The chief peridotite deposits lie on a slope toward the bottom of the largest hill about 1000 meters south of our camp. Rock tailings cover the entire area and most tunnels have been obliterated by dumps. Because these cover even older dumps, it is possible that all of the oldest workings lie beneath newer waste rock. Previous miners had used large screens to sift out crystals from the ore, and a careful search failed to reveal a single large crystal. Overlooked, however, were tiny peridot crystals up to 0.5 centimeters in length which were scattered about a few of the tailings. We collected a score or so of these little crystals–exact microminiatures of the larger crystals seen in museums.