
BIRD RIVER AREA REGIONAL COMPILATION
BIRD RIVER DRILLING
PAGE ZONE, LONGITUDINAL SECTION
In March 2005, North American Palladium Ltd. entered
into an Option Joint Venture Agreement with Gossan
Resources Ltd. to earn up to a 75% interest in
Gossan�s Bird River Project, located 40 kilometres
east of Lac du Bonnet, in southeastern Manitoba.
North American Palladium Ltd. can earn an initial
50% interest in the property by incurring work
expenditures of $2.5 million and cash payments
totaling $400,000 to Gossan by August 30, 2008.
North American Palladium can elect to increase its
interest a further 15% by completing a bankable
feasibility study and an additional 10% interest, by
arranging project financing.
The Bird River Property encompasses approximately
6,800 hectares and covers over 21 kilometres of the
Bird River Sill Complex. This is a layered
intrusive complex, averaging 1,000 metres in
thickness and consisting of a lower layered
ultramafic series and an upper gabbroic series. The
Bird River Sill was intruded along the contact of
the Lamprey Falls (meta-basalt) and Bernic River
(meta-conglomerate) formation of the Archean Rice
Lake Greenstone Belt.
The Bird River Sill hosts significant occurrences of
magmatic sulphides (Ni, Cu, and PGM) including the
past producing Dumbarton and Maskwa Deposits. Most
of these magmatic sulphide prospects occur at or
near the basal contact zone of the layered
ultramafic series or within adjoining iron
formation/mafic meta-volcanics.
The principle exploration target is for semi-massive
to massive sulphide (Ni, Cu, and PGM) deposits along
the lower contact zone of the Bird River Sill.
In June-July of this year North American Palladium carried out a short diamond
drill program consisting of eight (8) holes,
B5-05-01 to 08 (hole BR-05-03a had to be abandoned
in overburden) totaling 967.7 meters. Drilling
tested seven (7) airborne electromagnetic
conductors, identified from the Airborne VTEM Survey
flown earlier this year by North American Palladium,
along the inferred base of the Bird River Sill. Four
of the eight holes encountered significant sulphide
mineralization highlighted by hole BR-05-02 that
intersected 13.75 meters of 1.077% Ni and 0.501% Cu
including 4.75 meters grading 2.143% Ni and 0.440%
Cu.