
mineral
Small white mineral fragment
Likely quartz (SiO₂), possibly calcite (CaCO₃)
AI-generated identification · may be incorrectWhite, translucent-to-opaque, uneven granular surface with vitreous to dull luster; apparent hardness cannot be confirmed from the image. Quartz has Mohs hardness 7 and no cleavage; calcite is Mohs 3 and has prominent rhombohedral cleavage.
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Physical properties
White, translucent-to-opaque, uneven granular surface with vitreous to dull luster; apparent hardness cannot be confirmed from the image. Quartz has Mohs hardness 7 and no cleavage; calcite is Mohs 3 and has prominent rhombohedral cleavage.
Formation & geological history
Most likely a broken crystal or vein fragment from hydrothermal quartz/calcite mineralization in host rock; age depends on its source deposit and cannot be determined visually.
Uses & applications
Quartz is used in glass, electronics, abrasives, and collectors’ specimens; calcite is used in cement, lime, agricultural products, and decorative stone.
Geological facts
The key distinction is hardness: quartz will scratch ordinary glass, whereas calcite is readily scratched by a steel knife and may effervesce with dilute hydrochloric acid.
Field identification & locations
Commonly found in veins, cavities, and sedimentary or metamorphic rocks worldwide. Inspect crystal faces, cleavage, transparency, and matrix; perform hardness and acid tests only when appropriate and safe.
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Epidote
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Granite (Phaneritic intrusive igneous rock)
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