USA Graphite Inc fka USGT

[DITRstocks]

Fresh, broken hornfels look dark gray to black with pockets of flaked graphite. Two different hornfels units have been mapped based on the amount of the chiastolite content. These two units comprise 90% of the Blue Wing Mountains and both units are rich in high carbon content flake graphite. The hornfels unit without chiastolite is paler in tone while the chiastolite-bearing hornfels is dark gray to black. A pure quartzite unit is present on the east side of the collecting site. This unit is thinner to the south and thickens to the northeast. This quartzite is pale tan in color and relatively pure (that is, no macroscopic aluminum silicates are observed within it); float originating from it stands out against the very dark, graphite-rich hornfels and float.

USGT