
diopside
Sign in to saveDiopside 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 sectionsContents
- 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°.