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Makola-Hitura Nickel Area

The second nickel mine to be developed in Finland after Petsamo (Pechenga) was the Makola Mine in 1939 at the NW end of the Central Ore Belt. The discovery was a classic example of the use of ore boulder tracing combined with ground magnetic & EM surveys. Makola, along with nearby Hitura Mine, which is still in production, is closely associated with partially differentiated ultramafics which intrude highly metamorphosed Mid-Proterozoic mica schists, graphitic siliceous, sulfide-bearing schists, and gneisses. Nickel and copper mineralization in the area is also known from ultramafic phases of some larger mafic intrusion. The Kalajoki River drainage system, which covers a large portion of the area, comprises glacial clay deposits up to 10 meters thick that has hampered the effectiveness of EM surveys.

The Makola Mine was in production from 1941 to 1952 yielding 0.41million tons. Since 1964, the nearby Hitura mine, located 4 km NE of Makola, has produced 14 million tons of ore grading 0.8 - 1% combined Cu-Ni.

Magnus Minerals holds claims over the Makola Mine and has claims pending over 4 other nickel deposits as well several reservations over potential ultramafic intrusions in the area.







Makola Mine

Quick Facts:


  • Ni-Cu-Co deposit
  • 4 km from active Hitura Mine (production to-date 12.3 Mt@0.59% Ni, 0.2 Cu)
  • Mined in open pit and underground from 1941 to 1952
  • Exploration drilling indicated 1.2 to 1.4 Mt of 0.8% Ni & 0.45% Cu
  • Outokumpu mined 0.41 Mt grading 0.81% Ni & 0.45% Cu to 160m level
  • Remaining resources of 0.6 Mt possible and open at depth below 200m

Exploration History

The area has seen intermittent exploration by GTK and OKU since discovery of Makola Mine in 1939, however, extensive conductive overburden up to 20m deep and ‘black schists’ hamper geophysical interpretation. Very limited exploration has been done to explore for the additional ore at Makola, either at depth or in the immediate vicinity of the main mass serpentinite.

The Makola ore body is an inverted cone, reaching from surface to about the 200m level. Some satellite lenses and lower grade material occur outside the main ore. The ore is predominantly net-textured to disseminated sulfides in serpentinite (altered dunite) at the NE flank of a 700m long ultramafic body.

Although the average grade of the ore was 0.8% Ni and 0.45% Cu, portions of the ore zones assayed 1.5 to 2.3% Ni and 0.5 to 0.9% Cu over several meters. Waste rock from collapsed open pit material may have added to dilution in many of the upper level stopes.

Potential

Preliminary compilation of all existing data, including modeling of the original ore as determined by underground drilling and of the workings based on recently acquired level plans and sections, indicate potential for some ore remaining at Makola Mine to the 200m level.  In addition, some parallel zones detected in the drilling appear to have not been further explored since.

Additional potential exists at depth below the mine workings as well as several targets indicated by high-resolution magnetic surveys conducted recently by Magnus.



Other Nickel Deposits

Magnus has claim applications over 4 known nickel deposits in the area. They are Kusiaiskallio, Jakonmutka, Pitkäneva, and Ainaslampi.

At Kusiaiskallio, drilling by Outokumpu (6 holes), along three sections spaced 150m apart and totalling 1,987 m yielded a drill-indicated resource of 798,000t of 0.22 % Ni, 0.14% Cu (from bedrock surface to 150m). Although average grades are low, some higher-grade zones are also present (e.g. 6.3m of 0.45% Ni, 0.25% Cu). A large part of the 500m long mafic intrusion remains untested and uncertainty exists on the geometry of the mineralization.

At Jakonmutka, nickel mineralization has been intersected in 9 scattered drill holes put down in past exploration on two small serpentinite bodies located 1.7 km N of the Hitura Mine. Geophysical borehole surveys by Outokumpu indicated an un-tested, strong conductor at a depth of some 400m below surface.

Low-grade nickel mineralization within a circular serpentinite intruding sulfidic siliceous schists, similar to Hitura is widespread at Pitkäneva, located 2.5 km SW of Makola Mine. A drill-indicated resource of some 2 million tons of low-grade nickel on bedrock surface is reported.

Approximately 1km SW of Pitkäneva, limited drilling has indicated nickel mineralization in similar rocks at Ainaslampi.
      

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