Rock Identifier
Yellow Chalcedony (Carnelian/Yellow Agate) (Silicon Dioxide (SiO2) - Microcrystalline Quartz) — Mineral
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
Identified More mineral

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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.