Marble is a metamorphic rock that forms when limestone is subjected to significant heat and pressure within the Earth's crust. This natural transformation alters the crystal structure of the mineral grains, making marble distinct from its sedimentary precursor, limestone. The primary mineral in marble is calcite, which as mentioned earlier, is chemically known as calcium carbonate \(\text{CaCO}_{3}\).
The colorful veins seen in marble result from impurities such as iron oxides, silt, and clay present in the original limestone. These impurities can cause various colors like red, green, or black patterns within the predominantly white or gray marble.
Marble is prized for its aesthetic appeal and is commonly used in:
- Building materials and construction (e.g., marble tiles and countertops)
- Sculpture and fine art
- Decorative elements in architecture, such as columns and facades