I hand drew on the cross section view of 426 & 427 onto the older chargeability cross secion for DDH 422. The red portion of 427 shows the visible mineralized portion described in todays NR.

I placed failed DDH 429 on the cross section for comparison but this is not very accurate as it is actually located some 300-400 m south of the cross section shown.

...."Diamond drill hole (DDH) 2012CF426 with a core length of 788.1m intersected visible chalcopyrite mineralization over approximately 90% of its core length along with three intervals of molybdenite mineralization. The drill hole bottomed in weak chalcopyrite-molybdenite mineralization,

DDH 2012CF427 located 400m north of DDH 2012CF426 with a core length of 769.3m intersected visible copper +/- molybdenite mineralization from a core interval of 250.0m to the end of the drill hole at 769.9m. The chalcopyrite+/-molybdenite mineralization is open at depth,...

Diamond drill hole (DDH) 2012CF426 an inclined (-60 degrees, azimuth 090) HQ diameter hole located approximately 300m east of DDH 2011CF422 was completed to test the chargeability anomaly referred to as the Discovery zone. This hole intersected variable concentrations of visible chalcopyrite mineralization over approximately 90% of the core length of the hole. In addition to the chalcopyrite mineralization; visible molybdenite mineralization occurs sporadically throughout the core in quartz veinlets and in some instances also with chalcopyrite mineralization. The chalcopyrite-molybdenite mineralization occurs as disseminations, veins and veinlets in variably altered andesite.

DDH 2012CF427 an inclined (-60 degrees, azimuth 090) HQ diameter hole located approximately 400m northwest of DDH 2012CF426 was completed to test the strike extension of the chargeability anomaly referred to as the Discovery zone that was located in 2011. This hole intersected variable concentrations of visible chalcopyrite and sporadic molybdenite mineralization from a core interval of 250.0m to the end of the drill hole at 769.9m. The chalcopyrite+/-molybdenite mineralization occurs as disseminations, veins and veinlets in a granodiorite intrusive which exhibit a number of thin basic dikes. This hole contains large intervals of silicification. "...

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