Okayamalite is a very rare borosilicate mineral belonging to the melilite group, typically found as small, tabular crystals within contact metamorphic zones. It is named after the prefecture in Japan where it was first discovered. Collectors primarily seek it as a localized, exotic addition to systematic mineral collections.

Hardness
~5.5
Mohs
Luster
Earthy
Streak
White
Transparency
Translucent

Is this okayamalite?

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 okayamalite with a known reference. Okayamalite sits at Mohs ~5.5, 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: earthy.
  • 4
    Match the color range
    Compare against the expected color range: creamy white.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: microscopic crystals.

Often confused with

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

Often found alongside okayamalite

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

All properties

Chemical formula
Ca₂B₂SiO₇
Mohs hardness
~5.5
Density
3.3 g/cm³
Colors
Creamy white
Streak
White
Luster
Earthy
Transparency
Translucent
Crystal system
Tetragonal
Crystal habit
Microscopic crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
In skarn by boron metasomatism of a wollastonite-calcite aggregate (Japan); probably by desilication-dehydroxylation of datolite in a magnetite-hematite skarn deposit (Norway)

Where rockhounds find okayamalite

Classic worldwide localities

  • Fuka Mine, Bicchu-cho, Okayama Prefecture, Japan (type locality)
  • Arendal district, Sørlandet, Norway

Field-hunting tip

Where it forms: In skarn by boron metasomatism of a wollastonite-calcite aggregate (Japan); probably by desilication-dehydroxylation of datolite in a magnetite-hematite skarn deposit (Norway). If you start seeing wollastonite, vesuvianite, calcite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify okayamalite?+
Mohs hardness is ~5.5. Luster: earthy. The streak is white. Common colors include creamy white.
Where is okayamalite found?+
Notable localities include Fuka Mine, Bicchu-cho, Okayama Prefecture, Japan (type locality); Arendal district, Sørlandet, Norway.
What rocks look like okayamalite?+
Okayamalite is most often confused with Gehlenite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with okayamalite?+
Okayamalite commonly co-occurs with Wollastonite, Vesuvianite, Calcite, Johnbaumite, Datolite, Apophyllite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does okayamalite form in?+
Where it forms: In skarn by boron metasomatism of a wollastonite-calcite aggregate (Japan); probably by desilication-dehydroxylation of datolite in a magnetite-hematite skarn deposit (Norway). Working float back to the host body is the standard way to chase a fresh occurrence.
What is okayamalite used for?+
Okayamalite is used in collector.

Find okayamalite on the map

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