Rock Identifier
Likely calcite-rich limestone or marble (Calcite (CaCO₃); possibly recrystallized limestone (marble)) — metamorphic
metamorphic

Likely calcite-rich limestone or marble

Calcite (CaCO₃); possibly recrystallized limestone (marble)

AI-generated identification · may be incorrect

White to beige, dull-to-pearly luster, granular crystalline texture, and irregular cleavage/fracture; calcite has Mohs hardness 3 and specific gravity about 2.71. The layered, foliated-looking appearance may indicate marble, though the photograph cannot confirm it.

Identified More metamorphic
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Physical properties

White to beige, dull-to-pearly luster, granular crystalline texture, and irregular cleavage/fracture; calcite has Mohs hardness 3 and specific gravity about 2.71. The layered, foliated-looking appearance may indicate marble, though the photograph cannot confirm it.

Formation & geological history

If marble, it formed when limestone recrystallized during regional or contact metamorphism, commonly at various geologic ages. If unaltered limestone, it is sedimentary and formed from accumulated carbonate mud or shells in a marine environment.

Uses & applications

Used as crushed stone, cement and lime feedstock, aggregate, dimension stone, and—when attractive—雕? decorative marble; calcite specimens are also collected.

Geological facts

Calcite effervesces vigorously with dilute hydrochloric acid or strong vinegar, whereas dolomite reacts weakly unless powdered. Marble may show interlocking calcite grains and acid reaction across a fresh surface.

Field identification & locations

Common in carbonate terrains worldwide; test a fresh spot for fizz, inspect grain size, and check hardness against a copper coin or steel nail. The specimen appears relatively ordinary and weathered.