FIRE AGATE SPECIMENS

Fire agate is a variety of chalcedony that often displays a metallic, shimmering iridescence known as the Schiller Effect. It's believed to form when fluids evaporate within cavities already experiencing chalcedony deposition. In these cases, a thin, iridescent film floating on the stagnant, silica-rich fluids forms as ferrous iron oxidizes when coming in contact with air in the cavity, producing ferric iron (Fe202). Once the cavity experiences a dry period, the thin iridescent film collapses onto the pre-existing chalcedony, depositing the iridescent layer that creates the fire effect. A following chalcedony band encloses the iridescent film inside the agate.