Albertiniite is an extremely rare iron sulfite mineral found primarily in abandoned mine workings where it forms as a secondary mineral product. It typically occurs as small, delicate yellow tabular crystals or crusts that are highly sensitive to moisture and oxidation, requiring careful storage for collectors.
Is this albertiniite?
4-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 albertiniite with a known reference. Albertiniite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: colorless, yellowish.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crystalline crusts.
Often confused with
Albertiniite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside albertiniite
Minerals reported to co-occur with albertiniite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe²⁺(SO₃)·3H₂O
- Mohs hardness
- 2-3
- Density
- 2.458 g/cm³
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, crystalline crusts
- Cleavage
- Perfect on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Coating fractures as an intermediate product of oxidation between iron sulfides (pyrite and arsenopyrite)and sulfates
Where rockhounds find albertiniite
Classic worldwide localities
- Miniera Montevecchio, Sardinia, Italy
Field-hunting tip
Where it forms: Coating fractures as an intermediate product of oxidation between iron sulfides (pyrite and arsenopyrite)and sulfates. If you start seeing stolzite, pyromorphite, hinsdalite in float, you are in the right ground. Typical habit: tabular crystals, crystalline crusts. Train your eye for that shape before scanning the outcrop.






