Earth Record
Mineralogy and formation
Variety of Quartz
Lepidocrocite in quartz contains reddish-orange lepidocrocite (γ-FeOOH, an iron oxyhydroxide) as inclusions within clear quartz. The lepidocrocite formed first as thin flakes or plates, and was subsequently encased by quartz growing around it. The red to reddish-orange color comes from the specific iron oxyhydroxide polymorph: lepidocrocite is structurally different from goethite (α-FeOOH, which is brown to yellow) despite having the same chemistry.
The inclusions often appear as thin, platy flakes oriented along specific planes, creating internal reflections that can produce a strawberry-like or fire-like appearance. Found primarily in Brazil and Madagascar, this material is sometimes marketed as "strawberry quartz" or "fire quartz."
Chemical FormulaSiO2 (host: alpha-quartz) + gamma-FeO(OH) (inclusion: lepidocrocite, iron oxyhydroxide)Crystal SystemMixedMohs Hardness7Specific Gravity2.65 (quartz) to 2.70+ depending on inclusion density. Lepidocrocite itself is 3.96-4.09LusterVitreous (quartz exterior). Inclusions display subadamantine to silky luster internally.ColorRed-WhiteIMA Statustrade_nameIMA Numberpre-IMA BrazilIndiaMadagascar
Telling it apart
Lepidocrocite in quartz is quartz containing red to reddish brown platy inclusions of lepidocrocite, an iron oxyhydroxide. The market confusion involves hematite inclusions, goethite inclusions, and iron stained quartz all labeled under whichever inclusion name sounds most interesting. Lepidocrocite specifically forms thin platy to micaceous crystals within the quartz host, often appearing as reddish fire like patches or scattered red flakes.
Hematite inclusions tend to be more metallic and specular. Goethite inclusions often appear as needles or fibrous bundles in brown to yellow. The quartz host tests normally at Mohs 7 with no cleavage. If the red inclusions are platy and distributed as internal fire like patches, lepidocrocite is a reasonable identification. If they are metallic or needle like, a different iron mineral is more likely.
Spotting the real thing
Lepidocrocite in quartz: red-orange inclusions should be INSIDE the quartz host (Mohs 7). The inclusions are iron oxyhydroxide flakes or plates sealed during quartz growth. If the red-orange is only on the surface, it is surface staining, not genuine lepidocrocite inclusion.
The inclusions should show metallic to subadamantine luster internally.
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