
metamorphic
Polished brecciated jasper (likely picture jasper)
Silica-rich microcrystalline quartz/chalcedony, SiO₂, with iron-oxide and clay inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, reddish-brown, cream, gray-green, and black banding with a waxy to vitreous polish. Massive microcrystalline quartz has no visible cleavage; specific gravity is roughly 2.5–2.7.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, reddish-brown, cream, gray-green, and black banding with a waxy to vitreous polish. Massive microcrystalline quartz has no visible cleavage; specific gravity is roughly 2.5–2.7.
Formation & geological history
Formed when silica-rich fluids replaced or cemented fine sediment and breccia, with iron oxides producing the red-brown colors; the exact geological age depends on locality. This example is tumbled and polished.
Uses & applications
Used for cabochons, beads, carvings, ornamental objects, and lapidary collections; it has little industrial value compared with bulk quartz.
Geological facts
Jasper is an opaque variety of chalcedony or microcrystalline quartz, and its patterns commonly reflect sedimentary layering, fractures, and mineral replacement.
Field identification & locations
Identify it by its opaque patterned appearance, glassy polish, lack of cleavage, and resistance to scratching; common sources include Oregon, Utah, Idaho, Madagascar, and Australia. A steel file generally will not scratch it.
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