
mineral
Polished black-and-gold pebble, likely jasper or iron-rich chert
Microcrystalline quartz (SiO₂), probably jasper/chert with iron-oxide bands
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque black, brown, and mustard-yellow coloration with a waxy to glassy polish. No visible cleavage; dense, fine-grained, and likely conchoidal-fracturing.
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Physical properties
Hardness about 6.5–7 Mohs; opaque black, brown, and mustard-yellow coloration with a waxy to glassy polish. No visible cleavage; dense, fine-grained, and likely conchoidal-fracturing.
Formation & geological history
Formed from silica-rich sediment or volcanic material later replaced and colored by iron oxides; age is locality-dependent, commonly Paleozoic or younger. The rounded shape indicates stream or beach transport, followed by polishing.
Uses & applications
Used as a cabochon, tumbled stone, ornamental pebble, or minor lapidary material; rarely used industrially because of its small size.
Geological facts
The yellow-brown zones are likely limonite/goethite or hematite staining within the silica. A strong steel scratch should not easily mark it, while quartz can scratch glass.
Field identification & locations
Commonly found in gravel bars and weathered jasper/chert-bearing terrains worldwide, especially volcanic or iron-rich regions. Exact identification requires a fresh surface, streak, hardness, and locality information.
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