
sedimentary
Tumbled jasper/chert pebble (likely orbicular or brecciated jasper)
Microcrystalline quartz (SiO₂), with iron-oxide and other mineral impurities
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, smoothly rounded, waxy to dull luster, gray-green, cream, tan, and reddish-brown coloration with dark iron- or manganese-oxide patches. Massive, non-cleaving cryptocrystalline quartz; specific gravity about 2.6.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, smoothly rounded, waxy to dull luster, gray-green, cream, tan, and reddish-brown coloration with dark iron- or manganese-oxide patches. Massive, non-cleaving cryptocrystalline quartz; specific gravity about 2.6.
Formation & geological history
Formed when silica-rich groundwater replaced or cemented fine sediment, commonly incorporating iron oxides and volcanic or clay impurities; later rounded naturally or by tumbling. Exact age and locality cannot be determined from the photograph.
Uses & applications
Used as ornamental stone, cabochons, beads, polished specimens, and decorative aggregate; attractive pieces typically have stronger pattern contrast and polish.
Geological facts
Jasper is an opaque variety of chalcedony or microcrystalline quartz, and its colors commonly reflect iron, manganese, chlorite, or clay minerals. The specimen appears human-tumbled or naturally water-worn rather than freshly fractured.
Field identification & locations
Identify by its opaque appearance, very fine texture, waxy polish, and inability to scratch glass only variably depending on surface weathering; it should resist a steel knife. Common sources include volcanic terrains and silica-rich gravels worldwide.
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