Diopside
Diopside Gemstones
Hardness
5.5.
Occurrence
Myanmar (Burma), Russia, Pakistan, South Africa, Austria, Brazil,
Italy, North America, Sri Lanka (Ceylon) and Finland. Star diopside is
mainly from India.
Appearance
Diopside is found in two forms, the black star diopside, and the green emerald-like Chrome diopside.
Enhancements
Diopside is not known to be enhanced.
More information on gemstone enhancements.
Diopside
Diopside is a monoclinic pyroxene mineral with composition MgCaSi2O6. It forms complete solid solution series with hedenbergite (FeCaSi2O6) and augite, and partial solid solutions with orthopyroxene and pigeonite. It forms variably colored, but typically dull green crystals in the monoclinic prismatic class. It has two distinct prismatic cleavages at 87 and 93° typical of the pyroxene series.
Formation
Diopside is found in ultramafic (kimberlite and peridotite) igneous rocks, and diopside-rich augite is common in mafic rocks, such as olivine basalt and andesite. Diopside is also found in a variety of metamorphic rocks, such as in contact metamorphosed skarns developed from high silica dolomites. It is an important mineral in the Earth's mantle and is common in peridotite xenoliths erupted in kimberlite and alkali basalt.
Mineralogy and occurence
Chrome diopside ((Ca,Na,Mg,Fe,Cr)2(Si,Al)2O6) is a common constituent of peridotite xenoliths, and dispersed grains are found near kimberlite pipes, and as such are a prospecting indicator for diamonds. Occurrences are reported in Canada, South Africa, Russia, Brazil, and a wide variety of other locations. In the US, chromian diopside localities are described in the serpentinite belt in northern California, in kimberlite in the Colorado-Wyoming State Line district, in kimberlite in the Iron Mountain district, Wyoming, in lamprophyre at Cedar Mountain in Wyoming, and in numerous anthills and outcrops of the Tertiary Bishop Conglomerate in the Green River Basin of Wyoming. Much chromian diopside from the Green River Basin localities and several of the State Line Kimberlites have been gem in character.
As a gem
Gemstone quality diopside is found in two forms: the black star diopside and the chrome diopside (which includes chromium, giving it a rich green colour). At 5.5–6.5 on the Mohs scale, chrome diopside is relatively soft to scratch. The Mohs scale of hardness does not measure tensile strength or resistance to fracture.
Potential uses
Diopside based ceramics and glass-ceramics have potential applications
in various technological areas. A diopside based glass-ceramic named
'silceram' was produced by scientists from Imperial College, UK during
1980s from blast furnace slag and other waste products. The as produced
glass-ceramic is a potential structural material. Similarly, diopside
based ceramics and glass-ceramics have potential applications in the
field of biomaterials, nuclear waste immobilization and sealing
materials in solid oxide fuel cells.
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