Rock Identifier
Carrara Marble (Recrystallized Calcite (CaCO3)) — metamorphic
metamorphic

Carrara Marble

Recrystallized Calcite (CaCO3)

Hardness: 3 on Mohs scale; Color: Pure white to blue-gray; Luster: Waxy to pearly; Crystal Structure: Trigonal/Hexagonal (granular); Cleavage: Perfect rhombohedral (in individual crystals).

Hardness
3 on Mohs scale
Color
Pure white to blue-gray
Luster
Waxy to pearly
Identified More metamorphic
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Physical properties

Hardness: 3 on Mohs scale; Color: Pure white to blue-gray; Luster: Waxy to pearly; Crystal Structure: Trigonal/Hexagonal (granular); Cleavage: Perfect rhombohedral (in individual crystals).

Formation & geological history

Formed through the regional metamorphism of limestone under high pressure and temperature. The Carrara deposits in Italy date back to the Jurassic period (approx. 190 million years ago).

Uses & applications

Predominantly used for sculpture, architecture, flooring, and interior design. Historically favored by artists like Michelangelo for its homogeneity and softness.

Geological facts

This specimen is a bust of Joseph John Thomson, the physicist who discovered the electron. Marble is sensitive to acids and will effervesce (fizz) when in contact with dilute hydrochloric acid.

Field identification & locations

Identify by its characteristic sugary (saccharoidal) texture on broken surfaces and its ability to be scratched by a copper coin. Commonly found in the Apuan Alps of Italy.