Eudidymite is a rare beryllium silicate that often forms distinct pseudo-hexagonal, tabular crystals. It is chemically dimorphous with epididymite and is primarily found as a late-stage mineral in alkaline pegmatites, frequently appearing as white, bladed aggregates.

Hardness
6
Mohs
Luster
Vitreous, pearly on cleavage
Streak
White
Transparency
Transparent to translucent

Is this eudidymite?

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 eudidymite with a known reference. Eudidymite 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, pearly on cleavage.
  • 4
    Match the color range
    Compare against the expected color range: blue, colorless, violet, gray, yellow.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: tabular, twinning common.

Often confused with

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

Often found alongside eudidymite

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

All properties

Chemical formula
Na₂Be₂Si₆O₁₅·H₂O
Mohs hardness
6
Density
2.55 g/cm³
Streak
White
Luster
Vitreous, pearly on cleavage
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Tabular, twinning common
Cleavage
Perfect on {001}, imperfect on {551}
Rarity
Rare
Uses
Collector
Host rock
A late-stage mineral in alkalic nepheline syenite pegmatites

Where rockhounds find eudidymite

Classic worldwide localities

  • Arø Island, in the Langesundsfjord, Norway
  • Meldon, Okehampton, Devon, England
  • Věžná, Czech Republic
  • Mt. Alluaiv, Lovozero massif, and Mt. Yukspor, Khibiny massif, Kola Peninsula, Russia
  • Burpala massif, 120 km north of Lake Baikal, eastern Siberia, Russia
  • Seal Lake, Labrador, Newfoundland, and at Mont Saint-Hilaire, Quebec, Canada

Field-hunting tip

Where it forms: A late-stage mineral in alkalic nepheline syenite pegmatites. If you start seeing albite, neptunite, aegirine in float, you are in the right ground. Typical habit: tabular, twinning common. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify eudidymite?+
Mohs hardness is 6. Luster: vitreous, pearly on cleavage. The streak is white. Common colors include blue, colorless, violet, gray.
Where is eudidymite found?+
Notable localities include Arø Island, in the Langesundsfjord, Norway; Meldon, Okehampton, Devon, England; Věžná, Czech Republic; Mt. Alluaiv, Lovozero massif, and Mt. Yukspor, Khibiny massif, Kola Peninsula, Russia; Burpala massif, 120 km north of Lake Baikal, eastern Siberia, Russia.
Is eudidymite safe to handle?+
Eudidymite contains beryllium. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like eudidymite?+
Eudidymite is most often confused with Epididymite, Albite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with eudidymite?+
Eudidymite commonly co-occurs with Albite, Neptunite, Aegirine, Elpidite, Natrolite, Analcime. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does eudidymite form in?+
Where it forms: A late-stage mineral in alkalic nepheline syenite pegmatites. Working float back to the host body is the standard way to chase a fresh occurrence.
What is eudidymite used for?+
Eudidymite is used in collector.

Find eudidymite on the map

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