
sedimentary
Yellow Jasper
SiO2 (Silicon Dioxide)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Yellow, mustard, or sandy gold with spots/streaks; Luster: Dull/Greasy (raw) to Vitreous (polished); Crystal Structure: Hexagonal (Trigonal); Cleavage: None; SG: 2.58-2.91
- Hardness
- 6
- Color
- Yellow, mustard, or sandy gold with spots/streaks
- Luster
- Dull/Greasy (raw) to Vitreous (polished)
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Yellow, mustard, or sandy gold with spots/streaks; Luster: Dull/Greasy (raw) to Vitreous (polished); Crystal Structure: Hexagonal (Trigonal); Cleavage: None; SG: 2.58-2.91
Formation & geological history
Yellow jasper is a microcrystalline variety of quartz. It forms through the accumulation of silica-rich fluids in volcanic or sedimentary environments, where mineral impurities (mostly iron oxides like goethite) provide the yellow pigmentation. These deposits often date from the Precambrian to recent eras.
Uses & applications
Primary uses include lapidary work for jewelry (beads, cabochons), metaphysical products (worry stones, meditation tools), and decorative ornamental objects.
Geological facts
Jasper is known as the 'Supreme Nurturer.' The yellow color specifically comes from inclusions of iron-rich ochre or hydrated iron oxides. It has been used historically by travelers and shamans as a protective talisman.
Field identification & locations
To identify in the field, look for an opaque mineral with a conchoidal (shell-like) fracture that cannot be scratched by a steel knife. It is commonly found in India, Russia, Brazil, France, and the USA (California and Oregon).
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