| Mineral class | Silicates : Nesosilicates : Olivine group |
| Chemical formula | (Fe,Mg)2(SiO4) |
| Crystal system | Orthorombic |
| Habitus | Thick tabular dipyramidal crystals, frequently with wedge-shaped terminations. Mostly as grains or massive aggregates. |
| Cleavage | Imperfect, fracture conchoidal. |
| Hardness | 6.5 - 7 |
| Density | 3.3 - 3.5 |
| Color | Green to greenish yellow or colorless. |
| Streak | Colorless |
| Luster | Vitreous to greasy, transparent. |
| Description | Fayalite is the iron rich member of the olivine series. When the magnesium contents increases over 50% it turns into forsterite. |
| Occurance | Forms in rapidly cooled acidic igneous rocks. |
| Associates |   |
| Notes |
Clear gemmy olivine is called peridote. Olivine is soluble in hydrochloric acid with gelatinisation. |
| Localities | Not so common in Scandinavia, mostly found as small grains. Sweden :
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| To silicate index. |
Mineral group index. |
Main index. |
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