Alfredopetrovite is an extremely rare sulfate mineral identified by its occurrence in the oxidized zones of selenium-rich deposits. It typically forms small, clear, tabular crystals and is known for its distinct crystal chemistry within the copiapite group.
Is this alfredopetrovite?
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 alfredopetrovite with a known reference. Alfredopetrovite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Alfredopetrovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Alfredopetrovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular to blocky crystals.
Often confused with
Alfredopetrovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside alfredopetrovite
Minerals reported to co-occur with alfredopetrovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Al(SeO₄)₂(OH)₂·H₂O
- Mohs hardness
- 2-3
- Density
- 2.16 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular to Blocky Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Seleniferous Ore Deposits
- Typical price
- $100-500 thumbnail size specimens
Where rockhounds find alfredopetrovite
Classic worldwide localities
- Humberstone Mine, Chile
- Santa Maria Mine, Chile
Field-hunting tip
Look in oxidized zones of seleniferous ore deposits country — that is the host setting where alfredopetrovite typically forms. If you start seeing euchlorine, glockerite, metavoltine in float, you are in the right ground. Field specimens usually show a tabular to blocky crystals habit, so train your eye for that shape before scanning the outcrop.



