Murmanite is a rare phyllosilicate mineral that typically forms as soft, platy or micaceous masses within alkaline pegmatites. Collectors often identify it by its distinct pearly luster and thin, flexible plates that resemble dark mica when weathered.

Hardness
2-3
Mohs
Luster
Vitreous on cleavages, greasy on fractures
Streak
White
Transparency
Translucent to opaque

Is this murmanite?

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 murmanite with a known reference. Murmanite 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 on cleavages, greasy on fractures.
  • 4
    Match the color range
    Compare against the expected color range: pink, bright pink, silvery, yellow, brown.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: massive, tabular.

Often confused with

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

Often found alongside murmanite

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

All properties

Chemical formula
Na₂Ti₂Na₂Ti₂(Si₂O₇)₂O₄(H₂O)₄
Mohs hardness
2-3
Density
2.76-2.84 g/cm³
Colors
PinkBright pinkSilveryYellowBrown
Streak
White
Luster
Vitreous on cleavages, greasy on fractures
Transparency
Translucent to opaque
Crystal system
Triclinic
Crystal habit
Massive, tabular
Cleavage
{001}, perfect
Rarity
Rare
Uses
Collector, Scientific research
Host rock
In pegmatites and associated igneous rocks of alkalic complexes, as a primary magmatic mineral or altered from lomonosovite

Where rockhounds find murmanite

Classic worldwide localities

  • Chinglusuai Valley, on Mts. Flora, Punkaruaiv, and Angvundaschorr, Lovozero massif, and on Mts. Rasvumchorr and Koashva, Khibiny massif, Kola Peninsula, Russia

Field-hunting tip

Where it forms: In pegmatites and associated igneous rocks of alkalic complexes, as a primary magmatic mineral or altered from lomonosovite. If you start seeing lomonosovite, aegirine, arfvedsonite in float, you are in the right ground. Typical habit: massive, tabular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify murmanite?+
Mohs hardness is 2-3. Luster: vitreous on cleavages, greasy on fractures. The streak is white. Common colors include pink, bright pink, silvery, yellow.
Where is murmanite found?+
Notable localities include Chinglusuai Valley, on Mts. Flora, Punkaruaiv, and Angvundaschorr, Lovozero massif, and on Mts. Rasvumchorr and Koashva, Khibiny massif, Kola Peninsula, Russia.
What rocks look like murmanite?+
Murmanite is most often confused with Lomonosovite, Biotite, Astrophyllite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with murmanite?+
Murmanite commonly co-occurs with Lomonosovite, Aegirine, Arfvedsonite, Neptunite, Microcline, Albite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does murmanite form in?+
Where it forms: In pegmatites and associated igneous rocks of alkalic complexes, as a primary magmatic mineral or altered from lomonosovite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is murmanite used for?+
Murmanite is used in collector, scientific research.

Find murmanite on the map

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