Marble
Recrystallized Carbonate Rock (CaCO3)
Rock Type: metamorphic

Physical Properties
Hardness: 3 on Mohs scale; Color: White with grey veining; Luster: Vitreous to pearly; Crystal structure: Trigonal (granular/massive texture); Cleavage: Perfect rhombohedral in calcite grains; Specific gravity: 2.6-2.8.
Formation & Geological History
Formed from the regional or contact metamorphism of limestone or dolostone, where heat and pressure cause the recrystallization of carbonate minerals into an interlocking mosaic.
Uses & Applications
Extensively used in construction for flooring, countertops, and wall tiles; also used in sculpture and as an architectural decorative stone.
Geological Facts
Pure white marble results from the metamorphism of very pure limestone. The colorful swirls and veins are typically due to mineral impurities such as clay, silt, sand, or iron oxides.
Field Identification & Locations
Identify in the field by its softness (can be scratched by a copper coin) and vigorous reaction to dilute hydrochloric acid. It is commonly found in mountainous regions underlain by ancient carbonate sea beds.
Identified on: 5/4/2026
Mode: Standard