
metamorphic
Coarse-grained marble or calcite-rich metamorphic rock
Calcite (CaCO₃), likely marble with mica and silicate minerals
AI-generated identification · may be incorrectGray-white, coarse crystalline texture with a glassy to pearly luster; calcite has Mohs hardness 3, rhombohedral cleavage, and fizzes strongly in dilute hydrochloric acid. The dark grains may be mica, amphibole, or other silicates; crystal form is granular and interlocking.
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Physical properties
Gray-white, coarse crystalline texture with a glassy to pearly luster; calcite has Mohs hardness 3, rhombohedral cleavage, and fizzes strongly in dilute hydrochloric acid. The dark grains may be mica, amphibole, or other silicates; crystal form is granular and interlocking.
Formation & geological history
Likely recrystallized limestone or dolostone during regional or contact metamorphism, generally formed in the Precambrian to Phanerozoic. Exact age and identity require acid testing, thin-section study, or mineral analysis.
Uses & applications
Used as decorative stone, aggregate, and occasionally in sculpture or classrooms; attractive pieces may be collected but are usually low-value.
Geological facts
Calcite marble can resemble quartz-rich rocks, but calcite is softer and reacts with acid. A steel nail or knife may scratch exposed calcite, while quartz will not.
Field identification & locations
Common in metamorphic belts worldwide, including Italy, Greece, Vermont, Colorado, and India. Test a fresh surface with dilute acid, inspect cleavage, and check whether the pale crystals scratch with steel.
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