Paralstonite is a rare barium calcium carbonate mineral that is structurally related to alstonite. It is most famously found in the Illinois-Kentucky fluorspar district, often occurring as sharp, pseudo-hexagonal crystals embedded in or associated with fluorite.
Is this paralstonite?
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 paralstonite with a known reference. Paralstonite sits at Mohs 4-4.5, 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: trigonal. Typical habit: pseudo-hexagonal dipyramidal crystals.
Often confused with
Paralstonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paralstonite
Minerals reported to co-occur with paralstonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaCa(CO₃)₂
- Mohs hardness
- 4-4.5
- Density
- 3.60 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
- Crystal habit
- Pseudo-hexagonal dipyramidal crystals
- Cleavage
- Distinct on {1011}
- Fluorescence
- Bright white/yellow under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare mineral in low-temperature hydrothermal Pb–Zn deposits
Where rockhounds find paralstonite
Classic worldwide localities
- Minerva No. 1 and Annabel Lee mines, Cave-in-Rock, Hardin Co., Illinois, USA
- Kedrovyi massif, five km southeast of the Murun massif, Aldan Shield, Sakha, Russia
Field-hunting tip
Where it forms: A rare mineral in low-temperature hydrothermal Pb–Zn deposits. If you start seeing calcite, alstonite, fluorite in float, you are in the right ground. Typical habit: pseudo-hexagonal dipyramidal crystals. Train your eye for that shape before scanning the outcrop.







