Rock Identifier
Quartz-bearing metamorphic rock, likely quartzite with dark mica/amphibole (Quartzite or quartz-rich schist; chiefly SiO₂ quartz with biotite, hornblende/amphibole, and iron-oxide staining) — metamorphic
metamorphic

Quartz-bearing metamorphic rock, likely quartzite with dark mica/amphibole

Quartzite or quartz-rich schist; chiefly SiO₂ quartz with biotite, hornblende/amphibole, and iron-oxide staining

AI-generated identification · may be incorrect

White, translucent quartz forms a coarse crystalline vein or mass within a dark, foliated matrix; vitreous luster, no visible cleavage in quartz, and likely Mohs hardness 6.5–7. Dark minerals may show weak foliation and cleavage. Exact identification is limited by the photograph.

Identified More metamorphic
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Physical properties

White, translucent quartz forms a coarse crystalline vein or mass within a dark, foliated matrix; vitreous luster, no visible cleavage in quartz, and likely Mohs hardness 6.5–7. Dark minerals may show weak foliation and cleavage. Exact identification is limited by the photograph.

Formation & geological history

Likely metamorphosed sandstone or quartz-rich protolith intruded or segregated into quartz veins, then fractured and stained by oxidized iron-bearing fluids. Age depends on locality and cannot be determined visually.

Uses & applications

Used decoratively as ornamental stone and collected as a hand specimen; quartz-rich rock may be crushed for aggregate, but this irregular piece has little commercial value.

Geological facts

Quartz veins commonly appear white because of recrystallization and fluid deposition; rusty red-brown patches are typically hematite or limonite weathering products.

Field identification & locations

Test the white material with a steel file or glass: quartz should scratch glass and resist a steel knife. Look for foliation, mica flakes, and a sugary quartz texture; common in metamorphic belts worldwide.