
mineral
Agate (Geode nodule fragment)
Chalcedony (cryptocrystalline variety of Quartz), SiO2
Hardness: 6.5-7 on Mohs scale; Color: Creamy white, grey, and translucent with brown inclusions; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.64
- Hardness
- 6
- Color
- Creamy white, grey, and translucent with brown inclusions
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Creamy white, grey, and translucent with brown inclusions; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.64
Formation & geological history
Formed as a secondary deposit in cavities within volcanic or sedimentary rocks. Silica-rich groundwater percolates through voids, depositing layers of chalcedony over thousands to millions of years.
Uses & applications
Commonly used in lapidary work, jewelry (beads, cabochons), metaphysical collecting, and historically for mortar and pestles due to hardness.
Geological facts
Agates often form 'thunder eggs' and are characterized by their concentric banding, though this specimen appears to be a section of a small nodule or geode center with an inclusion or iron staining.
Field identification & locations
Identify in the field by its waxy luster, translucency when held to light, and its ability to scratch glass. Commonly found in riverbeds, desert pavements, and near ancient volcanic sites.
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