
metamorphic
Marble
Marble (metamorphosed limestone or dolostone), primarily composed of calcite (CaCO3) or dolomite (CaMg(CO3)2)
Hardness: 3-4 on Mohs scale (calcite), 3.5-4 (dolomite, slightly harder). Color: Highly variable, often white, grey, black, pink, red, green, or mixtures, with distinctive veining. Luster: Vitreous to dull. Crystal structure: Typically massive with interlocking granular crystals; fine to coarse-grained.…
- Hardness
- 3-4 on Mohs scale (calcite), 3
- Luster
- Vitreous to dull
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Physical properties
Hardness: 3-4 on Mohs scale (calcite), 3.5-4 (dolomite, slightly harder). Color: Highly variable, often white, grey, black, pink, red, green, or mixtures, with distinctive veining. Luster: Vitreous to dull. Crystal structure: Typically massive with interlocking granular crystals; fine to coarse-grained. Cleavage: Perfect rhombohedral (calcite and dolomite). Specific gravity: 2.7-2.8.
Formation & geological history
Formed from the regional or contact metamorphism of sedimentary carbonate rocks (limestone or dolostone). This process involves recrystallization during intense heat and pressure, leading to the interlocking crystal structure. Geological age varies widely depending on the age of the original sedimentary rock and the metamorphic event, ranging from Precambrian to Cenozoic.
Uses & applications
Widely used in construction for flooring, countertops, wall cladding, and decorative elements due to its aesthetic appeal and durability. Employed in sculpture for centuries, prized for its workability and fine grain. Also used as a dimension stone, crushed stone aggregate, and in agricultural lime.
Geological facts
The word 'marble' derives from Greek 'marmaros', meaning 'shining stone'. Famous ancient structures like the Parthenon in Greece and sculptures like Michelangelo's David are made from marble. Its distinctive veining is due to impurities present in the original limestone, such as clay minerals, iron oxides, or bituminous material, which recrystallize during metamorphism.
Field identification & locations
To identify in the field, look for a granular, interlocking crystalline texture. It will typically be soft enough to scratch with a knife (Mohs 3-4) and will effervesce (fizz) vigorously when a drop of dilute hydrochloric acid is applied to its surface (if primarily calcite). Common locations include areas that have undergone regional metamorphism, such as mountain ranges (e.g., Alps, Appalachians, Carrara in Italy, Vermont in the USA). For collectors, seek well-polished specimens to appreciate the intricate patterns and colors. Be aware that marble is susceptible to acid etching and weathering in outdoor environments.
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