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 4.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Paralstonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Paralstonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow.
- 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
- 4.5
- Density
- 3.62 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- 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
- Low-temperature Hydrothermal Veins in Sedimentary Rocks
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find paralstonite
Classic worldwide localities
- Minerva No. 1 Mine, Illinois, USA
- Cave-in-Rock, Illinois, USA
Field-hunting tip
Look in low-temperature hydrothermal veins in sedimentary rocks country — that is the host setting where paralstonite typically forms. If you start seeing fluorite, calcite, quartz in float, you are in the right ground. Field specimens usually show a pseudo-hexagonal dipyramidal crystals habit, so train your eye for that shape before scanning the outcrop.








