
sedimentary
Polished picture jasper slab
Silicified/lithified microcrystalline quartz (chalcedony), commonly with iron-oxide and clay-mineral bands
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque cream, brown, red, and yellow with intricate flowing patterns; waxy to dull luster and no visible cleavage. The patterned appearance reflects fine-grained quartz and iron-oxide inclusions rather than large crystals.
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Physical properties
Hardness about 6.5–7 Mohs; opaque cream, brown, red, and yellow with intricate flowing patterns; waxy to dull luster and no visible cleavage. The patterned appearance reflects fine-grained quartz and iron-oxide inclusions rather than large crystals.
Formation & geological history
Likely formed from silica-rich sediment or volcanic ash that was compacted and cemented, then variably replaced by chalcedony and stained by iron oxides. Exact geological age and locality cannot be determined from the photograph; picture jasper occurs in many volcanic-sedimentary terrains.
Uses & applications
Used for cabochons, beads, carvings, polished slabs, and decorative objects; occasionally sold as lapidary rough. It is primarily an ornamental collectible rather than a construction stone.
Geological facts
The natural, landscape-like banding is called “picture” or scenic jasper; similar material may be marketed as scenic jasper, scenic agate, or petrified wood depending on texture and locality.
Field identification & locations
Identify it by its opaque fine-grained body, hardness, smooth conchoidal fracture, and red-brown iron staining; a steel file should not easily scratch it. Common sources include Oregon and Idaho, USA, Mexico, Madagascar, and Australia.
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