Rock Identifier
Polished jasper pebble (Jasper, microcrystalline quartz (SiO₂), commonly with iron-oxide impurities) — metamorphic
metamorphic

Polished jasper pebble

Jasper, microcrystalline quartz (SiO₂), commonly with iron-oxide impurities

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; opaque burgundy, gray, cream, and brown coloration with fine brecciation or veining; typically dull to waxy luster and no visible cleavage. The rounded, smooth surface indicates water wear or tumbling/polishing.

Identified More metamorphic
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Physical properties

Hardness about 6.5–7 Mohs; opaque burgundy, gray, cream, and brown coloration with fine brecciation or veining; typically dull to waxy luster and no visible cleavage. The rounded, smooth surface indicates water wear or tumbling/polishing.

Formation & geological history

Jasper forms when silica-rich fluids replace or cement fine-grained sediments or volcanic material, with iron oxides producing red and brown colors. Most specimens are geologically ancient, commonly Paleozoic to Mesozoic, though age depends on locality.

Uses & applications

Used as a lapidary stone for cabochons, carvings, beads, tumbled stones, and decorative objects; occasionally used for ornamental architectural work.

Geological facts

Jasper is a variety of chert distinguished by its opacity and abundant impurities. The cream-colored patches may represent quartz-rich material, alteration zones, or breccia fragments.

Field identification & locations

Identify it by its opaque appearance, very fine texture, waxy luster, and resistance to scratching; it should not be scratched easily by a steel knife. Common sources include India, Madagascar, Brazil, the western United States, and Australia.