View east at Jeep Mine from the Blue Ribbon skarns located to the west, at the western end of the 3-4 km skarn and porphyry system at New Boston. The drill is visible in the left middle-ground, on the northern flank of the Jeep Mine hill where veins at surface contain moly, tungsten, copper and silver mineralization. Drill hole NB26-003 was inclined steeply to the south (towards the right in this photo), and intersected sulfide-bearing stockwork veining for 2,892 ft, across and down into the large, red-brown alteration zone that is clearly visible to the right of the drill in this photo. The drill hole tests the new, coincident conductivity and IP chargeability anomalies shown in profile in Figure 2, which plunge steeply across the country rock of north-dipping limestone and siltstone dipping from right to left in this photo, with sheeted and discordant quartz monzonite dykes themselves with quartz veins and sulfide.
View east at Jeep Mine from the Blue Ribbon skarns located to the west, at the western end of the 3-4 km skarn and porphyry system at New Boston. The drill is visible in the left middle-ground, on the northern flank of the Jeep Mine hill where veins at surface contain moly, tungsten, copper and silver mineralization. Drill hole NB26-003 was inclined steeply to the south (towards the right in this photo), and intersected sulfide-bearing stockwork veining for 2,892 ft, across and down into the large, red-brown alteration zone that is clearly visible to the right of the drill in this photo. The drill hole tests the new, coincident conductivity and IP chargeability anomalies shown in profile in Figure 2, which plunge steeply across the country rock of north-dipping limestone and siltstone dipping from right to left in this photo, with sheeted and discordant quartz monzonite dykes themselves with quartz veins and sulfide.