Antigorite is a common member of the serpentine group, often appearing as massive or platy, foliated green aggregates. It is a primary constituent of serpentinite rocks and is typically found in altered ultramafic environments where magnesium-rich rocks have undergone metamorphism.

Hardness
2.5-3.5
Mohs
Luster
Resinous, greasy, silky, waxy, earthy
Streak
White
Transparency
Translucent to opaque

Is this antigorite?

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 antigorite with a known reference. Antigorite sits at Mohs 2.5-3.5, 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, greasy, silky, waxy, earthy.
  • 4
    Match the color range
    Compare against the expected color range: green, yellow-green, brown, white, gray, bluish gray, black.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: massive, platy, scaly.

Often confused with

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

Often found alongside antigorite

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

All properties

Chemical formula
Mg₃Si₂O₅(OH)₄
Mohs hardness
2.5-3.5
Density
2.65 g/cm³
Streak
White
Luster
Resinous, greasy, silky, waxy, earthy
Transparency
Translucent to opaque
Crystal system
Monoclinic
Crystal habit
Massive, platy, scaly
Cleavage
Perfect on {001}, observed on {100} and {010}
Rarity
Common
Uses
Collector, Lapidary
Host rock
Commonly replaces ultramafic rocks, pervasively or in crosscutting veinlets

Where rockhounds find antigorite

Classic worldwide localities

  • Texas, Lancaster Co., Pennsylvania, USA
  • Baltimore, Baltimore Co., Maryland, USA
  • Brewster, Putnam Co., New York, USA
  • Buck Creek, Clay Co., North Carolina, USA
  • Val Antigorio, Piedmont, Italy
  • Prägraten, Tirol, Austria

Field-hunting tip

Where it forms: Commonly replaces ultramafic rocks, pervasively or in crosscutting veinlets. If you start seeing chromite, magnetite, chrysotile in float, you are in the right ground. Typical habit: massive, platy, scaly. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify antigorite?+
Mohs hardness is 2.5-3.5. Luster: resinous, greasy, silky, waxy, earthy. The streak is white. Common colors include green, yellow-green, brown, white.
Where is antigorite found?+
Notable localities include Texas, Lancaster Co., Pennsylvania, USA; Baltimore, Baltimore Co., Maryland, USA; Brewster, Putnam Co., New York, USA; Buck Creek, Clay Co., North Carolina, USA; Val Antigorio, Piedmont, Italy.
What rocks look like antigorite?+
Antigorite is most often confused with Chrysotile, Lizardite, Talc. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with antigorite?+
Antigorite commonly co-occurs with Chromite, Magnetite, Chrysotile, Olivine. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does antigorite form in?+
Where it forms: Commonly replaces ultramafic rocks, pervasively or in crosscutting veinlets. Working float back to the host body is the standard way to chase a fresh occurrence.
What is antigorite used for?+
Antigorite is used in collector, lapidary.

Find antigorite on the map

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