
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with iron inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Mustard yellow to golden brown. Luster: Vitreous to waxy. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Mustard yellow to golden brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Mustard yellow to golden brown. Luster: Vitreous to waxy. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
Formation & geological history
Formed primarily in sedimentary environments when silica-rich fluids permeate through volcanic ash or other porous materials, gradually replacing organic material or filling cavities. The yellow color is caused by the presence of Goethite or other iron oxides.
Uses & applications
Used extensively as a gemstone for jewelry (cabochons, beads), decorative carvings, lapidary arts, and as a collector's specimen. In industry, it was historically used for flintknapping tools due to its conchoidal fracture.
Geological facts
Yellow jasper has been used throughout history as a stone of protection and discernment. It is a variety of chalcedony and is often found as smooth river stones due to its durability against erosion.
Field identification & locations
Identify in the field by its opaque appearance, waxy luster, and lack of cleavage (smooth, curved break surfaces). It is common in the Pacific Northwest of the USA, Africa, and Brazil. Collectors should look for patterns like dendritic inclusions or orbicular structures.
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