| Mineral class | Silicates : Nesosilicates : Olivine group |
| Chemical formula | (Mg,Fe)2(SiO4) |
| Crystal system | Orthorombic |
| Habitus | Thick tabular dipyramidal crystals, frequently with wedge-shaped terminations. Mostly as grains or massive aggregates. |
| Cleavage | [001] good and [010] distinct, fracture conchoidal. |
| Hardness | 6.5 - 7 |
| Density | 3.21 - 3.33 |
| Color | Green to greenish yellow or colorless, also brown, pale red, gray or bluish gray. |
| Streak | Colorless |
| Luster | Vitreous to greasy, transparent. |
| Description | Forsterite is the magnesium rich member of the olivine series. When the iron contents increases over 50% it turns into fayalite. |
| Occurance | Forms in basic and ultrabasic igneous rocks (gabbro, pyroxenite or peridotite). Also formed in marbles. |
| Associates |   |
| Notes |
Clear gemmy olivine is called peridote. Other names used for forsterite is
chrysolite and olivine. Type Locality : Monte Somma, Vesuvio (Vesuvius), Napoli, Campania, Italy. Discovered in 1824. Named after Adolarius Jacob Forster (1739-1806). Forsterite is soluble in hydrochloric acid with gelatinisation. |
| Localities | A common mineral and a major part of many rocks. Sweden :
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| To silicate index. |
Mineral group index. |
Main index. |
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