ylylahti Copper Oy Distribution: Ministry of Trade and Industry 2 copies Kylylahti Copper Oy, Outokumpu 1 copy Vulcan Resources Ltd, Perth 1 copy

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1 K ylylahti Copper Oy Kummunkatu Outokumpu, Finland Facsimile: Distribution: Ministry of Trade and Industry 2 copies Kylylahti Copper Oy, Outokumpu 1 copy Vulcan Resources Ltd, Perth 1 copy Mineral Exploration Report on the Work carried out on Claims Tornio 1-12, Tornio Location of Claims Tornio 1 12 Key words: platinum-group elements, gabbro, layered intrusion A wholly owned subsidiary of Vulcan Resources Limited (ABN ) Ground Floor, 1 Altona Street, West Perth WA 6005, Australia Tel: Facsimile: Web:

2 Introduction This report describes PGE exploration work carried out on claims Tornio 1-12, which were granted to Polar Mining Oy on February 16, In 2005 all claims were transferred to Kylylahti Copper Oy, which after the initial testing of PGE potential on the claims decided not to carry out any further work on the property, and all Tornio claims were relinquished on October 27, Location Claims Tornio 1-12 are located in the City of Tornio, northwestern Finland (figure 1.). Co-ordinates for the claims are presented in table 1. Table 1. Claim locations Claim # Name Claim mid-points Northing (mn) Easting (me) 7677/1 Tornio /2 Tornio /3 Tornio /4 Tornio /5 Tornio /6 Tornio /7 Tornio /8 Tornio /9 Tornio /10 Tornio /11 Tornio /12 Tornio Co-ordinate system and survey methods Co-ordinate system and projection applied to all information in this report and appended digital data is Finnish KKJ Zone 2. Personnel Mr. Jarmo Vesanto (MSc, Geology) has been in charge of all work carried out on the property. Mr. Jani Impola (MSc, Geology) has supervised all field activities. Geology The Tornio intrusion is part of the 2440 Ma age belt of layered intrusion complexes of Tornio Näränkävaara representing the westernmost known layered intrusion of that age in the Fennoscandian shield (J. Lahtinen, 2003). The Tornio-Näränkävaara belt intrusions can be divided into two categories based on the magma composition: Cr-Mg poor (tholeiitic) and Cr-Mg -rich (boninitic) types. Cr Mg rich represents the lower and Cr Mg poor the upper parts of intrusions.

3 General structures within these units are roughly similar, the lower part is composed of ultramafic cumulates, pyroxenites and peridotites and the upper part is composed of gabbroic and anorthositic cumulates (J. Lahtinen, 2003). The most significant geochemical marker horizon in layered complexes in a matter of PGE potential is the level, where the transition from the Cr-Mg rich to the Cr-Mg poor type takes place. These marker horizons host the well known SJ and SK reefs of the Suhanko - Konttijärvi intrusion (J. Lahtinen, 2003). Structurally the Tornio intrusion is located around an ellipsoidal shaped Archaean basement dome (figure 2.). The northern border of the intrusion dips to N NE and the southern to S SW (J. Lahtinen, 2003). The Tornio intrusion is poorly known and the geological interpretation of layering and outlines of the intrusion are mainly based on magnetic and gravimetric data. The amount of bedrock outcrops and drilling is very limited. Drilling completed by Outokumpu in late 1970 s to early 1980 s showed the presence of the lower high Cr Mg part of the layered intrusion, but the possibility for the upper low Cr Mg portion is poorly known and therefore also the potential for PGE mineralisation related to the transition zone between these types (J. Lahtinen, 2003).

4 Figure 2. Simplified geological map of the Tornio layered intrusion showing Kylylahti Copper`s claims in black and the area of Kylylahti`s exploration activities in white. Claim rationale Most of intrusion complexes of the Fennoscandian Province include at least some kind of PGE mineralization and at least some degree of PGE mineralization is typical for the most layered complexes of this style (J. Lahtinen, 2003). PGE reef type mineralization can be expected to occur both at the base and within the fully untested upper stratigraphic portion of the Tornio intrusion. The lowermost

5 stratigraphic units drilled for chromite can be correlated with the chromium-rich magma pulses of the Penikat intrusion. Significant PGE reefs of the Penikat intrusion are located on the boundary between Cr-rich and Cr-poor magma pulses (SJ Reef), and within the Cr- poor magma pulse (AP- and PV-Reefs). Work carried out Previous work The initial work carried out on the Tornio layered intrusion was focused on chromite exploration. Outokumpu`s exploration programme in late 1970`s and early 1980`s lead by geologists Osmo Inkinen and Krister Söderholm returned several narrow chromitite seams related to ultramafic rocks within the lower parts of the intrusion. A total of 12 holes were drilled at that time. Potential for PGE (platinum group elements) was studied by Jarmo Lahtinen of Outokumpu Mining Oy by re-assaying the chromitite intersections drilled in early 1980 s. This work returned low PGE values (<0.5 ppm) related to chromitites. Other work carried out in the area include low altitude geophysical survey completed by the Geological Survey of Finland (GTK), gravimetric survey by Outokumpu and national geochemical till sampling (density of 1 sample / 4 sq km) by the GTK. Kylylahti Copper`s work in 2006 Ground magnetic survey A total of 4.5 line kms of ground magnetic surveys were completed in June The program comprised four traverses over the interpreted transition zone between the lower and upper parts of the layered intrusion (figure 3.). Lithogeochemical drilling program A total of seven holes and 185,20 meters of T-56 coring were drilled by Geopale Oy in August 2006 (table 2 and figures 3 and 4). Table 2. Tornio drilling in August 2006 by Kylylahti Copper Oy. HOLEID TOR/KO-1 TOR/KO-2 TOR/KO-3 TOR/KO-4 TOR/KO-5 TOR/KO-6 TOR/KO-7 EASTING NORTHING LENGTH_m AZIMUTH STARTING_DIP

6 Results The ground magnetic survey was planned to locate the contacts of magnetic anomalies representing possible stratigraphic positions of PGE reefs. All anomalies known from historic magnetic data were located at 10 meter accuracy and the survey proved that the old ground magnetic data was accurate. The main target for the lithogeochemical drilling programme was to explore the magnetic anomaly northeast from the known ultramafics representing the lower, high Cr Mg part of the intrusion (figure 3). The source for this magnetic horizon turned out to be felsic, weakly banded and porphyric rock instead of peridotitic layer representing the lowermost part of the tholeitic upper portion of the intrusion. Four holes (KO-2 KO-5) west from the first hole are comprised of weakly sheared and coarse grained (leuco-) gabbros (figure 4.). Two holes drilled east from the first hole intersected weakly sheared mafic volcanic rocks. Figure 3. Ground magnetic survey traverses on top of magnetic image. Drill hole collars are shown as white dots and labels.

7 Figure 4. Cross section of diamond drill section, holes TOR/KO-1-7 with the magnetic data. Digital database Digital database appended to this report includes the report text and the results of all work carried out on the property during the validity period of the claims. Conclusions The work carried out showed that the targeted area does not represent the prospective part of layered intrusion for PGE mineralization and therefore Kylylahti Copper Oy decided to relinquish the claims Tornio References J. Lahtinen, 2003; Tornio intrusion, untested potential for PGE mineralisation, Status report. Unpublished internal report of Outokumpu Mining Oy. KYLYLAHTI COPPER OY Jani Impola

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