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, 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.








