Diopside from Persberg.
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Chromian diopside from Outokumpu, Finland.
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Diopside in wollastonite from Snösjön.
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Chromian diopside in limestone from Elsfjord, Norway.
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| Mineral class | Silicates : Inosilicates : Diopside - Augite group. |
| Chemical formula | CaMg(Si2O6) |
| Crystal system | Monoclinic. |
| Habitus | Often as well formed crystals with squarish or octaedric cross section, often twinned. Other habits are grainy, columnar, massive and lamellar aggregates. |
| Cleavage | Good, with two cleavage planes in 87 degrees angle. Fracture uneven. |
| Hardness | 5.5-6.5 |
| Density | 3.22-3.38 |
| Color | Colorless, white, gray, green, greenish black, yellowish brown, reddish brown. Transparent to nearly opaque. |
| Streak | White to gray. |
| Luster | Vitreous. |
| Description |   |
| Occurance | Often in contact metamorphic limestones and dolomites. In many metamorphic rocks and in basic igneous rocks. |
| Associates | Garnet, Wollastonite, Forsterite. |
| Notes | Insoluble in acids. |
| Locations | A common mineral in Sweden.
Good crystal localities are old limestone and marble quarries.
Also in scarn in many iron mines.
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| To silicate index. |
Mineral group index. |
Main index. |
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