Tinticite is a rare hydrated iron phosphate mineral typically found as earthy, botryoidal, or yellowish-white crusts. It is named after the Tintic mining district in Utah, where it occurs as a secondary mineral in oxidized zones of ore deposits.
Is this tinticite?
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 tinticite with a known reference. Tinticite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tinticite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tinticite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-brown, white, pale-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: botryoidal, earthy, massive.
Often confused with
Tinticite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tinticite
Minerals reported to co-occur with tinticite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe³⁺₃(PO₄)₂(OH)₃·3.5H₂O
- Mohs hardness
- 3
- Density
- 2.8 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Botryoidal, Earthy, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Mineral Deposits in Carbonate Rocks
- Typical price
- $20-150 for small specimens
Where rockhounds find tinticite
Classic worldwide localities
- Tintic District, Utah, USA
- Near Eureka, Utah, USA
Field-hunting tip
Look in hydrothermal mineral deposits in carbonate rocks country, the host setting where tinticite typically forms. If you start seeing jarosite, goethite, hematite in float, you are in the right ground. Field specimens usually show a botryoidal, earthy, massive habit, so train your eye for that shape before scanning the outcrop.





