Rock Identifier
Banded slate or phyllite (Fine-grained foliated metasedimentary rock; likely slate with light-colored quartz veins) — metamorphic
metamorphic

Banded slate or phyllite

Fine-grained foliated metasedimentary rock; likely slate with light-colored quartz veins

AI-generated identification · may be incorrect

Dark gray, fine-grained, matte surface with parallel pale bands or veins. Slate is typically Mohs 2.5–4 and splits along cleavage; the photo alone cannot confirm exact mineralogy or distinguish slate from phyllite.

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Physical properties

Dark gray, fine-grained, matte surface with parallel pale bands or veins. Slate is typically Mohs 2.5–4 and splits along cleavage; the photo alone cannot confirm exact mineralogy or distinguish slate from phyllite.

Formation & geological history

Formed when clay-rich sedimentary rock was compressed and mildly metamorphosed; the pale bands may be quartz veins deposited in fractures. Its age and precise formation setting cannot be determined from the image.

Uses & applications

Slate is used for roofing, flooring, paving, and decorative stone; this small piece is most suitable as a teaching or collecting specimen.

Geological facts

Slate’s strong planar cleavage reflects aligned microscopic minerals, while contrasting quartz veins record fluid movement through cracks.

Field identification & locations

Look for fine grain and flat, planar splitting surfaces; phyllite often has a subtle silky sheen. Slate and related rocks occur in metamorphic belts worldwide.