Rastsvetaevite is a rare member of the eudialyte group found in hyper-alkaline pegmatites of the Kola Peninsula. It typically occurs as small, reddish-pink massive grains associated with other rare-earth-bearing silicate minerals. Collectors identify it through its structural similarity to eudialyte, often requiring X-ray diffraction or microprobe analysis to confirm its identity.

Hardness
5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this rastsvetaevite?

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 rastsvetaevite with a known reference. Rastsvetaevite sits at Mohs 5-6, 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.
  • 4
    Match the color range
    Compare against the expected color range: pink.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: equant grains, anhedral crystals.

Often confused with

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

Often found alongside rastsvetaevite

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

All properties

Chemical formula
Na₂₇K₈Ca₁₂Fe₃Zr₆Si₅₂O₁₄₄(OH,H₂O)₆Cl₂
Mohs hardness
5-6
Density
2.86 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Trigonal
Crystal habit
Equant grains, anhedral crystals
Cleavage
None
Rarity
Rare
Uses
Collector, Mineralogical study
Host rock
In alkaline pegmatite in zоnes of late intense potassium metasomatism

Where rockhounds find rastsvetaevite

Classic worldwide localities

  • Mt. Rasvumchorr, Khibiny alkaline massif, Kola Peninsula, Russia

Field-hunting tip

Where it forms: In alkaline pegmatite in zоnes of late intense potassium metasomatism. If you start seeing nepheline, sodalite, potassium feldspar in float, you are in the right ground. Typical habit: equant grains, anhedral crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify rastsvetaevite?+
Mohs hardness is 5-6. Luster: vitreous. The streak is white. Common colors include pink.
Where is rastsvetaevite found?+
Notable localities include Mt. Rasvumchorr, Khibiny alkaline massif, Kola Peninsula, Russia.
What rocks look like rastsvetaevite?+
Rastsvetaevite is most often confused with Eudialyte, Kentbrooksite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with rastsvetaevite?+
Rastsvetaevite commonly co-occurs with Nepheline, Sodalite, Potassium feldspar, Aegirine, Scherbakovite, Villiaumite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does rastsvetaevite form in?+
Where it forms: In alkaline pegmatite in zоnes of late intense potassium metasomatism. Working float back to the host body is the standard way to chase a fresh occurrence.
What is rastsvetaevite used for?+
Rastsvetaevite is used in collector, mineralogical study.

Find rastsvetaevite on the map

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