
sedimentary
Polished or naturally smoothed jasper/chalcedony pebble
Microcrystalline quartz (SiO₂), likely iron-stained jasper with chalcedony
AI-generated identification · may be incorrectOpaque cream, orange, yellow, and dark green-black mottling; waxy to slightly vitreous luster and no visible cleavage. Quartz hardness is about 6.5–7 Mohs, with a fine-grained cryptocrystalline structure; the dark areas may include iron or manganese oxides and other inclusions.
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Physical properties
Opaque cream, orange, yellow, and dark green-black mottling; waxy to slightly vitreous luster and no visible cleavage. Quartz hardness is about 6.5–7 Mohs, with a fine-grained cryptocrystalline structure; the dark areas may include iron or manganese oxides and other inclusions.
Formation & geological history
Formed when silica-rich groundwater filled cavities or replaced material in volcanic or sedimentary rocks, with iron and other impurities creating the colors. Exact geological age and locality cannot be determined from the image.
Uses & applications
Used for cabochons, beads, carvings, tumbled stones, and decorative objects; attractive patterned pieces have modest jewelry and collecting value.
Geological facts
The orange-red coloration commonly reflects hematite or limonite, while green-black patches may represent chlorite, epidote, manganese oxides, or matrix minerals. A glassy scratch test can help distinguish quartz-rich jasper from softer decorative stone.
Field identification & locations
Commonly found in silica-rich volcanic terrains, river gravels, and agate/jasper deposits worldwide. Identify by its opaque fine texture, strong hardness, waxy luster, and resistance to scratching by a steel knife.
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