
sedimentary
Polished jasper pebble
Jasper (microcrystalline quartz, SiO₂)
AI-generated identification · may be incorrectOpaque, smooth brown-and-tan pebble with subtle internal veining and a lighter outer rind; quartz hardness is 6.5–7 Mohs, with a waxy to vitreous luster and no visible cleavage. Jasper is microcrystalline and has a trigonal crystal structure.
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Physical properties
Opaque, smooth brown-and-tan pebble with subtle internal veining and a lighter outer rind; quartz hardness is 6.5–7 Mohs, with a waxy to vitreous luster and no visible cleavage. Jasper is microcrystalline and has a trigonal crystal structure.
Formation & geological history
Jasper forms when silica-rich fluids or sediments become mineralized, often with iron oxides adding color; it occurs in deposits of many geological ages. The pebble has been naturally rounded and then polished.
Uses & applications
Used for beads, cabochons, ornaments, and lapidary collecting; jasper is not generally used as structural stone.
Geological facts
Jasper is an opaque variety of chalcedony, and its colors and patterns vary widely with mineral impurities.
Field identification & locations
Look for an opaque, dense, fine-grained surface and earthy patterns rather than distinct crystals; common sources include Brazil, India, Madagascar, and the western United States. A small polished pebble like this typically sells for about $2–$15 USD.
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