Earth Record
Mineralogy and formation
Tiger iron is a banded metamorphic rock composed of alternating layers of tiger eye (silicified crocidolite), red jasper (iron-stained microcrystalline quartz), and hematite (iron oxide). It originates from banded iron formations (BIFs), Precambrian sedimentary deposits laid down 2. 2 to 2. 7 billion years ago when Earth's atmosphere was transitioning from anoxic to oxygenated conditions.
The original sediment consisted of alternating layers of iron-rich and silica-rich material precipitated in shallow marine environments. Cyanobacterial oxygen production periodically oxidized dissolved iron, precipitating iron oxide layers between silica-rich layers. Subsequent metamorphism and hydrothermal alteration transformed the silica layers into jasper and chalcedony, while some layers were infiltrated by crocidolite (blue asbestiform amphibole) that was later replaced by quartz, creating the chatoyant tiger eye component.
The hematite layers retained their iron oxide composition. The primary source is the Hamersley Basin in Western Australia, part of one of the world's largest BIF deposits. The interplay of metallic hematite, golden chatoyant tiger eye, and deep red jasper creates a visually distinctive material. Mohs hardness ranges from 5 (hematite) to 7 (quartz components).
Chemical FormulaSiO2 and Fe2O3Crystal SystemN/AMohs Hardness6.5Specific Gravity3.2-4.0 (higher than typical quartz due to hematite content)LusterVitreous to silky (tiger's eye bands show characteristic chatoyancy); metallic to submetallic (hematite bands)ColorRed-Yellow-BlackIMA StatusrockIMA NumberNot IMA-approved (rock, trade/variety name) Australia (Western Australia)South Africa
Telling it apart
Dealers routinely sell tiger iron as if it were just a darker tiger eye, but that shortcut hides the most important fact: tiger iron is a layered rock, not a single chatoyant quartz material.
Tiger eye contains silicified crocidolite with a golden sheen and usually lacks the thick red jasper and metallic hematite bands that define tiger iron. Banded iron formation is even broader. It refers to the ancient iron-silica rock unit itself, often without enough tiger eye replacement to create strong chatoyancy. Tiger iron sits between them: a decorative lapidary material built from tiger eye, jasper, and hematite in obvious parallel bands.
The fastest check is visual and tactile together. If the stone shows gold shimmer, brick-red zones, and silver-black metallic layers in one polished piece, it is likely tiger iron. Plain tiger eye will be lighter, more uniform, and far less metallic. Generic jasper may carry red and brown tones but will not flash.
The price gap is real, but so is the geology. Calling every striped brown cabochon tiger iron flattens a very specific story about Precambrian oceans, iron deposition, and later quartz replacement.
Spotting the real thing
Tiger iron: banded rock with three components: tiger eye (chatoyant, silky), red jasper (opaque, red), and hematite (metallic, dark). SG 3. 2-4.
0 (heavier than pure quartz due to hematite). All three layers should be naturally intergrown. If the banding looks painted or if any layer is absent, it is a different banded rock.
The chatoyancy should be visible in the tiger eye bands when rotated under light.
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