Simmonsite is an extremely rare fluoride mineral typically found as small, colorless to pale yellow granular masses within alkaline pegmatite environments. It is chemically distinct for its sodium-lithium-aluminum composition and is primarily prized by advanced mineral collectors for its scarcity and unique locality origins.

Hardness
2.5-3
Mohs
Luster
Greasy
Streak
White
Transparency
Transparent to translucent

Is this simmonsite?

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 simmonsite with a known reference. Simmonsite sits at Mohs 2.5-3, 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: greasy.
  • 4
    Match the color range
    Compare against the expected color range: pale buff cream.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: inclusions, microscopic crystals.

Often confused with

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

Often found alongside simmonsite

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

All properties

Chemical formula
Na₂LiAlF₆
Mohs hardness
2.5-3
Density
3.05 g/cm³
Colors
Pale buff cream
Streak
White
Luster
Greasy
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Inclusions, microscopic crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
A late-stage hydrothermal mineral in a breccia pipe that cuts an amazonite-topaz-zinnwaldite pegmatite

Where rockhounds find simmonsite

Classic worldwide localities

  • Zapot amazonite-topaz-zinnwaldite pegmatite, Gillis Range, Mineral Co., Nevada (type locality), USA
  • Katugin massif, Transbaikalia, Russia

Field-hunting tip

Where it forms: A late-stage hydrothermal mineral in a breccia pipe that cuts an amazonite-topaz-zinnwaldite pegmatite. If you start seeing cryolite, cryolithionite, elpasolite in float, you are in the right ground. Typical habit: inclusions, microscopic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify simmonsite?+
Mohs hardness is 2.5-3. Luster: greasy. The streak is white. Common colors include pale buff cream.
Where is simmonsite found?+
Notable localities include Zapot amazonite-topaz-zinnwaldite pegmatite, Gillis Range, Mineral Co., Nevada (type locality), USA; Katugin massif, Transbaikalia, Russia.
What rocks look like simmonsite?+
Simmonsite is most often confused with Cryolite, Chiolite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with simmonsite?+
Simmonsite commonly co-occurs with Cryolite, Cryolithionite, Elpasolite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does simmonsite form in?+
Where it forms: A late-stage hydrothermal mineral in a breccia pipe that cuts an amazonite-topaz-zinnwaldite pegmatite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is simmonsite used for?+
Simmonsite is used in collector.

Find simmonsite on the map

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