Na-Al pyroxene — no transition metal in pure form.
Test with rare-earth magnet (N42 or N52 neodymium). Suspend specimen on thread for sensitive paramagnetic detection. Diamagnetic minerals are weakly repelled (visible only with strong magnets like bismuth).
Diagnostic Field Tests
Click test→ Bell-like sound when struck
Hung pieces of jadeite ring; nephrite also rings but lower.
UV test→ B-jade fluoresces blue-white (LW UV)
Detects polymer impregnation.
SG check→ ~3.34 — heavier than nephrite
Hydrostatic test separates jadeite from nephrite.
⚠ 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
3.30–3.38
g/cm³
medium
Heavier than nephrite; one diagnostic test.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Synthetics & Imitations
Lab-grown methods
High-pressure synthesis1984 · General Electric
Lab jadeite never reached gem grade commercially.
Common imitations
Nephrite
Different mineral (Ca-Mg-Fe amphibole) often sold as "jade".
Serpentine ("new jade")
Softer (Mohs 3); waxy not vitreous.
Aventurine quartz
Sparkle from fuchsite inclusions; sold as "Indian jade".
Dyed green imitation; UV fluorescence orange-red under longwave reveals dye.
As a buyer: request written disclosure of treatments and confirm whether the price reflects treated or untreated material.
Care notesVery tough; light water + neutral detergent OK. Avoid ultrasonic if untreated detection is needed (filled jade reveals under UV). Full cleaning guide →
Formation eraHigh-P metamorphic; Burmese type formed 70-90 Ma at subduction zone.
Cleavage & Fracture
Cleavage:
good2 directions ~87°/93°
Fracture:
splintery / tough
Tough due to interlocked microcrystals — jade.
🟡
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.
Mohs6.5–7
Vickers (~)1400 HV
Knoop (~)1100 HK
Nickel–Strunz9.DA.25
Dana65.01.03a.04
Geological setting
🗜Metamorphic
Element composition by mass
Formula: NaAlSi₂O₆ · molar mass: 202.14 g/mol
O
47.49%
Si
27.79%
Al
13.35%
Na
11.37%
Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.
Jadeite sits at 6.5–7 on the Mohs scale —
harder than glass; scratches steel.
Colors:
Streak White
Crystal system Monoclinic
Pronunciation/ˈdʒeɪdaɪt/
Type localityTawmaw, Kachin State, Myanmar (Burma)
SilicatesSilicates (Inosilicates — Pyroxenes)
TL;DR · 1 min read
Jadeite (NaAlSi₂O₆) is the sodium-aluminum pyroxene and one of the two distinct minerals sold as "jade" (the other being nephrite, an amphibole). Imperial green Jadeite from Myanmar (Burma) is the world's most valuable jade material.
Jadeite (NaAlSi₂O₆) is the sodium-aluminum pyroxene and one of the two distinct minerals sold as “jade” (the other being nephrite, an amphibole). Imperial green Jadeite from Myanmar (Burma) is the world’s most valuable jade material. Jadeite forms in high-pressure low-temperature metamorphic environments — subducted oceanic crust and serpentinite-hosted blocks.
Jadeite is a silicate mineral in the pyroxene group (clinopyroxene subgroup) and has the chemical formula NaAlSi2O6. It crystallizes in the monoclinic 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
Jadeite typically forms massive; rare prismatic crystals. Its color range is broad, including apple-green, vivid emerald-green (imperial jade — cr-bearing), white, pale green, lavender/violet, pink, yellow, orange, and black. The luster is vitreous, greasy, waxy (massive), the streak is white, and specimens range from translucent to opaque (most material); transparent (rare crystals). The cleavage is good on {110}, two directions at ~87°. The fracture is splintery, conchoidal, which aids identification.
Collector context
How it forms
Jadeite forms in high-pressure, low-temperature metamorphism (blueschist to eclogite facies) in subduction zones; found in serpentinites and blocks within subduction mélanges. It is commonly found in association with omphacite, glaucophane, lawsonite, serpentine, chromite, natrolite (as alteration).
Classic Chinese localities
Jadeite is widely represented across Chinese provinces, including Yunnan, Inner Mongolia, Jiangxi, Liaoning.
Why collectors care
Jadeite is central to Chinese material culture and is judged as jade, not as a crystal specimen. Collectors value fine pieces for dense fibrous fabric, quiet translucency, greasy luster, and a tradition of carving and connoisseurship spanning thousands of years. A good piece of jadeite feels cool, dense, and slightly greasy in the hand, with a quiet glow no photograph fully captures.
What affects value
Value in Jadeite is assessed, in typical order of weight, against: (1) verified source and historical provenance; (2) size and carvable volume; (3) color tone and evenness; (4) texture and compactness; (5) translucency and greasy luster; (6) polish response and surface quality; (7) workmanship on carved pieces. For culturally significant material, verified Hetian / Khotan provenance can weigh heavily beyond any single physical factor.
Naming history
The name Jadeite 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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