
mineral
Chalcedony (Agate/Carnelian variant)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Translucent grey, white, and orange; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Translucent grey, white, and orange
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Translucent grey, white, and orange; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.
Formation & geological history
Formed from the deposition of silica from groundwater in cavities of volcanic and sedimentary rocks. This specimen shows typical cryptocrystalline structure associated with low-temperature hydrothermal environments.
Uses & applications
Used primarily in lapidary arts for jewelry, carvings, and tumbled stones. Historically used for making tools due to its conchoidal fracture and hardness.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen even under a microscope. It has been used for seals and jewelry for thousands of years, dating back to the Bronze Age in the Mediterranean.
Field identification & locations
Identify in the field by its waxy luster, translucency, and lack of visible grains. It often occurs as nodules or fillings in rock cavities. Found globally, particularly in volcanic regions like the Pacific Northwest, Brazil, and India.
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