
metamorphic
Biotite-rich schist
Mica schist, chiefly quartz + biotite mica (locally muscovite); composition varies
AI-generated identification · may be incorrectDark gray to purplish, strongly foliated and sparkly, with platy mica flakes and irregular quartz-rich bands. Hardness is about 2.5–3 for biotite and 7 for quartz; mica has perfect basal cleavage, while the rock splits along foliation. Specific gravity is roughly 2.7–3.0;…
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Physical properties
Dark gray to purplish, strongly foliated and sparkly, with platy mica flakes and irregular quartz-rich bands. Hardness is about 2.5–3 for biotite and 7 for quartz; mica has perfect basal cleavage, while the rock splits along foliation. Specific gravity is roughly 2.7–3.0; luster is pearly to submetallic on mica surfaces.
Formation & geological history
Formed when shale or another clay-rich sediment was regionally metamorphosed under elevated pressure and temperature, producing aligned mica and recrystallized quartz. It is commonly Precambrian to Paleozoic, though exact age cannot be determined from the photograph.
Uses & applications
Used locally as decorative stone, landscaping material, and occasionally dimension stone, but its pronounced foliation limits structural construction use. Attractive mica-rich pieces are collected as specimens.
Geological facts
The glitter comes from aligned mica rather than abundant metal. The apparent pink-purple tones may reflect weathering, feldspar, or iron staining.
Field identification & locations
Look for planar foliation, mica sparkle, and flakes that peel or separate; a steel nail usually scratches mica but not quartz grains. The reported southeastern DRC location is geologically compatible with ancient metamorphic basement rocks, though locality confirmation requires a map or testing.
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