QCYR aquires property from PIGCO
March 8, 2004
Quincy Resources Acquires Millers Project, Esmeralda County, NV
Carson City, Nevada -- Quincy Resources Inc. (OTCBB - QCYR) is pleased to announce the acquisition
of the Millers project located in the Walker Lane of central Nevada. The Millers property consists of 21
unpatented lode claims located in Esmeralda County, Nevada that have been leased from Pacific
Intermountain Gold Corporation (PIGCO). PIGCO is a 75% owned subsidiary of Seabridge Gold
Corporation (CDNX-SEA); Platoro West Incorporated, a privately held Nevada corporation, owns the
minority 25% of PIGCO. Quincy has paid an initial consideration of $5,000 advance royalty for the first
12 months and must complete a $20,000 work commitment. The lease agreement calls for escalating
yearly advance royalty payments, escalating work commitments, and a sliding scale NSR ranging from
2% for gold prices under $300.00/oz to 5% for gold prices in excess of $500.00/oz.
Quincy’s interest in the property centers on a large chalcedonic vein that has been traced along surface for
more than a mile. This vein ranges from 5 to more than 30 feet in width and displays classic high level,
low temperature quartz textures. Calcite veining accompanies the chalcedony locally and in select vein
segments is dominant. The main vein is the largest of at least 5 parallel to sub-parallel veins occurring in
a broad vein zone measuring up to 400 feet in width. The veins cut a number of rock types including a
Jurassic granite and sediments and metasediments of Cambrian age intruded by and partially covered by a
variety of Tertiary rhyolitic intrusives and volcanics.
A number of small prospects dating to the late 1800s are found throughout the area. Dickenson-Nevada
held the property in the late 1980s and conducted extensive soil sampling which identified a rather large
anomalous area in excess of one mile in length. Six holes totaling 2470 feet were drilled ranging from 355
to 505 feet in depth. Although the anomalies were targeted, the ve in characteristic of the chalcedony was
not clearly recognized explaining why the veins were only intersected in two holes. Hole MS-1
intersected the quartz veining at about 115 feet with a high assay of .03 opt. Hole MS-2 hit a 40 foot thick
zone of chalc edonic veining at 160-200 feet which ran .01 opt. Based upon the field observations of the
texture of the veining, the boiling zone is likely to be 300-700 feet below the surface. The boiling zone
would be the preferred target for bonanza style mineralization. It is significant to note that there is not a
single vein trending N-S as suggested by some of the existing data but rather there is a zone on enechelon
high-level epithermal veins each of which trends to the NNE. The existence of multiple veins, the
length of the vein zone being well in excess of 5000 feet along strike, the evidence of multiple phase
Tertiary igneous activity, the lack of modern exploration, along with the untested pediment potential are
all positive indicators suggesting the potential of bonanza style epithermal mineralization at depth. The
regional setting of Millers with respect to the Walker Lane, the nearby Castle -Black Rock deposit, and the
Midway-Tonopah area further the attractiveness of this project.
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Quincy Resources Inc. has assembled a select portfolio of advanced vein projects in the major gold
producing areas of Nevada and adjacent states along with a distinguished technical team providing its
shareholders with maximum exposure to potential high grade gold and silver discoveries within Nevada,
Oregon and Idaho.
For further information please see our website at www.quincyresources.com or contact:
Dan Farrell, President and C.E.O.
T: 416-540-6436
E: dfarrell@quincyresources.com
Information Regarding Forward-Looking Statements: Except for historical information contained herein, the statements in
this Press Release are forward-looking statements that are made pursuant to the safe harbor provisions in the Private Securities
Legislation Reform Act of 1995. Forward-looking settlements involve known and unknown risks and uncertainties, which may
cause Quincy’s actual results in future periods to differ materially from forecasted results. These risks and uncertainties include,
among other things: volatility of natural resource prices; product demand; market competition; and risks inherent in Quincy’s
operations. These and other risks are described in the Company’s Annual Report or Form 10-K and other filings with the
Securities and Exchange Commission.