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Schist is medium-grade metamorphic rocks, chiefly notable for the preponderance of lamellar minerals such as micas, chlorite, talc, hornblende, graphite, and others. Most schists have been derived from clays and muds which have passed through a series of metamorphic processes involving the production of shales, slates and phyllites as intermediate steps. Certain schists have been derived from fine-grained igneous rocks such as basalts and tuffs.

Type Solid block
Physics No
Transparency No
Luminance No
Inflammable No
Generated No
Renewable No
Stackable Yes(99)
Since Version 0.2