
mineral
Honey calcite crystal cluster
Calcite (calcium carbonate, CaCO₃)
AI-generated identification · may be incorrectTypically Mohs hardness 3, vitreous to pearly luster, transparent to translucent, and rhombohedral cleavage; this specimen is pale honey-yellow to colorless with blocky, cleaved crystals. Calcite effervesces strongly in dilute hydrochloric acid and has specific gravity about 2.71.
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Physical properties
Typically Mohs hardness 3, vitreous to pearly luster, transparent to translucent, and rhombohedral cleavage; this specimen is pale honey-yellow to colorless with blocky, cleaved crystals. Calcite effervesces strongly in dilute hydrochloric acid and has specific gravity about 2.71.
Formation & geological history
Forms commonly from carbonate-rich groundwater, hydrothermal fluids, and sedimentary limestone environments; the specimen likely crystallized in a cavity or vein, with coloration caused by impurities such as iron. Calcite occurs from ancient to modern geological settings.
Uses & applications
Used in cement, lime, aggregate, soil treatment, chemical processing, and optical instruments; attractive transparent clusters are collected as display minerals, though calcite is generally too soft for durable jewelry.
Geological facts
Calcite has three perfect cleavage directions and exhibits strong birefringence, producing double images when viewed through clear crystals. Honey coloration can fade with prolonged sunlight or heat.
Field identification & locations
Common worldwide, especially in Mexico, the United States, Iceland, England, and China; identify by rhombohedral cleavage, low hardness, and acid reaction. Avoid scratching or acidic cleaners.
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