Rock Identifier
Dark gray foliated metamorphic rock, likely slate or phyllite (Slate/phyllite; commonly quartz, muscovite/illite, chlorite, and graphite or carbonaceous matter) — metamorphic
metamorphic

Dark gray foliated metamorphic rock, likely slate or phyllite

Slate/phyllite; commonly quartz, muscovite/illite, chlorite, and graphite or carbonaceous matter

AI-generated identification · may be incorrect

Fine-grained, dark gray, silky to dull luster with visible planar foliation; slate has hardness ~3–4 and excellent cleavage, while phyllite is slightly softer and more lustrous. The blurred image prevents confident separation from schist.

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Physical properties

Fine-grained, dark gray, silky to dull luster with visible planar foliation; slate has hardness ~3–4 and excellent cleavage, while phyllite is slightly softer and more lustrous. The blurred image prevents confident separation from schist.

Formation & geological history

Forms when shale or mudstone is regionally metamorphosed under low-grade pressure and heat, typically during mountain building; age depends on the source terrain and may range from Paleozoic to Precambrian.

Uses & applications

Used for roofing, floor and wall tiles, paving, blackboards, landscaping, and architectural cladding; attractive phyllite may be collected as a specimen.

Geological facts

Foliation records directed tectonic pressure, and slate commonly splits into thin, flat sheets. Phyllite represents a higher metamorphic grade than slate.

Field identification & locations

Look for strong, closely spaced planar splitting and a fine texture; a silky sheen suggests phyllite, whereas very smooth dull cleavage suggests slate. Common worldwide in metamorphic belts, including Wales, Vermont, Spain, and Brazil.