Holfertite is a very rare uranyl titanate mineral found primarily in rhyolite gas cavities. It is most commonly identified by its distinctive radiating clusters of yellow needles that grow in association with topaz and bixbyite.
Is this holfertite?
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 holfertite with a known reference. Holfertite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: canary yellow, orange yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: acicular.
Often confused with
Holfertite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside holfertite
Minerals reported to co-occur with holfertite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (UO₂)₁.₇₅Ca₀.₂₅TiO₄·3H₂O
- Mohs hardness
- 4
- Density
- 4.22-4.26 g/cm³
- Streak
- Pale yellow
- Luster
- Adamantine
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
- Crystal habit
- Acicular
- Cleavage
- Perfect on {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A pneumatolytic phase in rhyolite
Where rockhounds find holfertite
Classic worldwide localities
- Starvation (formerly Searle) Canyon, Thomas Range, Utah, USA
Field-hunting tip
Where it forms: A pneumatolytic phase in rhyolite. If you start seeing hematite, bixbyite, fluorite in float, you are in the right ground. Typical habit: acicular. Train your eye for that shape before scanning the outcrop.







