
mineral
Botryoidal Chalcedony in Geode/Vug
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs); Color: Waxy tan to brownish-yellow interior; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Waxy tan to brownish-yellow interior
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Waxy tan to brownish-yellow interior; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
Formation & geological history
Formed by the low-temperature deposition of silica-rich groundwater within cavities of volcanic or sedimentary rocks. The botryoidal (grape-like) texture occurs as mineral layers grow outward from multiple nuclei simultaneously.
Uses & applications
Commonly used as a semi-precious gemstone in jewelry (cabochons), for decorative carvings, and as popular specimens for mineral collectors.
Geological facts
The term 'botryoidal' comes from the Greek word 'botrys,' meaning a bunch of grapes. Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen under a standard microscope.
Field identification & locations
Identify in the field by its waxy luster, rounded bubble-like surface, and hardness (it will scratch glass). Commonly found in desert regions, volcanic ash beds, and inside geodes or hollowed agates.
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