Amphiboles are double chain silicate minerals that occur in a wide range of environments in igneous and metamorphic rocks. They can crystallize in either orthorhombic or monoclinic crystal systems, with those containing calcium and sodium always being monoclinic. Amphiboles are characterized by their prismatic habit, vitreous luster, and two cleavage sets. They range from black to brown in color and are translucent with densities from 2.9 to 3.5. Optically, amphiboles are anisotropic, pleochroic from green to brown, and exhibit moderate birefringence under crossed polars.