Bohseite is a rare beryllium silicate mineral that typically forms as delicate, fibrous, or acicular radiating clusters. It is almost exclusively found in highly evolved pegmatites and is best identified through laboratory analysis due to its visual similarity to other beryllium silicates like bavenite.

Hardness
5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this bohseite?

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 bohseite with a known reference. Bohseite sits at Mohs 5-6, 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: white.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: fibrous aggregates, radiating clusters.

Often confused with

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

Often found alongside bohseite

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

All properties

Chemical formula
Ca₄Be₄Al₀Si₉O₂₅₋₂₄(OH)₄
Mohs hardness
5-6
Density
2.719 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Translucent
Crystal system
Orthorhombic
Crystal habit
Fibrous aggregates, radiating clusters
Cleavage
Perfect on {001}, fair on {010}
Rarity
Rare
Uses
Collector
Host rock
In strongly fractionated parts of zoned anatectic (NYF-LCT) pegmatite dikes that cut amphibolite

Where rockhounds find bohseite

Classic worldwide localities

  • Piława Górna quarry, eastern part of the Góry Sowie Block, NE part of the Bohemian massif, ∼50 km southwest of Wrocław, Poland and from the Ilímaussaq alkaline complex, South Greenland

Field-hunting tip

Where it forms: In strongly fractionated parts of zoned anatectic (NYF-LCT) pegmatite dikes that cut amphibolite. If you start seeing microcline, cs-rich beryl, phenakite in float, you are in the right ground. Typical habit: fibrous aggregates, radiating clusters. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify bohseite?+
Mohs hardness is 5-6. Luster: vitreous. The streak is white. Common colors include white.
Where is bohseite found?+
Notable localities include Piława Górna quarry, eastern part of the Góry Sowie Block, NE part of the Bohemian massif, ∼50 km southwest of Wrocław, Poland and from the Ilímaussaq alkaline complex, South Greenland.
Is bohseite safe to handle?+
Bohseite contains beryllium. Contains beryllium, which is toxic if inhaled or ingested; handle with care and wash hands thoroughly after handling mineral specimens.
What rocks look like bohseite?+
Bohseite is most often confused with Bavenite, Epididymite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with bohseite?+
Bohseite commonly co-occurs with Microcline, Cs-rich beryl, Phenakite, Helvite, Lepidolite, Bertrandite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does bohseite form in?+
Where it forms: In strongly fractionated parts of zoned anatectic (NYF-LCT) pegmatite dikes that cut amphibolite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is bohseite used for?+
Bohseite is used in collector.

Find bohseite on the map

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