Paracelsian is a rare barium aluminosilicate that belongs to the feldspar group. It is typically found in manganese-rich deposits or metamorphic environments, often forming small, clear to white tabular crystals that require careful examination to distinguish from more common feldspars.
Is this paracelsian?
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 paracelsian with a known reference. Paracelsian sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Paracelsian leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Paracelsian typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, granular.
Often confused with
Paracelsian vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paracelsian
Minerals reported to co-occur with paracelsian. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaAl₂Si₂O₈
- Mohs hardness
- 6
- Density
- 3.31 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Granular
- Cleavage
- Distinct On {001} and {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Manganese Deposits and Hydrothermal Veins
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find paracelsian
Classic worldwide localities
- Gisburn, England
- Benallt mine, Wales
- Franklin, New Jersey, USA
- Khibiny Massif, Russia
Field-hunting tip
Look in metamorphic manganese deposits and hydrothermal veins country, the host setting where paracelsian typically forms. If you start seeing quartz, albite, muscovite in float, you are in the right ground. Field specimens usually show a tabular crystals, granular habit, so train your eye for that shape before scanning the outcrop.






