Shlykovite is a rare potassium-calcium silicate mineral primarily found in hyperalkaline pegmatites. It typically forms thin, transparent, tabular crystals that can be difficult to distinguish from associated apophyllite group members without analytical testing.

Hardness
2.5-3
Mohs
Luster
Vitreous; aggregates, pearly to silky
Streak
White
Transparency
Transparent

Is this shlykovite?

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 shlykovite with a known reference. Shlykovite sits at Mohs 2.5-3, 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; aggregates, pearly to silky.
  • 4
    Match the color range
    Compare against the expected color range: grayish white, beige.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: platy crystals, tabular aggregates.

Often confused with

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

Often found alongside shlykovite

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

All properties

Chemical formula
KCa[Si₄O₉(OH)]·3H₂O
Mohs hardness
2.5-3
Density
2.244 g/cm³
Streak
White
Luster
Vitreous; aggregates, pearly to silky
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Platy crystals, tabular 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 shlykovite

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 cryptophyllite in float, you are in the right ground. Typical habit: platy crystals, tabular aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify shlykovite?+
Mohs hardness is 2.5-3. Luster: vitreous; aggregates, pearly to silky. The streak is white. Common colors include grayish white, beige.
Where is shlykovite found?+
Notable localities include Central mine, Mt. Rasvumchorr, Khibiny massif, Kola Peninsula, Russia.
What rocks look like shlykovite?+
Shlykovite is most often confused with Apophyllite, Okenite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with shlykovite?+
Shlykovite commonly co-occurs with Cryptophyllite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does shlykovite 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 shlykovite used for?+
Shlykovite is used in collector.

Find shlykovite on the map

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