Rock Identifier
Calcite (likely a tumbled specimen) (Calcite (CaCO
3
)) — Mineral
Mineral

Calcite (likely a tumbled specimen)

Calcite (CaCO 3 )

Hardness: 3 (Mohs scale), Color: White, pink, grey (common); can be yellow, blue, green, black. Luster: Vitreous to pearly or dull. Crystal Structure: Trigonal. Cleavage: Perfect rhombohedral. Specific Gravity: 2.71.

Hardness
3 (Mohs scale), Color: White, pink, grey (common)
Color
White, pink, grey (common)
Luster
Vitreous to pearly or dull
Identified More mineral

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Physical properties

Hardness: 3 (Mohs scale), Color: White, pink, grey (common); can be yellow, blue, green, black. Luster: Vitreous to pearly or dull. Crystal Structure: Trigonal. Cleavage: Perfect rhombohedral. Specific Gravity: 2.71.

Formation & geological history

Calcite forms in various geological environments. It can precipitate from supersaturated waters, form biogenically from marine organisms (shells, corals), or be deposited from hydrothermal fluids. It's a key component of limestones and marbles. Can also form stalactites and stalagmites in caves. Geological age varies widely depending on the specific formation.

Uses & applications

Industry: Principal component of cement and lime, used in construction (limestone, marble). Agriculture: Soil conditioner. Environmental: Flue gas desulfurization. Art/Sculpture: Marble is a metamorphic rock composed of calcite. Jewelry/Collecting: Specific varieties can be polished or carved for ornamental purposes. The pictured specimen, being smooth and rounded, appears to be a tumbled stone, often used in crafts, decoration, or spiritual practices.

Geological facts

Calcium carbonate is a very common substance found in rocks as the minerals calcite and aragonite. Calcium carbonate is the main component of mollusc shells and eggshells. It's also the primary substance in pearls. Antacids often contain calcium carbonate to neutralize stomach acid.

Field identification & locations

Identify in the field: Calcite is relatively soft and can be scratched by a copper coin. It reacts vigorously with dilute hydrochloric acid (or even strong vinegar) by effervescing (fizzing) due to the release of carbon dioxide gas. Its perfect rhombohedral cleavage is distinctive, causing it to break into rhomb-shaped fragments. Common locations: Found globally in sedimentary rocks (limestone, chalk), metamorphic rocks (marble), and as a common mineral in hydrothermal veins. Tips for collectors: Its softness means it can be easily scratched, so care should be taken with specimens. Tumbled stones like the one pictured are widely available at rock shops and online.