Fayalite is the iron-rich end member of the olivine solid solution series and is typically found in high-silica volcanic rocks and certain granitic environments. It is noted for its high density and tendency to oxidize into hematite or magnetite when exposed to air. Collectors look for dark, well-formed crystals often embedded in light-colored volcanic matrix.
Is this fayalite?
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 fayalite with a known reference. Fayalite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Fayalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Fayalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-green, brown, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Fayalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside fayalite
Minerals reported to co-occur with fayalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂SiO₄
- Mohs hardness
- 6.5-7
- Density
- 4.39 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Poor in Two Directions
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Igneous Rocks Such as Rhyolites, Granites, And Iron-rich Basaltic Rocks
- Typical price
- $10-50 per specimen depending on crystal quality
Where rockhounds find fayalite
Classic worldwide localities
- Mourne Mountains, Ireland
- Rockport, Massachusetts, USA
- Jan Mayen Island, Norway
- Pantelleria, Italy
Field-hunting tip
Look in igneous rocks such as rhyolites, granites, and iron-rich basaltic rocks country — that is the host setting where fayalite typically forms. If you start seeing quartz, tridymite, magnetite in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





