
mineral
Howlite
Calcium borosilicate hydroxide (Ca2B5SiO9(OH)5)
Hardness: 3.5 on Mohs scale; Color: Chalky white with web-like black, grey, or brown veins; Luster: Sub-vitreous to earthy; Crystal Structure: Monoclinic; Cleavage: None; Specific Gravity: 2.53–2.59
- Hardness
- 3
- Color
- Chalky white with web-like black, grey, or brown veins
- Luster
- Sub-vitreous to earthy
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Physical properties
Hardness: 3.5 on Mohs scale; Color: Chalky white with web-like black, grey, or brown veins; Luster: Sub-vitreous to earthy; Crystal Structure: Monoclinic; Cleavage: None; Specific Gravity: 2.53–2.59
Formation & geological history
Formed in evaporite deposits, usually found as nodules, masses, or sometimes as tabular crystals in continental or saline lake environments. Primarily found in deposits from the Neogene period (2.5 million to 23 million years ago).
Uses & applications
Commonly used for decorative carvings, jewelry (tumbled stones or beads), and as a base for imitation turquoise because its porous nature allows it to take blue or green dye well.
Geological facts
Howlite was first discovered by Henry How in 1868 near Windsor, Nova Scotia. It is often colloquially known as 'white turquoise' or 'cabbie stone' in the trade, though those names are geologically inaccurate.
Field identification & locations
Identify in the field by its distinct white color with web-like veining and its low hardness (it can be scratched by a copper coin). Major deposits are located in Canada (Nova Scotia), the USA (California and Nevada), and parts of Turkey.
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