
sedimentary
Jasper pebble
Silicon Dioxide (SiO2 with iron oxide inclusions)
Hardness of 6.5 to 7 on the Mohs scale, earthy to sub-vitreous or waxy luster, opaque, sub-conchoidal fracture, microcrystalline quartz aggregate structure. Displays a dual-tone reddish-brown and dark charcoal hue.
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Physical properties
Hardness of 6.5 to 7 on the Mohs scale, earthy to sub-vitreous or waxy luster, opaque, sub-conchoidal fracture, microcrystalline quartz aggregate structure. Displays a dual-tone reddish-brown and dark charcoal hue.
Formation & geological history
Formed through the deposition of silica from water solutions into cracks, cavities, or volcanic ash layers, enriched with hematite and other iron minerals which impart the deep red and dark colors. Typically water-worn and rounded in riverbeds or coastal environments.
Uses & applications
Used widely for lapidary arts, tumbling, jewelry making (cabochons and beads), decorative stone carvings, and personal rock collections.
Geological facts
Jasper is an opaque variety of chalcedony that gets its distinctive red, brown, and yellow colors from iron oxide inclusions. Rounded smooth river-pebble forms like this are popular among rockhounds and tumblers.
Field identification & locations
Identified by its high hardness (cannot be scratched by a steel nail), smooth water-rounded surface, completely opaque body, and rich reddish-brown coloration. Commonly found in gravel bars, riverbeds, beaches, and glaciated regions near iron-bearing volcanic or sedimentary deposits.
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