
sedimentary
Yellow jasper (likely iron-stained chert)
Microcrystalline quartz (SiO₂), chiefly chalcedony/quartz with iron-oxide pigments
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; mustard-yellow, opaque, and waxy to dull luster with a fine, massive texture. No visible cleavage; conchoidal fracture is expected, with specific gravity near 2.6.
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Physical properties
Hardness about 6.5–7 Mohs; mustard-yellow, opaque, and waxy to dull luster with a fine, massive texture. No visible cleavage; conchoidal fracture is expected, with specific gravity near 2.6.
Formation & geological history
Forms when silica-rich groundwater replaces or cements sediment, commonly incorporating goethite or hematite that produces the yellow color. It may range from Paleozoic to Cenozoic in age depending on locality.
Uses & applications
Used as ornamental stone, cabochons, beads, carvings, and tumbled specimens; too small here for construction use.
Geological facts
Jasper is an opaque variety of chalcedony/chert rather than a single strictly defined mineral. Yellow coloration commonly reflects hydrated iron oxides.
Field identification & locations
Identify by its opaque fine grain, silica-like hardness, and inability to scratch with a steel knife; it should scratch glass, though this test can damage the specimen. Common in volcanic and sedimentary terrains worldwide, including the western United States, Brazil, India, and Madagascar.
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