Destinezite is a rare phosphate mineral typically found as secondary crusts or nodules in sedimentary deposits. Collectors should look for its characteristic earthy, reniform appearance, which often results from the alteration of iron-bearing minerals in phosphate-rich environments.
Is this destinezite?
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 destinezite with a known reference. Destinezite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Destinezite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Destinezite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, white, yellow-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: massive, reniform, concretionary, or powdery encrustations.
Often confused with
Destinezite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside destinezite
Minerals reported to co-occur with destinezite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe³⁺₂(PO₄)(SO₄)(OH)·6H₂O
- Mohs hardness
- 3-4
- Density
- 2.2-2.5 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Massive, Reniform, Concretionary, Or Powdery Encrustations
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Phosphate Deposits
- Typical price
- $20-100 for small study specimens
Where rockhounds find destinezite
Classic worldwide localities
- Belgium
- Czech Republic
- Germany
Field-hunting tip
Look in sedimentary phosphate deposits country, the host setting where destinezite typically forms. If you start seeing vivianite, limonite, pyrite in float, you are in the right ground. Field specimens usually show a massive, reniform, concretionary, or powdery encrustations habit, so train your eye for that shape before scanning the outcrop.




