Parakeldyshite is a rare sodium zirconium silicate mineral typically found in complex alkaline igneous rocks. Collectors primarily seek it from the classic pegmatite localities of the Kola Peninsula and Mont Saint-Hilaire, where it occurs as small, glassy tabular crystals.

Hardness
5.5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this parakeldyshite?

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 parakeldyshite with a known reference. Parakeldyshite sits at Mohs 5.5-6, 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: bluish white, white.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: tabular crystals, massive, granular.

Often confused with

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

Often found alongside parakeldyshite

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

All properties

Chemical formula
Na₂ZrSi₂O₇
Mohs hardness
5.5-6
Density
3.37-3.39 g/cm³
Streak
White
Luster
Vitreous
Transparency
Translucent
Crystal system
Triclinic
Crystal habit
Tabular crystals, massive, granular
Cleavage
Perfect on {001}; very good on {110} and {110}; good on {011}
Fluorescence
Orange-white under SW UV
Rarity
Rare
Uses
Collector, Research
Host rock
As masses in nepheline syenite pegmatites which cut a foyaite (Bratthagen, Norway)

Where rockhounds find parakeldyshite

Classic worldwide localities

  • Mt. Takhtarvumchorr, in the Khibiny massif, and on Mt. Alluaiv, in the Lovozero massif, Kola Peninsula, Russia
  • Bratthagen, near Larvik, Norway
  • Mont Saint-Hilaire, Quebec, Canada

Field-hunting tip

Where it forms: As masses in nepheline syenite pegmatites which cut a foyaite (Bratthagen, Norway). If you start seeing alkalic feldspar, nepheline, aegirine 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 parakeldyshite?+
Mohs hardness is 5.5-6. Luster: vitreous. The streak is white. Common colors include bluish white, white.
Where is parakeldyshite found?+
Notable localities include Mt. Takhtarvumchorr, in the Khibiny massif, and on Mt. Alluaiv, in the Lovozero massif, Kola Peninsula, Russia; Bratthagen, near Larvik, Norway; Mont Saint-Hilaire, Quebec, Canada.
What rocks look like parakeldyshite?+
Parakeldyshite is most often confused with Keldyshite, Zircon. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with parakeldyshite?+
Parakeldyshite commonly co-occurs with Alkalic feldspar, Nepheline, Aegirine, Pyrophanite, Loparite, Biotite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does parakeldyshite form in?+
Where it forms: As masses in nepheline syenite pegmatites which cut a foyaite (Bratthagen, Norway). Working float back to the host body is the standard way to chase a fresh occurrence.
What is parakeldyshite used for?+
Parakeldyshite is used in collector, research.

Find parakeldyshite on the map

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