the serpentinite on the other side of 101, but that road obscures any indication of the actual nature of the contact between the two. In addition to the breccia, a number of patches of the secondary mineralization- probably quartz- are apparent, most notably in the upper left corner.
Photo run through autolevel routine for contrast and saturation. May 7, 2013. FlashEarth location.
Is This Your Hat?
2 years ago