
mineral
Howlite
Calcium borosilicate hydroxide (Ca2B5SiO9(OH)5)
AI-generated identification · may be incorrectHardness: 3.5 on Mohs scale; Color: Chalky white with fine grey or black veining; Luster: Sub-vitreous to pearly; Crystal structure: Monoclinic (usually found in nodules); Cleavage: Indistinct; Specific Gravity: 2.53–2.59
- Hardness
- 3
- Color
- Chalky white with fine grey or black veining
- Luster
- Sub-vitreous to pearly
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Physical properties
Hardness: 3.5 on Mohs scale; Color: Chalky white with fine grey or black veining; Luster: Sub-vitreous to pearly; Crystal structure: Monoclinic (usually found in nodules); Cleavage: Indistinct; Specific Gravity: 2.53–2.59
Formation & geological history
Howlite is an evaporite mineral, typically forming in continental salt lakes and arid environments from alkaline solutions enriched with boron. It is commonly found in nodules that look like cauliflower heads.
Uses & applications
Predominantly used for ornamental purposes, such as jewelry, beads, and figurines. Because of its porous nature, it is frequently dyed blue to imitate Turquoise or red to imitate Coral.
Geological facts
It was first discovered near Windsor, Nova Scotia, in 1868 by Henry How, a Canadian mineralogist, for whom it is named. Natural howlite is often called 'White Turquoise' by vendors, though it is chemically unrelated.
Field identification & locations
Identify in the field by its distinctive 'spider-web' or 'matrix' veining and chalky texture. It is softer than quartz and will not scratch glass. Common locations include Nova Scotia, Canada, and various sites in California and Nevada, USA.
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