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.

Lawyers Gold & Silver Project: Our Neighbour

Lawyers Mine (owned by Benchmark Metals*)

-Past producer with ~$50 million in existing infrastructure
-Large Resource Expansion Areas with New Discovery Potential
-Planning 50,000 m of expansion and definition drilling
-Potential link to deeper porphyry system
-High grade drill intercepts:
7.0 m* at 108 g/t gold & 911 g/t silver
33.53 m* at 5.76 g/t gold & 128.65 g/t silver
25 m* at 2.79 g/t gold & 177 g/t silver – AGB
36.5 m* at 2.68 g/t gold & 82.57 g/t silver – Cliffs
26 m* at 2.42 g/t gold & 100.26 g/t silver – Phoenix

Williams Gold Property Analog ?
-Williams has the same geological terrain
-Williams has similar vein / epithermal showing
-In the neighbourhood of multiple deeper porphyry systems
-The Williams is fully permitted to test these theories.

Information from Benchmark Metals news releases of 2019-01-11, 2019-02-08, 2019-03-11, 2019-08-16, & 2019-11-22

ISS’s qualified person has been unable to verify Benchmark’s information and it does not indicate that the same mineralization will be found on the Williams Gold Property

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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