Talcschist

Talcschist is a metamorphic rock characterized by its predominantly talc mineral composition. It is formed under conditions of moderate to high-grade metamorphism, typically involving serpentinites or dolomitic limestones subjected to heat and pressure. The talc crystals in talcschist are often small and intergrown, giving the rock a soapy or greasy feel and a characteristic softness, ranking it low on the Mohs hardness scale. The color of talcschist can vary from white to gray, green, or even black, depending on the presence of other impurities such as chlorite, amphibole, or magnetite. Its texture is foliated, meaning the mineral grains are aligned in parallel layers, which can make it cleave or split easily. Historically, talcschist has been quarried for its softness and workability, finding uses in carving, decorative objects, and as a source for powdered talc. While it shares the name "talc" with the mineral, talcschist is a rock that is composed primarily of this mineral, often alongside other metamorphic minerals. Due to its softness and platy structure, it is not typically used as a building material in load-bearing applications.