WILLIAMS PROPERTY

North-Central BC: 70 km NW of Kemess.
The Williams gold property hosts two large targets: mesothermal gold with two metres of 24.8 g/t gold and two metres of 35 g/t gold and a porphyry copper-gold-molybdenum prospect. Widespread alteration zone coincident with a large 1,200-metre-by-2,300-metre gold-in-soil anomaly. Historical drilling on a small segment of the anomaly (300 metres by 300 metres) intercepted 11 separate two-metre intervals with greater than 12 g/t gold.

Prolific belt of copper & gold porphyry and also epithermal gold & silver deposits throughout

The Lawyers mine is a past producer and is now owned by Benchmark Metals Inc. CSE-BNCH, in 2018 Benchmark started a new drill program to test beside and under the old mine, The 2018 program discovered several new zones and they will expand the program 2019.

ISS has similar gold veining, with grades equal to or exceeding those of Benchmark, in addition ISS has identified a 1800X500M Porphyry signature with IP data, No work has been done on this property since 2003

BENCHMARK DRILLS 52 G/T GOLD AND 846 G/T SILVER OVER 3 METRES WITHIN A LARGER INTERVAL OF 5.8 G/T GOLD AND 128.7 G/T SILVER OVER 33.52 METRES, IDENTIFIES +3KM OF CONTINUOUS MINERALIZATION ALONG LAWYERS TREND

Drilling in 2018 has expanded the potential resource area, indicating gold-silver mineralization with a total strike length of at least 530 metres that is open at depth below 80 metres

Benchmark Metals Inc. has completed the field exploration program at the Lawyers gold and silver project

BENCHMARK EXPANDS THE PHOENIX ZONE, DRILLING AN INTERSECTION OF 11 G/T GOLD AND 819 G/T SILVER OVER 3.95 METRES

VIEW OUR PROPERTY PRESENTATION

EXPLORING THE TOODOGGONE

VISIBLE GOLD IS NOTED IN MOST HIGH GRADE SAMPLES

GIC PROSPECT

Southern IP boundary marked by chip sample of 0.22% Cu and 0.22 g/t Au over 3.73 m

Northern IP anomaly margin overlaps Cu and Au soil anomaly

1800 m wide chargeability and resistivity anomaly

“Golden Triangle” aged magmatism and untested Cu-in-soil anomalies on margin of strong IP anomaly

Needs follow-up geological work (alteration map, extend soil surveys)

MODEL GOLD DISTRIBUTIONS AT T-BILL

Gold at has areas of 1.0g/t
Open on three ends

3 x 2 km Au (>100 ppb) and As (>100 ppm) soil anomaly
Coincident with muscovite-carbonate-quartz alteration of chlorite schists that is pervasive over a 1.2 by 1.3 km central core
Alteration is typical of halos to Au-mineralized quartz veins
Visible gold is noted in most high grade samples
Four rock and core samples that exceeded 5000 ppb Au on initial analysis were subjected to metallic screen assaying. Three of the four samples showed coarse gold to be a significant factor, with the grade increasing by 22 to 113%
Potential that some of the grades are under-reported
Six interpreted NW trending QZ–ASP–Au vein corridors associated with Fe–carbonate alteration
Consists of eleven separate 2 m intercepts > 12 g/t Au
WG03-10 is the only drill hole drilled to intersect this mineralization in the correct orientation

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