Olivine (forsterite, Mg2SiO4)

Mg2SiO4 · orthorhombic, Pbnm

Forsterite (Mg2SiO4), the magnesium end member of the olivine group, has a calculated bulk density of 3.25 g/cm3 (WebMineral, Calculated Properties) and a calculated refractive index (Ncalc) of 1.65 to 1.68 (WebMineral, Optical Properties).

10 sources · Updated 2026-11-01 · CC BY 4.0

Evidence level

2 of 5

Lab-measured

Density

3.25 g/cm³

Refractive index

1.636 to 1.73 -

Hardness

7 -

Oxide split

57.29 %

Simulant content

9 %

Recipe, share of the weight

  • Mg not statedMagnesium
  • Si not statedSilicon
  • O not statedOxygen

Best for

Reference values for forsterite, and the olivine share of two lunar simulants (9.0% in JSC-1A, 11.1 wt.% in LMS-1)

Weakest at

No measured density with a printed unit, no melting point, and no flight, space-environment or ISRU data in the sources read in this run

Risk at a glance

  • People None found. Eye irritant under GHS in the PubChem record
  • If it fails No data. No failure risks recorded
  • Corrosion Low. Forsterite dissolves more slowly as water activity falls, according to a 2007 Virginia Tech dissertation.

Quick facts: Olivine (forsterite, Mg2SiO4)

Key properties of Olivine (forsterite, Mg2SiO4)
PropertyValueBasis
Density3.25 g/cm³1 sourced value

What is the density of Olivine?

Olivine has a density of 3.25 g/cm³. The source and test conditions are listed in the properties table on this page.

What is Olivine used for?

Uses recorded in the sources include Lunar mare simulant LMS-1 (ground test material); JSC-1A lunar regolith simulant (ground test material); Refractory linings (industrial use, not a space application).

Why it exists

Forsterite (Mg2SiO4) is the magnesium end member of the olivine group, and fayalite (Fe2SiO4) is the iron end member (Wikipedia). The Handbook of Mineralogy lists its occurrence in mafic and ultramafic igneous rocks. Wikipedia's olivine page shows an olivine basalt from the Moon, collected by the Apollo 15 crew. Two lunar simulant pages read for this profile list olivine as a mineral phase: 9.0% of JSC-1A by modal mineralogy, and 11.1 wt.% of LMS-1.

Where it's used

Ground test simulants

NASA's ARES page says JSC-1A is crushed from basaltic ash, and lists olivine at 9.0% in its modal mineralogy. The CLASS Exolith Lab page for LMS-1 lists olivine at 11.1 wt.%.

Refractories

The US Geological Survey says that the remaining magnesium compounds used in the United States went to refractories, in the form of dead-burned magnesia, fused magnesia and olivine.

Recipe

Mg2SiO4

Forsterite is Mg2SiO4: two magnesium atoms, one silicon atom and four oxygen atoms per formula unit (WebMineral and the Handbook of Mineralogy). Natural olivine is a series between forsterite and fayalite, Fe2SiO4, the iron end member (Wikipedia).

What Olivine (forsterite, Mg2SiO4) is made of
IngredientShare of the weightWhat it does
Magnesium Mg not stated The main metal in forsterite. Forsterite is the magnesium end member of the olivine group.
Silicon Si not stated The silicon atom in the formula Mg2SiO4.
Oxygen O not stated The four oxygen atoms per formula unit.

Weight shares are as printed in the sources.

What it can do

Density

3.25 g/cm³

worked out from the formula

WebMineral prints a calculated bulk density of 3.25 g/cm3 for forsterite. No measured density with a printed unit was found in the sources read.

Refractive index

1.636 to 1.73 -

measured

WebMineral gives a calculated refractive index (Ncalc) of 1.65 to 1.68, and printed ranges of 1.636 to 1.73 for index a, 1.65 to 1.739 for index b and 1.669 to 1.772 for index g.

Hardness

7 -

measured

The Handbook of Mineralogy gives a hardness of 7, and WebMineral gives 6 to 7. Neither page names the scale.

Oxide split

57.29 %

worked out from the formula

The theoretical composition is 57.29% MgO and 42.71% SiO2, per WebMineral's stoichiometric composition.

Simulant content

9 %

measured

Olivine is 9.0% of the modal mineralogy of JSC-1A (NASA ARES) and 11.1 wt.% of LMS-1 (CLASS Exolith Lab).

How it compares

Olivine is a named phase in the two lunar simulants read here: 9.0% of JSC-1A by modal mineralogy and 11.1 wt.% of LMS-1 by the CLASS mineralogy table. The forsterite end member is the magnesium-rich form, with a theoretical 57.29% MgO and a calculated bulk density of 3.25 g/cm3. A density comparison with other regolith materials was not made in this run, because their figures were not read here.

The same measurements for each material, so you can compare them. Each row names the key condition under the value; the full conditions and methods are in the numbered notes under Technical details.

Benchmarks
MeasurementOlivine (forsterite, Mg2SiO4)
Thermal behavior and safety
SiO2, theoretical oxide content of forsteriteComposition section of WebMineral, Silicon row42.71 %
Physical and electrical
Bulk density, forsterite (calculated, as printed by WebMineral)3.25 g/cm³1
Hardness, Handbook of Mineralogy7 -3
Hardness range, WebMineralRange printed on WebMineral, Physical Properties6 to 7 -
Other measurements
Refractive index, calculated (Ncalc), forsterite1.65 to 1.68 -2
Refractive index range printed as a, WebMineralRange printed on WebMineral, Optical Properties1.636 to 1.73 -
Refractive index range printed as b, WebMineralRange printed on WebMineral, Optical Properties1.65 to 1.739 -
Refractive index range printed as g, WebMineralRange printed on WebMineral, Optical Properties1.669 to 1.772 -
Birefringence range, WebMineralRange printed on WebMineral, Optical Properties0.033 to 0.042 -
molecular weight140.7 gm4
MgO, theoretical oxide content of forsteriteComposition section of WebMineral, Magnesium row57.29 %
Olivine in JSC-1A, modal mineralogyModal mineralogy printed on the NASA ARES page9 %
Olivine in LMS-1, mineralogy table11.1 wt.%5

Why choose it, and why not

Good for

  • Ground-test simulant work: NASA's JSC-1A page and CLASS's LMS-1 page both name olivine as a phase, at 9.0% and 11.1 wt.%.
  • A reference silicate with a printed formula, space group and oxide split (57.29% MgO and 42.71% SiO2 in theory).

Watch out for

  • The 9.0% and 11.1 wt.% figures describe olivine as one phase of a whole simulant. They are not properties of pure forsterite.
  • WebMineral's printed refractive index ranges are wide, for example 1.636 to 1.73 for index a.
  • PubChem's hazard record is for a mixed magnesium-iron olivine (formula Fe2Mg8O20Si5), not for pure forsterite.

Forsterite is well described as a mineral in the sources read, but this profile has no flight, space-environment or processing data for it. Its role here is as a named phase in lunar simulants and as a magnesium-bearing silicate, not as a proven engineering material.

Technical details

For scientists and researchers. Everything above comes from the record below: every number with its method, its conditions and its source.

Notes

The method, full conditions and any caveat for the numbered rows above.

Notes for the numbered rows
#MeasurementMethodConditionsCaveat
1Bulk density, forsterite (calculated, as printed by WebMineral)Calculated value printed on WebMineral; the page prints the unit as gm/cc, which is the same unit as g/cm3basis bulk density from electron density, listed under Calculated Properties on the pageunit in source gm/ccmineral forsterite, Mg2SiO4—
2Refractive index, calculated (Ncalc), forsteriteCalculated value printed on WebMineral, Optical Propertiesbasis Ncalc as printed on WebMineral; the page gives no wavelengthmineral forsterite—
3Hardness, Handbook of MineralogySingle value printed in the Physical Properties block of the Handbookscale not named in the source; the Handbook prints Hardness = 7mineral forsterite—
4molecular weightPrinted as 140.69 gm in the Composition section of WebMineral; the unit is kept as printedbasis molecular weight of Mg2SiO4 as printedmineral forsterite—
5Olivine in LMS-1, mineralogy tableMineralogy table on the CLASS Exolith Lab LMS-1 pagematerial LMS-1 lunar mare simulant; olivine is one phase of the simulant, not pure forsteritecolumn Wt.% as printed—

Corrosion and compatibility

What happens when it meets other materials and environments.

Corrosion and compatibility
EnvironmentConcernWhat happens
Aqueous acidic solution (oxalic acid, pH 0 to 7, 25°C), laboratory dissolution test low Forsterite dissolves more slowly as water activity falls, according to a 2007 Virginia Tech dissertation.1
Corrosion details
#EnvironmentDetailsTest conditions
1 Aqueous acidic solution (oxalic acid, pH 0 to 7, 25°C), laboratory dissolution test The dissertation abstract states 'However, decreasing aH2O slows forsterite dissolution rates.' It attributes this to water acting as a ligand in the dissolution process. The experiments used oxalic acid solutions, not humid air, so this is a dissolution result and not a measured corrosion rate. basis laboratory dissolution kinetics in oxalic acid solutions over a pH range of 0 to 7 at 25°C, as printed in the abstractmaterial forsteritetest no exposure time or numeric dissolution rate is quoted in this entry

Risks and side effects

Hazards to people, what happens when a cell overheats, and how the material is handled and stored.

For people

The PubChem record for olivine is an eye irritant in most reports. That record is a mixed magnesium-iron silicate, not pure forsterite, and no forsterite safety data sheet was read in this run.

Eyes
PubChem's GHS summary gives H319, causes serious eye irritation, for 95.7% of notifications, with the signal word Warning.
Notifications
22 of 23 reports gave a hazard code. 1 of 23 reports (4.3%) says the record does not meet GHS hazard criteria.
Dust
PubChem's uses section describes low levels of free silica in this sand. No dust exposure limit was read in this run.

Handling and storage

The sources read give only short precautionary codes.

Precautionary codes
PubChem lists P264+P265, P280, P305+P351+P338 and P337+P317 for the olivine record. The wording of these statements was not read in this run.
Storage
No storage or incompatibility advice for pure forsterite was read in this run.

Test details
The original wording and numbers from the sources, for readers who want them.

Handling and storage

  • No supplier safety data sheet for pure forsterite was read in this run. The hazard codes above come from a PubChem record for a mixed magnesium-iron olivine.

Supply and geography

How common the raw materials are and where they come from.

Magnesium (the metal in olivine; the critical-list entries name magnesium, not olivine)

USGS: resources of dolomite, forsterite, magnesium-bearing evaporite minerals and magnesia-bearing brines are estimated at billions of tons. No tonnage for forsterite alone is printed.

Critical mineral lists
US: listed, EU: listed
Recycling
USGS magnesium chapter: some magnesia-based refractories are recycled as construction aggregate, reused in refractory, and as foundry sand. Olivine recycling is not mentioned.
Substitutes
USGS: alumina, chromite and silica substitute for magnesia in some refractory applications. Olivine is not named.

Updated