Trailbreaker Defines a 10 Km Copper-IN-Soil Anomaly and Assays 23.71% Copper IN ROCK Sample at Liberty Property
TRAILBREAKER DEFINES A 10 KM COPPER-IN-SOIL ANOMALY AND ASSAYS 23.71% COPPER IN
ROCK SAMPLE AT LIBERTY PROPERTY
September 16, 2024 – Trailbreaker Resources Ltd. (TBK.V) (“Trailbreaker” or “the Company”) is pleased
to announce the results from surface sampling at the Liberty Property, central British Columbia (BC). Soil
sampling defined a property-scale (~10 km in length and up to 1.8 km wide ) arc shaped, copper (Cu)-in-
soil anomaly (Figure 1). Prospecting near the southwestern extent of the soil anomaly resulted in rock
samples assaying up to 15.62% Cu (float grab sample) and 23.71% Cu (subcrop grab sample). A continuous
chip sample near these rock samples assayed 2.15% Cu over 3.0 m.
Subsequent to completion of the surface program, additional claims totalling 1,841 hectors were staked
to the southwest to cover the open-ended soil anomaly and the strike extent of the high-grade copper
mineralization. Results from this surface program are being utilized in the preparation and design of a
new area -based permit application for Liberty, which will allow for advanced exploration beyond the
limited area drilled in the spring.
Message from the President
“This surface program has demonstrated that there is a very large area of prospective geological setting
at Liberty. It is clear that the drilling conducted in the spring test ed only a small area within this large
anomaly. High grade copper values from sampling provide further evidence of the potential for high-grade
zones within the mineralized system. Results to date at Liberty show many similarities to early exploration
results at the Gibraltar Mine, where a large low -grade copper – molybdenum ( Cu-Mo) system is
accentuated by zones of high-grade Cu-Mo mineralization.” -Daithi Mac Gearailt
High-Grade Copper
Prospecting in the southwestern portion of the property returned numerous rock samples with >1% Cu.
including 23.71% Cu from a malachite vein striking 140° - 320° (Figure 2). This area displays iron-carbonate,
talc, and actinolite alteration along the contact between ultramafic rocks to the northeast and an argillite
unit to the southwest. This contact was also identified in outcrop 900 m to the northwest, with similar
iron-carbonate alteration and elevated Cu values (up to 0.23% Cu in float around the contact). The Cu-in-
soil anomaly is particularly strong along this contact and extends to the northeast, with an average width
of 1.8 km.
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The malachite mineralization in the southwest Liberty property area shares similarities with the highest-
grade mineralization encountered from the Spring, 2024 drilling which returned 34.2 m* of 0.47% Copper
Equivalent** (CuEq), including 5.9 m of 2.02% CuEq , in hole LIB24-003. The high-grade mineralization in
LIB24-003 is located along the contact of a granodiorite intrusion with ultramafic rocks. This high-grade
interval is part of a wider interval of mineralized granodiorite (194.3 m of 0.16% CuEq). In t he
southwestern area, where the high -grade malachite was sampled, mineralization also occurs along the
contact of ultramafic rocks with the argillite unit, which display similar iron-carbonate, talc and actinolite
alteration. This near -surface high-grade mineralization may be associated with a mineralized intrusion,
similar to that encountered in drilling.
Figure 1: Contoured Cu-in-soil data across the Liberty property, highlighting the extensive property scale
area of high mineral potential. High-grade Cu-bearing grab and chip samples in the southwestern area
occur along a structural break (dashed lines are inferred faults are based on regional magnetic data)
between ultramafic rocks to the northeast and argillites to the southwest. Wetland conditions defined
by areas of deeper organic material and of high, near-surface groundwater content are outlined in the
central and northern portions of the surveyed area. These soil conditions may result in locally subdued
geochemical responses.
* Reported widths are drill width. Not enough geological information exists at this point to define true width. However, vein -
hosted copper and molybdenum mineralization commonly occurs at high angles to core axis.
** Copper Equivalent formula used is:
CuEq = Cu grade in % + (Mo grade in % * (Mo recovery/Cu recovery) * (Mo price/lb*2200 lb) / (Cu price /lb*2200 lb) using copper
price of US$3.75/lb and molybdenum price of US$25/lb. 100% metallurgical recoveries are assumed for both metals.
Figure 2: Photos of malachite mineralization along the contact between argillites and ultramafic rocks.
Left: Grab sample from subcrop 1879956 assayed 23.71% Cu. Right: Grab sample from f loat 3831604
(~60 m southeast of sample 1879956) assayed 15.62% Cu.
Surface Sampling Program
Soil sampling and prospecting were designed to cover prospective geological and regional structural
settings across the entire property. A total of 1,601 soil samples and 47 rock samples were collected. Cu-
in-soil values are anomalous through an arcuate zone that transects the center of the property. This zone
extends northeast for 4.1 km (~1.8 km width) from the southwestern limit of sampling to the centre of
the property. From there, it extends northwest for an additional 6.3 km (~1.0 km width) to the northern
property boundary.
This extensive Cu-in-soil is locally coincident with anomalous gold (Au), silver (Ag), molybdenum (Mo), and
arsenic (As) values, defining more constrained multi-element soil anomalies. The most significant of these
occur in the southwestern area, the area of Spring, 2024 drilling, and the northern area. The multi-element
anomalies align well with the highest Cu-in-soil anomalies.
Two areas within the soil survey are marked by wetland conditions, with deeper organic horizons and
shallow groundwater levels with water-saturated soil. These areas may cause a subdued geochemical
response in soil, as the soil development has occurred in a different environment than elsewhere on the
property. They are outlined in Figure 1, and occur in the central and northern boundary areas of the
property.
Liberty Property Description
The 6,895-hectare Liberty Property is located approximately 60 km northwest of Quesnel, BC. The
property is fully accessible by resource roads.
Drilling at Liberty has encountered widespread Cu-Mo porphyry-style mineralization at the northeastern
margin of a large Cu -in-soil geochemical anomaly. Mineralization is coincident with an Induced
Polarization (IP) chargeability feature. However, historic IP surveying covered only a small portion of the
much larger geochemical anomaly. Highlights of drill results include: 34.2 m of 0.47% CuEq , including
5.9 m of 2.02% CuEq in LIB24-003; 13.5 m of 0.33% CuEq, including 6.6 m of 0.67% CuEq in LIB24-001; and
6.0 m of 0.45% CuEq and 2.3 m of 0.36% CuEq in LIB24-004.
Prospecting within the southwestern portion of the property-scale geochemical anomaly has defined an
area of high-grade copper mineralization, with grab samples assaying up to 23.71% Cu.
For more information on this target see the Liberty Project webpage.
About Trailbreaker Resources
Trailbreaker Resources is a mining exploration company focused primarily on mining -friendly British
Columbia and Yukon Territory, Canada. Trailbreaker is committed to continuous exploration and research,
allowing maintenance of a portfolio of quality mineral properties which in turn provides value for
shareholders. The company has an experienced management team with a proven track record as
explorers and developers throughout the Yukon Territory, British Columbia, Alaska and Nevada.
ON BEHALF OF THE BOARD
Daithi Mac Gearailt
President and Chief Executive Officer
Carl Schulze, P. Geo., Consulting Geologist with Aurora Geosciences Ltd, is a qualified person as defined
by National Instrument 43 -101 for Trailbreaker's BC and Yukon exploration projects, and has reviewed
and approved the technical information in this release.
Other
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