The Columbia Belle (Rift) Property is located in the Big Bend area of the northern Selkirk Mountains of southeastern British Columbia, approximately 100 kilometres north of Revelstoke and 12 kilometres south of Mica on the east side of Revelstoke Lake reservoir (Columbia River). The property is located on NTS map sheet 82M/15 and centered at latitude 51°53'N and longitude 118°35'W. It is comprised of 24 contiguous mineral claims covering 11,349.75 hectares. Goldstar Minerals Inc., a private company registered in British Columbia, has optioned the Columbia Belle property from the claim owners, KGE Management Ltd. (held on behalf of KGE by Gerald G. Carlson) and John A. Chapman. D.G. MacIntyre & Associates Ltd. has been retained by the management of Goldstar to examine the geological setting and results of historical work on the Columbia Belle (formerly Rift) property in order to prepare an independent technical report on the project that can be used in support of Goldstar’s application to become listed on TSX-V exchange. Goldstars’s Columbia Belle property covers the former Rift massive sulphide showings although the subsurface base metal rights to these showings reside with surface rights held by Beaumont Timber. Previous chip sampling of the Rift massive sulphide has averaged 29.74% Zn and 5.38% Pb over an average thickness of 0.95m. Two samples collected by the author confirm these high grades. One of the holes drilled by E&B Explorations in 1985, which was collared east of the Rift showing and outside of Beaumont’s land holdings and base metal rights, intersected 1.82 metres averaging 22.21% zinc and 4.82% lead. Together these showings and drill hole intersections indicate the early Paleozoic metasedimentary rocks exposed on the Columbia Belle property host significant strataform zinc and lead massive sulphide mineralization. The inferred shallow marine depositional environment and style and tenor of mineralization suggest the occurrences are of the sedimentary-exhalative (SEDEX) type. The host rocks are probably part of the Index Formation which is known to host other important massive sulphide deposits in the Big Bend area. In August 2010, Goldstar Minerals contracted Geotech Ltd. to fly a helicopter borne Versatile Time Domain Electromagnetic (VTEM) and Magnetometer survey over the property. This work defined a southeast trending conductive area in the central part of the claim block. In early September the author and a two-person sampling crew under the direction of Craig Lynes of Rich River Exploration did geologic mapping, prospecting and soil, silt and rock geochemical sampling in the area covered by this anomaly. This work failed to locate any new showings or produce any significant soil anomalies that correspond with the area of elevated conductivity as defined by the VTEM survey. The anomaly appears to coincide with a moderately southwest dipping sequence of rusty weathering pelitic schists T

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Targets The target at Columbia Belle is a high grade zinc (+20%), lead (+4%) and silver stratiform massive
sulphide deposit. The property also has potential for quarrying of limestone.
Description The Columbia Belle (Rift) property is a SEDEX Zn-Pb-Ag prospect discovered in August 1980 on
Rift Creek adjacent to Highway 23 near its confluence with the Columbia River, 10 km south of
Mica Dam. The stratabound massive sulfide discovery showing, located 800 m asl, assayed 30%
zinc and 7% lead over 0.8 m. Several other massive sulphide occurrences have been subsequently
discovered within a 400 m thick unit of metasedimentary and metavolcanic rocks that are bounded
by marble units and are intruded by sills and dykes of porphyritic quartz monzonite. The best
intersection from a 5 hole, 1985 drill program included 1.82 m of high-grade sulfides (22% zinc,
5% lead) at a point approximately 400 m east of the original discovery.
The Property is located in the northern Selkirk Mountains in southeastern British Columbia, some
150 km north of the town of Revelstoke. The region is well serviced by grid electric power,
mainline logging roads and Revelstoke with service shops for welding, electrical, machining and
heavy equipment maintenance as well as a 1,460 m paved runway at the airport. The property is
located on NTS map sheet 082M15 and centered at latitude 51°53'N and longitude 118°35'W
(390344E, 5749684N UTM, NAD83 Zone 11). Logging roads provide access to much of the
Property.
The Property is located 30 km north of the Goldstream mine (VMS deposit), and 27 km northeast
of the Ruddock Creek SEDEX deposit, within a zone of highest ranking for mineral discovery
potential by the British Columbia Geological Survey.
Access The resource and transportation hub city of Revelstoke (population ~7,200) is on the CPR mainline
and on Trans-Canada Highway No. 1, about 6 hours driving time (640 km) east of Vancouver,
British Columbia. Access to the eastern part of the property is via paved Highway 23, 150 km
north of Revelstoke. From here, B.C. Hydro access roads and private logging roads owned by
Beaumont Timber Co. Ltd. (“Beaumont”), Louisiana-Pacific Canada Ltd. (“Louisiana-Pacific”)
and Revelstoke Community Forest Corporation extend eastward into the central part of the
Property and the area of the Rift showing. Access to the southern part of the Property is via the
Bigmouth Forest Service Road which crosses Bigmouth Creek at 6.5 km and at 7.4 km and which
connects to a network of active logging roads north of the creek.
Land
Ownership
The Property consists of eleven BCMTO mineral tenures covering 5,389 ha, owned by John A.
Chapman (50%) and Gerald G. Carlson on behalf of KGE Management Ltd. (50%). The Columbia
Belle Property is available for Option. Beaumont owns base metal rights to a small portion of the
Property along the east side of the Columbia River, including the original Rift showing area.
Area
History
 1980: E&B Explorations, Inc. (“E&B”) discovered the Rift massive sulphide occurrence
during a reconnaissance prospecting program. By 1981, E&B had staked 749 claims.
 1981-1985: E&B carried out grid based exploration including soil sampling, a
magnetometer survey, mapping, prospecting and five drill holes. Best intersection was
27% Zn+Pb over 1.8 m. One of the holes intersected the massive sulphide horizon to the
east of the Beaumont tenure boundary.
 Mid 1980’s: Beaumont discovered several more massive sulfide occurrences and
completed a diamond drilling program. Results have not been released.
 1990: Corona Corp. drilled one hole east of the showing area.
 1999: Orphan Boy Resources Inc. completed a rock and soil sampling program,
magnetometer survey, mapping and prospecting, confirming the earlier massive sulphide
discoveries and discovered the new Roe massive sulphide occurrence with anomalous
silver (2.5 ppm) and copper (800 ppm).
 2010: The Property was acquired by John Chapman and Gerald G. Carlson who

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subsequently significantly expanded the claim block by staking.
 2010: The Property was optioned to Goldstar Minerals Inc. (“Goldstar”) who contracted
Geotech Ltd. to fly a property-wide, low level airborne VTEM electromagnetic and
magnetic survey. Later in the year, soil sampling and prospecting were carried out over
select VTEM targets. Subsequent work has suggested that VTEM was not a good choice as
the massive sulphide horizon does not appear to be a strong conductor, while the major
EM anomaly detected appears to have been caused by graphite-bearing sediments (see drill
results, next bullet).
 2011: Goldstar carried out a small grid soil geochemical survey followed by drilling of
503.5 m of core in two holes, testing one of the conductors identified by the VTEM survey.
The drill holes cut thick sections of quartz-biotite schist, marble, quartz-muscovite schist
and a 16m thick sub-vertical graphitic rich fault/breccia zone. No significant base metal or
precious metal mineralization was intersected in the drilling. However, the graphite-rich
fault/breccia zone encountered in DDH CB11-001 does explain in part the thin conductive
anomaly from the VTEM survey.
Geology The Big Bend area of the northern Selkirk Mountains is part of the eastern margin of the Omineca
Tectonic Belt, situated between the fold and thrust-fault belt of the southern Canadian Rockies on
the east and the Horsethief Creek Group and Shuswap Metamorphic Complex to the west. The area
is underlain by strongly deformed Neoproterozoic to Late Paleozoic metasedimentary and
metavolcanic rocks of the Kootenay Terrane which have been intruded by a number of granitic
plutons. The Shuswap and Monashee Complex is separated from the rocks of the Big Bend area by
the east dipping Columbia River fault zone, a major extensional fault of Eocene age.
The geology of the Rift property has been mapped by Gibson (1981, 1982 and 1983), Gibson and
Höy (1985), Hicks (1982), Bellamy (1990) and Payne (1999). The Rift Zn-Pb occurrence has been
shown to be underlain by a generally northeasterly striking, shallow to moderate southeasterly
dipping, isoclinally deformed sequence of metavolcanic and metasedimentary rocks of the Lower

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Cambrian, Lardeau Group. A distinctive marble unit of the Badshot Formation or lower Lardeau
Group has been traced northerly from the Goldstream River area (Logan and Colpron, 1995).
These host rocks are part of the Selkirk Allochthon and are situated in the hangingwall of the
Columbia River fault system.
The massive sulphide horizon was mapped as part of a 400 metre thick, largely schistose interval
of the Lardeau Group. Porphyritic K-feldspar-garnet-biotite quartz monzonite has intruded the
metasedimentary rocks as sills, dykes and <10cm layer-parallel, anastomosing lenses.
Approximately 100m upslope from the sulphide layer is a 15m thick sheared ultramafic body.
Mineral-
ization
The British Columbia Geological Survey Branch ranks the Big Bend region among the top ten
percent in the province for metallic and industrial mineral deposit discovery potential.
The Rift showing consists of a number of layers of massive sphalerite, pyrite, pyrrhotite, and
galena with traces of chalcopyrite, arsenopyrite, marcasite and hematite and is exposed on surface
for some 25m of strike length. The massive sulphide layer is up to 2m thick; mapping and
sampling by Hicks (1982) suggests an average width of less than a metre. The main Rift showing
was chip sampled by Hicks (1982) with 25 samples from the massive sulphide averaging 29.74%
Zn and 5.28% Pb over an average width of 0.95m (Payne, 1999). A number of thin discontinuous
massive sulphide lenses, separated by country rock with disseminated sulphides occur in the
immediate 2-3m of footwall rocks (Gibson and Höy, 1985). Sampling of the footwall by Hicks
(1982) gave a weighted average grade of 3.11% Zn, 0.48% Pb, and 0.01% Cu. A second massive
sulphide zone, called the 'upper showing' by Hicks (1982), is exposed approximately 90m
stratigraphically above the main Rift creek showing. During the 1999 field program, 34 rock
samples were collected from the property which confirm reported zinc and lead values from the
1980 to 1985 rock sampling. The Roe showing consists of siliceous banded massive iron sulphide
with anomalous copper and silver values.
Potential The Columbia Belle has demonstrated high grade of zinc-lead massive sulphide mineralization
observed on surface and in drill holes over a relatively small area. Geological mapping has shown
that the favourable horizon potentially extends through a large portion of the property. Massive
sulphide mineralization of this type can typically occur over a large areal extent, deposits often
occur in clusters, and in deformed rocks such as these, the best deposits often occur in the nose of
folds, where the strata have been significantly thickened.
Recom-
mended
Explor-
ation
The best prospecting tools are detailed geological mapping and soil sampling, followed by drilling.
The mapping and sampling have already been carried out over the main showing area, but should
be expanded to cover the area to the east and northeast of the main Rift showing area. The
extension of the main mineralized zone to the east is ready for drill testing from the area of a recent
clear cut by Louisiana-Pacific.
Status The Columbia Belle property is available for option. Contact John A. Chapman at 604.612.9438
(jacms1@telus.net) or Gerald G. Carlson at 604.816.3012 (gerrycarlson@gmail.com).
Selected Recent References
Payne, Craig W, 2002, Summary Report on the Rift Property, prepared for Orphan Boy Resources Inc.
MacIntyre, Don, 2010, Technical Report: Columbia Belle Zn‐Pb Property, prepared for Goldstar Minerals Inc.
Payne, Craig W., 2012, Assessment Report: 2011 Soil Geochemical and Core Drilling Report, prepared for
Goldstar Minerals Inc.

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Google Earth image of Columbia Belle property showing the Columbia River and Mica Dam in the background.

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