
mineral
Prehnite
Prehnite (Ca2Al(AlSi3O10)(OH)2)
Hardness: 6-6.5 on Mohs scale; Color: Pale green to yellow-green; Luster: Vitreous to pearly; Crystal structure: Orthorhombic; Cleavage: Good in one direction; Specific gravity: 2.80-2.95.
- Hardness
- 6-6
- Color
- Pale green to yellow-green
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Pale green to yellow-green; Luster: Vitreous to pearly; Crystal structure: Orthorhombic; Cleavage: Good in one direction; Specific gravity: 2.80-2.95.
Formation & geological history
Formed in low-grade metamorphic conditions, typically in cavities and veins of mafic volcanic rocks (basalt). It is a secondary mineral resulting from the hydrothermal alteration of plagioclase feldspars.
Uses & applications
Primarily used as a gemstone for jewelry (cabochons and beads) and as a decorative collector's specimen. It was also once used as a minor ore of aluminum in specific contexts.
Geological facts
Prehnite was the first mineral to be named after a person (Colonel Hendrik von Prehn) in 1788. It often forms 'botryoidal' (grape-like) clusters and is frequently found associated with Zeolites.
Field identification & locations
Identify in the field by its distinct oil-green color, brittle tenacity, and appearance in volcanic gas bubbles (amygdules). Common locations include South Africa, Australia, and the United States (New Jersey/Virginia).
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