Alpersite is a rare magnesium-dominant sulfate mineral that typically forms as efflorescent crusts or fibrous aggregates in mine environments. It is most commonly found as a secondary mineral resulting from the oxidation of sulfide ores, particularly in sites affected by acid mine drainage.
Is this alpersite?
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 alpersite with a known reference. Alpersite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Alpersite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Alpersite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, blue-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, crystalline crusts.
Often confused with
Alpersite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside alpersite
Minerals reported to co-occur with alpersite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Cu)SO₄·7H₂O
- Mohs hardness
- 2
- Density
- 1.97 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Crystalline Crusts
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Acid Mine Drainage Environments, Weathered Sulfide Deposits
- Typical price
- $20-100 for small specimens
Where rockhounds find alpersite
Classic worldwide localities
- Iron Mountain Mine, California, USA
- Rio Tinto, Spain
Field-hunting tip
Look in acid mine drainage environments, weathered sulfide deposits country — that is the host setting where alpersite typically forms. If you start seeing melanterite, goslarite, chalcanthite in float, you are in the right ground. Field specimens usually show a fibrous, crystalline crusts habit, so train your eye for that shape before scanning the outcrop.




