metamorphic
Parian marble statue
White marble, chiefly recrystallized calcite (CaCO₃), likely Carrara marble
AI-generated identification · may be incorrectFine-grained, white, translucent calcitic stone with vitreous-to-satin luster; Mohs hardness 3, perfect rhombohedral calcite cleavage, and specific gravity about 2.7. The image shows a polished and carved sculpture rather than an unworked specimen.
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Physical properties
Fine-grained, white, translucent calcitic stone with vitreous-to-satin luster; Mohs hardness 3, perfect rhombohedral calcite cleavage, and specific gravity about 2.7. The image shows a polished and carved sculpture rather than an unworked specimen.
Formation & geological history
Marble forms when limestone undergoes heat and pressure-driven recrystallization during metamorphism, commonly in Paleozoic–Mesozoic mountain belts; Carrara marble formed during the Mesozoic. The statue itself is human-worked and museum-displayed.
Uses & applications
Used extensively for sculpture, architectural cladding, flooring, monuments, and countertops; high-quality white marble is prized for classical-style carving.
Geological facts
White marble’s low impurity content gives it a luminous appearance and allows fine carving. Acid causes calcite marble to fizz, distinguishing it from quartz-rich stone.
Field identification & locations
Identify by its white color, cool smooth surface, fine crystalline texture, and vigorous reaction to dilute hydrochloric acid; common sources include Carrara, Italy, and Paros, Greece. Exact provenance cannot be confirmed from the photograph.
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