Rock Identifier
White Marble (Recrystallized Carbonate Rock (CaCO3)) — metamorphic
metamorphic

White Marble

Recrystallized Carbonate Rock (CaCO3)

Hardness: 3 on Mohs scale; Color: pure white to off-white; Luster: crystalline to sugary; Crystal structure: Trigonal/Hexagonal; Cleavage: rhombohedral; Specific gravity: 2.7

Hardness
3 on Mohs scale
Color
pure white to off-white
Luster
crystalline to sugary
Identified More metamorphic

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Physical properties

Hardness: 3 on Mohs scale; Color: pure white to off-white; Luster: crystalline to sugary; Crystal structure: Trigonal/Hexagonal; Cleavage: rhombohedral; Specific gravity: 2.7

Formation & geological history

Formed from the regional or contact metamorphism of limestone or dolostone under intense heat and pressure, causing recrystallization of calcite grains.

Uses & applications

Used in sculpture, high-end construction (flooring, countertops), pharmaceuticals as an antacid, and as a filler in paper and paint.

Geological facts

The Taj Mahal is constructed almost entirely of white Makrana marble. Pure white marble is the result of metamorphism of very pure limestone.

Field identification & locations

Identified by its sugary texture and reaction to dilute hydrochloric acid (it will fizz). Commonly found in mountainous regions with a history of tectonic activity.