
mineral
Prehnite
Prehnite - Ca2Al(AlSi3O10)(OH)2
Hardness: 6-6.5 on Mohs scale; Color: Pale green to yellow-green, translucent to semi-transparent; 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, translucent to semi-transparent
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Pale green to yellow-green, translucent to semi-transparent; Luster: Vitreous to pearly; Crystal structure: Orthorhombic; Cleavage: Good in one direction; Specific gravity: 2.80 - 2.95.
Formation & geological history
Formed as a secondary mineral in hydrothermal veins and cavities within mafic volcanic rocks (like basalt). It typically occurs in low-grade metamorphic environments and is often associated with zeolites.
Uses & applications
Primarily used as a semi-precious gemstone in jewelry, such as beads, cabochons, and carvings. It is also highly sought after by mineral collectors for its unique globular or 'botryoidal' crystal habits.
Geological facts
Prehnite was the first mineral to be named after a person (Colonel Hendrik Von Prehn) and was first discovered in South Africa in the late 18th century. It is sometimes referred to as 'Grape Jade' due to its common round growth habit.
Field identification & locations
Identify by its distinct pale 'sea-foam' green color and its tendency to form in rounded, translucent aggregates. Common locations include South Africa, Australia (Wave Hill), USA (New Jersey), and Scotland.
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