an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. The minerals in this series are abundant in regionally metamorphosed rocks, such as schists. Tremolite may weather to talc, and both tremolite and actinolite may alter to chlorite or carbonates. For chemical formula and detailed physical properties, see amphibole (table).

The fibres of the magnesium-rich members in the series are asbestos; these varieties, sometimes known as amphibole asbestos, constitute the material to which the name asbestos was originally given. The fibres are fine and silky and possess appreciable tensile strength; those that occur in thin, felted sheets of interwoven fibres are called mountain leather; in thicker sheets, mountain cork; and in compact masses resembling dry wood, mountain wood.