monoclinic Inosilicates
Chrome Diopside
CaMg1-xCrxSi2O6
Crystal Structure
#! Species: Chrome Diopside (CaMgSi2O6:Cr)
#! System: Monoclinic (2/m)
#! Habit: Short prismatic; vivid green from Cr3+
monoclinic[2/m]:{110}@1.0 + {010}@0.7 + {001}@0.4
monoclinic
2/m
{110} {010} {001}
Quick Facts
Hardness
5.5
Specific Gravity
3.22
Refractive Index
1.664
Optical Character
Biaxial +
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Open in PlaygroundPhysical Properties
Crystal Systemmonoclinic
Hardness (Mohs)5.5
Specific Gravity3.22
CleavageTwo perfect {110} pyroxene cleavages at ~90°
FractureConchoidal
LustreVitreous
Optical Properties
Refractive Index1.664
Birefringence0.024-0.031
Optical CharacterBiaxial +
Dispersion0.013-0.020
Pleochroismweak: Vivid green / Pale green (Three shades of green; less dramatic than tourmaline or alexandrite)
Colours
Vivid emerald-green to medium green
Localities
Russia (Inagli deposit, Yakutia/Sakha Republic; also described as Sayan Mountains in trade; primary world source)Finland (minor green diopside)Pakistan (chromiferous diopside)Myanmar (minor)Canada (Ontario, Quebec; minor chrome diopside in kimberlites)
Common Inclusions
Silicate and sulfate melt inclusions (from Inagli deposit)Two-phase fluid inclusionsOccasional chromite crystals
Known Treatments
Generally not treatedLow-quality material may be fracture-filled (rare)
Crystal Forms
prismpinacoid
Diagnostic Features
Biaxial positive (distinguishes from emerald biaxial negative, chrome tourmaline uniaxial negative, tsavorite isotropic); moderate birefringence 0.024-0.031 (visible doubling in deeper stones); RI 1.664-1.701 (higher than emerald 1.565-1.602, much lower than tsavorite 1.734-1.759); Chelsea filter red (Cr3+ — same as emerald, NOT diagnostic for separation); Inagli deposit Yakutia as primary source
Notes
Chromiferous variety of diopside (CaMgSi2O6); Cr3+ substitutes for Mg2+ in M1 site. Colour from Cr3+ (same chromophore as ruby and emerald, but different field strength producing green). Monoclinic 2/m. Note: this file is the chromiferous variety; diopside.yaml is the general species entry. Use id: chrome-diopside to avoid collision. Inagli deposit as primary source confirmed by Naumov, Kamenetsky et al. 2008, Geochemistry International 46(6) (DOI 10.1134/s0016702908060025) [VERIFIED]: silicate and sulfate melt inclusions in chrome diopside from Inagli, Yakutia. Gem localities confirmed by Shigley et al. 2000 (DOI 10.5741/gems.36.4.292) [VERIFIED]. Constants from Read 7th ed. (DOI 10.4324/9780080507224) [PARTIALLY_SUPPORTED]. Key separation from lookalikes: biaxial positive optic sign (emerald biaxial negative; tsavorite isotropic; tourmaline uniaxial negative). RI 1.664-1.701 is intermediate.
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Open in PlaygroundRelated Minerals
Other minerals in the monoclinic system