
mineral
Tumbled honey quartz (likely iron-stained quartz)
Quartz, silicon dioxide (SiO₂), with limonite/goethite inclusions or surface staining
AI-generated identification · may be incorrectTranslucent golden-brown to amber, vitreous luster, irregular conchoidal fracture, no visible cleavage; Mohs hardness 7 and specific gravity about 2.65. The rounded form is mechanically tumbled and polished.
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Physical properties
Translucent golden-brown to amber, vitreous luster, irregular conchoidal fracture, no visible cleavage; Mohs hardness 7 and specific gravity about 2.65. The rounded form is mechanically tumbled and polished.
Formation & geological history
Quartz crystallizes from silica-rich hydrothermal fluids in veins, cavities, and igneous or metamorphic rocks; yellow-brown coloration commonly results from iron oxides/hydroxides. Quartz ranges from Precambrian to recent in age, depending on its host deposit.
Uses & applications
Used as an inexpensive lapidary and carving material, ornamental stone, and collector specimen; suitable for jewelry when well polished, though this piece appears opaque and cabochon-grade rather than gem-grade.
Geological facts
Golden coloration can also indicate citrine, but natural citrine is typically clearer and more evenly colored; iron-stained quartz is the safer identification from this image.
Field identification & locations
Identify by its glassy luster, hardness, lack of cleavage, and inability to scratch it with a steel knife easily; common worldwide in quartz veins and gravel deposits. Acid testing is unnecessary, and avoid assuming it is citrine without locality or testing.
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