Rock Identifier
Iron-rich weathered rock, possibly limonite/goethite-bearing breccia (Limonite (FeO(OH)·nH₂O), goethite (α-FeO(OH)), and iron oxides; host uncertain) — mineral
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 incorrect

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.

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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.