Filed by Automated Filing Services Inc. (604) 609-0244  - Chilco River Holdings Inc. - Exhibit 10.2





 EXHIBIT 10.2

 Geology Report 

 On the

 Peg Claim Mineral Claim



 Harrison Lake, British Columbia, Canada

	 	 Northing  	  	 5509600m 	 
	 	 	 	 	 
	 	 Easting  	  	 598000m 	 
	 	  	 	 	 
	 Longitude 121o 44' W  	  	 Latitude 49o 44' N 




 UTM Zone 10



 Map Sheet M092H072

 For

 Chilco River Holdings Inc. 

  Suite 420 – 625 Howe Street 

  Vancouver, British Columbia, Canada 

  V7C 2T6 

 

 Geologist

 Laurence Stephenson, P.Eng. 

  Date: December, 2003 

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 Table Of Contents



	 	 	  	 Page  
	 1.	 Summary	 4  
	 	 	 	 
	 2.	 Introduction	 5 
    
	 	 	 	 
	 3.	 Property Description
      and Location	 6 
    
	 	 	 	 
	 4.	 Access, Climate,
      Local Resources, Infrastructure and Physiography	 7 
    
	 	 	 	 
	 5.	 History	 8 
    
	 	 	 	 
	 6.	 Recent Exploration
      Work	11
	 	 	 	 
	 7.	 Geological
      Setting	 12
	 	 	 	 
	 8.	 Deposit Type	 13
	 	 	 	 
	 9.	 Geophysics	 15
	 	 	 	 
	 10.	 Regional Geochemistry	16
	 	 	 	 
	 11.	 Conclusions	 17
	 	 	 	 
	 12.	 Recommended Program	18
	 	 	 	 
	 13.	 Budget	 18
	 	 	 	 
	 14.	 Statement of Qualifications	19
	 	 	 	 
	 15.	 References	 20




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List Of Figures


	  	 Following page  
	  	 
	 Figure 1: Claims Location Map  	 (at end)  
	 Figure 2: Regional Geology Map  	 (at end)  
	 Figure 3: Regional Geophysics Map  	 (at end)  
	 Figure 4: Peg Claim Map  	 (at end)  





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	 1.	 Summary  
	  	 
	 	 The Harrison Lake Region
        north west of Hope, British Columbia, has yeilded significant mining production
        from various commodities and hosts numerous mineralized showings. 
      

	 
	 
	  	 
	 	 The Pacific Nickel Mine,
        located near the town of Hope, was a significant producer of copper and
        nickel and precious metals from an ultramafic intrusive geologic environment.
        The GEM molybdenum property south of Chilco River Holdings Inc. Peg Claim
        property has published tonnage and grade. New discoveries have been made
        in the last few years in this highly potential belt of rocks.  

	 
	 
	 
	 
	 
	  	 
	 	 An initial review of the
        geology and the geophysics has identified anomalous gold in pegmatite
        areas on the property requiring further follow-up exploration. 

	 
	  	 
	 	 An initial exploration program
        is proposed for the property to assess the potential for discovery of
        further precious metals. It is recommended that a program of geological
        mapping, sampling and prospecting be undertaken to further define areas
        of potential interest. This will cost some $3,500. Continuing work will
        involve a more detailed geology, geochemical sampling and ground geophysics
        programme costing approximately $25,000 for the claims. 

	 
	 
	 
	 
	 






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	 2.	 INTRODUCTION 
      

	  	 
	 	 Following all
        the activity in the region and after careful research for local potential
        for base and precious metal deposits, Chilco River Holdings Inc. focussed
        on the Pacific Nickel Mine ultramafic belt, 7 kilometres north of Hope,
        BC which was the fourth most productive Nickel-Copper area of Canada (After
        Sudbury, Ontario; Thompson, Manitoba; and Lynn Lake, Manitoba). The acquisition
        of the mineral claim by Chilco River Holdings Inc. was completed in November
        of 2003.  

	 
	 
	 
	 
	 
	 
	  	 
	 	 This report
        was initiated by Robert Krause, President of Chilco River Holdings Inc.
        to report on the recently completed acquisition, evaluate the results
        and to recommend further exploration work to develop the property's mineral
        prospects.  

	 
	 
	 
	  	 
	 2.1 	 Disclaimer 
      

	  	 
	 	 In order to
        write this report, previous reports on the area by the author and work
        completed on the claims was reviewed. As well, the report includes the
        initial prospecting and preliminary geological work completed by Mr. Deering,
        P.Eng. and Mr. Nicholson, P.Geol. on the adjacent Harrison Lake Property
        . It represents the first known compilation of data for the area in over
        25 years. The author has been involved in the area since March, 2000 assessing
        the geological potential, access, and general conditions.  

	 
	 
	 
	 
	 
	 
	  	 
	 	 It should be
        noted that over the last three years, several public and private companies
        have now started exploring the region and the BC government initiated
        an aggressive program in the Harrison Lake-British Columbia Nickel Mine
        area consisting of detailed cross-sectional geologic mapping, sampling,
        and age dating to foster further exploration.  

	 
	 
	 
	 
	  	 
	 	 The author disclaims responsibility
        for information in the public domain.  







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	3. 	Property Description and Location

       The Property is located east of Harrison Lake and northwest
        of Hope in southwestern British Columbia (Figure 1, UTM Zone 10, Map Sheet
        M092H072) and the area has recently been further opened by logging operations
        which provide new access to the region. Logging roads are located within
        300 metres of the claim group. Permitting for initial exploration work
        has already been obtained.

       The Property consists of one (1) unpatented mineral
        claim representing 16 units that has been staked and recorded as a four
        post claim. Details of the claim of Chilco River Holdings Inc. is found
        below and the claim location and general size is displayed in Figure 1.






  Table 1. Chilco River Holdings Inc. Claims


	
      

      Claim Name  

      

    	 
    	
      Units  	 
    	
      Record #  	 
    	
      Expiry Date  	 
    	
      Map Sheet  	 
    	
      Locator  	 
    	
      Agent for: *  
	 PEG  	  	 16  	  	 401581  	  	 12-Apr-05  	  	 MO92H072  	  	 D. Deering.  	  	 self  
	 	 	 	 	 	 	 	 	 	 	 	 	 
	 TOTAL  	  	 16  	  	        UNITS 
    	 	 	  	  	  	  	  	  


In British Columbia, each unit equals 25 hectares. 



	 	All claims staked in British Columbia require $100
        worth of assessment work per unit to be undertaken in Years 1 and 2, followed
        by $200 per unit per year thereafter. There are no known environmental
        concerns or parks designated for any area contained within the claims.
        Harrison Lake is used extensively for recreational pursuits however it
        has no official designation. One valley east of Harrison Lake has a spotted
        owl preserve however this has no relevance to the ground covered by these
        claims. 

       The property has no encumbrances. As advanced exploration
        proceeds there may be bonding requirements for reclamation.

      Chilco River Holdings Inc. has acquired outright, a 100%
        interest in the property subject to a 2.5% Net Smelter Royalty, for a
        total cost of $12,500 U.S.






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	4. 	Access, Climate, Local Resources, Infrastructure,
        and Physiography

       Access to the Property is along well maintained logging
        roads on the west side of the Property from the town of Agassiz, British
        Columbia. The area has been permitted for mining in the past and a major
        power line exists in the region. There is no difficulty accessing the
        claim block along the logging road networks by 4-wheel drive truck or
        4-trax vehicle. Access for the proposed program will be off the Clear
        Creek Main Road. 

       Topography is rugged rising from Harrison Lake 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 is typical with 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 similar track mounted vehicles. The most snow observed
        on the tops of the hills was 3 metres in late January. 

       All the major river drainages flow year round as do
        many subsidiary creeks. Harrison Lake is an active logging region with
        plenty 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. 






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	5. 	HISTORY

       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.
        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.
        Full scale production was achieved in 1958/59 by Pacific Nickel Mines
        Ltd. 

       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. 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 value of only the Ni/Cu ore recovered
        in today's prices would be in excess of $455 million US. 

       Mining continued until 1974 when a variety of factors
        interceded to curtail operations – the mill burned down, a mine accident
        caused loss of life and most significantly the Japanese smelters that
        were processing the Ni-Cu ore, curtailed their nickel smelting operations.
        Alternative smelting facilities were not economically available and the
        mining operations ceased.

       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 was limited and






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	 	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 parameters on its
        calculation, therefore it is regarded as highly speculative. This zone
        is currently under option to Leader Mining International Inc. 

       Another zone, located to the north along Settler Creek
        by Giant Mascot in the mid 1970's, was reported in Minfile 092HNW045 to
        be in a "similar setting as the Pacific Nickel Mine" in ultramafic rocks
        intruding the "Cretaceous Settler Schist."

       In the late 1960's, a showing of molybdenum was discovered
        associated with a younger intrusion, approximately one kilometre to the
        south. A 15 million tonne resource grading 0.125 % molybdenum was outlined
        by drilling. This resource figure is reported in government publications
        but has no technical data available and parameters on its calculation,
        therefore it is regarded as speculative. 

       The zone covered by the Peg Claim was discovered in
        1980 and a small sampling program was conducted on the precious metal
        carrying veins. The values of gold and silver were not followed up. 

       Since that time little to no recorded exploration was
        carried out in the region.

       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 magnetic high anomalies were not
        investigated at that time but most have been covered by the recent activity
        and some association with mineralization has been determined. No regional
        government geological mapping party has detailed the area. A government
        regional geochemistry survey has been completed that shows anomalous data
        corresponds favourably 






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	 	to the old mine site. More specifically, the drainages
        covered by the Property all report indicator minerals (Cu, Ni, Co, Cr).
        This is the same as the mine site drainage. 

       In early 2000 with the increase in Pd, Pt and Au prices,
        an area of a 100 million tonne resource, discovered by Giant Mascot, was
        acquired by private interests, rekindling interest in the area. In addition,
        with the available access greatly enhanced by the current logging operations
        since March 2000 it has been possible by numerous prospecting traverses
        to identify the ultramafic rocks that match the tenor and character of
        those within the mine area.

       With this increase of exploration many new and untested
        zones were examined, advancing the geological and mineral data base of
        the area. New ideas were applied to both new and old zones with significant
        success in developing the overall potential of the area. This encouraged
        the prospector to acquire the staked area. 






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	6. 	Recent Exploration Work

       No recent exploration has been reported in the vicinity
        of the mineral claims. Work in the Harrison Lake area by the author and
        others has been on claims over one kilometre to the west and south of
        this claim group. The geology of the surrounding area can be projected
        to this area. 







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	 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 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. Specifically
        just north of the Cogburn Creek a small massive sulphide lens was located
        (west of the North Fork of the Cogburn Creek) which graded 2-4% Cu with
        up to 1.5% Zn and up to 1.5 ounces per ton Ag over widths up to 3 metres.
      

	 
	 	 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 





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	 	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. 

	 	 
	7.2	Peg Property Geology

       This initial description of geology of the area of the
        Property is based on the initial preliminary identification of some outcrops
        in the area to the south and interpreting the regional mapping completed
        by the government. A trend of gossanous Settler Schist is projected to
        cross the property. Felsic and mafic intrusives into the Settler Schist
        units are reported on the claims and the discovered precious metal veins
        are associated with the felsic granodiorite. Younger similar to those
        associated with the molybdenum zone to the south are reported to occur
        as small plugs and dikes in the Peg Claim area.

       A vein of quartz up to 2 metres wide striking 80o
        and dipping 80o-85o N was traced for over 160 metres on the
        claim had reported precious metal values of up to 0.027 ounces per ton
        gold and 0.10 ounces per ton silver.

	 	 
	8. 	Deposit Type 

       Three deposit types can be modelled as potentials for
        a successful mineral exploration program. 





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	 	 As the most comprehensive and proximal exploration
        model, the geology and characteristics of the Pacific Nickel Mine should
        not be over looked as a guide in the recommended exploration program.
      

	 
	 	 The main ultramafic belt intruded the Cogburn, Slollicum
        and Settler metasedimentary (Chilliwack equivalents) schists and the Spuzzum
        Diorite intrusive during the late Paleozoic period. The metasediments
        with sulphides are intruded by the Spuzzum diorite and form xenoliths
        in that body. Both units are cut by ultramafic rocks with some intermingling
        of the diorite and ultramafic. These units occur or are projected to occur
        on the property. 

	 
	 	 The intrusive porphyry breccia model similar to
        that located on the claims immediate to the south should also be investigate
        since there is reported similar intrusives occurring in the vicinity of
        the claims. 

	 
	 	 Veins of precious metals were the main focus of
        previous exploration and the presence of additional veins would enhance
        the prospects of the property having significant potential. 

	 
	 8.1     
      
	 Mineralization 

	 
	 	 The mineralization reported on the property associated
        with the gold and silver values is pyrite and arsenopyrite in quartz vein.
        No further details to the style or quantity of the sulphides and its relationship
        to the precious metal values is available except that the vein contains
        "scattered" sulphides. 

	 
	 8.2     
      
	 Alteration 

	 
	 	 No alteration is reported. 





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	 8.3     
      
	 Structure 

	 
	 	 The main mineralized veins are reported to trend
        80o with a dip steeply to the north. Fine grained intrusive "trap"
        dikes are interpreted to "occupy structural breaks" and only one is reported
        as striking parallel to the mineralized quartz vein. Interpreted structure
        from the drainages and contours does correspond to this trend established
        by the vein and suggests that the precious metal vein is structurally
        controlled. 

	 
	 9.     
      
	 Geophysics 

	 
	 9.1
	 Regional Geophysics 

	 
	 	 The area of the claim has been covered by a Geological
        Survey of Canada airborne magnetometer survey (Figure 3), which highlighted
        certain broad, highly anomalous magnetic features. These magnetic "thumb
        print" features are very similar to the "thumb print" signature related
        to that found immediately north of the Pacific Nickel mine area. The ore
        pods of the Pacific Nickel Mine are located along the southern edge of
        the elliptical magnetic anomaly associated with the mine area's ultramafic
        intrusion. 

	 
	 	 A review of the geophysical map suggests a significant
        magnetic feature occurs in the northern area of the claim. Follow up investigation
        by ground geophysics and prospecting is warranted. 

	 
	 9.2
	 Geophysics of Claims 

	 
	 	 No ground geophysical surveying has been reported
        for the Property. Local testing with magnets of the pyrrhotite demonstrates
        its magnetic character. Ground magnetic surveying on adjacent claims has
        been useful in delineating areas of interest. 





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	10. 	Regional Geochemistry

       Regional government stream sediment geochemical surveying
        was completed which identifies the Property as an area of anomalous base
        metal and indicator values. It should be noted that anomalous values,
        including those near the mine, appear to correlate with the magnetic highs
        identified in the 1972 government airborne geophysical survey. 

       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 a few of the drainages of the southern
        portion of the Property that identify the region in the 50th
        -percentile of anomalous samples.






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	11. 	CONCLUSIONS

       The Harrison Lake ultramafic belt provides a very attractive
        exploration prospect for precious and base metal 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.

       Initial exploration by other companies continues to
        identify the high potential of this belt which hosts claim of Chilco River
        Holdings. Locally the rocks of the Property are very similar to those
        found at the Pacific Nickel Mine and associated with nearby mineralization.
      

       A quartz vein with values of gold and silver has been
        identified on the property and other potential parallel veins have been
        indicated but remain untested. 

       It is concluded that detailed exploration as recommended
        will likely locate further mineralized zones. Further work is warranted.





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  	12. 	RECOMMENDED PROGRAM

         After a careful review of the results obtained on
          the adjacent properties, it is recommended that traverses be completed
          along the ridgeline in the central portion of the claim and two to four
          contour traverses separated by approximately 500 metres be completed.
          These traverses will collect geological and geochemical samples for
          further analysis.

	 	 
	13. 	BUDGET

         The budget to execute the proposed program is estimated
          to cost $3,500 as described below.





Budget – Phase I


  	 	 1.	 Senior Geologist  	 3 days @ $500/day  	 $ 	 1,500 
	 	 2.	 1 Geotechnicians  	 3 days @ $250/day  	 $ 	 750 
	 	 3.	 Equipment rental  	 4 wheel drive vehicle 3 days@$75/day  	 $ 	 225 
	 	 4.	 Assays 	30 @ $20 each  	 $ 	 600 
	 	 5.	 Food, fuel & supplies  	 	 $ 	 200 
	 	 6.	 Report  	 	 $	225 
	 	 	 	 	 	 
	 	Total	 	$	3,500



  

  	 	Upon receipt of favourable results, follow-up geological
          investigations including a ground geophysical survey will be required.



  Budget 



	 	 1 .	 VLF EM Survey  	 $ 	 15,000  
	 	 	 	 	 
	 	 2 .	 Detailed geological investigations  	 $ 	 10,000  
	 	 	 	 
	 	 TOTAL  	 $ 	 25,000  






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	14. 	Statement of Qualifications


I, LAURENCE STEPHENSON, of 1136 Martin St., White Rock, BC hereby certify that:

	 	 1.     
      
	 I am a graduate of the Carleton University, Ottawa,
        Ontario, Canada with a Bachelor of Science degree in Geology (1975) and
        of York University, Toronto, Ontario, Canada with a Masters of Business
        Administration degree (1985); 

	 
	 	 2.      
	 I have worked as Geologist for over 33 years; 

	 
	 	 3.      
	 I have worked as the District Geologist for Duval
        International Corporation (Battle Mountain Gold) and as geological and
        financial consultant to First Marathon Securities, Yorkton Securities,
        BGO Securities and several other Securities firms evaluating mining properties
        and as a consultant and President of Kokanee Explorations Ltd (now Standard
        Mining), as a consultant and director of Glencairn Explorations, as a
        consultant and Vice President of Golden Chief Explorations, and as President
        of GeoFin Inc. consulted for several other companies writing reports for
        their use and am therefore qualified to write this report and recommend
        the proposed exploration program and budget in this report; 

	 
	 	 4.      
	 I am a member of the Association of Professional
        Engineers of Ontario. 

	 
	 	 5.      
	 I visited the property specifically on August 23
        and August 24, 2001, along the Clear Creek Road. As well I visited the
        old British Columbia Nickel Mine site On several occasions and have been
        intimately involved with the preliminary mapping of the adjacent property.
      

	 
	 	 6.      
	 I am responsible for this report and the opinions
        expressed therein. 

	 
	 	 7.      
	 There are no material facts or material changes
        in the subject matter of this report that would mislead the reader. 

	 
	 	 8.      
	 I have no interest, direct or indirect, in the properties
        or shares of Chilco River Holdings Inc, nor do I expect to receive any.
      

	 
	 	 9.      
	 I have no prior involvement with this property and
        have read Instrument and Form 43-101 F1 and this technical report has
        been prepared in compliance with this instrument and Form 43-101 F1. 

	 
	 	 12.      
	 I hereby grant my permission for Chilco River Holdings
        Inc. to use this report for any corporate use normal to the business of
        the Company. 



 Dated at Vancouver, BC, this 22nd day of December, 2003.

 /s/ Laurence Stephenson

Laurence Stephenson P. Eng.


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	 15.	 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; 092HNW041;
      092HNW 040; 092HNW 045; 092HNW058; 092HNW 070; 092 HNW073; 
	 	  	 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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	 	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; 8539G Mount Urquahart; 8540G Scuzzy Mountain; 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 
	 	 	 
	 	Murphy, J.D. (1980) 	Prospecting Report on the Wren Group of Mineral Claims, Assessment file
      Report # 9701 




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