Galileiite is an extremely rare phosphate mineral first discovered in lunar meteorites and later identified in alkaline igneous complexes on Earth. It typically occurs as minute, colorless to pale yellow grains that require microscopic analysis for definitive field identification. It is highly sought after by advanced systematic mineral collectors due to its unique extraterrestrial discovery history.
Is this galileiite?
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 galileiite with a known reference. Galileiite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Galileiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Galileiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: small tabular crystals, anhedral grains.
Often confused with
Galileiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside galileiite
Minerals reported to co-occur with galileiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaFe²⁺₄(PO₄)₃
- Mohs hardness
- 5
- Density
- 3.55 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Small Tabular Crystals, Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- unavailable
Where rockhounds find galileiite
Classic worldwide localities
- Norra Kärr, Sweden
- Moon (Lunar samples)
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where galileiite typically forms. If you start seeing nepheline, aegirine, microcline in float, you are in the right ground. Field specimens usually show a small tabular crystals, anhedral grains habit, so train your eye for that shape before scanning the outcrop.





