
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with iron hydroxides (Goethite or Limonite)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Mustard yellow to golden brown, Luster: Dull to waxy, Crystal structure: Microcrystalline/Cryptocrystalline (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58–2.91
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Mustard yellow to golden brown, Luster: Dull to waxy, Crystal structure: Microcrystalline/Cryptocrystalline (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58–2.91
Formation & geological history
Formed from the deposition of silica-rich fluids in volcanic ash or sedimentary basins. Its mustard yellow hue is typically caused by inclusion of goethite (hydrated iron oxide). It can range from millions to hundreds of millions of years in age depending on the deposit.
Uses & applications
Used primarily in lapidary arts for cabochons, beads, and decorative carvings. Industrially used as an abrasive or in minor construction fill, and highly valued in spiritual 'crystal healing' communities.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'jasper' comes from the Greek 'iaspis', meaning 'spotted stone.' Yellow jasper was traditionally used as a stone of protection and travelers' luck.
Field identification & locations
Identify in the field by its opacity (does not let light through, unlike agate), smooth water-worn texture on beaches, and extreme hardness—it will easily scratch a glass bottle or steel knife. Common in riverbeds and along Pacific Northwest coastlines.
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