Silver47 Drills 2.9m of 1,078.8 g/t Silver Equivalent (417.4 g/t Silver, 0.74 g/t Gold, 9.1% Zinc, 4.7% Lead) at the West Tundra Flats Zone at Its Red Mountain Project, Alaska

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - November 21, 2024) - Silver47 Exploration Corp. (TSXV: AGA) ("Silver47" or the "Company), is pleased to announce results from two diamond drill core holes at the West Tundra Flats resource area for a combined 331m at its wholly owned flagship Red Mountain Project in Alaska, USA. Both drill holes cut high-grade silver-zinc-lead-gold-copper zones within a wider sulfide mineralization horizon.

Highlights from 2024 West Tundra Flats Drill Holes:

  • WT24-33 returned a 22.03m interval of sulfide mineralization grading 177.10 g/t AgEq
    (57.5 g/t silver, 0.14 g/t gold 1.6% zinc, 0.67% lead, 0.09% copper)

  • WT24-34 returned 4.37m 656.2 g/t AgEq from 92.25m depth

Mr Alex Wallis, P.Geo., Vice President of Exploration, stated: "The successful confirmation and infill holes drilled at West Tundra Flats suggest a path to increasing the size and grade of the resource by utilizing modern drilling to fill the widely spaced historical drilling. Historical drilling had poor core recovery at West Tundra Flats, including through mineralized intervals. The high-percentage core recovery achieved in 2024 gives us an opportunity to improve upon the already robust grade reported from the 1980's drilling."

West Tundra Flats Resource Area

The West Tundra Flats prospect was first identified in 1981 as a surface gossan on the south bank of Dry Creek. Volcanogenic Massive Sulphide (VMS) mineralization was initially confirmed by widespread geochemical sampling and later drill tested in 1982, with zone expansion drilling in 1983. The mineralized horizon consists of semi-massive to massive sulfides including pyrite, sphalerite and galena, and is commonly enriched with silver and gold. This horizon historically occurs at the base of a black chlorite schist and overlying a metarhyolite in the upper formations of the Totatlanika Schist. The surface expression has a 1,000m strike and dips shallowly to the southwest for at least 1,600m. The West Tundra Flats horizon remains open laterally and at depth, and exhibits pinching and swelling of sulfide lenses typical of VMS mineralization.

Figure 1. Plan map of drill holes at Dry Creek and West Tundra Flats resource areas.

To view an enhanced version of this graphic, please visit:
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Table 1. Significant intervals for holes WT24-33 and WT24-34 at West Tundra Flats.

Hole ID

From
 (m)

To
 (m)

Interval
(m)

ZnEq
 (%)

AgEq
 (g/t)

Ag
 (g/t)

Au
 (g/t)

Zn
 (%)

Pb
 (%)

Cu
 (%)

WT24-33

102.62

124.65

22.03

3.7

177.1

57.5

0.14

1.6

0.67

0.09

incl.

121.70

124.60

2.90

22.6

1078.8

417.4

0.74

9.1

4.77

0.105

WT24-34

92.25

96.62

4.37

13.7

656.2

157.4

1.05

6.3

3.03

0.076

incl.

94.59

96.06

1.47

31.1

1488.4

356.0

2.90

13.7

6.21

0.166