
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7.0 (Mohs); Color: Yellow to mustard-brown with dark dendritic or spotty inclusions; Luster: Vitreous to waxy; Crystal Structure: Hexagonal (Microcrystalline quartz); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7.0 (Mohs); Color: Yellow to mustard-brown with dark dendritic or spotty inclusions; Luster: Vitreous to waxy; Crystal Structure: Hexagonal (Microcrystalline quartz); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the accumulation of fine-grained silica in sedimentary environments like hydrothermal veins or volcanic ash beds. The yellow color results from high concentrations of Goethite or Limonite (iron hydroxides) within the silicate structure.
Uses & applications
Commonly used for lapidary work, cabochons, polished river stones, decorative ornaments, and metaphysical jewelry.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'Jasper' is derived from the Greek word 'iaspis', meaning spotted stone. It has been used by ancient civilizations for seals and talismans for over 5000 years.
Field identification & locations
Identify by its opacity (does not let light through even at edges), distinctive earthy yellow hue, and smooth, waxy surface after tumbling. It is often found as rounded cobbles in riverbeds or gravel deposits in volcanic regions.
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