
metamorphic
Serpentine
Antigorite, Lizardite, or Chrysotile; Mg3Si2O5(OH)4
Hardness: 3-6 Mohs; Color: Mottled green, dark green to black-green, or brownish-yellow; Luster: Waxy, greasy, or silky; Crystal system: Monoclinic; Cleavage: Poor; Specific Gravity: 2.5-3.2
- Hardness
- 3-6 Mohs
- Color
- Mottled green, dark green to black-green, or brownish-yellow
- Luster
- Waxy, greasy, or silky
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Physical properties
Hardness: 3-6 Mohs; Color: Mottled green, dark green to black-green, or brownish-yellow; Luster: Waxy, greasy, or silky; Crystal system: Monoclinic; Cleavage: Poor; Specific Gravity: 2.5-3.2
Formation & geological history
Formed through serpentinization, a metamorphic process where low-silica ultramafic rocks (like peridotite) from the Earth's mantle are hydrothermalized by water at relatively low temperatures.
Uses & applications
Used as a decorative architectural stone, for carving sculptures, as a source for magnesium and asbestos (historically), and as lapidary material for jewelry and ornaments.
Geological facts
Serpentine is the state rock of California. Its name is derived from its snake-like green color and mottled texture. It is often confused with jade but is significantly softer.
Field identification & locations
Identify by its characteristic waxy luster and soapy feel. It is found in mountain belts formed by plate tectonics, such as the Appalachian Mountains, Cascades, and the Alps.
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