Rock Identifier
Pale green rough mineral fragment, possibly green calcite (Calcite (CaCO₃), tentative identification) — mineral
mineral

Pale green rough mineral fragment, possibly green calcite

Calcite (CaCO₃), tentative identification

AI-generated identification · may be incorrect

Translucent pale green-white fragment with a dull to vitreous luster and irregular cleavage surfaces. If calcite, hardness is 3 Mohs and crystals are trigonal; the image alone does not confirm the mineral.

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Physical properties

Translucent pale green-white fragment with a dull to vitreous luster and irregular cleavage surfaces. If calcite, hardness is 3 Mohs and crystals are trigonal; the image alone does not confirm the mineral.

Formation & geological history

Calcite commonly forms in sedimentary settings, hydrothermal veins, and cavities in igneous rocks; it occurs from many geological ages. This small fragment’s source cannot be determined visually.

Uses & applications

Calcite is used in cement, lime, and construction aggregate; attractive translucent pieces are collected or occasionally used decoratively.

Geological facts

Calcite effervesces in dilute acid and is readily scratched by a copper coin—useful checks when distinguishing it from harder green minerals.

Field identification & locations

The pale color and apparent cleavage are consistent with calcite, but identification needs simple tests such as hardness and acid reaction. Calcite is widespread worldwide.