Iridescent Minerals Appraisal

Iridescent Mineral Fragment

This is a small, irregularly shaped mineral specimen, likely a fragment of a larger deposit, resting in the palm of a hand for scale, suggesting a size of approximately 2-3 cm at its longest dimension. The item exhibits remarkable metallic luster with a distinctive and vibrant iridescent coloration, commonly referred to as "peacock ore." Dominant hues include brilliant electric blue, transitioning into subtle purples, coppery bronzes, and flashes of silver-grey, particularly prominent in the central areas. This iridescence is a natural tarnish (patina) forming on the surface, indicative of minerals such as bornite or tarnished chalcopyrite. The material appears dense and metallic. The surface texture is rough and crystalline in places, typical of a naturally formed ore, with no signs of artificial shaping, cutting, or polishing. There are no discernible maker's marks, signatures, or stamps, as it is a geological formation rather than a manufactured item. Its current condition appears stable and natural, free from obvious damage, human-induced wear, or repairs beyond its inherent rough and fractured texture. The vibrant, multi-layered colors are a key quality indicator, highlighting its natural beauty and making it an aesthetically appealing piece for collectors of mineral specimens. Its estimated age is geological, having formed over millions of years within the Earth's crust. This unique piece stands out due to its striking natural coloration and unrefined, raw form.