
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with Goethite/Iron inclusions
Hardness: 6.5-7 (Mohs scale); Color: Mustard yellow, tan, or ochre; Luster: Dull to vitreous; Crystal Structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Mustard yellow, tan, or ochre
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Mustard yellow, tan, or ochre; Luster: Dull to vitreous; Crystal Structure: Microcrystalline (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 environments. The yellow color is primarily due to the presence of goethite or other iron hydroxide minerals throughout the quartz matrix.
Uses & applications
Commonly used for lapidary work including cabochons, beads, and carvings. In metaphysical circles, it is used as a grounding stone. Historically used for making stone tools due to its conchoidal fracture.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'jasper' is derived from the Greek for 'spotted stone.' Large deposits are found in South Africa, Brazil, and the United States (Oregon and Idaho).
Field identification & locations
Identify in the field by its opacity (even on thin edges), smooth conchoidal fracture, and inability to be scratched by a steel knife. It is often found as water-worn pebbles in riverbeds or as nodules in volcanic rock.
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