
Natural Iron Pyrite Specimen
This is a raw, unpolished specimen of iron pyrite, commonly known as 'Fool's Gold' due to its metallic luster and brassy-yellow hue. The specimen appears to be approximately 3-5 centimeters in diameter with a dense, heavy composition characteristic of iron disulfide. The physical structure is a crystalline cluster displaying the mineral's classic isometric crystal system, with visible cubic facets and irregular, jagged edges. Its color is a rich, pale brass-yellow with occasional darker tarnish and metallic sheen that reflects light across various angled faces. Notable features include the distinct striations on some of the crystal faces and the presence of smaller, micro-crystalline formations nestled within larger pits. The condition is consistent with a natural geological find, showing minor weathering, some crumbling or 'flaking' of smaller crystals, and a slight natural patina. There are no maker's marks or signatures as this is a natural mineral sample. The lack of quartz matrix suggests a high-quality, nearly pure cluster of pyrite. It is an enduring mineral that belongs to a geologic period millions of years old, though as a collected item, its age is indeterminate. The specimen serves as an excellent example of natural geometric crystallization without human intervention.
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Estimated Value
$25.00 - $45.00
Basic Information
Category
Minerals and Geological Specimens
Appraised On
April 11, 2026
Estimated Value
$25.00 - $45.00
Item Description
This is a raw, unpolished specimen of iron pyrite, commonly known as 'Fool's Gold' due to its metallic luster and brassy-yellow hue. The specimen appears to be approximately 3-5 centimeters in diameter with a dense, heavy composition characteristic of iron disulfide. The physical structure is a crystalline cluster displaying the mineral's classic isometric crystal system, with visible cubic facets and irregular, jagged edges. Its color is a rich, pale brass-yellow with occasional darker tarnish and metallic sheen that reflects light across various angled faces. Notable features include the distinct striations on some of the crystal faces and the presence of smaller, micro-crystalline formations nestled within larger pits. The condition is consistent with a natural geological find, showing minor weathering, some crumbling or 'flaking' of smaller crystals, and a slight natural patina. There are no maker's marks or signatures as this is a natural mineral sample. The lack of quartz matrix suggests a high-quality, nearly pure cluster of pyrite. It is an enduring mineral that belongs to a geologic period millions of years old, though as a collected item, its age is indeterminate. The specimen serves as an excellent example of natural geometric crystallization without human intervention.
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