
mineral
Agate (specifically Carnelian Agate or Sardagate)
Silicon dioxide (SiO2) - variety of chalcedony
Hardness: 6.5–7 (Mohs scale); Color: Orange, red, reddish-brown, and white concentric bands; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific gravity: 2.58–2.64
- Hardness
- 6
- Color
- Orange, red, reddish-brown, and white concentric bands
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Orange, red, reddish-brown, and white concentric bands; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific gravity: 2.58–2.64
Formation & geological history
Formed in gas cavities (vesicles) of volcanic rocks (basalts/andesites) where silica-rich fluids deposit layers over time. The red/orange hue comes from iron oxide impurities. Most specimens are from the Phanerozoic eon.
Uses & applications
Used primarily in jewelry (cabochons), lapidary arts, decorative items (coasters, bookends), and historically for cylinder seals and amulets.
Geological facts
The name 'Carnelian' comes from the Latin word 'carne' meaning flesh, due to its reddish tint. Agates have been used by humans as gemstones for over 3,000 years, with the famous 'Lake Superior Agate' being highly sought after in North America.
Field identification & locations
Identify in the field by looking for a waxy luster, translucent edges when held to light, and distinct concentric banding. Common locations include Brazil, Uruguay, India, and the Lake Superior region of the USA.
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