Pyroxferroite is a rare pyroxenoid mineral best known for its discovery in lunar basalt samples brought back by the Apollo 11 mission. It typically occurs as small brown to amber grains in iron-rich igneous or metamorphic environments and is a distinct high-pressure polymorph of iron silicate.
Is this pyroxferroite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch pyroxferroite with a known reference. Pyroxferroite sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pyroxferroite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pyroxferroite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, amber, tan.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Pyroxferroite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pyroxferroite
Minerals reported to co-occur with pyroxferroite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe,Ca)SiO₃
- Mohs hardness
- 5.5
- Density
- 3.8-3.9 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Good in Two Directions
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Lunar Basalt, Metamorphic Rocks
- Typical price
- $50-500 depending on specimen size and source
Where rockhounds find pyroxferroite
Classic worldwide localities
- Moon (Apollo 11 mission samples)
- Sweden
- Scotland
- Japan
Field-hunting tip
Look in lunar basalt, metamorphic rocks country, the host setting where pyroxferroite typically forms. If you start seeing plagioclase, ilmenite, cristobalite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






