
Mineral
Yellow Chalcedony (Carnelian/Yellow Agate)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 6.5–7 (Mohs scale); Color: Yellow to golden-orange; Luster: Vitreous to waxy; Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None; Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Yellow to golden-orange
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Yellow to golden-orange; Luster: Vitreous to waxy; Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None; Specific Gravity: 2.58–2.64.
Formation & geological history
Formed through the deposition of silica from groundwater in cavities of igneous or sedimentary rocks. This specimen is likely from a volcanic or hydrothermal environment where silica-rich fluids cooled slowly. Geologically, these can range from very young to hundreds of millions of years old.
Uses & applications
Primarily used in jewelry as cabochons, beads, and carvings. Also used in industrial applications for precision bearings and pivot points due to its hardness, and highly valued by gem collectors.
Geological facts
Yellow chalcedony is often associated with sun deities in ancient cultures. While technically a form of Agate if banded, when it is solid and translucent like this, it is referred to simply as Chalcedony. The yellow hue is often caused by trace amounts of iron hydroxides (limonite).
Field identification & locations
Identify by its waxy luster, translucency, and lack of visible crystal faces. It is common in regions with volcanic activity like India, Brazil, and Madagascar. Collectors look for uniform color and high translucency with minimal internal inclusions.
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