D'Ansite-(Fe) is an exceptionally rare sulfate mineral found exclusively in active volcanic fumarole environments. It typically forms as small, tabular yellow crystals associated with other volcanic sublimates like chlorothionite.
Is this d'ansite-(fe)?
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 d'ansite-(fe) with a known reference. D'Ansite-(Fe) 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: tabular crystals.
Often confused with
D'Ansite-(Fe) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside d'ansite-(fe)
Minerals reported to co-occur with d'ansite-(fe). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂₁Fe(SO₄)₁₀Cl₃
- Mohs hardness
- 3.5
- Density
- 2.62 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As encrustations on pyroclastic breccia in volcanic fumaroles; also reported as a secondary mineral (Solvenia)
Where rockhounds find d'ansite-(fe)
Classic worldwide localities
- La Fossa crater, Vulcano, Aeolian Islands, Italy, Republic of Slovenia
- Mežica, Republic of Slovenia
Field-hunting tip
Where it forms: As encrustations on pyroclastic breccia in volcanic fumaroles; also reported as a secondary mineral (Solvenia). If you start seeing sassolite, adranosite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.



