IP Survey At The Sandy Gold Project

VANCOUVER - NV Gold Corporation has initiated its planned IP Survey at the Sandy Gold Project, located within the Walker Lane, Lyon County, Nevada. Combined with the Leapfrog modeling and detailed mapping earlier in the 3rd Quarter, the outcome of the IP Survey will be used for better target definition to guide a 2nd Phase drilling program projected for the 1st Quarter of 2022 or earlier depending on equipment availability.

Hydrothermal alteration at Sandy is predominantly clay to silica-clay alteration (of the tuffaceous rocks) in the Southwest Zone, mostly seen as float around epithermal quartz vein pieces, while stronger (massive and "near-massive") silicification forms ridgelines and broader structural zones in the upper Northeast Zone. Very white clay, possibly illite, is interpreted in the strongest silica-clay altered zones, both in the Southwest and Northeast Zones. The alteration is consistent with low sulfidation vein alteration and looks to be clay alteration developed on the margins or above epithermal veins. Based on the size, elevation range, zonation (silica above, clay below) and apparent geometry of the alteration, the Northeast Zone could be an altered cap overlying a preserved epithermal vein system.

The upcoming IP survey should be especially useful to interpret the 3D geometry of the alteration at the Northeast zone. Even if high resistivity is relatively shallow (shallow silicification) and any subsurface veins are too narrow to detect, the widespread clay alteration should produce moderate resistivity/conductivity anomalies in 3D and any roots or zones of greater resistivity or conductivity (near vein halo alteration) may be considered as vein drill targets. Deeper zones of greater chargeability may indicate broader sulfide rich zones around deeper veins and would also be potential drill targets. Once the IP surveying is completed, deeper drill targeting should be straightforward.