Lizardite is a common member of the serpentine group and is typically found as dense, massive, or scaly green to grey aggregates. Collectors should look for its characteristic greasy luster and waxy feel, which differentiates it from harder silicate minerals in similar environments.

Hardness
2.5
Mohs
Luster
Waxy
Streak
White
Transparency
Translucent

Is this lizardite?

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 lizardite with a known reference. Lizardite sits at Mohs 2.5, 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: waxy.
  • 4
    Match the color range
    Compare against the expected color range: green, yellow-green, white, gray, brown, green blue, yellow.
  • 5
    Look at form & habit
    Crystal system: hexagonal. Typical habit: massive, foliated, or scaly aggregates.

Often confused with

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

Often found alongside lizardite

Minerals reported to co-occur with lizardite. 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
Density
2.55 g/cm³
Streak
White
Luster
Waxy
Transparency
Translucent
Crystal system
Hexagonal
Crystal habit
Massive, foliated, or scaly aggregates
Cleavage
Perfect on {0001}
Rarity
Common
Uses
Collector, Decorative, Ornamental
Host rock
Typically a product of retrograde metamorphism, replacing olivine, orthopyroxene, or other minerals in ultramafic igneous rocks

Where rockhounds find lizardite

Classic worldwide localities

  • Stillwater complex, Montana, USA
  • Kennack Cove, The Lizard, Cornwall, England
  • Unst, Shetland Islands, Scotland
  • Val Sissone, Lombardy, and Val Trebbia, Piacenza, Italy
  • Maruo Odori and Kodo, Yamaguchi Prefecture, and at Hamao, Fukuoka Prefecture, Japan
  • Woodsreef, New South Wales, Australia

Field-hunting tip

Where it forms: Typically a product of retrograde metamorphism, replacing olivine, orthopyroxene, or other minerals in ultramafic igneous rocks. If you start seeing chrysotile, brucite, magnetite in float, you are in the right ground. Typical habit: massive, foliated, or scaly aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify lizardite?+
Mohs hardness is 2.5. Luster: waxy. The streak is white. Common colors include green, yellow-green, white, gray.
Where is lizardite found?+
Notable localities include Stillwater complex, Montana, USA; Kennack Cove, The Lizard, Cornwall, England; Unst, Shetland Islands, Scotland; Val Sissone, Lombardy, and Val Trebbia, Piacenza, Italy; Maruo Odori and Kodo, Yamaguchi Prefecture, and at Hamao, Fukuoka Prefecture, Japan.
What rocks look like lizardite?+
Lizardite is most often confused with Antigorite, Chrysotile, Talc. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with lizardite?+
Lizardite commonly co-occurs with Chrysotile, Brucite, Magnetite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does lizardite form in?+
Where it forms: Typically a product of retrograde metamorphism, replacing olivine, orthopyroxene, or other minerals in ultramafic igneous rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is lizardite used for?+
Lizardite is used in collector, decorative, ornamental.

Find lizardite on the map

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