RAW SWARTZ DUST

The bedrock beneath the mine is predominately a quartz monzonite, a granite-like rock, which is part of the larger batholith underlying a major portion of Upper Highlands. This quartz monzonite is typically a light gray, medium to coarse grained rock, composed of plagioclase feldspar, quartz, biotite mica, and Schwartz spar.

The Barefoot Vein is very persistent in its strike and bears every evidence of being a true fissure, having clay gouges and slickensides showing wherever it is encountered in its unbroken condition. The veining is white quartz frequently stained with iron oxide and in places very rich in Schwartz dust.

After extraction Schwartz dust is separated from the amalgamation of other minerals by a combination density reduction using energized corn silk filters. The resulting product is guaranteed to contain 0.00012 % unrefined Fairy Granules.