
metamorphic
Iron-stained metamorphic rock, likely quartzite or jasper
Quartz-rich rock dominated by SiO₂, with iron oxides/hydroxides (hematite, goethite) and possible clay or mica
AI-generated identification · may be incorrectHardness likely 6–7 Mohs; mottled red, brown, yellow, gray, and cream coloration; earthy to slightly vitreous luster; massive, fine-grained texture with no obvious cleavage. The red-yellow colors are typical of iron staining, but the photograph cannot confirm the exact mineralogy.
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Physical properties
Hardness likely 6–7 Mohs; mottled red, brown, yellow, gray, and cream coloration; earthy to slightly vitreous luster; massive, fine-grained texture with no obvious cleavage. The red-yellow colors are typical of iron staining, but the photograph cannot confirm the exact mineralogy.
Formation & geological history
Probably formed by metamorphism or silicification of a quartz-rich sediment, followed by weathering and oxidation of iron-bearing minerals. Its precise geological age and locality cannot be determined from the image.
Uses & applications
May be used as a decorative or lapidary stone if it takes a polish; otherwise it is mainly a field or teaching specimen. It has little industrial value as an unverified hand sample.
Geological facts
The rusty colors commonly result from hematite and goethite coatings or cement. A white streak, hardness testing, acid testing, and a fresh broken surface would help distinguish quartzite from jasper, ironstone, or altered volcanic rock.
Field identification & locations
Likely found in weathered quartz-rich metamorphic or sedimentary terrains worldwide; quartz grains should scratch glass, while a steel nail generally will not scratch it. Collector value is typically $1–$15 for a hand-sized ordinary specimen, potentially $20–$50 if it polishes attractively.
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