
mineral
Yellow Agate
Agate (Microcrystalline Silicon Dioxide, SiO2)
Hardness: 6.5–7 (Mohs scale); Color: Translucent yellow with milky white concentric banding; Luster: Vitreous to waxy; Structure: Cryptocrystalline trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Translucent yellow with milky white concentric banding
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Translucent yellow with milky white concentric banding; Luster: Vitreous to waxy; Structure: Cryptocrystalline trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
Formation & geological history
Formed through the deposition of silica from groundwater into cavities (vugs) within volcanic lavas or metamorphic rocks. The distinct yellow hue is often caused by trace amounts of iron oxides or inclusions. Common across many geological ages from the Precambrian to Cenozoic.
Uses & applications
Predominantly used for ornamental purposes, including jewelry (pendants, beads), decorative carvings, and as 'healing' crystals in holistic communities. Historically used in precise balances and mortars due to its hardness.
Geological facts
Agate is named after the Achates River in Sicily where it was first discovered. The circular patterns visible on this specimen are characteristic of the 'eye' or 'banding' effect that occurs as silica-rich fluids cool and solidify in layers.
Field identification & locations
Identify in the field by its waxy appearance, translucency, and inability to be scratched by a steel knife. It is commonly found in riverbeds, shorelines, or areas with former volcanic activity. Popular locations include Brazil, India, and the Midwestern USA.
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