Rock Identifier
Quartz–calcite sulfide-bearing mineral specimen (Quartz (SiO₂) with likely calcite (CaCO₃) and iron sulfides, possibly pyrite (FeS₂); exact species requires testing) — mineral
mineral

Quartz–calcite sulfide-bearing mineral specimen

Quartz (SiO₂) with likely calcite (CaCO₃) and iron sulfides, possibly pyrite (FeS₂); exact species requires testing

AI-generated identification · may be incorrect

White druzy quartz and pale translucent calcite crystals coat a gray metallic matrix with brassy grains and reddish iron-oxide staining. Quartz hardness 7, vitreous luster; calcite hardness 3 with rhombohedral cleavage and effervescence in dilute acid; pyrite hardness 6–6.5, metallic luster.

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Physical properties

White druzy quartz and pale translucent calcite crystals coat a gray metallic matrix with brassy grains and reddish iron-oxide staining. Quartz hardness 7, vitreous luster; calcite hardness 3 with rhombohedral cleavage and effervescence in dilute acid; pyrite hardness 6–6.5, metallic luster.

Formation & geological history

Likely a hydrothermal vein specimen formed when hot, mineral-rich fluids deposited quartz, carbonate, and sulfides in fractures; age depends on its mining district and cannot be determined visually.

Uses & applications

Primarily a collector specimen; quartz and calcite are industrial minerals, while pyrite may be an ore indicator but this piece is not economically useful for extraction.

Geological facts

The red-orange coloration commonly reflects hematite or limonite weathering of iron-bearing minerals. Acid testing, streak, hardness, and crystal examination would distinguish calcite and pyrite from similar minerals.

Field identification & locations

Look for six-sided quartz crystals, rhombohedral calcite, and brassy cubic or granular sulfides. Common settings include hydrothermal veins and metal-mining districts worldwide.