Imayoshiite is an extremely rare calcium aluminum borosilicate mineral known primarily from the Fuka Mine in Japan. It typically occurs as small, colorless, prismatic crystals within skarn environments associated with high-temperature contact metamorphism of limestone.

Hardness
2-3
Mohs
Luster
Vitreous (crystals); silky (aggregates)
Streak
White
Transparency
Transparent

Is this imayoshiite?

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 imayoshiite with a known reference. Imayoshiite sits at Mohs 2-3, 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: vitreous (crystals); silky (aggregates).
  • 4
    Match the color range
    Compare against the expected color range: colorless crystals.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: prismatic crystals.

Often confused with

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

Often found alongside imayoshiite

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

All properties

Chemical formula
Ca₃Al(CO₃)[B(OH)₄](OH)₆·12H₂O
Mohs hardness
2-3
Density
1.79 g/cm³
Colors
Colorless crystals
Streak
White
Luster
Vitreous (crystals); silky (aggregates)
Transparency
Transparent
Crystal system
Hexagonal
Crystal habit
Prismatic crystals
Cleavage
Distinct on {101̄0}
Rarity
Rare
Uses
Collector
Host rock
In cavities in an altered gabbro xenolith in serpentinized dunite, where rims of the xenoliths were hydrothermally altered

Where rockhounds find imayoshiite

Classic worldwide localities

  • Suisho-dani valley, Ise City, Mie Prefecture, Japan

Field-hunting tip

Where it forms: In cavities in an altered gabbro xenolith in serpentinized dunite, where rims of the xenoliths were hydrothermally altered. If you start seeing oyelite, xonotlite, tobermorite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify imayoshiite?+
Mohs hardness is 2-3. Luster: vitreous (crystals); silky (aggregates). The streak is white. Common colors include colorless crystals.
Where is imayoshiite found?+
Notable localities include Suisho-dani valley, Ise City, Mie Prefecture, Japan.
What rocks look like imayoshiite?+
Imayoshiite is most often confused with Sakhaite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with imayoshiite?+
Imayoshiite commonly co-occurs with Oyelite, Xonotlite, Tobermorite, Bultfonteinite, Apophyllite, Prehnite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does imayoshiite form in?+
Where it forms: In cavities in an altered gabbro xenolith in serpentinized dunite, where rims of the xenoliths were hydrothermally altered. Working float back to the host body is the standard way to chase a fresh occurrence.
What is imayoshiite used for?+
Imayoshiite is used in collector.

Find imayoshiite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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