
mineral
Howlite
Howlite (Calcium borosilicate hydroxide, Ca2B5SiO9(OH)5)
Hardness: 3.5 on Mohs scale; Color: White to milky grey with dark grey or black veins; Luster: Sub-vitreous to dull; Crystal Structure: Monoclinic; Cleavage: None; Specific Gravity: 2.53-2.59
- Hardness
- 3
- Color
- White to milky grey with dark grey or black veins
- Luster
- Sub-vitreous to dull
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Physical properties
Hardness: 3.5 on Mohs scale; Color: White to milky grey with dark grey or black veins; Luster: Sub-vitreous to dull; Crystal Structure: Monoclinic; Cleavage: None; Specific Gravity: 2.53-2.59
Formation & geological history
Formed in evaporite deposits in arid environments through the evaporation of boron-rich waters. Primarily found in sedimentary basins and often occurs in nodules that resemble cauliflower.
Uses & applications
Used primarily in jewelry as beads and carvings. It is famously used as a 'simulant' for more expensive stones like Turquoise or Lapis Lazuli because its porous nature allows it to be easily dyed. It is also a minor source of borax.
Geological facts
Howlite was first discovered in 1868 near Windsor, Nova Scotia, by Canadian geologist Henry How, who initially described it as silico-boro-calcite. It is often sold under the trade name 'White Turquoise' despite having no relation to actual turquoise.
Field identification & locations
Identify by its characteristic 'spider-web' dark veining against a white background; it can be scratched by a knife unlike quartz or turquoise. Commonly found in California and Nevada (USA), and Nova Scotia (Canada). Collectors look for large, un-dyed nodules.
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