
mineral
Carnelian and White Quartz Bracelet
Silicon Dioxide (SiO2) - specifically Carnelian (Chalcedony) and Rock Crystal/Snow Quartz
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Translucent reddish-orange and opaque-to-milky white; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 – 2.7.
- Hardness
- 7 (Mohs scale)
- Color
- Translucent reddish-orange and opaque-to-milky white
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Translucent reddish-orange and opaque-to-milky white; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 – 2.7.
Formation & geological history
Formed through the deposition of silica-rich groundwater in volcanic rock cavities or sedimentary environments throughout various geological eras (Cretaceous to modern).
Uses & applications
Primarily used in jewelry, lapidary arts, and ornamental beadwork. Historically used for making signet rings, seals, and amulets due to its durability.
Geological facts
Carnelian was used as a gemstone in Ancient Egypt and Sumer; it was believed to give courage in battle. Quartz is the most abundant mineral in the Earth's continental crust.
Field identification & locations
Identify by its waxy luster and lack of cleavage. Common in Brazil, India, Madagascar, and Uruguay. Field collectors look for cryptocrystalline quartz nodules in riverbeds or volcanic outcrops.
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Sandstone (with potential mineral staining/concretions)
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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