Rock Identifier
Likely tumbled quartz or calcite (Quartz (SiO₂) or calcite (CaCO₃); exact identification requires hardness and acid tests) — mineral
mineral

Likely tumbled quartz or calcite

Quartz (SiO₂) or calcite (CaCO₃); exact identification requires hardness and acid tests

AI-generated identification · may be incorrect

Creamy-white, rounded, opaque to slightly translucent, with a dull to waxy luster. Quartz has Mohs hardness 7 and no cleavage; calcite has hardness 3, prominent rhombohedral cleavage, and effervesces in dilute hydrochloric acid.

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Physical properties

Creamy-white, rounded, opaque to slightly translucent, with a dull to waxy luster. Quartz has Mohs hardness 7 and no cleavage; calcite has hardness 3, prominent rhombohedral cleavage, and effervesces in dilute hydrochloric acid.

Formation & geological history

A naturally formed mineral fragment later smoothed by tumbling or abrasion; quartz commonly crystallizes in igneous and hydrothermal settings, while calcite forms in sedimentary environments and veins. Geological age cannot be determined from the image.

Uses & applications

Quartz is used in glass, electronics, abrasives, and ornaments; calcite is used in cement, lime, aggregate, and decorative stone. This specimen has modest decorative or educational value.

Geological facts

The image alone cannot reliably distinguish quartz from calcite or other pale minerals such as feldspar. A steel nail scratches calcite but not quartz; glass scratches quartz.

Field identification & locations

Common sources include quartz veins, pegmatites, limestone, and marble deposits worldwide. Test on an inconspicuous area: hardness, cleavage, and dilute acid response are diagnostic.