Leucophoenicite is a rare manganese silicate mineral typically found in metamorphosed zinc-manganese ore bodies. It is most famous from the Franklin and Sterling Hill mines in New Jersey, where it appears as small, reddish-pink crystals or compact masses associated with other rare zinc minerals.

Hardness
5.5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this leucophoenicite?

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 leucophoenicite with a known reference. Leucophoenicite 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. Leucophoenicite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Leucophoenicite typically shows a vitreous luster.
  • 4
    Match the color range
    Compare against the expected color range: red, pink, brownish-red, orange.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: tabular crystals, massive, granular.

Often confused with

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

Often found alongside leucophoenicite

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

All properties

Chemical formula
Mn₇(SiO₄)₂(OH)₂
Mohs hardness
5.5-6
Density
3.84 g/cm³
Streak
White
Luster
Vitreous
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Tabular Crystals, Massive, Granular
Cleavage
Good On {001}
Rarity
Rare
Uses
Collector, Mineralogical Research
Host rock
Metamorphosed Zinc Ore Deposits
Typical price
$50-500 depending on specimen size and clarity

Where rockhounds find leucophoenicite

Classic worldwide localities

  • Franklin, New Jersey, USA
  • Sterling Hill, New Jersey, USA
  • Langban, Sweden
  • Pajsberg, Sweden

Field-hunting tip

Look in metamorphosed zinc ore deposits country — that is the host setting where leucophoenicite typically forms. If you start seeing willemite, franklinite, zincite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify leucophoenicite?+
Mohs hardness is 5.5-6. It typically shows a vitreous luster. The streak is white. Common colors include red, pink, brownish-red, orange.
Where is leucophoenicite found?+
Notable localities include Franklin, New Jersey, USA; Sterling Hill, New Jersey, USA; Langban, Sweden; Pajsberg, Sweden.
How much is leucophoenicite worth?+
Typical asking prices fall in the range of $50-500 depending on specimen size and clarity. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like leucophoenicite?+
Leucophoenicite is most often confused with Hodgkinsonite, Alleghanyite, Margarosanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with leucophoenicite?+
Leucophoenicite commonly co-occurs with Willemite, Franklinite, Zincite, Gahnite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does leucophoenicite form in?+
Leucophoenicite typically forms in metamorphosed zinc ore deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is leucophoenicite used for?+
Leucophoenicite is used in collector, mineralogical research.

Find leucophoenicite on the map

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