
Mineral
Botryoidal Black Chalcedony Geode (Black Grape Agate)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Black to dark charcoal grey; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Habit: Botryoidal (grape-like clusters); Specific Gravity: 2.6-2.65
- Hardness
- 6
- Color
- Black to dark charcoal grey
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Black to dark charcoal grey; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Habit: Botryoidal (grape-like clusters); Specific Gravity: 2.6-2.65
Formation & geological history
Formed through the precipitation of silica from groundwater in volcanic cavities or sedimentary pockets. These often form in basaltic gas bubbles (vesicles) over millions of years. This specific specimen likely originates from Indonesian or Moroccan volcanic deposits.
Uses & applications
Primary use is for lapidary work, high-end interior decoration, and metaphysical crystal collecting. It is popular in jewelry when sliced or cabbed to show the internal banding.
Geological facts
The term 'botryoidal' comes from the Greek word 'botrys,' meaning a bunch of grapes. While clear or white chalcedony is common, the deep black coloration is caused by inclusions of minerals like manganese oxide or iron during the formation process.
Field identification & locations
Identify by its 'bubbly' or rounded surface texture and high hardness (it cannot be scratched by a steel knife). Look for the lack of visible crystal faces, which distinguishes it from black quartz or tourmaline. Commonly found in Indonesia, Brazil, and Morocco.
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