Pyroxene is a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks. They are known for their significant role in the formation of the Earth's crust and mantle. Pyroxenes have a monoclinic or orthorhombic crystal structure and are composed of single chains of silica tetrahedra.
Pyroxenes are generally composed of combinations of magnesium, iron, calcium, sodium, and aluminum, along with silicon and oxygen. The general chemical formula for pyroxene is (Ca,Na)(Mg,Fe,Al)(Si,Al)2O6.
Pyroxene minerals typically exhibit a prismatic or columnar crystal habit with two cleavage directions at approximately 90 degrees. They have a hardness ranging from 5 to 7 on the Mohs scale and can occur in various colors such as black, green, brown, or white.
Some common types of pyroxene include augite, diopside, enstatite, and hypersthene. Each type has its own distinct chemical composition and physical properties, contributing to their unique characteristics and geological significance.
Pyroxenes are crucial in understanding the formation and evolution of igneous and metamorphic rocks. Their presence and composition provide valuable insights into the conditions under which these rocks were formed, as well as the processes involved in their alteration over time.
When studying pyroxene, consider the following key points:
By mastering these aspects of pyroxene, you will develop a solid understanding of its significance in the field of geology and earth sciences.