Lomalampi. Mineral deposit type. Dimension. Holder history Previous holders:

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1 Mineral Deposit Report Page 1 OF Lomalampi Occurence type: prospect Commodity Rank Total Total production Total resource Importance measure group metal 1 1,16 t 1,16 t Small deposit nickel t 4896 t Small deposit copper t 1530 t Occurrence 3 0,21 t 0,21 t Occurrence 5 0,36 t 0,36 t Occurrence 5 0,79 t 0,79 t Occurrence Easting EUREF: ,261 Easting YKJ: Northing EUREF: ,78 Northing YKJ: Discovery year: 2004 Discovered by: References: 2, 4 Mineral deposit type Group: Metallogenic deposit Main type: Ultramafic (magmatic) Sub type 1: Komatiitic Ni Comments: Komatiite-hosted PGE-enriched, disseminated sulphide deposit, with relatively low Ni-Cu contents Dimension Expression: exposed Area (ha): Form: concordant Dip azim: 135 Shape: Dip: 80 Length (m): 550 Plunge azim: Width (m): Plunge dip: Thickness (m): 10 Orientation method: Depth (m): 130 Holder history Previous holders: Company Years Holding type Comments Claim (old law) 1

2 Mineral Deposit Report Page 2 OF EXPLORATION ACTIVITY Years Activity type Geologist Exploration result Ref detailed geophysics Mgnetic-, VLF-R-, IP- and SAMPO profile measurements core drilling Markku Iljina, Pertti Heikura mineralized zone identified 1 Core drilling, 39 drill holes, meters. Intersections M372306R416 From-To 45,9-47,9 Length 2m 0,19ppm copper 0,16% nickel 0,38% 1,32ppm 0,67ppm group 2,01ppm metal M372307R0427 From-To 28,1-29,6 Length 1,5m 0,12ppm 0,09ppm copper 0,4% nickel 0,12% 3,4ppm M372308R0437 From-To 93,1-94,6 Length 1,5m 0,55ppm 0,23ppm 0,64% copper 8650ppm nickel 7320ppm detailed geology Mapping and boulder sampling subsurface exploration Jorma Räsänen, Pertti Heikura, Markku Iljina detailed geology Jorma Räsänen, Pertti Heikura, Markku Iljina Mapping and boulder sampling core drilling Jorma Räsänen, Pertti Heikura, Markku Iljina Discovered in GTK-CSIRO komatiite research project when doing drilling for bedrock mapping purposes; Core drilling (reconnaissance drilling): nine drill holes, meters. Intersections 2

3 Mineral Deposit Report Page 3 OF From-To Length 1m 0,05ppm copper 0,16% 1,11ppm 0,47ppm nickel 0,33% From-To Length 0,6m 0,1ppm copper 0,11% 0,96ppm 0,46ppm nickel 0,31% From-To Length 0,9m 0,06ppm copper 0,11% 0,98ppm 0,55ppm nickel 0,34% detailed geophysics Jorma Räsänen, Pertti Heikura, Markku Iljina Systematic ground magnetic and VLF-R- measurements. Figures 3

4 Mineral Deposit Report Page 4 OF 11 Results of MMI geochemistry:

5 Mineral Deposit Report Page 5 OF RESOURCES AND RESERVES Most recent Type: Company: Year: Date: Calc Method: Reference: Resource Geological Survey of Finland 2010 Non-compliant resource estimate 5 Category: Inferred mineral resource Tonnage: 3,06 Mt copper 0,05 % 0,07 ppm nickel 0,16 % 0,12 ppm 0,26 ppm group 0,38 ppm metal Cutoff: 0,1 ppm Comments: PGE calculated by GTK 5

6 Mineral Deposit Report Page 6 OF GEOLOGY Host rock: Komatiite, Graphite Schist Wall rock: Basaltic komatite Komatiite (Host rock) Rock type: Host rock Proportion: all Grain size: Fine grained mm Color: References: 3 Comments: Disseminated sulphides in metamophosed olivine cumulate, some mobilized cm thick veins. The olivine cumulate host represent low MgO komatiitic or basaltic komatiitic cumulate part of a flow unit or alternatively a sill. Ore minerals: Mineral Proportion Mineral texture Arsenopyrite trace Grain Chalcopyrite present Dissemination Gersdorffite trace Grain Pentlandite present Dissemination Pyrrhotite present Dissemination Sperrylite trace Grain Other minerals: Mineral Proportion Mineral texture Calcite present Alteration product Chlorite less than half Alteration product Magnetite present Alteration product Serpentine major Alteration product Talc present Alteration product Tremolite present Alteration product Structures Veined Alteration: Distribution: Degree: Relation to mineralization: serpentinisation Pervasive Strong Comments: Rather extensive. Skarns close the deposit. carbonate alteration Moderate Comments: Talc-carbonate alteration locally present in the footwall part of the cumulate body Metamorphic description: Type: Facies: Degree: Relation to mineralization: Regional greenschist low metamorphic metamorphic facies grade Min P- Max P (kbar) MIn T- Max T ( C) 6

7 Mineral Deposit Report Page 7 OF Geological age: Geological era: Paleoproterozoic ( Ma) Max age - Minage Inferred age (Ma): Age of mineralization: (Ma): N Graphite Schist (Host rock) Rock type: Host rock Proportion: present Grain size: Fine grained mm Color: References: 3 Comments: Elevated PGE and Ni also in sulphide-graphite schists in some samples, close to the contact with the olivine cumulate. Volcano-sedimentary association including carbonate, sulphide, and graphite bearing schists, komatiitic and less ultramafic lavas and smaller cumulate bodies. Metamorphic description: Ore minerals: Mineral Proportion Mineral texture Graphite present Dissemination, Vein Pyrrhotite present Dissemination, Vein Type: Facies: Degree: Relation to mineralization: Regional greenschist low metamorphic metamorphic facies grade Geological age: Min P- Max P (kbar) MIn T- Max T ( C) Geological era: Paleoproterozoic ( Ma) Max age - Minage Inferred age (Ma): Age of mineralization: (Ma): N Basaltic komatite (Wall rock) Rock type: Wall rock Proportion: present Grain size: Fine grained mm Comments: Amphibole-chlorite-serpentine altered komatiitic basalt flows and hyaloclastic units Other minerals: Mineral Proportion Mineral texture Amphibole major Biotite present Chlorite major Serpentine less than half 7

8 Mineral Deposit Report Page 8 OF 11 Figures Drill hole intersection DDM 407:

9 Mineral Deposit Report Page 9 OF Geological cross-section, cartoon: 9

10 Mineral Deposit Report Page 10 OF Lomalampi geological map: 10

11 Mineral Deposit Report Page 11 OF REFERENCES 1. Koistinen, Esko and Heikura, Pertti Mineral resource assesment and 3D modelling of the Lomalampi deposit, Sodankylä Finland. GTK, arkistoraportti M19/3723/2010/50 2. Konnunaho, J., Halkoaho, T., Hanski, E. & Törmänen, T Komatiite-hosted Ni-Cu-PGE deposits in Finland. In: Maier, W.D., Lahtinen, R. & O'Brien, H. (eds) Mineral deposits of Finland. Amsterdam: Elsevier, Räsänen, J., SANI-hankkeessa vuosina tehdyt geologiset tutkimukset. 28 s., 8 liites. Geologian tutkimuskeskus, arkistoraportti, K 21.42/2004/ Tömänen, T., Konnunaho, J.P., Hanski, E., Moilanen, M., & Heikura, P The Paleoproterozoic komatiite-hosted PGE mineralization at Lomalampi, Central Lapland Greenstone Belt, northern Finland. Mineralium Deposita, Törmänen, T., Heikura, P., Salmirinne, H The komatiite-hosted Lomalampi PGE-Ni-Cu-Au deposit, Northern Finland.. Mineral deposit report M19/3723/2010/ p. 11