
sedimentary
Iron-rich jasper / hematite-bearing breccia
Ferruginous jasper, chiefly microcrystalline SiO₂ with hematite/goethite (Fe₂O₃/FeO(OH)) and possible limonite
AI-generated identification · may be incorrectHardness typically 6.5–7 for jasper, about 5–6 for hematite-rich areas; opaque red, brown, black, and yellow, with earthy to locally submetallic luster. Massive, brecciated texture; no visible cleavage; high density, commonly about 2.7–4.5.
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Physical properties
Hardness typically 6.5–7 for jasper, about 5–6 for hematite-rich areas; opaque red, brown, black, and yellow, with earthy to locally submetallic luster. Massive, brecciated texture; no visible cleavage; high density, commonly about 2.7–4.5.
Formation & geological history
Silica-rich material was cemented or replaced by iron oxides, producing the red-brown brecciated pattern; some pieces may be weathered banded iron formation or hydrothermal jasper. Precise age and locality cannot be determined from the photograph.
Uses & applications
Used as ornamental stone, cabochons, lapidary slabs, and collectible specimens; iron-rich varieties have minor historical importance as iron ore but this piece is primarily decorative.
Geological facts
The red color is mainly hematite, while yellow-orange zones commonly indicate goethite or limonite. A streak test can distinguish components: hematite gives a reddish-brown streak.
Field identification & locations
Likely jasper if it is hard, opaque, and takes a good polish; test with a steel file and inspect the streak on unglazed ceramic. Common in hydrothermal veins, volcanic terrains, and iron-rich sedimentary deposits worldwide.
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