Parasibirskite is a rare calcium borate mineral known primarily from the skarn deposits of the Tayozhnoye region in Siberia. It is typically found as small, white, translucent prismatic crystals associated with other boron-bearing minerals and magnetite in metamorphic environments.

Hardness
3
Mohs
Luster
“Weak”, pearly
Streak
White
Transparency
Semitransparent

Is this parasibirskite?

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 parasibirskite with a known reference. Parasibirskite sits at Mohs 3, 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: “Weak”, pearly.
  • 4
    Match the color range
    Compare against the expected color range: white.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: microscopic crystals, tabular.

Often confused with

Parasibirskite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside parasibirskite

Minerals reported to co-occur with parasibirskite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Ca₂B₂O₅(H₂O)
Mohs hardness
3
Density
2.50 g/cm³
Colors
Streak
White
Luster
“Weak”, pearly
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Microscopic crystals, tabular
Cleavage
Perfect on {100}
Rarity
Rare
Uses
Collector
Host rock
A late-stage hydrothermal alteration of takedaite in a borate-rich vein cutting limestone and gehlenite-spurrite skarn

Where rockhounds find parasibirskite

Classic worldwide localities

  • Fuka, near Bicchu, Okayama Prefecture, Japan

Field-hunting tip

Where it forms: A late-stage hydrothermal alteration of takedaite in a borate-rich vein cutting limestone and gehlenite-spurrite skarn. If you start seeing takedaite, frolovite, olshanskyite in float, you are in the right ground. Typical habit: microscopic crystals, tabular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify parasibirskite?+
Mohs hardness is 3. Luster: “Weak”, pearly. The streak is white. Common colors include white.
Where is parasibirskite found?+
Notable localities include Fuka, near Bicchu, Okayama Prefecture, Japan.
What rocks look like parasibirskite?+
Parasibirskite is most often confused with Sibirskite, Borax. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with parasibirskite?+
Parasibirskite commonly co-occurs with Takedaite, Frolovite, Olshanskyite, Sibirskite, Pentahydroborite, Calcite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does parasibirskite form in?+
Where it forms: A late-stage hydrothermal alteration of takedaite in a borate-rich vein cutting limestone and gehlenite-spurrite skarn. Working float back to the host body is the standard way to chase a fresh occurrence.
What is parasibirskite used for?+
Parasibirskite is used in collector.

Find parasibirskite on the map

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