
mineral
Tumbled green gemstone, likely dyed howlite or serpentine
Most consistent with dyed howlite (Ca2B5SiO9(OH)5); exact identification requires testing
AI-generated identification · may be incorrectOpaque blue-green with dark gray-black veining and a polished vitreous-to-waxy luster; likely Mohs 3–6 depending on material. Massive, non-crystalline appearance; no visible cleavage.
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Physical properties
Opaque blue-green with dark gray-black veining and a polished vitreous-to-waxy luster; likely Mohs 3–6 depending on material. Massive, non-crystalline appearance; no visible cleavage.
Formation & geological history
Howlite forms as a borate mineral in evaporite-associated deposits, commonly in arid regions; serpentine forms by hydration of ultramafic rocks. The vivid color and strong veining may result from human dyeing, so geological age cannot be determined from the image.
Uses & applications
Used as an inexpensive tumbled bead, cabochon, or ornamental stone; not suitable for durable fine jewelry if it is howlite because it scratches relatively easily.
Geological facts
Dyed howlite is often marketed as “turquoise,” though it is not turquoise. Similar green material may be serpentine, dyed magnesite, or imitation turquoise.
Field identification & locations
Check hardness, streak, and magnification: howlite is relatively soft and commonly shows fine gray webbing; turquoise is usually harder and has a blue-green waxy appearance. Common sources include California and Nova Scotia for howlite, and global ultramafic belts for serpentine.
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