The document summarizes exploration work done on the Major Hart property, which contains a pluton that shows highly anomalous stream sediment geochemistry indicative of a rare-element granite. Several key points are made: 1) Stream samples from the property contain anomalies of rare earth elements, tin, tantalum, and tungsten that are amongst the highest levels in BC. 2) The pluton shares similar geochemistry with deposits elsewhere that contain rare earth element pegmatites and tin mines. 3) Distal dykes from the pluton are associated with high-grade gold veins, and the property has potential for contact-related gold and emerald deposits. 4) The property

1. Major Hart Project Salient Point Summary
No detailed exploration has been done on property. BCGS RGS stream sampling and
GSC regional mapping at 1:50,000 scale are the only previously recorded work.
The Major Hart Pluton had an extremely evolved, fractionated source melt demonstrated
by rubidium and fluorine anomalies, and “alaskite” composition. Abundant fluorite was
noted at the contact with the ultramafics, readily visible from horseback (H. Gabrielse,
personal communication 2010). The rubidium RGS stream results are some of the highest
in the province of B.C., and constitute the most localized single cluster of significant size.
The stream geochemistry is indicative of a specialty, or “tin-type” granite. It should be
noted the Tanco Mine, Manitoba was found while investigating the area for tin potential.
Tantalum stream sample results are 5 times stronger than surrounding the Fir-Verity area.
Of the 7 samples comprising the Major Hart anomaly cluster, 7 are >99th percentile for
Bismuth, Lutetium, Rubidium, Tantalum & Tungsten; 6 are >99th percentile for Fluorine in
water; 5 are >99th percentile for Ytterbium, and 4 are >99th percentile for Cesium & Hafnium
in comparison to the B.C. provincial RSG stream sample database. The partial rare earth
element results to date indicate a propensity towards the more valuable heavy rare earths.
The pluton has similar stream sediment geochemistry to the Surprise Lake Batholith
(Ruby Creek mine, 115 Minfile showings), Glunderberry Batholith (Swan), Ash
Mountain, and Storie Moly areas. A linear trend is evident through these areas, ending at
the Major Hart Pluton.
The closest match to the tenor of the anomalous stream samples in the Canadian
Cordillera is the O’Grady Batholith, NWT, which contains a 10 km long elbaite-type,
rare-element pegmatite, up to 1 km wide, at the head of the anomalous drainages. It is
located 100 km NW of Tungsten, NWT. The pegmatite was discovered while researching
anomalous stream samples with potential pegmatite indicator elements. The stream
samples at the O’Grady area contain lower level anomalies than the Major Hart area.
The stream sample anomaly cluster is very well constrained. The northern contact of the
Major Hart Pluton with the enclosing rocks is at the head of all of the anomalous source
drainages, although the rest of the pluton’s drainages are still elevated in the elements
associated with fractionated granites.
The Major Hart Pluton is situated at the crossroads of Slide Mountain Terrane, Ancestral
North America, and Dorsey Assemblage. The regional structure present is sufficient to
have allowed the pluton to tap a considerable volume of melt, possibly including a mantle
component. Since the pluton is the only Eocene intrusion within 120 km, the volatile
phase of the melt may have had a considerable volume of rock/melt from which to
concentrate the incompatible elements.
The anomalous stream drainage trend, and coincident pluton-host contact zone is
over 10 km long.

2. Distal dykes and probable outliers of the Major Hart pluton have a strong association
with gold at Nizi and Yursi vein showings, and probably underlie Beale Lake system, 15
to 20 km from exposed pluton. Gold is associated with bismuth-tungsten anomalies,
especially in the Beale Lake area. At the Nizi showing, historical channel samples of the
Discovery vein returned the following selected near-surface high-grade values: 27.09
grams per tonne gold and 1,220.6 grams per tonne per tonne silver over two metres;
15.09 grams per tonne gold and 1,073.2 grams per tonne silver over 3.5 metres and 8.91
grams per tonne gold and 596.6 grams per tonne silver over one metre (British Columbia
Geological Branch Assessment Report 22840). Strong bismuth and tungsten anomalies
are noted in the Major Hart anomaly cluster.
The contact of the pluton with the Slide Mountain ultramafic rocks may have ophilite-
hosted gold potential.
There may be emerald potential where volatile flux-rich fluids may have mixed with
chrome-rich rocks. Emeralds are known in the Yukon in a similar environment.
Beryllium has never been analysed for in the Major hart area.
The area of the three-way contact with Slide Mountain ultramafics, Slide Mountain
volcanics and sediments, and the Major Hart Pluton likely has the strongest structural
preparation for the development of lode ore zones. Air photo analysis shows parallel
(bedded) structures in the area mapped as volcanics, at the contact.
The emplacement of the pluton is contemporaneous with up to 450 km of dextral
movement along the northwest trending Ketichka Fault. The outlying dykes to the
northwest, regional northwest trending faults, northwest alignment of host rock contacts,
and northwest position of correlated volcanics (Nizi) suggest a possible northwest
position of the apex of the Major Hart Pluton is likely. This may have resulted in the bulk
of the roof of the pluton being preserved at present. The roof of a specialty granite
intrusion is where the highest degree of concentration of volatile and incompatible
elements is concentrated during emplacement. Tin griesens, pegmatites, rare elements,
and rare earth element concentrations are most commonly located in the immediate
vicinity of the apex and thermal areole of the most fractionated granites.
The anomalous area is currently 95% contained within the claim area. The main area of
interest is 100% contained within mineral claims held by the joint owners, not a
checkerboard of disparate owners and interests.
The Major Hart Property is the most likely place in B.C. to host a brand new discovery of
real significance, in our opinion. This is not a promotional gimmick, a tag-on play, or
closeology maybe. This is the real deal, with real potential for something really big,
really new and truly different from the rest of properties out there currently. It is a freak
of nature…… and that is what mines are made of.