Collection: Amphibole

Amphibole is a group of silicate minerals commonly found in igneous and metamorphic rocks. These minerals have a complex crystal structure and are characterized by the presence of double chains of silica (SiO₄) tetrahedra , which distinguishes them from other groups such as pyroxenes (which have single chains).


🔬 General characteristics

  • General formula : A 0 1 B 2 C 5 T 8 O 22 ( O H , F , C l ) 2 A_0-1B_2C_5T_8O_{22}(OH, F, Cl)_2
    (where A, B, C, T represent different cations like Ca, Na, Mg, Fe, Al...)

  • Crystal system : Monoclinic or orthorhombic

  • Color : Green, brown, black, sometimes white (depending on the composition)

  • Hardness (Mohs) : 5 to 6

  • Luster : Vitreous to silky

  • Cleavage : Good at 56° and 124°, typical of amphiboles


🧱 Examples of minerals from the amphibole group

  • Hornblende : very common in igneous rocks (such as granites and diorites)

  • Tremolite and actinolite : common in metamorphic rocks (schists, marbles)

  • Anthophyllite : present in certain types of ultramafic rocks

  • Glaucophane : indicator of high-pressure metamorphism (e.g., blue schists)


🧭 Formation and occurrence

Amphiboles are mainly formed:

  • In water-rich igneous (plutonic or volcanic) rocks

  • In metamorphic rocks resulting from the transformation of clayey or basic rocks, under high pressure and temperature


⚠️ Health and environment

Some fibrous varieties of amphiboles (such as tremolite or actinolite ) are part of amphibolic asbestos , a family of minerals that are hazardous to health. Inhaling their fibers can cause serious respiratory diseases such as asbestosis or mesothelioma .

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Amphiboles are a family of minerals, silicates of iron, calcium or magnesium. They crystallize in orthorhombic and monoclinic systems in very elongated prisms, with typical cleavage along the faces of the prism. They belong to the group of inosilicates.