Roeblingite is a rare lead-calcium silicate mineral primarily known from the unique zinc mines of Franklin and Sterling Hill, New Jersey. It is most easily identified by its striking bright yellow to orange fluorescence under shortwave UV light. Collectors typically find it in massive form associated with other fluorescent minerals like willemite.

Hardness
<3
Mohs
Luster
Dull to somewhat resinous
Streak
White
Transparency
Translucent

Is this roeblingite?

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 roeblingite with a known reference. Roeblingite sits at Mohs <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: dull to somewhat resinous.
  • 4
    Match the color range
    Compare against the expected color range: white, pink.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: massive.

Often confused with

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

Often found alongside roeblingite

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

All properties

Chemical formula
Pb₂Ca₆Mn(Si₃O₉)₂(SO₄)₂(OH)₂(H₂O)₄
Mohs hardness
<3
Density
3.433 g/cm³
Colors
Streak
White
Luster
Dull to somewhat resinous
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Massive
Cleavage
Perfect on {001}
Rarity
Rare
Uses
Collector
Host rock
As nodular masses in calcium silicate lenses containing abundant garnet (Franklin, New Jersey, USA); as fracture fillings in a metamorphosed Fe{Mn orebody (Långban, Sweden)

Where rockhounds find roeblingite

Classic worldwide localities

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

Field-hunting tip

Where it forms: As nodular masses in calcium silicate lenses containing abundant garnet (Franklin, New Jersey, USA); as fracture fillings in a metamorphosed Fe{Mn orebody (Långban, Sweden). If you start seeing garnet, titanite, zircon in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify roeblingite?+
Mohs hardness is <3. Luster: dull to somewhat resinous. The streak is white. Common colors include white, pink.
Where is roeblingite found?+
Notable localities include Franklin, Sussex Co., New Jersey, USA; Långban, Värmland, Sweden.
Is roeblingite safe to handle?+
Roeblingite contains lead. Contains lead; wash hands thoroughly after handling and avoid inhaling dust.
What rocks look like roeblingite?+
Roeblingite is most often confused with Hardystonite, Willemite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with roeblingite?+
Roeblingite commonly co-occurs with Garnet, Titanite, Zircon, Phlogopite, Axinite, Willemite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does roeblingite form in?+
Where it forms: As nodular masses in calcium silicate lenses containing abundant garnet (Franklin, New Jersey, USA); as fracture fillings in a metamorphosed Fe{Mn orebody (Långban, Sweden). Working float back to the host body is the standard way to chase a fresh occurrence.
What is roeblingite used for?+
Roeblingite is used in collector.

Find roeblingite on the map

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