
mineral
Iron-rich weathered rock, possibly limonite/goethite-bearing breccia
Limonite (FeO(OH)·nH₂O), goethite (α-FeO(OH)), and iron oxides; host uncertain
AI-generated identification · may be incorrectEarthy, porous, and strongly multicolored with red-brown, yellow, greenish, and bluish surface coatings. Likely low-to-moderate hardness (about 4–5.5), dull to earthy luster, and no obvious cleavage; exact properties require testing.
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Physical properties
Earthy, porous, and strongly multicolored with red-brown, yellow, greenish, and bluish surface coatings. Likely low-to-moderate hardness (about 4–5.5), dull to earthy luster, and no obvious cleavage; exact properties require testing.
Formation & geological history
Probably formed by oxidation and weathering of iron-bearing rock or sulfide minerals, producing hydrated iron oxides and secondary coatings. The reported Marin County, California area commonly contains weathered volcanic, sedimentary, and serpentinite-related rocks, but the specimen’s exact source is uncertain.
Uses & applications
Usually a cabinet or curiosity specimen; limonite/goethite may serve as an iron ore or natural pigment, but this small piece has little industrial value.
Geological facts
Red, yellow, and brown colors are typical of hematite and goethite/limonite. Green-blue areas could reflect copper minerals, serpentinite, or staining, but they are not identifiable confidently from the photograph.
Field identification & locations
Streak on unglazed porcelain is diagnostic: yellow-brown suggests limonite/goethite, red-brown suggests hematite. Check magnetism, specific gravity, and whether dilute hydrochloric acid reacts; avoid assuming copper minerals without chemical testing.
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