Ammonioleucite is a rare tectosilicate mineral characterized by its ammonium content replacing potassium in the leucite structure. It typically occurs as small, sharp trapezohedral crystals within cavities of alkaline volcanic rocks and is often discovered through microscopic analysis of mineral suites.

Hardness
5.5-6
Mohs
Luster
Resinous to vitreous
Streak
White
Transparency
Translucent

Is this ammonioleucite?

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 ammonioleucite with a known reference. Ammonioleucite 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: resinous to vitreous.
  • 4
    Match the color range
    Compare against the expected color range: white.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: trapezohedral crystals.

Often confused with

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

Often found alongside ammonioleucite

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

All properties

Chemical formula
(NH₄)AlSi₂O₆
Mohs hardness
5.5-6
Density
2.29 g/cm³
Colors
Streak
White
Luster
Resinous to vitreous
Transparency
Translucent
Crystal system
Tetragonal
Crystal habit
Trapezohedral crystals
Cleavage
None
Rarity
Rare
Uses
Collector, Scientific research
Host rock
In veinlets, fractures, and cavities in hydrothermally altered crystalline schist, as powdery pseudomorphous replacements of analcime crystals

Where rockhounds find ammonioleucite

Classic worldwide localities

  • Tatarazawa quarry, Fujioka, Gumma Prefecture, Japan

Field-hunting tip

Where it forms: In veinlets, fractures, and cavities in hydrothermally altered crystalline schist, as powdery pseudomorphous replacements of analcime crystals. If you start seeing analcime, dolomite in float, you are in the right ground. Typical habit: trapezohedral crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ammonioleucite?+
Mohs hardness is 5.5-6. Luster: resinous to vitreous. The streak is white. Common colors include white.
Where is ammonioleucite found?+
Notable localities include Tatarazawa quarry, Fujioka, Gumma Prefecture, Japan.
What rocks look like ammonioleucite?+
Ammonioleucite is most often confused with Leucite, Analcime. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ammonioleucite?+
Ammonioleucite commonly co-occurs with Analcime, Dolomite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ammonioleucite form in?+
Where it forms: In veinlets, fractures, and cavities in hydrothermally altered crystalline schist, as powdery pseudomorphous replacements of analcime crystals. Working float back to the host body is the standard way to chase a fresh occurrence.
What is ammonioleucite used for?+
Ammonioleucite is used in collector, scientific research.

Find ammonioleucite on the map

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