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, 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.




