Rock Identifier
Dark foliated metamorphic rock, probably schist (Mica schist, likely quartz–muscovite/biotite schist) — metamorphic
metamorphic

Dark foliated metamorphic rock, probably schist

Mica schist, likely quartz–muscovite/biotite schist

AI-generated identification · may be incorrect

Gray-green, fine- to medium-grained, weakly shiny from aligned mica; likely Mohs 2–7 depending on grains, with mica cleavage and quartz/feldspar hardness. The rounded shape appears naturally weathered or water-worn; individual crystals are not clear enough for certainty.

Identified More metamorphic
Explore Dark foliated metamorphic rock, probably schist in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Gray-green, fine- to medium-grained, weakly shiny from aligned mica; likely Mohs 2–7 depending on grains, with mica cleavage and quartz/feldspar hardness. The rounded shape appears naturally weathered or water-worn; individual crystals are not clear enough for certainty.

Formation & geological history

Formed when shale or another clay-rich sediment was subjected to regional heat and pressure, producing mica alignment and foliation. Its precise age cannot be determined from the photograph; metamorphic rocks in Yemen may range from Precambrian basement to younger tectonic units.

Uses & applications

Used locally as building or paving stone and occasionally as decorative material, but this ordinary specimen has little commercial value.

Geological facts

The reflective specks are probably mica rather than metallic ore. The reported location in Yemen is geologically plausible for metamorphic basement rocks, although a dark weathered basalt or serpentinite remains possible without testing.

Field identification & locations

Look for planar splitting, glittering mica flakes, and bands or foliation; a streak, hardness test, and fresh broken surface would help distinguish schist from basalt or serpentinite. Commonly found in metamorphic terranes and stream gravels.