as recommended could locate
     further mineralized zones. This exploration will map the various rock
     units; and a compilation of stream silt , rock and soil geochemical surveys
     with geophysical surveys, will evaluate the potential of the property. The
     belt of ultramafic rocks presently being considered for further exploration
     represents a unique situation: similar geological environment to a near-by
     past producing mine as a model; a new network of access roads; and a new
     base of technical information . Further work is warranted at the Emmy Claim
     to define drill targets.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 16
<PAGE>
15. RECOMMENDED PROGRAM

     A detailed program (Phase I) of geological review and exploration is
     proposed to develop a detailed geological base model for the claims.

     Both Phase I and Phase II are necessary to complete the initial evaluation
     of the Property and to select drill targets (Phase III).

16. BUDGET

     The initial phase of exploration for the claims will consist of detailed
     geological mapping along all roads and silt sampling of every drainage or
     draw (soil sampling if necessary). This work is important to establish base
     and anomalous geochemical values for the area and to confirm earlier
     results; and to assess the structural implication of the drainages as
     faults or contact zones

     The Phase I budget will cover detailed geological mapping; silt (soil if
     necessary) geochemical sampling of defined drainages; and prospecting. It
     is estimated to cost $10,000 as described below. Phase II, which will
     utilize the Phase I results to facilitate compilation all the known
     technical data, is estimated to cost $25,000, and will allow the Company to
     select initial drill sites. Phase III, which will be preliminary drill
     testing of selected targets, is estimated to cost $50,000 will follow at
     that time.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 17
<PAGE>
BUDGET - PHASE I

     1. Senior Geologist& Geological technician @ $900/day               $ 4,500
     2. Equipment rental Fuel, Food, Field Supplies $ 500/day            $ 2,500
     3. Soil sampling and Assays                                         $ 1,750
     4. Report                                                           $ 1,000
     5. Filing Fees                                                      $   250
                                                                         -------
     SUBTOTAL                                                            $10,000

PHASE II

     1.  Review of  Geochem and Detailed Geology sampling                $ 7,200
     2.  Review of geophysical magnetometer surveys                      $ 7,500
     3.  Field Survey of drill sites $500/day                            $ 4,500
     4.  Soil Sampling & Assays                                          $ 2,500
     5.  Report                                                          $ 1,800
     6.  Contingency                                                     $ 2,000
                                                                         -------

         GRAND TOTAL - PHASE II                                          $25,000


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 18
<PAGE>
17. STATEMENT OF QUALIFICATIONS

I, GLEN MACDONALD, of 488-625 Howe Street, Vancouver, BC, hereby certify that:

1.   I am a graduate of the University of British Columbia with degrees in
     (B.A., 1971) and Geology (B.Sc., 1973);

2.   I have practiced my profession as Geologist since graduation; over 28
     years;

3.   I have worked as a Geologist for Whitehorse Copper Mine and acted as
     District Manager for Exploration for Yukon/Western N.W.T. for Noranda
     Exploration and am therefore qualified to write this report and recommend
     the proposed exploration program and budget in this report;

4.   I have practised Geology as an Independent Consulting Geologist since 1983;

5.   I am a member of the Association of Professional Engineers, Geologists and
     Geophysicists of Alberta (No. 36214);

6.   I am a member of the Association of Professional Engineers and
     Geoscientists of the Province of British Columbia (No. 20464);

7.   I visited the property in October, 2004 and in July 2009;

8.   I am responsible for this report and the opinions expressed therein.

9.   There are no material facts or material changes in the subject matter of
     this report that would mislead the reader.

10.  I have no interest, direct or indirect, in the properties or shares of Deer
     Bay Resources Inc., nor do I expect to receive any.

11.  I have no prior involvement with this property and have no interest
     therein;

12.  I hereby grant my permission Deer Bay Resources Inc. Inc. to use this
     report use normal to the business of the Company.

Dated at Vancouver, BC, this 15th day of March,2010

Glen C. Macdonald, P.Geol., P.Geo.


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 19
<PAGE>
18. REFERENCES

     Aho, A. "Geology and Genesis of Ultramafic Nickel Copper Pyrrhotite
     Deposits at the Pacific Nickel Property, Southwestern British Columbia":
     Economic Geology, v 51 p444 - 481

     Minefile Capsule Geology and Bibliography; 092HNW058; 092HNW 070;
     092HNW073; 092HNW076; 092HSW004; 092HSW081

     Ministry of Energy, Mines and Petroleum Resources , British Columbia; Open
     File Report 1990-27 p43 -47

     Vining, Mark R. Regional Setting of Giant Mascot Mine (92H/5W, 6E)
     Geological Fieldwork 1975 Paper1976 -1 p 49-52

     Monger, J.W.H. Hope Map Area, West Half (92HW1/2) British Columbia, q
     Geological Survey of Canada, Paper 69-47, Pages 63-64

     Ministry of Energy, Mines and Petroleum Resources, British Columbia;
     various presentation notes and slides on the BC Nickel Mine

     Schroder, T. Ministry of Energy, Mines and Petroleum Resources, British
     Columbia; District Geologist, pers. Communication

     Christopher, P. Consultant; Pers. Communication. From his work "Giant
     Mascot Mine," Geological Fieldwork 1974 Paper 1975-2 pages 17-21


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 20
<PAGE>
     Ministry of Energy , Mines and Petroleum Resources , British Columbia;
     Summary - Giant Mascot(Pacific Nickel, British Columbia Nickel) 1986-87 p
     30-33

     Department of Energy, Mines and Resources, Geological Survey of Canada;
     Open File 2948a - Tectonic Assemblage Map of Vancouver Open File 2490 -
     Guide to the Geology and Tectonic Evolution of the Southern Coast Mountains
     - 1994, Preliminary Map - Terranes of the Southern Coast and Intermontane
     Belts, British Columbia 1994, Journeay J. M. and Monger, J.W.H Geology MapS
     12 -1969; 1386A; 41 -1989 Aeromagnetic Maps: 8534G Harrison Lake; 8538G
     -Hope; 8535G Spuzzum, RGS 1994 - Hope Regional Geochemical Survey, RGS 39

     Clarke W.E (1969) Geology and Ore Control, Giant Mascot Mines Ltd. Western
     Miner, Volume 42 #6 p. 41-46


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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 21
<PAGE>
APPENDIX 1:  REGIONAL SHOWINGS




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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 22
<PAGE>
<TABLE>
<CAPTION>
<S>            <C>                 <C>               <C>              <C>            <C>             <C>
Number          Names              Status         Commodities    NTS Maps        Lat./Long.     Deposit Types
------          -----              ------         -----------    --------        ----------     -------------
                 GEM,                             Molybdenum
                 MEG,            Developed         Copper
                 HLM,             Prospect          Zinc
                 SASH,           Inventory         Tungsten                    49 42 42 N     Porphyry Mo (Low F-
092HNW001    BAILEY GROUP          Report           Bismuth       092H12E      121 43 11 W           type)

                                                                               49 44 03 N
092HNW006        WREN             Showing            Gold         092H12E      121 43 24 W

              QUEEN MINE,                           Silver                     49 34 34 N
092HNW020    QUEEN (L.63)         Prospect           Gold         092H11W      121 26 48 W

                                                                  092H11W      49 34 00 N     Kyanite-sillimanite
092HNW028     EMMY CREEK          Showing         Sillimanite     092H12E      121 30 00 W          schists.

              PROVIDENCE
               (L.1737),
              SILVER BELL      Past Producer                                                    Au-quartz veins.
               (L.1738),         Production          Gold                      49 37 19 N      Epithermal Au-Ag:
092HNW030     ELIZABETH 1          Report           Silver        092H12W      121 56 56 W      low sulphidation

                                                                                                   Tholeiitic
                                                    Copper                     49 33 22 N       intrusion-hosted
092HNW040         AL              Showing           Nickel        092H12E      121 43 05 W           Ni-Cu

                                                                                                    Fe skarn

                  OX,                               Copper
                SCUZZY,                              Gold                      49 30 39 N          Cu skarn.
092HNW041       SCRUNGY           Showing           Silver        092H12E      121 38 44 W         Au skarn.

                 PIPE,                              Copper
                 JAY,                             Molybdenum                   49 36 30 N     Porphyry Mo (Low F-
092HNW044    SAWMILL CREEK        Showing            Zinc         092H11W      121 27 49 W           type).

            SETTLER CREEK,                                                                         Tholeiitic
                  NI,                               Nickel                     49 33 39 N       intrusion-hosted
092HNW045       ZONE 4            Showing           Copper        092H12E      121 39 19 W           Ni-Cu.

                                                    Nickel
               CITATION,                            Copper                     49 30 53 N          Tholeiitic
092HNW046    MORGAN GROUP         Showing            Zinc         092H11W      121 27 08 W      intrusion-hosted

                                                                                               Ultramafic-hosted
             GORDON CREEK                          Asbestos                    49 32 52 N          asbestos.
092HNW057      ASBESTOS           Showing          Chromium       092H11W      121 27 01 W     Podiform chromite.

             HARRISON LAKE                                                     49 32 20 N      Ultramafic-hosted
092HNW058      ASBESTOS           Showing          Asbestos       092H12E      121 44 12 W         asbestos.

                                                                                                Microcrystalline
                                                                                                   graphite.
                                                                               49 30 50 N      Crystalline flake
092HNW064        HOPE             Showing          Graphite       092H12W      121 45 42 W          graphite

                                                    Copper
                                                     Zinc
                                                    Silver                     49 34 33 N        Besshi massive
092HNW070     NORTH FORK          Prospect           Gold         092H12E      121 44 50 W       sulphide Cu-Zn

                                                    Kyanite                    49 34 13 N     Kyanite-sillimanite
092HNW073    COGBURN CREEK        Showing         Sillimanite     092H12E      121 39 30 W          schists

                                                    Nickel                                         Tholeiitic
                                                    Copper                     49 32 56 N       intrusion-hosted
092HNW076        JASON            Showing          Chromium       092H12E      121 41 35 W           Ni-Cu.
                                                                  092G12W
                                                    Granite
              RAVEN BLACK,                       Dimension Stone                49 36 00 N      Dimension stone -
092GNW071   GRANITE CREATIONS   Past Producer    Building Stone    092G12E      121 37 00 W          granite.
</TABLE>

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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 23
<PAGE>
<TABLE>
<CAPTION>
<S>             <C>                 <C>               <C>              <C>            <C>             <C>
Number           Names              Status         Commodities    NTS Maps        Lat./Long.     Deposit Types
------           -----              ------         -----------    --------        ----------     -------------
             PRIDE OF EMORY,
             PRIDE OF EMORY
                (L.793),
             PRIDE OF EMORY
                  MINE,
              GIANT NICKEL,
             PRIDE OF EMORY                          Nickel
              NO.2 (L.794),                          Copper
               DISCOVERY,                            Cobalt
                GIANT MASCOT,                         Gold
                B.C. NICKEL,      Past Producer      Silver
               PACIFIC NICKEL,    Production        Chromium
             WESTERN NICKEL,        Report          Platinum                                        Tholeiitic
                 ZOFKA,           Inventory         Palladium      092H05E      49 28 30 N       intrusion-hosted
092HSW004   GIANT NICKEL MINE       Report            Zinc         092H06W      121 30 46 W           Ni-Cu

                                                     Copper
                                                      Gold                      49 25 09 N
092HSW024      IDEAL GOLD          Showing           Silver        092H06W      121 26 16 W      Au-quartz veins.

                   NI,
                 NI 752,
                   AL,
                   OX,                                                                              Tholeiitic
                  COG,                               Nickel                     49 29 49 N       intrusion-hosted
092HSW081        COGBURN           Prospect          Copper        092H05E      121 39 28 W           Ni-Cu.

                 SWEDE,                                                                             Tholeiitic
                  BEA,                               Nickel                     49 26 00 N       intrusion-hosted
092HSW082         GIANT            Showing           Copper        092H06W      121 29 56 W           Ni-Cu

            STAR OF EMORY 3,                         Nickel
             PRIDE OF EMORY,                         Copper
           GIANT NICKEL, STAR                       Chromium
           OF EMORY (L.1414),                         Gold                                          Tholeiitic
               BRUNSWICK,                           Platinum                    49 28 08 N       intrusion-hosted
092HSW093     GIANT MASCOT      Past Producer       Palladium      092H05E      121 32 16 W           Ni-Cu

                                                     Nickel
              CHOATE, GIANT                          Copper                                         Tholeiitic
              NICKEL, GIANT                         Chromium                    49 29 02 N       intrusion-hosted
092HSW125        MASCOT         Past Producer        Cobalt        092H06W      121 29 00 W           Ni-Cu.

                                                                                49 28 37 N
                                                     Copper        092H05W      121 45 17 W     Porphyry Cu+/-Mo+/-
092HSW138      GOLDEN BEAR         Showing         Molybdenum      092H05E         SKARN                Au

                                                   Sillimanite                  49 27 00 N     Kyanite-sillimanite
092HSW143      ZOFKA RIDGE         Showing           Garnet        092H05E      121 31 00 W          schists
</TABLE>

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Ni-Cu MASSIVE SULPHIDE PROJECT                                           PAGE 24