
mineral
Grape Agate (Amethystine Chalcedony)
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Pale lavender, white, or light gray; Luster: Waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None (Conchoidal fracture); Habit: Botryoidal (grape-like) aggregates.
- Hardness
- 6
- Color
- Pale lavender, white, or light gray
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Pale lavender, white, or light gray; Luster: Waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None (Conchoidal fracture); Habit: Botryoidal (grape-like) aggregates.
Formation & geological history
Formed through volcanic processes in the cavities of andesite or basalt. Silica-rich hydrothermal fluids precipitate in voids, creating spherical aggregates. Most specimens date from the Miocene epoch.
Uses & applications
Primarily used as decorative specimens for collectors, metaphysical use, and high-end artisanal lapidary work.
Geological facts
Despite the name 'Grape Agate,' it is technically a botryoidal chalcedony rather than a true banded agate. It was only discovered/marketed widely from Indonesia (the Manakarra region) around 2016.
Field identification & locations
Identified by its unique 'bubbly' or tiny ball-like surface texture. Look for the distinctive botryoidal habit and the characteristic violet or pale waxy white color. Mostly found in Indonesia.
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