Forsterite

Crystal system · Orthorhombic

Forsterite is a silicate mineral recognized for its hardness and durability, with notable Chinese occurrences.

About Forsteriteextended article

Crystal Structure
Mg end-member of olivine.
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen45.49%
Mg Magnesium34.55%
Si Silicon19.96%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Fo
→ Forsterite
Mg end-member
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈfɔːrstəraɪt/
FOR-stuh-rite
for J. Forster
Market availability: Uncommon
Found at major shows and select dealers. Quality varies by locality.
PolymorphsShares the formula Mg2SiO4 with: Wadsleyite · Ringwoodite — same chemistry, different crystal structure.
Mohs 6.5–7
Vickers (~) 1400 HV
Knoop (~) 1100 HK
Geological setting
VolcanicKimberlite
Element composition by mass

Formula: Mg₂SiO₄ · molar mass: 140.69 g/mol

O 45.49%
Mg 34.55%
Si 19.96%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

GroupOlivine Group
Related members: Fayalite
Mohs Hardness 6.5–7

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).

More minerals to explore

About Forsterite

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.