
mineral
Howlite
Hydrous calcium borosilicate (Ca2B5SiO9(OH)5)
Hardness: 3.5 on Mohs scale; Color: Milky white to grey with dark grey or black veins; Luster: Sub-vitreous to pearly; Crystal structure: Monoclinic; Cleavage: None (conchoidal fracture); Specific gravity: 2.53–2.59.
- Hardness
- 3
- Color
- Milky white to grey with dark grey or black veins
- Luster
- Sub-vitreous to pearly
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Physical properties
Hardness: 3.5 on Mohs scale; Color: Milky white to grey with dark grey or black veins; Luster: Sub-vitreous to pearly; Crystal structure: Monoclinic; Cleavage: None (conchoidal fracture); Specific gravity: 2.53–2.59.
Formation & geological history
Formed in evaporite deposits as a result of the evaporation of saline waters in arid environments. It is often found in association with other borate minerals and gypsum.
Uses & applications
Primarily used for decorative purposes, carvings, and in jewelry. Because of its porous nature, it is frequently dyed blue to look like turquoise or red to look like coral.
Geological facts
Howlite was first discovered in 1868 by Henry How in Nova Scotia, Canada. It is nicknamed 'white turquoise' or 'cwhite buffalo stone' though it is chemically unrelated to true turquoise.
Field identification & locations
Identify by its characteristic irregular black or dark grey 'web-like' veins over a white backdrop. It is reactve to hydrochloric acid. Commonly found in California and Nova Scotia.
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
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Metamorphic Rock
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mineral