Amphibole

Amphibole sample on white background
Pascal founder of Geoscopy

Pascal 

Fact Sheet:

  • Chemical Composition: A group of inosilicate minerals with a general formula (Ca, Na, K)₂–₃(Mg, Fe, Al)₅(Si, Al)₈O₂₂(OH, F)₂
  • Hardness: 5 to 6 on the Mohs scale
  • Crystal System: Monoclinic or orthorhombic
  • Color Varieties: Green, black, brown, yellow, blue
  • Major Localities: United States, Canada, Italy, Norway, and Japan
  • Common Uses: Geological research, asbestos (some forms), ornamental stone, and industrial materials

Introduction: Amphibole is a diverse group of minerals that includes several important rock-forming members. Known for their fibrous crystal habit and presence in both igneous and metamorphic rocks, amphiboles play a crucial role in understanding geological processes. Their complex chemical compositions and structures make them a fascinating subject for mineralogists and geologists alike.

Formation: Amphiboles are typically found in both igneous and metamorphic rocks. They form during the crystallization of magma and can also be produced during metamorphism at moderate to high pressures and temperatures. Amphiboles can be present in a variety of rock types, including basalt, gabbro, diorite, and schist.

Types and Colors: The amphibole group includes many different minerals, each with its own color and chemical composition. Some of the major members include:

  • Hornblende: The most common type, typically dark green to black; found in many igneous and metamorphic rocks.
  • Tremolite: White to light green, found in metamorphic rocks and some serpentinites.
  • Actinolite: Light green to dark green, forms in low- to medium-grade metamorphic rocks.
  • Glaucophane: Blue to dark blue, a key mineral in blueschist facies rocks.
  • Riebeckite: Blue to black, found in alkali igneous rocks.

Localities and Mining: Amphibole minerals are found worldwide, with significant deposits in the United States, Canada, Italy, Norway, and Japan. While amphibole minerals are not mined commercially for their own sake, some asbestos minerals (such as tremolite and riebeckite) are part of the amphibole group and have been historically mined. Today, due to health risks associated with asbestos, mining of asbestos-related amphiboles is strictly regulated or banned in many countries.

Applications: Amphibole minerals have various uses:

  • Geological Indicators: Amphiboles are used as geological indicators, providing information about the pressure and temperature conditions during rock formation.
  • Asbestos: Some forms of amphibole, like tremolite and riebeckite, are classified as asbestos and were historically used in insulation and construction materials due to their fibrous nature.
  • Ornamental Stone: Some amphibole-rich rocks, such as nephrite (a form of actinolite), are used as ornamental stones and in sculptures.
  • Industrial Use: While the use of asbestos amphiboles is now limited due to health risks, non-fibrous amphiboles are used in some industrial applications, including cement and stonework.

Environmental Impact and Health Risks: Amphibole asbestos has significant health risks, as inhalation of asbestos fibers can lead to diseases such as asbestosis and mesothelioma. As a result, the mining and use of amphibole asbestos minerals are highly regulated. Environmental impacts of amphibole mining, particularly in areas where asbestos is present, must be carefully managed to prevent contamination and health hazards.

Sources and further reading:

https://www.alexstrekeisen.it/english/vulc/amphiboles.php

https://www.britannica.com/science/amphibole

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