Rock Identifier
Quartz-rich stone, possibly calcite or quartz (Likely quartz (SiO₂) or calcite (CaCO₃); exact identification requires testing) — mineral
mineral

Quartz-rich stone, possibly calcite or quartz

Likely quartz (SiO₂) or calcite (CaCO₃); exact identification requires testing

AI-generated identification · may be incorrect

Small irregular cream-white specimen with a dull to slightly vitreous luster and apparent granular/crystalline texture. Quartz has Mohs hardness 7 and no cleavage; calcite has hardness 3, prominent rhombohedral cleavage, and fizzes in dilute hydrochloric acid.

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Physical properties

Small irregular cream-white specimen with a dull to slightly vitreous luster and apparent granular/crystalline texture. Quartz has Mohs hardness 7 and no cleavage; calcite has hardness 3, prominent rhombohedral cleavage, and fizzes in dilute hydrochloric acid.

Formation & geological history

Likely a fragment from a quartz vein, limestone, or weathered hydrothermal mineral deposit; its geological age cannot be determined from the image. Cream coloration may result from impurities or surface weathering.

Uses & applications

Common quartz is used in glass, electronics, abrasives, and ornamental objects; calcite is used in cement, lime, construction aggregate, and as a mineral specimen. This small, unidentified fragment has little commercial value.

Geological facts

Visual inspection alone cannot reliably distinguish quartz from calcite, feldspar, or a pale weathered rock. A hardness test and acid test are diagnostic.

Field identification & locations

Test whether it scratches glass (quartz likely) or a copper coin (calcite may not), and check for acid effervescence; avoid destructive tests if valuable. Pale quartz and calcite occur worldwide in veins, limestones, and metamorphic rocks.