
sedimentary
Jasper (likely yellow-brown jasper/chert)
Microcrystalline quartz (chalcedony), SiO₂, colored by iron oxides and other impurities
AI-generated identification · may be incorrectOpaque mustard-brown to olive-brown, earthy to waxy luster, massive with no visible crystals or cleavage; Mohs hardness about 6.5–7, specific gravity approximately 2.6. The rounded, polished appearance suggests natural water wear or tumbling.
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Physical properties
Opaque mustard-brown to olive-brown, earthy to waxy luster, massive with no visible crystals or cleavage; Mohs hardness about 6.5–7, specific gravity approximately 2.6. The rounded, polished appearance suggests natural water wear or tumbling.
Formation & geological history
Forms when silica-rich groundwater fills cavities or replaces sediments, with iron oxides producing the brown-yellow coloration; commonly Precambrian to younger, depending on locality. This specimen may also be iron-rich chert or weathered jasper.
Uses & applications
Used as ornamental stone, beads, cabochons, carvings, lapidary material, and occasionally decorative aggregate; too small and irregular for construction use.
Geological facts
Jasper is a variety of opaque chalcedony and is defined more by appearance and texture than by a single chemical impurity. Its colors commonly reflect hematite, goethite, clay, or manganese minerals.
Field identification & locations
Identify it by its opaque appearance, glassy-to-waxy fracture, lack of cleavage, and ability to scratch ordinary glass; it should not fizz in dilute hydrochloric acid. Common in volcanic terrains, sedimentary iron formations, and river gravels worldwide.
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