
mineral
Calcite
Calcite (CaCO₃), likely crystalline limestone or marble fragment
AI-generated identification · may be incorrectPale cream to honey-colored, translucent, with pearly-to-glassy luster and prominent rhombohedral cleavage; Mohs hardness 3, specific gravity about 2.71. The image suggests a rough, cleaved specimen rather than a diagnostic crystal form.
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Physical properties
Pale cream to honey-colored, translucent, with pearly-to-glassy luster and prominent rhombohedral cleavage; Mohs hardness 3, specific gravity about 2.71. The image suggests a rough, cleaved specimen rather than a diagnostic crystal form.
Formation & geological history
Calcite precipitates from marine, groundwater, hydrothermal, and metamorphic fluids; limestone deposits commonly formed in Paleozoic–Cenozoic seas, while marble forms by recrystallization during metamorphism. Exact age and host rock cannot be determined visually.
Uses & applications
Used in cement, lime, aggregate, soil treatment, glass, and chemical production; transparent varieties are collected, and optical Iceland spar is used for polarization demonstrations.
Geological facts
Calcite effervesces strongly with dilute hydrochloric acid or vinegar if freshly powdered; it is easily scratched by a copper coin or steel edge. Its double refraction is a notable optical property.
Field identification & locations
Look for rhombohedral cleavage, low hardness, and acid reaction; common worldwide in limestone caves, veins, sedimentary beds, and marbles. Similar pale quartz is harder and lacks cleavage.
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