Calciomurmanite is a rare phyllosilicate mineral typically found in agpaitic nepheline syenite pegmatites. It most commonly appears as platy, micaceous crystals that exhibit a distinct pearly luster on cleavage surfaces, often found in association with sodium-rich minerals.
Is this calciomurmanite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch calciomurmanite with a known reference. Calciomurmanite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Calciomurmanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Calciomurmanite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: pink, brown, lavender.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, foliated aggregates.
Often confused with
Calciomurmanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside calciomurmanite
Minerals reported to co-occur with calciomurmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂MnTi₂Si₂O₈(OH,F)·nH₂O
- Mohs hardness
- 3-4
- Density
- 2.8-3.0 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Foliated Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nepheline Syenite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find calciomurmanite
Classic worldwide localities
- Khibiny Massif, Russia
- Lovozero Massif, Russia
Field-hunting tip
Look in nepheline syenite pegmatites country — that is the host setting where calciomurmanite typically forms. If you start seeing aegirine, nepheline, microcline in float, you are in the right ground. Field specimens usually show a platy crystals, foliated aggregates habit, so train your eye for that shape before scanning the outcrop.






