Rock Identifier
Dark gray metamorphic rock fragment, likely slate or schist (Fine-grained foliated silicate rock; composition likely quartz, feldspar, mica, and/or chlorite) — metamorphic
metamorphic

Dark gray metamorphic rock fragment, likely slate or schist

Fine-grained foliated silicate rock; composition likely quartz, feldspar, mica, and/or chlorite

AI-generated identification · may be incorrect

Gray-black, dull to slightly silky luster, irregular edges, and visible foliation or platy texture. Estimated Mohs hardness 3–6; cleavage/parting may allow splitting along layers; specific gravity roughly 2.7–2.9.

Identified More metamorphic
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Physical properties

Gray-black, dull to slightly silky luster, irregular edges, and visible foliation or platy texture. Estimated Mohs hardness 3–6; cleavage/parting may allow splitting along layers; specific gravity roughly 2.7–2.9.

Formation & geological history

Likely formed when shale or mudstone underwent low- to medium-grade regional metamorphism, recrystallizing clay minerals into mica or chlorite. Exact age and identification cannot be established from the photograph alone.

Uses & applications

Slate is used for roofing, flooring, and writing surfaces; schist is mainly decorative or collected as a specimen. This small fragment has minimal commercial value.

Geological facts

The layered texture and dark color are consistent with slate, phyllite, or fine schist, but the image does not show enough detail for a definitive species-level identification.

Field identification & locations

Common in metamorphic mountain belts worldwide, including Wales, the northeastern United States, Canada, and the Alps. Check for consistent planar splitting, a silky sheen, and a streak or hardness test; avoid assuming it is meteorite material from color alone.