Rock Identifier
Likely blue-gray slate fragment (Slate, a fine-grained metamorphic rock composed chiefly of mica-group minerals and quartz) — metamorphic
metamorphic

Likely blue-gray slate fragment

Slate, a fine-grained metamorphic rock composed chiefly of mica-group minerals and quartz

AI-generated identification · may be incorrect

Appears blue-gray, dull, and fine-grained with a flat, platy shape suggestive of slaty cleavage. Slate is typically Mohs 3–4; the specimen’s small size and image limit confident identification.

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Physical properties

Appears blue-gray, dull, and fine-grained with a flat, platy shape suggestive of slaty cleavage. Slate is typically Mohs 3–4; the specimen’s small size and image limit confident identification.

Formation & geological history

Forms when shale or mudstone is subjected to low-grade metamorphism, developing cleavage; its age depends on the source formation and cannot be determined from the image.

Uses & applications

Slate is used for roofing, paving, flooring, and decorative pieces; this small fragment has little practical or jewelry value.

Geological facts

Slate commonly splits into thin, relatively flat sheets along its cleavage planes.

Field identification & locations

The flat shape and muted blue-gray color fit slate, but other fine-grained rocks can look similar; check whether it splits into smooth sheets. Slate occurs in metamorphic belts worldwide, including Wales, the northeastern United States, and parts of Spain.