Apatite
Caâ (POâ)â(F,Cl,OH)
CuAlâ(POâ)â(OH)â¡4HâO
Turquoise is a hydrated copper-aluminum phosphate celebrated for its unmistakable sky-blue to blue-green color and extraordinarily long cultural history. It is one of the oldest known gemstones used by humans, worn by pharaohs, Aztec emperors, Native American peoples, and Persian aristocrats alike. Fine natural turquoise is increasingly rare in the modern jewelry market, making knowledge of treatments and quality distinctions more important than ever for buyers.
Turquoise forms as a secondary mineral in arid, oxidizing environments through the chemical weathering of preexisting rocks. The process requires the coincidence of several geological factors: a copper-bearing host rock or ore deposit (the source of Cu²⺠ions), aluminum-rich country rock such as volcanic tuff or feldspar-rich granite (providing Al), phosphate from organic decomposition or phosphatic groundwater, and an arid climate that concentrates these dissolved ions through evaporation rather than flushing them away.
The mineral precipitates in fractures, cavities, and pore spaces within the host rock, typically forming thin veinlets, nodules, and irregular masses rather than discrete crystals. Individual turquoise crystals are microscopic and rarely visible without magnificationâthe stone is essentially a microcrystalline to cryptocrystalline aggregate.
The worldâs primary turquoise-producing regions share this arid oxidizing chemistry: the copper-rich porphyry systems of Iran, the United States Southwest (Arizona, Nevada, New Mexico), northern China, Egyptâs Sinai Peninsula, and parts of Mexico all provide the necessary geological ingredients.
Turquoise is consistently opaque, even in the finest specimens. This opacity results from the microcrystalline aggregate structureâlight cannot pass through the dense, fine-grained mass. Luster ranges from waxy to subvitreous depending on the compactness and silica content of the material; the finest natural specimens have a smooth, even waxy polish.
Hardness varies considerably, from 5 to 6 on the Mohs scale. This variation reflects differences in microporosity and silica contentâharder, denser turquoise is typically less porous and more stable than soft, chalky material. The most durable natural turquoise grades have enough hardness to take and hold a polish without treatment.
The specific gravity range of 2.60 to 2.90 is broader than most gem minerals, reflecting variations in microporosity and compositional variation. Purer, denser turquoise falls toward the higher end of this range.
The color of turquoise is controlled by the balance between two key chemical components:
Copper (Cu²âş): Responsible for the pure sky-blue color. High copper content in the right structural environment produces the most prized blue hues. The finest Persian and Sleeping Beauty turquoise owes its pure blue to optimized copper content with minimal iron.
Iron (FeÂłâş): Iron substitutes for aluminum in the turquoise structure, shifting the color progressively toward green as iron content increases. Apple-green turquoise has relatively high iron and lower copper proportions. Many American Southwest turquoise varieties contain moderate iron, producing the characteristic blue-green hues.
Zinc: Some turquoise deposits contain zinc-rich varieties that produce a lighter, more yellowish-green color. Faustite, an almost entirely zinc-substituted end member, represents an extreme of this substitution.
Most natural turquoise contains inclusions of the host rock within or surrounding the turquoise mass. These host-rock fragments, limonite veins, and iron oxide staining produce the âmatrixâ patterns familiar in decorative turquoise.
Spiderweb Matrix: A network of fine, dark veins distributed evenly through the turquoise, creating an intricate web pattern. Highly desirable in the American Southwest and collector markets when the lines are fine and well-distributed. The Lander Blue and Number Eight mines in Nevada produced famous spiderweb examples.
No Matrix (Solid): Clean, matrix-free turquoise commands premium prices in most markets. Sleeping Beauty Mine turquoise was particularly valued for its consistent, pure sky-blue color without matrix.
Black Matrix: Dark manganese oxide or other carbonaceous material creates bold black veining that contrasts dramatically with blue turquoise, popular in many modern jewelry styles.
Brown/Tan Matrix: Limonite-rich host rock produces warm brown matrix veining that gives a more earthy character to the stone.
Matrix preference is partly cultural and subjective. While international high-end markets often prefer matrix-free material, many collectors, Native American jewelry traditions, and some European markets specifically prize certain matrix types for their aesthetic character.
Understanding turquoise treatment is essential, as a large proportion of market material has been processed in ways that significantly affect value:
Natural Untreated (Grade A): Dense, hard turquoise that requires no treatment to accept and hold a polish. This represents a small fraction of total production and commands the highest prices. Persian (Iranian) blue turquoise historically exemplified this category.
Stabilized: The most common commercial treatment. Porous, low-grade rough that would otherwise be too soft for jewelry use is impregnated under vacuum with colorless resin (epoxy or acrylic). This hardens the stone, improves color uniformity, and makes it workable as a gem. Stabilization is widely accepted in the trade when properly disclosed. Most turquoise in mass-market jewelry at moderate price points is stabilized.
Color-stabilized (Dyed and Stabilized): Porous material is impregnated with colored resin to enhance or alter color, not just harden the stone. This is more controversial and should be clearly disclosed because it crosses from preservation into color manipulation.
Reconstituted or Block Turquoise: Chalky, low-grade turquoise powder is compressed and bound with resin into blocks that are then cut as gems. May technically be turquoise-derived but is a manufactured composite product. Should be disclosed and priced accordingly.
Imitation Turquoise: Materials such as howlite, magnesite, or glass dyed to look like turquoise. Not turquoise at all. Increasingly sophisticated in appearance and widely sold in tourist and low-end markets without adequate disclosure.
Iran (Nishapur, Khorasan): The Nishapur region has been the most celebrated source of premium natural turquoise for over two millennia. Persian blueâa pure, sky-blue color without green undertones and without significant matrixâis the historical standard of excellence. Fine Nishapur material is among the hardest natural turquoise and requires no stabilization. Supply has declined significantly, and genuine Persian natural turquoise commands high premiums.
United States (Arizona, Nevada, New Mexico): The American Southwest hosts dozens of historically significant turquoise mines. Arizonaâs Morenci, Bisbee, and Kingman mines have produced distinctive material with unique color fingerprints. Nevadaâs minesâincluding the Lander Blue (producing the rarest American turquoise), Lone Mountain, Number Eight, and Pilot Mountainâare famous for both color and matrix characteristics. The Sleeping Beauty Mine in Arizona (now closed) was the dominant source for pure, matrix-free sky-blue material for decades. New Mexicoâs Cerrillos Hills represent one of the oldest mining districts in the Western Hemisphere.
China (Hubei Province): China has become a major producer of turquoise, with the Zhushan County deposits in Hubei yielding significant quantities. Chinese turquoise ranges from high-quality material suitable for fine jewelry to lower grades requiring stabilization.
Egypt (Sinai Peninsula): The Serabit el-Khadim and Wadi Maghareh mines on the Sinai Peninsula represent some of the oldest turquoise mines in the world, exploited by the ancient Egyptians as far back as 3100 BCE. The color of Sinai turquoise tends toward blue-green rather than pure blue.
No gemstone has a broader or more diverse cultural history than turquoise. Its use spans at least 7,500 years and virtually every inhabited continent where it could be obtained.
Ancient Egypt: Turquoise was among the first gemstones deliberately mined and traded. Pharaohs wore it as a symbol of divine kingship. The burial mask of Tutankhamun incorporated turquoise, as did countless amulets and pectoral ornaments throughout Egyptian dynastic history. The goddess Hathor was called âLady of Turquoise.â
Persia: Iranian culture elevated turquoise to a national symbol over millennia. Persian turquoise adorned the thrones, armor, bridles, and architecture of emperors and nobles. The word âturquoiseâ itself entered Western languages through the French âturquoisâ meaning âTurkish,â reflecting the trade route by which Persian turquoise reached Europe via Turkish merchants.
The Americas: Turquoise held sacred status in Mesoamerican and Southwestern cultures. The Aztec used turquoise mosaic to create masks, shields, and ceremonial objects of extraordinary craftsmanship. The Pueblo peoples of the American Southwest incorporated turquoise into ceremonial objects and personal adornment for over a thousand years before European contact. Today, turquoise remains integral to Navajo, Zuni, and Hopi jewelry traditions.
Central Asia and Tibet: Turquoise is a traditional gemstone in Tibetan jewelry and religious objects, appearing in gonkyi (ritual implements) and traditional dress ornaments.
For buyers and collectors, distinguishing natural from treated material requires attention to several factors:
Turquoise requires careful handling to maintain its appearance:
Sky blue, blue-green, apple green
Turquoise is porous. If it is untreated (natural), it can absorb skin oils, lotions, soaps, and sweat over time. This absorption can cause the stone to slowly turn from blue to a darker, greener hue. This is sometimes called "antiquing" but is essentially damage.
It is a famous variety from the Sleeping Beauty Mine in Arizona (now closed). It is revered for its pure, solid sky-blue color with little to no matrix (veining). Because the mine is closed, its value has skyrocketed.
Turquoise has a hardness of 5 - 6 on the Mohs scale.
Turquoise is primarily found in Iran (Nishapur) - historical source, United States (Arizona, Nevada, New Mexico), China (Hubei).
Turquoise typically occurs in sky blue, blue-green, apple green.