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.

Hardness
~6
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent to translucent

Is this paracelsian?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch paracelsian with a known reference. Paracelsian sits at Mohs ~6, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: colorless, white.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: pseudo orthorhombic.

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
3.29-3.32 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Pseudo orthorhombic
Cleavage
{110}, poor; (110) ^ (110) = 87°
Rarity
Rare
Uses
Collector
Host rock
In a band through shales and sandstones, associated with a metamorphosed manganese deposit (Benallt mine, Wales)

Where rockhounds find paracelsian

Classic worldwide localities

  • Candoglia, Valle d'Ossola, Piedmont, Italy
  • Benallt mine, Rhiw, Lleyn Peninsula, Wales

Field-hunting tip

Where it forms: In a band through shales and sandstones, associated with a metamorphosed manganese deposit (Benallt mine, Wales). If you start seeing celsian in float, you are in the right ground. Typical habit: pseudo orthorhombic. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify paracelsian?+
Mohs hardness is ~6. Luster: vitreous. The streak is white. Common colors include colorless, white.
Where is paracelsian found?+
Notable localities include Candoglia, Valle d'Ossola, Piedmont, Italy; Benallt mine, Rhiw, Lleyn Peninsula, Wales.
What rocks look like paracelsian?+
Paracelsian is most often confused with Celsian, Danburite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with paracelsian?+
Paracelsian commonly co-occurs with Celsian. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does paracelsian form in?+
Where it forms: In a band through shales and sandstones, associated with a metamorphosed manganese deposit (Benallt mine, Wales). Working float back to the host body is the standard way to chase a fresh occurrence.
What is paracelsian used for?+
Paracelsian is used in collector.

Find paracelsian on the map

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