I like our oddsMillions of years ago when an orogenic event happened, ie. violent clashing of plates occurred along the Appleton fault. Depending on the permittivity, or porosity of surrounding rock walls, high grade material would have been either forced into surrounding side shutes, and/or expelled to surface and gradually being depleted due to surficial errosion over time.
I'm betting that with the fault running completely thru our claim from South to north, that the odds are very good that we will find one or more areas that the porisity conditions will be such that we may well have a duplicate or two to that of nfg.
Of course it would be nice to hit on first hole, I'll not be too quick to pull the trigger on this one, remember that the same violent events that occurred to our south, occurred up and down the entire fault.
I love our chances
Best
S