Talc is a sheet silicate distinguished from all other minerals by its extreme softness, a property caused by talc’s loosely connected sheets that slip easily under pressure.
Talc 3D Model by Rutgers University Geology Museum
Talc is a sheet silicate distinguished from all other minerals by its extreme softness, a property caused by talc’s loosely connected sheets that slip easily under pressure.
Talc 3D Model by Rutgers University Geology Museum