This specimen is a green-gray slate. The color of the specimen suggests significant chlorite presence. Owning to the aphanitic nature of the material, many of the constituent minerals in this specimen cannot be identified through microscopy. Visible Quartz/feldspar grains are relatively rare with a maximum dimension of .06 mm, most are smaller. Various species of mica presumably form the majority of the specimen’s fabric, but these are generally too small to be individually perceived. Identifiable crystals of mica are mostly .1 mm and less in length. Visible mica crystals show moderate orientation preference. Carbonate minerals are rare and occupy about 5 percent of slide area with a maximum crystal dimension of about .14 mm. Most carbonate crystals have rhombohedral edges. There are a few forms that may be diamond shaped alteromorph, now filled with opaque material with a max dimension of .125 mm. Minimal relict sedimentary features are visible on macro-inspection of the slide in the form of banding. These are difficult to discern under the microscope and appear only in ppl as slight differences in the translucency of the aphanitic component. Overall the lack of more significant grain elongation and orientation prevalence indicates very low grade metamorphism. This may be due to the slide’s orientation, which is perpendicular to the likely direction of maximum tectonic stress.