Forsterite sits at 6.5–7 on the Mohs scale —
harder than glass; scratches steel.
Colors:
Streak White
Crystal system Orthorhombic
Type localityMt. Vesuvius, Naples, Italy
Discovery First described 1824 by Armand Lévy (Italy)
SilicatesSilicates (Nesosilicates)
TL;DR · 1 min read
Forsterite (Mg₂SiO₄) is the magnesium end-member of the olivine group and one of the most abundant minerals in Earth's upper mantle. The gem variety peridot supplies the August birthstone.
Forsterite (Mg₂SiO₄) is the magnesium end-member of the olivine group and one of the most abundant minerals in Earth’s upper mantle. The gem variety peridot supplies the August birthstone. Forsterite is a diagnostic kimberlite indicator mineral — co-occurring with pyrope garnet and ilmenite as evidence of mantle-sourced magma at diamond-bearing localities like Mengyin (Shandong) and Wafangdian (Liaoning).
Forsterite belongs to the silicate class in the olivine group and has the chemical formula Mg2SiO4. It crystallizes in the orthorhombic system and ranks among the harder species, with lasting durability.
Identification & care
Specimens usually show tabular, prismatic, massive (dunite, peridotite). Its color range is broad, including colorless, pale yellow, pale green, and gem variety = peridot. The luster is vitreous, the streak is white, and specimens range from transparent to translucent. The cleavage is imperfect {010} and {100}. The fracture is conchoidal, which aids identification.
Collector context
Collector notes
For collectors, Forsterite is a benchmark crystalline species. Documented Chinese occurrences are recorded at Jiama Cu-polymetallic deposit, among others.
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