Viscount Mining Commences Drilling Significant Large Geophysical Anomaly Indicating Potential Porphyry Type Deposit at Silver Cliff, Colorado.

In This Article:

  • According to Quantec geoscientists, a deposit with this large size and this high of a conductivity (extremely low resistivity) is likely explained by a significant system of interconnected mineralized fractures.

  • The main body of the conductive anomaly starts at a depth of ~400m and continues to a depth of ~1.5km, maybe deeper. The detectable length of the anomaly is ~1.4km in the SW-NE direction with a width of at least 700m and an open interpretation to the untested NW. This represents a total volume of over 665,000,000m3 as determined by Quantec.

Vancouver, British Columbia--(Newsfile Corp. - January 22, 2025) - Viscount Mining Corp. (TSXV: VML) (OTC Pink: VLMGF) ("Viscount" or "the Company") is pleased to announce drilling has commenced on the Passiflora in Silver Cliff, Colorado.

During the Viscount drill campaign in 2017 at the Kate Silver Resource, field reconnaissance noted that areas to the north seemed to exhibit phyllic/argillic alteration. This was confirmed by drilling in this area in 2020 to 2022, and showed anomalous precious and base metal concentrations. The only historic report available on the Passiflora target is one written by R. A. Rivera for Coca Mines in 1983. In this report, Rivera gives a brief history of the exploration efforts, and a reserve calculation for the Passiflora target released indicated at least 64M oz. silver at 51.9 G/T (not NI 43-101 compliant). It is noted in his report that the deposit was presented as "a set of steeply dipping, NNW striking, tabular mineralized zones" (Rivera, 1983). It is also implied that the deposit could go much deeper as Rivera states that some drill holes presented high assay values at their total depths but they did not test the conductive anomaly at depth as identified by Quantec.

The Quantum Geophysics TITAN MT completed resistive survey under took by Viscount showed that a strong conductor was present staring at a depth of around 400 meters, and continues to ~ 1.5km (the lower limit might be somewhat different). Viscount is inaugurating an 8000m drill program starting with drilling a 1500m core exploratory discovery hole to try to determine the nature of this anomaly. The geologic setting, in a caldera, the associated alteration and the presence of Manto deposits, make it possible that a porphyry style deposit may be reason for the geophysical anomaly.

Figure 1, below, is a cross section of through line L1E which depicts a view of the massive, low resistivity anomaly described by Quantec. As shown, the bowl-shaped anomaly extends ~1400m (~4590 ft) across the center of the caldera, and at least 1500m (~4920 ft) deep, maybe deeper, depending upon the accuracy of resistivity detection below the conductive body.

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