VR Resources Ltd. has received its first NOI drill permit for its New Boston property and polymetallic copper-moly-silver porphyry system located in west-central Nevada. For strategic reasons, two separate NOI permit applications have been prepared to cover both the large IP chargeability anomaly at Jeep Mine and the large conductivity anomaly at East Zone (EZ), respectively. The conductivity anomaly at East Zone is the priority and, as such, its NOI permit was submitted first and has been approved and received within the standard 15-day timeframe.

The Jeep Mine NOI application has been similarly prepared for submission and timely approval. The ground DCIP conductor at East Zone has been given top priority based on its size, and on its proximity to known copper mineralization: the best anywhere on the property covering the entire 4 km vein system: · Copper at surface. The core of the conductor comes to surface into a patch of maroon-coloured soil amongst hematite skarn and intense quartz vein stockworks, with up to 0.8% copper in soil; · Copper Intersections.

A 2010 drill hole located 300m to the south of the conductor, up-dip in limestone, intersected 279ft @ 0.24% Cu from 12ft depth, coincident with a small conductor; · Strike length. Starting from the maroon soil surface expression, the EZ conductor extends 900 m to the northwest on plan map, and converges with the Jeep Mine conductor at depth; · Open to depth. The EZ conductor plunges from surface through the 500 metre depth extent of the 3D voxel model; amplitude strengthens and volume increases with depth, and is open.

The new conductor at East Zone offers the potential to discover a mineralized porphyry stock that is the source of the system of mineralized, sheeted quartz veins exposed on surface over a 4 km strike. 1. There are bona fide polyphase stockwork vein geometries of quartz with copper sulfide, at surface; 2. There are bona fide dacite porphyry dykes together with quartz monzonite stocks, at surface, and; 3. There are bona fide high temp. potassic alteration mineral assemblages with biotite and magnetite.