
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with iron hydroxides
AI-generated identification · may be incorrectHardness: 6.5-7.0 (Mohs scale), Color: dull mustard yellow to golden brown, Luster: dull to vitreous, Crystal Structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: none (conchoidal fracture), Specific Gravity: 2.58-2.91
- Hardness
- 6
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Physical properties
Hardness: 6.5-7.0 (Mohs scale), Color: dull mustard yellow to golden brown, Luster: dull to vitreous, Crystal Structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: none (conchoidal fracture), Specific Gravity: 2.58-2.91
Formation & geological history
Formed from the deposition of silica-rich fluids in volcanic or sedimentary environments, often associated with hydrothermal activity. The yellow color is due to the presence of goethite or other iron hydroxides. It can form in various geological ages ranging from Precambrian to Cenozoic.
Uses & applications
Commonly used for lapidary work, jewelry (cabochons), carvings, metaphysical collecting, and as a durable material for decorative ornamentation.
Geological facts
Yellow jasper is a variety of chalcedony that is opaque due to high mineral inclusions. It has been used since ancient times for both ornamental and protective amulets. It is often found in banded patterns known as Picture Jasper.
Field identification & locations
Identified in the field by its hardness (it will scratch glass), its opaque nature, and its distinct smooth, waxy fracture surface. Common locations include South Africa, India, USA (Oregon, Idaho), and Brazil.
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