Pyroxene Group
Pyroxene group gems including jadeite, spodumene (kunzite, hiddenite), and diopside (chrome diopside) with properties and identification.
Introduction
Pyroxenes are single-chain inosilicates crystallising in the monoclinic system,
producing three gem-significant species: jadeite, spodumene, and diopside. Jadeite
(NaAlSi₂O₆), the more valuable of the two jade minerals, occurs as an interlocking
microcrystalline aggregate with spot RI 1.654–1.667, SG 3.30–3.38, and hardness
6.5–7 Mohs; these properties reliably separate it from nephrite (RI 1.606–1.632,
SG 2.90–3.02) and serpentine simulants (SG 2.5–2.6). [1] Spodumene
(LiAlSi₂O₆) provides kunzite (manganese-pink, RI 1.660–1.676, strong pleochroism and
orange-pink phosphorescence) and rare chromium-coloured hiddenite (intense green).
Chrome diopside (CaMgSi₂O₆) from Siberia offers Cr³⁺-driven vivid green at accessible
prices, with RI 1.675–1.701 and SG 3.22–3.38. All pyroxene gems share good to perfect
cleavage in two directions at approximately 87°, a durability consideration in ring
settings. Fine Imperial jadeite (vivid chromium-green, semi-transparent, from Myanmar's
Hpakant mines) is among the world's most commercially valuable gem materials; top
cabochons have exceeded $3 million per carat at Hong Kong auction. [2]
[3]
Jadeite
Jadeite (NaAlSi₂O₆) is the more valuable of the two jade minerals,
prized especially in Asian cultures.
Properties
| Property | Value |
|---|---|
| Crystal system | Monoclinic |
| Hardness | 6.5–7 Mohs |
| Specific gravity | 3.30–3.38 |
| Refractive index | 1.654–1.667 (spot) |
| Character | Aggregate (no single crystal) |
| Toughness | Exceptional (interlocking crystals) |
Colour Varieties
| Colour | Cause | Trade Name |
|---|---|---|
| Imperial green | Chromium | Imperial jade (most valuable) |
| Lavender | Manganese + iron | Lavender jade |
| White | Pure composition | Mutton fat jade |
| Yellow to orange | Iron staining | Yellow jade |
| Black | Iron inclusions | Black jade |
Imperial Jade
Major Sources
- Myanmar: Premier source; Imperial green [1]
- Guatemala: Historic; Mesoamerican significance
- Japan: Small deposits
- Russia: Limited production
Imperial Jade Value
Jadeite Identification
Distinguishing jadeite from nephrite and simulants:
Jadeite vs Nephrite
| Property | Jadeite | Nephrite |
|---|---|---|
| Specific gravity | 3.30–3.38 | 2.90–3.02 |
| Refractive index | 1.654–1.667 | 1.606–1.632 |
| Lustre | Vitreous to greasy | Greasy to waxy |
| Colours | More vivid greens; lavender | Greens, creams, browns |
| Value | Higher for fine material | Generally lower |
Spodumene
Spodumene (LiAlSi₂O₆) is a lithium aluminium pyroxene with two important
gem varieties.
Properties
| Property | Value |
|---|---|
| Crystal system | Monoclinic |
| Hardness | 6.5–7 Mohs |
| Specific gravity | 3.15–3.20 |
| Refractive index | 1.660–1.676 |
| Birefringence | 0.014–0.016 |
| Cleavage | Perfect in two directions (90°) |
Kunzite
Pink to lilac spodumene:
- Colour cause: Manganese (Mn³⁺) [3]
- Range: Pale pink to intense lilac-pink
- Pleochroism: Strong (pink to colourless)
- Fluorescence: Strong orange-pink; phosphorescence
- Sources: Afghanistan, Brazil, Madagascar, USA
Hiddenite
Green spodumene:
- Colour cause: Chromium (Cr³⁺) for true hiddenite
- Rarity: True Cr-coloured hiddenite is very rare
- Source: North Carolina (type locality); Afghanistan
- Note: Iron-coloured green spodumene is less valuable
Spodumene Challenges
Chrome Diopside
Chromium-coloured diopside offers affordable green colour:
Properties
- Formula: CaMgSi₂O₆
- Colour: Rich green (Cr-coloured)
- RI: 1.675–1.701
- SG: 3.22–3.38
- Birefringence: 0.024–0.031
Characteristics
- Vivid green rivaling emerald
- Generally available in smaller sizes
- Softer than emerald (H 5.5–6.5)
- Good value for intense green
- Source: Russia (Siberia), Pakistan
Limitations
- Tends to be dark in larger sizes
- Relatively soft for jewellery
- Two cleavage directions
- Best in smaller stones (<1 carat)
Identification Summary
References
- ↑ 1. Hughes, R.; Galibert, O.; Bosshart, G.; Ward, F.; Oo, T.; Smith, C.; Sun, T.; Harlow, G. (2000). Burmese Jade: The Inscrutable Gem. Gems & Gemology, 36(1), 2–26. DOI: 10.5741/gems.36.1.2.
- ↑ 2. Read, P. (2008). Gemmology (3rd ed.). Butterworth-Heinemann. ISBN: 978-0-7506-6449-3. DOI: 10.4324/9780080507224.
- ↑ 3. Fritsch, E.; Rossman, G. (1987). An Update on Color in Gems. Part 1: Introduction and Colors Caused by Dispersed Metal Ions. Gems & Gemology, 23(3), 126–139. DOI: 10.5741/gems.23.3.126.