
rock
Tumbled brown jasper / iron-rich breccia
Microcrystalline quartz (SiO₂), likely with iron oxides and assorted silicate fragments
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque brown, gold, gray, and black coloration; dull to waxy luster when polished; no visible cleavage; fine-grained, heterogeneous texture and typical silica-rich density around 2.6 g/cm³.
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Physical properties
Hardness about 6.5–7 Mohs; opaque brown, gold, gray, and black coloration; dull to waxy luster when polished; no visible cleavage; fine-grained, heterogeneous texture and typical silica-rich density around 2.6 g/cm³.
Formation & geological history
Likely silica-rich sedimentary or hydrothermal material later cemented and stained by iron oxides, then rounded by tumbling; exact geological age and locality cannot be determined from the image.
Uses & applications
Used as a decorative stone, lapidary cabochon, polished pebble, and inexpensive collector specimen; not generally used as an architectural stone in this small form.
Geological facts
The brown and golden colors commonly come from hematite, goethite, or limonite, while gray translucent areas may be chalcedony or quartz. “Jasper” is a trade and field term for opaque, silica-rich chalcedony/quartz aggregates.
Field identification & locations
Identify by its opaque, nonmetallic appearance, glassy-to-waxy polish, lack of cleavage, and resistance to scratching; a steel file should generally scratch less readily than the specimen. Similar material occurs worldwide, especially in volcanic and hydrothermal regions.
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