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diopside
EntityQ316671· pop 45· linked from 307 articles

Diopside is a monoclinic pyroxene mineral with composition . It forms complete solid solution series with hedenbergite () 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. It has a Mohs hardness of six, a Vickers hardness of 7.7 GPa at a load of 0.98 N, and a specific gravity of 3.25 to 3.55. It is transparent to translucent with indices of refraction of nα=1.663–1.699, nβ=1.671–1.705, and n

Key facts

Mineral.name
Diopside
Mineral.category
Inosilicate minerals (single chain)
Mineral.group
Pyroxene group, clinopyroxene subgroup
Mineral.boxbgcolor
fff9b4
Mineral.image
Diopside Aoste.jpg
Mineral.imagesize
260px
Mineral.caption
Diopside – Bellecombe, Châtillon, Aosta Valley, Italy
Mineral.formula
MgCaSi2O6
Mineral.IMAsymbol
Di
Mineral.strunz
9.DA.15
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
C2/c
Mineral.unit cell
a = 9.746 Å, b = 8.899 Å c = 5.251 Å; β = 105.79°; Z = 4
Mineral.color
Commonly light to dark green; may be blue, brown, colorless, white to snow white, grey, pale violet
Mineral.habit
Short prismatic crystals common, may be granular, columnar, massive
Mineral.twinning
Simple and multiple twins common on {100} and {001}
Mineral.cleavage
Distinct/good on {110}

via Wikipedia infobox

Wikidata facts

Image
Diopside Aoste.jpg
Show 6 more facts
Nickel-Strunz 9th edition (updated 2009)
9.DA.15
Commons category
Diopside
chemical formula
CaMgSi₂O₆
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.DA.15
IMA Mineral Symbol
Di
Strunz 8th edition (series ID, updated)
VIII/D.01b
Sources (3)

via Wikidata · CC0

~7 min read

Article

6 sections
Contents
  • Formation
  • Mineralogy and occurrence
  • As a gem
  • Etymology and history
  • Potential uses
  • References

{{Infobox mineral | name = Diopside | category = Inosilicate minerals (single chain) | group = Pyroxene group, clinopyroxene subgroup | boxwidth = | boxbgcolor =#fff9b4 | image = Diopside Aoste.jpg | imagesize = 260px | caption = Diopside – Bellecombe, Châtillon, Aosta Valley, Italy | formula = MgCaSi2O6 | IMAsymbol = Di | molweight = | strunz = 9.DA.15 | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = C2/c | unit cell = a = 9.746 Å, b = 8.899 Å c = 5.251 Å; β = 105.79°; Z = 4 | color = Commonly light to dark green; may be blue, brown, colorless, white to snow white, grey, pale violet | habit = Short prismatic crystals common, may be granular, columnar, massive | twinning = Simple and multiple twins common on {100} and {001} | cleavage = Distinct/good on {110} | fracture = Irregular/uneven, conchoidal | tenacity = Brittle | mohs = 5.5–6.5 | luster = Vitreous to dull | polish = | refractive = nα= 1.663 – 1.699, nβ= 1.671 – 1.705, nγ= 1.693 – 1.728 | opticalprop = Biaxial (+) | birefringence = δ = 0.030 | dispersion = Weak to distinct, r>v | pleochroism = | 2V = Measured: 58° to 63° | fluorescence= | absorption = | streak = white | gravity = 3.278 | density = | melt = 1391 °C | fusibility = | diagnostic = | solubility = | diaphaneity = | other = | references = }}

Diopside is a monoclinic pyroxene mineral with composition . It forms complete solid solution series with hedenbergite () 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. It has a Mohs hardness of six, a Vickers hardness of 7.7 GPa at a load of 0.98 N, and a specific gravity of 3.25 to 3.55. It is transparent to translucent with indices of refraction of nα=1.663–1.699, nβ=1.671–1.705, and nγ=1.693–1.728. The optic angle is 58° to 63°.

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