
mineral
Turquenite (Dyed Howlite)
Dyed Ca2B5SiO9(OH)5 (Calcium Borosilicate Hydroxide)
AI-generated identification · may be incorrectHardness: 3.5 (Mohs scale), Color: Sky blue to turquoise (surface dyed), Luster: Sub-vitreous to earthy, Crystal Structure: Monoclinic (usually massive), Cleavage: None/Indistinct, Specific Gravity: 2.58
- Hardness
- 3
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Physical properties
Hardness: 3.5 (Mohs scale), Color: Sky blue to turquoise (surface dyed), Luster: Sub-vitreous to earthy, Crystal Structure: Monoclinic (usually massive), Cleavage: None/Indistinct, Specific Gravity: 2.58
Formation & geological history
Formed in evaporite deposits as nodules. Natural howlite is white with grey/black veins; the specimen shown is an imitation turquoise created by immersion in blue dye under pressure.
Uses & applications
Primarily used in costume jewelry, beadwork, decorative carvings, and as a 'healing stone' in metaphysical markets. It is a common substitute for genuine turquoise.
Geological facts
Natural howlite was discovered in 1868 by Henry How. It is a very porous mineral, which makes it perfect for taking dye. When dyed blue, it is often sold as 'Turquenite' or 'Magnesite' (though true Magnesite is a different mineral).
Field identification & locations
Identify by performing a 'rub test' with acetone on a cotton swab; if color comes off, it is dyed. Real turquoise is much harder (5-6) and cool to the touch. It is widely available at gem shows and craft stores.
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