
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with iron oxide inclusions
Hardness: 6.5-7 (Mohs scale); Color: Opaque mustard yellow to brownish-yellow; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None; Specific gravity: 2.58–2.91
- Hardness
- 6
- Color
- Opaque mustard yellow to brownish-yellow
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Opaque mustard yellow to brownish-yellow; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None; Specific gravity: 2.58–2.91
Formation & geological history
Formed typically in sedimentary environments when silica-rich fluids permeate through volcanic ash or mud, gradually precipitating quartz over millions of years. The yellow color is due to high iron hydroxide (goethite/limonite) content.
Uses & applications
Commonly used in jewelry (cabochons, pendants), decorative carvings, and as a popular choice for lapidary work due to its ability to take a high polish.
Geological facts
Jasper is a variety of chalcedony. In ancient times, yellow jasper was often associated with protection during travel and was believed to harbor the power of the sun. Unlike most translucent agates, jasper is defined by its opacity.
Field identification & locations
Identify in the field by its smooth, conchoidal fracture, high hardness (cannot be scratched by a steel knife), and opaque appearance. Frequently found in riverbeds and coastal regions of South Africa, Brazil, and the USA.
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