![Stilbite (Stilbite (Hydrated calcium sodium aluminum silicate, NaCa4[Al9Si27O72]·28H2O)) — mineral](https://media.rock.id/stilbite-5a06dea9-afb7-4c83-9d16-5ab7a10a8fb2-compressed.jpg)
mineral
Stilbite
Stilbite (Hydrated calcium sodium aluminum silicate, NaCa4[Al9Si27O72]·28H2O)
Hardness: 3.5–4 Mohs; Color: White, cream, or peach/light orange; Luster: Vitreous to pearly; Crystal structure: Monoclinic with characteristic bowtie or sheaf-like aggregates; Cleavage: Perfect in one direction.
- Hardness
- 3
- Color
- White, cream, or peach/light orange
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 3.5–4 Mohs; Color: White, cream, or peach/light orange; Luster: Vitreous to pearly; Crystal structure: Monoclinic with characteristic bowtie or sheaf-like aggregates; Cleavage: Perfect in one direction.
Formation & geological history
Formed as a secondary mineral in volcanic rocks, specifically in the cavities (vesicles) of basalt or andesite, through hydrothermal activity at relatively low temperatures.
Uses & applications
Primarily a collector's mineral and display specimen. Also used in industrial water filtration systems as a molecular sieve due to its zeolite structure.
Geological facts
Stilbite is a member of the zeolite group. Its name comes from the Greek word 'stilbein,' which means 'to shine,' referring to the pearly luster on its cleavage faces.
Field identification & locations
Identify by its distinctive 'bowtie' or 'wheat sheaf' crystal clusters and pearly luster. Commonly found in the Deccan Traps of India, Iceland, and the Faroe Islands. Collectors should avoid cleaning with acidic solutions which damage zeolites.
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Epidote
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