Margarosanite is a rare lead-calcium silicate best known to collectors for its intense and distinctive bright white-to-blue fluorescence under shortwave ultraviolet light. It typically occurs as white, pearly platy crystals or massive granular aggregates in metamorphic environments, most notably the famous zinc mines of Franklin, New Jersey, and the mines at Långban, Sweden.

Hardness
2.5-3
Mohs
Luster
Pearly on cleavage
Streak
White
Transparency
Transparent

Is this margarosanite?

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 margarosanite with a known reference. Margarosanite 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: pearly on cleavage.
  • 4
    Match the color range
    Compare against the expected color range: colorless, pearl white.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: cleaveable, granular, prismatic.

Often confused with

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

Often found alongside margarosanite

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

All properties

Chemical formula
Ca₂PbSi₃O₉
Mohs hardness
2.5-3
Density
3.99-4.33 g/cm³
Streak
White
Luster
Pearly on cleavage
Transparency
Transparent
Crystal system
Triclinic
Crystal habit
Cleaveable, granular, prismatic
Cleavage
Perfect on {010}, good on {100}, fair on {001}
Fluorescence
Red sky blue under SW UV; red orange under LW UV
Rarity
Rare
Uses
Collector
Host rock
In a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA)

Where rockhounds find margarosanite

Classic worldwide localities

  • Franklin, Sussex Co., New Jersey, USA
  • Långban and Jakobsberg, Värmland, Sweden

Field-hunting tip

Where it forms: In a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA). If you start seeing nasonite, minehillite, almandine in float, you are in the right ground. Typical habit: cleaveable, granular, prismatic. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify margarosanite?+
Mohs hardness is 2.5-3. Luster: pearly on cleavage. The streak is white. Common colors include colorless, pearl white.
Where is margarosanite found?+
Notable localities include Franklin, Sussex Co., New Jersey, USA; Långban and Jakobsberg, Värmland, Sweden.
Is margarosanite safe to handle?+
Margarosanite contains lead. Contains lead; wash hands thoroughly after handling and avoid ingestion or inhalation of dust.
What rocks look like margarosanite?+
Margarosanite is most often confused with Wollastonite, Pectolite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with margarosanite?+
Margarosanite commonly co-occurs with Nasonite, Minehillite, Almandine, Hancockite, Roeblingite, Franklinite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does margarosanite form in?+
Where it forms: In a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA). Working float back to the host body is the standard way to chase a fresh occurrence.
What is margarosanite used for?+
Margarosanite is used in collector.

Find margarosanite on the map

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