The Spius Property is located in southwestern British Columbia and hosts a significant copper anomaly within an area of porphyry copper deposits. Historic soil and drilling data uncovered a large zone of anomalous copper values over 1 km in diameter that remains open. The property has good access and infrastructure. An initial program of geological mapping and soil sampling is recommended to further define the copper anomaly and evaluate the property's potential to host a significant porphyry copper-molybdenum deposit. The property is available for option, joint venture or purchase.

1. CHRIS PAUL
chris_paul001@hotmail.com
604-721-7896
SPIUS PROPERTY FACT SHEET – FEB 2016
COPPER-MOLY PORPHYRY - Merritt, BC
The Spius Property is located within BC’s Southern Quesnellia Terrane, which is host to
numerous significant porphyry deposits including Highland Valley Copper, Copper Mountain,
Prosperity, Afton, Ajax, Gibraltar, Mt Polley and Mt Milligan to name a few. Historic soil
sampling by Canadian Occidental Petroleum Ltd. uncovered an extremely anomalous zone of
Cu-in-soil up to 4640 ppm approximately 1 km in diameter and open in all directions (AR06145,
33913). Molybdenum up to 230 ppm occurs on the western flank of the copper anomaly. Historic
drilling at the time focused on the high Mo to the west and a chargeability anomaly but avoided
the bulk of the copper anomaly. The results of this drilling are not publicly available.
The Property has good forestry road access, with many new roads constructed since the previous
historical work programs. It is located in Southern BC, 40 km from the city of Merritt, with
excellent infrastructure for mine development including major rail, highways and grid power.
MIKE BLADY
mikeblady@gmail.com
604-720-3474
CONTACTS
*NOTICE - BC MINERAL CLAIMS MAY ONLY BE USED FOR MINERAL EXPLORATION

2. CHRIS PAUL
chris_paul001@hotmail.com
604-721-7896
CONTACTS
MIKE BLADY
mikeblady@gmail.com
604-720-3474
Location
The Property is located in southwestern British Columbia, at 49°55’17” N latitude and 121°16’05” W
longitude. The Property lies 40 km southwest of Merritt, along the eastern edge of the rugged Coast
Mountains. Elevations range from 800 to 1,940 masl. The claims cover a south facing slope overlooking
the upper Spius Creek, which empties into the Coldwater River. Most of the rock outcrop is limited to
the higher elevations and creek valleys. Depending on elevation, seasonal exploration surveys can
commence from about early April to mid-May and normally end by late October. Drilling can occur year
round.
Access
The Property is accessible by road from Merritt on the Coldwater Road heading SE, then by travelling
for another 35 km on the Patchett/Spius FSR. Alternatively, a helicopter can be chartered from Hope for
access.
Claims
The Property is comprised of 4 mineral tenures covering a total area of 1082 hectares, owned 25% by
Christopher R. Paul, 25% by Michael A Blady, 25% by John A Chapman and 25% by Gerald G. Carlson

3. CHRIS PAUL
chris_paul001@hotmail.com
604-721-7896
CONTACTS
MIKE BLADY
mikeblady@gmail.com
604-720-3474
Geology
The Spius Property is underlain by the Cretaceous Eagle Granodiorite, an elongate, northwest-trending
pluton. The main lithologies are foliated quartz diorite and granodiorite. These have been cut by a
presumably younger feldspar and quartz-feldspar porphyry phase and late stage felsic dikes, pegmatite,
quartz veins and minor lamprophyre. The Property is cut by a major northeast trending shear zone
which is evident in regional geology and magnetics maps.
Exploration History
• 1968 – Work by Orequest included soil geochemistry (Cu, Mo), geophysics (SP and EM survey), 5
percussion holes (1,000 ft.).
• 1969 – Murray Mines drilled 2,000 ft. of core in 10 holes.
• 1970 – Arrow International completed geological mapping, a soil geochemical survey and ground
geophysics (magnetometer, IP survey).
• 1971 – Orequest completed 2,300 ft. of percussion drilling in 7 holes.
• 1975 – Brascan drilled seven core holes.
• 1976 – Canadian Occidental completed a program of prospecting and soil sampling.

4. CHRIS PAUL
chris_paul001@hotmail.com
604-721-7896
CONTACTS
MIKE BLADY
mikeblady@gmail.com
604-720-3474
Mineralization/Alteration
Propylitic alteration with extensive pyrite is pervasive throughout the Property, while widespread quartz-
sericite-pyrite alteration occurs with malachite and chalcopyrite within the undrilled central portion of the
property (AR06145). Extremely kaolinized, highly friable exposures are also reported from the central zone
(AR06145). Better mineralization is observed to be associated with k-feldspar+quartz veining (AR05389).
Initial soil sampling surveys outlined an area approximately 2000’ x 1500’ of >500 ppm Cu surrounding an
area 2000’ x 400’ of >1000 ppm Cu (AR 06145). Spotty anomalous Mo values up to 230 ppm occur within this
anomaly. Gold/silver was not analysed in this program. The copper anomaly is open to the south and east and
possibly also to the west and northwest. A single line of soil samples collected by J. Shearer (AR 33913),
extended the historical anomaly 500 m southeast of previous sampling, with values ranging from 150 ppm Cu
to 4,640 ppm Cu (most values >500 ppm Cu).
Potential
There is excellent potential for the discovery of a significant Cu-Mo porphyry deposit on the Property. It
appears that early drilling focused mainly on IP anomalies, rather than geology and geochemistry, which
were likely a response to the widespread pyrite that surrounds the central copper anomaly. The historical
and more recent soil geochemistry shows the strong and large central copper anomaly is associated with
intense phyllic and argillic alteration. Most of the historic drilling is on the periphery of this anomaly.

5. CHRIS PAUL
chris_paul001@hotmail.com
604-721-7896
MIKE BLADY
mikeblady@gmail.com
604-720-3474
Recommended Program
An initial program of geological mapping and geochemical soil sampling with a complete multi-element
analysis is recommended for a first phase of work on Spius. The aim of the geochemical survey would
be to confirm the historical values, test for other elementals and extend the current Cu-Mo anomaly
which is wide open. Geological mapping should be focused on defining the various intrusive phases
and their alteration assemblages, as well as structural mapping. Previous operators have noted that NE-
trending shear zones may be an important control on the mineralization.
In addition to the porphyry style mineralization at Spius, some of the highest scandium (Sc) assays for
the entire province occur in RGS stream sediment samples surrounding the Property. The scandium
may be hosted within local pegmatite intrusions, which have been mapped by previous operators, or
may be associated with the porphyry mineralization itself. Lithogeochemical sampling of the numerous
pegmatite and porphyry phases is recommended to help pinpoint the source(s) of anomalous scandium.
A second phase of work would involve geophysics, trenching and potentially core drilling.
Outlook
The Spius porphyry copper-molybdenum porphyry property is currently available for option, joint
venture or purchase. For more information please contact the owners listed below.
CONTACTS
*NOTICE - BC MINERAL CLAIMS MAY ONLY BE USED FOR MINERAL EXPLORATION