Rock Identifier
Soapstone (Steatite (composed primarily of Talc, Mg3Si4O10(OH)2)) — metamorphic
metamorphic

Soapstone

Steatite (composed primarily of Talc, Mg3Si4O10(OH)2)

Hardness: 1.0 - 2.5 on Mohs scale (can be scratched with a fingernail); Color: shades of gray, green, brown, or reddish-tan due to iron oxidation; Luster: greasy to pearly; Structure: massive/foliated; soapy or slick feel.

Hardness
1
Luster
greasy to pearly
Identified More metamorphic

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Physical properties

Hardness: 1.0 - 2.5 on Mohs scale (can be scratched with a fingernail); Color: shades of gray, green, brown, or reddish-tan due to iron oxidation; Luster: greasy to pearly; Structure: massive/foliated; soapy or slick feel.

Formation & geological history

Formed through the regional or contact metamorphism of ultramafic igneous rocks (like peridotite) or siliceous dolostones in subduction zones or mountain-building environments. Ages vary from Precambrian to Cenozoic.

Uses & applications

Used for decorative carvings, sculptures, kitchen countertops, wood-burning stoves (due to high heat capacity), and electrical insulators.

Geological facts

Soapstone is naturally acid and heat resistant. It has been used for over 3,000 years by various cultures for cooking vessels and seals because it is easy to carve and retains heat exceptionally well.

Field identification & locations

Identify by its 'soapy' feel and very low hardness. It is commonly found in metamorphic belts in Brazil, India, China, Finland, and the USA (Appalachia). Collectors should look for smoothness and the absence of sharp mineral grains.