Cryptophyllite is a rare hydrated potassium calcium silicate found primarily in alkaline igneous rocks like nepheline syenites. It typically occurs as small tabular crystals or crusts and is best identified by its association with unique minerals in the Kola Peninsula massifs.

Hardness
3.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this cryptophyllite?

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 cryptophyllite with a known reference. Cryptophyllite sits at Mohs 3.5, 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: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: colorless.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: tabular crystals, aggregates.

Often confused with

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

Often found alongside cryptophyllite

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

All properties

Chemical formula
K₂Ca[Si₄O₁₀]·5H₂O
Mohs hardness
3.5
Density
2.185 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Tabular crystals, aggregates
Cleavage
Perfect on {001}
Rarity
Rare
Uses
Collector
Host rock
A late-stage hydrothermal mineral along fractures in a high-potassium peralkaline pegmatite in urtite rocks near the contact with nepheline-apatite rock

Where rockhounds find cryptophyllite

Classic worldwide localities

  • Central mine, Mt. Rasvumchorr, Khibiny massif, Kola Peninsula, Russia

Field-hunting tip

Where it forms: A late-stage hydrothermal mineral along fractures in a high-potassium peralkaline pegmatite in urtite rocks near the contact with nepheline-apatite rock. If you start seeing shlykovite in float, you are in the right ground. Typical habit: tabular crystals, aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify cryptophyllite?+
Mohs hardness is 3.5. Luster: vitreous. The streak is white. Common colors include colorless.
Where is cryptophyllite found?+
Notable localities include Central mine, Mt. Rasvumchorr, Khibiny massif, Kola Peninsula, Russia.
What rocks look like cryptophyllite?+
Cryptophyllite is most often confused with Narsarsukite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with cryptophyllite?+
Cryptophyllite commonly co-occurs with Shlykovite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does cryptophyllite form in?+
Where it forms: A late-stage hydrothermal mineral along fractures in a high-potassium peralkaline pegmatite in urtite rocks near the contact with nepheline-apatite rock. Working float back to the host body is the standard way to chase a fresh occurrence.
What is cryptophyllite used for?+
Cryptophyllite is used in collector.

Find cryptophyllite on the map

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