Emeleusite is an exceptionally rare sodium-lithium-iron silicate mineral found primarily in hyper-alkaline igneous rocks. It typically forms small, pale, tabular crystals in syenite pegmatites, often requiring microscopic examination for positive identification. It is highly prized by advanced mineral collectors specializing in rare-earth or alkaline igneous minerals.

Hardness
5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this emeleusite?

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 emeleusite with a known reference. Emeleusite 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: colorless, pink white.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: tabular crystals, massive, granular.

Often confused with

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

Often found alongside emeleusite

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

All properties

Chemical formula
Na₂LiFe³⁺Si₆O₁₅
Mohs hardness
5-6
Density
2.76 g/cm³
Colors
ColorlessPink white
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Orthorhombic
Crystal habit
Tabular crystals, massive, granular
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
A minor constituent of a peralkalic trachyte dike, in flow-banded aegirine-albite-rich layers

Where rockhounds find emeleusite

Classic worldwide localities

  • Island of Igdlutalik, Julianehåb district, Greenland

Field-hunting tip

Where it forms: A minor constituent of a peralkalic trachyte dike, in flow-banded aegirine-albite-rich layers. If you start seeing albite, aegirine, quartz in float, you are in the right ground. Typical habit: tabular crystals, massive, granular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify emeleusite?+
Mohs hardness is 5-6. Luster: vitreous. The streak is white. Common colors include colorless, pink white.
Where is emeleusite found?+
Notable localities include Island of Igdlutalik, Julianehåb district, Greenland.
What rocks look like emeleusite?+
Emeleusite is most often confused with Aegirine, Arfvedsonite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with emeleusite?+
Emeleusite commonly co-occurs with Albite, Aegirine, Quartz, Riebeckite, Micas, Zircon. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does emeleusite form in?+
Where it forms: A minor constituent of a peralkalic trachyte dike, in flow-banded aegirine-albite-rich layers. Working float back to the host body is the standard way to chase a fresh occurrence.
What is emeleusite used for?+
Emeleusite is used in collector.

Find emeleusite on the map

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