Coffee Comparison......Tim, after your posts on the Kam comparison, I went in to see those rocks again for myself and, indeed, I now see why the company themselves have made that, visual, comparison. Of course, the drills will reveal the real story or at least the flow of first samplings that should be on the doorstep any day now.
Having said that, here's what I seen and then talked it up with a hard rock assay bud.:
White River.......... - Malachite, azurite & chalcocite have all been detected, along with limonite in this environment
- 4.41 g/t sample
- Quartz Carbonate veining is present
- weathering has created numerous red-brown limonite & jarosite-rich gossaneous zones.
- A strip of malachite & yellow secondary suphates
- An extensive intrusion of homblende-rich diorite to granodiorite occurs.
- Magnetite& pyrrhotite are present in the intrusive rocks.
Kaminak (Supremo Zone) ........ sample 00342 - 4.84 g/t - limonitic quartz veinlets
sample 003563 5.24 g/t - limonitc filled micro fractures
sample 000447 6.45 g/t - unfolicated dacite, limonite microveinlet networks
sample 000448 5.36g/t - strongly limonitic feldspathic rock, limonite
veins & veinlets.
Limonitic - very common mineral in sulphide mines. Associated with pyrite, galena, sphaterite &
other sulphides.
Limonitic = Pyrrhotite = Sulphide
And of course, the presence of high grade silver and copper are existent as well. There is more descriptions and mineral noted for each of these samples as well but these were the instant comparisons that jumped out.