Turquoise

Crystal system · Triclinic

Turquoise is a phosphate mineral prized by collectors for its exceptional color range, with known Chinese sources.

About Turquoiseextended article

China-iconic

China is a defining locality for Turquoise · 绿松石. See the Chinese collector page →

Elemental Composition (by mass)
ElementMass %Visual
O Oxygen51.72%
Al Aluminum21.81%
P Phosphorus16.69%
Cu Copper8.56%
H Hydrogen1.22%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Tq
→ Turquoise
Cu-Al phosphate
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
⏳ Long-term Aging & Care Timeline
color shift to greenyears
Trigger: oils + UV
Intervention: Cu-Al phosphate absorbs oils and UV-shifts toward green. Sealed dry case + no oil contact.
Pronunciation
/ˈtɜːrkwɔɪz/
TUR-koyz
French "Turkish"
Lapidary & Faceting Recommendations
Recommended cut:
cabochon
Also seen:
inlay, free-form
Typical yield:
60% of rough
Always cabbed. Spider-web matrix material cut to display matrix lines. Stabilized material allows larger cabs.
Birthstone & Anniversary Gift Reference
January (zodiac)zodiac: Capricorn / Aquarius
December (traditional, zodiac)zodiac: Sagittarius / Capricorn
⚠ Safety & Handling
💧water-sensitivemoderate
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:
Apatite replacement (rare)
Phosphate replacement in dolomitic host rocks.
Iran, USA Southwest.
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.
Type Locality
(French "Turkish stone") — Iran (Nishapur)
Source: Mined since 6000 BCE
Diagnostic Field Tests
Hot needle→ No melt; faint chemical smell
Plastic/composite turquoise melts/smokes — diagnostic.
Acetone swab→ Removes dye if treated
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 process 1972 · 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.
Geological Setting
Environment:
supergene
Host rock:
altered Cu-Al-rich volcanic / sedimentary
Companions:
Chalcosiderite · Chrysocolla · Limonite
Forms by groundwater alteration of aluminous host rock in arid copper districts.
Treatments & Enhancements
Stabilization (epoxy/wax)universalstable-care· detection: easy
Most natural turquoise is impregnated with polymer or wax to harden chalky material. Disclosure required.
Dyeingcommonstable-care· detection: moderate
Color enhancement of pale material. Often combined with stabilization.
Reconstitutedcommonstable· detection: easy
Powdered turquoise reformed with polymer binder. Not natural turquoise — must be disclosed.
As a buyer: request written disclosure of treatments and confirm whether the price reflects treated or untreated material.
Formation eraSupergene; recent weathering of Al-Cu-bearing rocks in arid climates.
Market availability: Uncommon
Found at major shows and select dealers. Quality varies by locality.
Collector tier: Cabinet Classic
World-class display species — sought after for cabinet collections, well-documented localities, frequent show-piece pieces.
Mohs 5–6
Vickers (~) 540 HV
Knoop (~) 620 HK
Nickel–Strunz 8.DD.15
Dana 42.09.03.01
Element composition by mass

Formula: CuAl₆(PO₄)₄(OH)₈·4H₂O · molar mass: 759.39 g/mol

O 52.67%
Al 21.32%
P 16.32%
Cu 8.37%
H 1.33%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

Mohs Hardness 5–6

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).

More minerals to explore

About Turquoise

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.