
metamorphic
Iron-stained quartzite or ironstone pebble
Quartzite (mostly SiO₂) with iron-oxide/hydroxide minerals, likely hematite/goethite
AI-generated identification · may be incorrectHardness about 6.5–7 for the quartz-rich matrix; dark olive-brown, fine-grained, and weakly waxy to dull luster, with a sparkly metallic-looking crust. Quartz has no cleavage and conchoidal fracture; the apparent crystals may be iron oxides or drusy quartz.
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Physical properties
Hardness about 6.5–7 for the quartz-rich matrix; dark olive-brown, fine-grained, and weakly waxy to dull luster, with a sparkly metallic-looking crust. Quartz has no cleavage and conchoidal fracture; the apparent crystals may be iron oxides or drusy quartz.
Formation & geological history
Likely a water-worn cobble derived from metamorphosed sandstone or iron-rich silica rock, later coated or cemented by iron oxides in a weathering or hydrothermal environment. Exact age and locality cannot be determined from the photograph.
Uses & applications
Primarily a curiosity, lapidary, or collection specimen; iron-rich quartzite can be used as decorative stone or aggregate, though this small piece has no practical industrial value.
Geological facts
The brown coloration commonly comes from goethite and limonite weathering products, while darker metallic areas may contain hematite or magnetite. A streak, magnet test, and hardness test would substantially improve identification.
Field identification & locations
Commonly encountered in river gravels and iron-rich terrains worldwide; it should resist scratching by a steel knife if quartzite. Avoid damaging tests if it is a valued specimen.
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