
mineral
Orbicular jasper (polished jasper slab)
Orbicular jasper; microcrystalline quartz/chalcedony (SiO₂) with iron-oxide and other mineral inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, waxy to dull luster, with cream, gray-green, salmon-red, and brown concentric orbicules. It has a cryptocrystalline quartz structure and no obvious cleavage; density is typically about 2.5–2.7.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, waxy to dull luster, with cream, gray-green, salmon-red, and brown concentric orbicules. It has a cryptocrystalline quartz structure and no obvious cleavage; density is typically about 2.5–2.7.
Formation & geological history
Forms when silica-rich volcanic or hydrothermal fluids replace or cement volcanic rock, producing radiating/concentric mineral aggregates; iron oxides create the red coloration. Specific age depends on locality, commonly Paleozoic to Cenozoic.
Uses & applications
Used for cabochons, beads, carvings, decorative slabs, and lapidary displays; attractive patterns give quality pieces modest collector value.
Geological facts
The orbicules are mineral-rich growth zones, not fossils; patterns vary greatly even within one deposit.
Field identification & locations
Identify by testing for quartz-like hardness, opaque fine-grained texture, and natural concentric orbs in a silicified matrix. Similar material occurs in Madagascar, Mexico, Australia, Indonesia, and the western United States.
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