Porous; absorbs oils and chemicals causing color change.
Handling: No water. No oils. No perfume. Wipe with soft dry cloth.
⚗acid-sensitivemoderate
Phosphate dissolves slowly in acids.
Handling: No acids.
Information provided in good faith. Consult local hazmat regulations for transport and disposal. Severely hazardous specimens may require special storage cabinets.
UV Fluorescence
SW (254 nm)
—
none
LW (365 nm)
—
none
Untreated inert. Polymer-stabilized may fluoresce blue-white LW.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Pseudomorph Relationships
Replaces — this mineral is often a pseudomorph after:
A pseudomorph (Greek "false form") is a mineral with the external shape of another species — the chemistry has changed but the crystal habit is inherited.
Tenacity
Behavior:
brittle
Under stress:
Crumbles if untreated
Chalky material very fragile — reason for routine stabilization.
Luster
waxy
Subdued waxy luster — diagnostic.
Color Cause (Chromophore)
Chromophore:
Cu²⁺ + Fe²⁺
Mechanism:
idiochromatic
Color produced:
blue-green
Cu dominates blue; Fe shifts toward green.
Diaphaneity (Transparency)
translucent-to-opaque
Most turquoise opaque; spider-web matrix shows through edges.
White cotton swab + acetone reveals dye on dyed howlite imitation.
⚠ Use dilute HCl (~10%) only on inconspicuous spots; rinse promptly. Smell-tests should be brief and ventilated. Taste-test ONLY halite/sylvite — never lead, arsenic, or sulfur minerals.
Specific Gravity
2.60–2.80
g/cm³
light
Stabilized turquoise has slightly lower SG than natural.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
white / pale blue
Pale streak — confirms vs dyed howlite (pure white when scraped).
Streak = color of the powdered mineral. Drag specimen across unglazed white porcelain plate (Mohs 6.5). For minerals harder than the plate, crush a small flake into powder and observe color.
Synthetics & Imitations
Lab-grown methods
Gilson process1972 · Pierre Gilson
Synthetic turquoise; lacks natural matrix and limonite spots.
Common imitations
Howlite (dyed)
White howlite dyed blue — very common imitation in tourist markets.
Magnesite (dyed)
White magnesite dyed; same trick.
Plastic / resin
Lightweight; melts under hot needle test.
Reconstituted turquoise
Powdered turquoise + polymer binder; sold as natural in tourist trade.
Turquoise sits at 5–6 on the Mohs scale —
just hard enough to scratch glass.
Colors:
Streak White
Crystal system Triclinic
Pronunciation/ˈtɜːrkwɔɪz/
Type localitySinai Peninsula, Egypt (ancient)
Discovery First described 1546 by Georgius Agricola
PhosphatesPhosphates
TL;DR · 1 min read
Turquoise (CuAl₆(PO₄)₄(OH)₈·4H₂O) is a hydrous copper aluminum phosphate, prized for its sky-blue to apple-green color since prehistoric times. Persia (Nishapur, Iran), Hubei (China), and the American Southwest (Sleeping Beauty Mine, Arizona) supply iconic gem-quality material.
Turquoise (CuAl₆(PO₄)₄(OH)₈·4H₂O) is a hydrous copper aluminum phosphate, prized for its sky-blue to apple-green color since prehistoric times. Persia (Nishapur, Iran), Hubei (China), and the American Southwest (Sleeping Beauty Mine, Arizona) supply iconic gem-quality material. Color depends on copper content (sky-blue) vs. iron (greenish).
Turquoise is a phosphate mineral in the turquoise group and has the chemical formula CuAl6(PO4)4(OH)8 · 4H2O. It crystallizes in the triclinic system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Crystals commonly develop as massive, nodular, botryoidal; veins, crusts; tiny crystals very rare. Its color range is broad, including bright blue, sky-blue, pale green, blue-green, turquoise-blue, apple-green, and green-gray. The luster is sub-vitreous, resinous, waxy, dull, earthy, the streak is pale greenish blue to white, and specimens are typically transparent, translucent, opaque. The cleavage is perfect on {001}, good on {010}. The fracture is conchoidal to uneven, which aids identification.
Collector context
How it forms
Turquoise forms in secondary mineral in oxidized zones of copper-rich arid-region deposits; forms by weathering of feldspar-bearing rocks with copper-rich fluids and phosphate ions; requires arid conditions. It is commonly found in association with chalcopyrite, malachite, azurite, limonite, kaolin, quartz.
Classic Chinese localities
Turquoise is widely represented across Chinese provinces, including Yunnan, Hubei, Henan, Shaanxi.
Why collectors care
Collectors pursue Turquoise for its patterns, color depth, and polish response rather than for pattern character. Good material has a surface that polishes cleanly, a visual character that holds up in direct light, and enough size to anchor a display on its own. Chinese sources, where present, supply much of the material currently cut and sold as decorative pieces.
What affects value
Value in Turquoise is assessed, in typical order of weight, against: (1) source locality; (2) size; (3) pattern and visual character; (4) color depth and distribution; (5) polish response and surface finish; (6) piece integrity (absence of major cracks or chips). Uniqueness of pattern and verified source region add significantly to decorative pieces.
Naming history
The name Turquoise has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.
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