
sedimentary
Polished ironstone concretion with quartz/iron-oxide vein
Goethite–hematite-rich ironstone concretion, likely veined by quartz or chalcedony
AI-generated identification · may be incorrectDark gray-black, rounded and highly polished, with a rusty orange-brown vein. Likely Mohs hardness 5–7, submetallic to dull luster, massive rather than crystalline, and high specific gravity (~3–4); cleavage is absent.
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Physical properties
Dark gray-black, rounded and highly polished, with a rusty orange-brown vein. Likely Mohs hardness 5–7, submetallic to dull luster, massive rather than crystalline, and high specific gravity (~3–4); cleavage is absent.
Formation & geological history
Probably formed as an iron-rich concretion in sediment, later fractured and filled by silica and oxidized iron minerals. Its exact geological age cannot be determined from the photograph; similar concretions occur in many sedimentary formations.
Uses & applications
Primarily a lapidary and collecting specimen; polished pieces may be used as display stones or paperweights, but it has little industrial value in this form.
Geological facts
The dark material is consistent with hematite, magnetite, or goethite-rich ironstone, while the orange vein may contain limonite/goethite and iron-stained silica.
Field identification & locations
Identify it by its unusually heavy feel, dark opaque surface, rounded concretion shape, and contrasting rusty fracture vein; a streak test and magnet test would help distinguish hematite from magnetite. Common examples occur in iron-rich sedimentary terrains worldwide.
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