
Pyrite Cluster
The item is a natural mineral specimen identified as a pyrite cluster. It presents as an irregularly shaped, rugged mass composed of numerous small, interlocking pyrite crystals. The overall color is a bright, metallic brassy yellow, characteristic of iron pyrite (FeS2), often referred to as 'fool's gold.' The surface is highly textured, with a granular, crystalline aggregate appearance. Individual crystals appear to be rather small, likely cubic or pyritohedral forms, but the resolution of the image does not permit precise identification of crystal habits. Many individual crystal faces reflect light, creating a sparkling and lustrous effect, though some areas appear slightly dulled or oxidized, suggesting a natural patina consistent with pyrite. There are visible crevices and depressions within the cluster, indicating its natural formation and unrefined state. The specimen does not show any signs of artificial polishing or shaping. No discernible maker's marks, signatures, or stamps are present, as expected for a natural mineral specimen. The item's estimated age is geological, having formed over millions of years. It appears to be generally intact with no obvious signs of recent damage like chipping or breakage, though the natural rough texture could obscure minor flaws. The piece is a fine example of a raw mineral formation, valued for its aesthetic appeal and geological interest rather than its intrinsic material value.
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Estimated Value
$40 - $70
Basic Information
Category
Mineral Specimen
Appraised On
December 3, 2025
Estimated Value
$40 - $70
Item Description
The item is a natural mineral specimen identified as a pyrite cluster. It presents as an irregularly shaped, rugged mass composed of numerous small, interlocking pyrite crystals. The overall color is a bright, metallic brassy yellow, characteristic of iron pyrite (FeS2), often referred to as 'fool's gold.' The surface is highly textured, with a granular, crystalline aggregate appearance. Individual crystals appear to be rather small, likely cubic or pyritohedral forms, but the resolution of the image does not permit precise identification of crystal habits. Many individual crystal faces reflect light, creating a sparkling and lustrous effect, though some areas appear slightly dulled or oxidized, suggesting a natural patina consistent with pyrite. There are visible crevices and depressions within the cluster, indicating its natural formation and unrefined state. The specimen does not show any signs of artificial polishing or shaping. No discernible maker's marks, signatures, or stamps are present, as expected for a natural mineral specimen. The item's estimated age is geological, having formed over millions of years. It appears to be generally intact with no obvious signs of recent damage like chipping or breakage, though the natural rough texture could obscure minor flaws. The piece is a fine example of a raw mineral formation, valued for its aesthetic appeal and geological interest rather than its intrinsic material value.
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