
sedimentary
Tumbled jasper, likely brecciated or mookaite jasper
Microcrystalline quartz (SiO₂) with iron-oxide inclusions; possibly brecciated jasper
AI-generated identification · may be incorrectOpaque reddish-brown and cream stone with a polished, waxy-to-vitreous luster and irregular color patches. Quartz hardness is about 6.5–7 Mohs; no visible cleavage, conchoidal fracture, and typical specific gravity near 2.6.
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Physical properties
Opaque reddish-brown and cream stone with a polished, waxy-to-vitreous luster and irregular color patches. Quartz hardness is about 6.5–7 Mohs; no visible cleavage, conchoidal fracture, and typical specific gravity near 2.6.
Formation & geological history
Jasper forms when silica-rich groundwater replaces or cements sediment and volcanic material, with iron oxides producing red-brown colors; brecciated varieties preserve angular fragments. Formation ages vary widely, commonly Paleozoic to Mesozoic or younger depending on locality.
Uses & applications
Used for cabochons, beads, ornaments, carvings, and inexpensive tumbled-stone collections; occasionally used as decorative facing stone.
Geological facts
The image shows a polished/tumbled specimen, so natural surface texture and diagnostic crystal grains are largely concealed. Exact variety and locality cannot be confirmed from appearance alone.
Field identification & locations
Identify by its opacity, fine texture, red-brown iron staining, and resistance to scratching; it should not be scratched by a steel knife easily. Common sources include Australia, Brazil, Madagascar, India, and the western United States.
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