Gordonite is a rare hydrated phosphate mineral often found as delicate, colorless to white tabular crystals or radiating sprays. It is most famous among collectors for specimens from the variscite deposits of Fairfield, Utah, where it occurs within phosphate nodules.
Is this gordonite?
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 gordonite with a known reference. Gordonite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gordonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gordonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, radiating aggregates.
Often confused with
Gordonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside gordonite
Minerals reported to co-occur with gordonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgAl₂(PO₄)₂(OH)₂·8H₂O
- Mohs hardness
- 3.5
- Density
- 2.54 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Radiating Aggregates
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate Nodules in Clay, Hydrothermal Veins
- Typical price
- $20-150 for micro-mounts or small specimens
Where rockhounds find gordonite
Classic worldwide localities
- Fairfield, Utah, USA
- Rapid Creek, Yukon, Canada
- Boa Vista, Brazil
Field-hunting tip
Look in phosphate nodules in clay, hydrothermal veins country — that is the host setting where gordonite typically forms. If you start seeing variscite, wardite, pseudowavellite in float, you are in the right ground. Field specimens usually show a tabular crystals, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.





