
mineral
Chalcedony (Agate/Chert)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: White, tan, and yellowish-brown with translucent areas, Luster: Waxy to vitreous, Crystal structure: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific gravity: 2.58-2.64
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: White, tan, and yellowish-brown with translucent areas, Luster: Waxy to vitreous, Crystal structure: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific gravity: 2.58-2.64
Formation & geological history
Formed via the deposition of silica from groundwater in cavities or veins of volcanic or sedimentary rocks. It often occurs as nodules or botryoidal masses as silica-rich fluids precipitate over time.
Uses & applications
Used frequently in lapidary work, jewelry (beads and cabochons), and as a collector's specimen. Historically used for making stone tools due to its sharp conchoidal fracture.
Geological facts
Agate and Chalcedony are often called 'earth diamonds' by rockhounds due to their durability. This specific piece shows characteristic iron staining and a smooth, water-worn texture likely from a riverbed.
Field identification & locations
Identify in the field by its waxy luster, translucency when held to a light source, and inability to be scratched by a steel knife. Common in gravel pits, riverbeds, and volcanic regions.
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Sandstone (with potential mineral staining/concretions)
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Epidote
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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