ALUMOKLYUCHEVSKITE Meaning and
Definition
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Alumoklyuchevskite is a rare mineral that belongs to the family of sulfate minerals. It is an intermediate hydrate between the minerals klinoaluminite and alumohydrocalcite. The term "alumoklyuchevskite" is derived from the names of these two minerals.
Alumoklyuchevskite has a chemical formula of Ca4Al2(SO4)(OH)12·12H2O. It crystallizes in the trigonal system, forming prismatic crystals that are usually colorless or white. The mineral has a vitreous to pearly luster, and its hardness ranges between 2 and 3 on the Mohs scale.
This mineral is primarily found in volcanic environments, specifically in the vicinity of fumaroles and hot springs. It is most commonly associated with other minerals such as gypsum, thenardite, and trona.
The physical and chemical properties of alumoklyuchevskite make it an interesting mineral for scientific research. Its unique crystal structure and composition provide insights into the formation of sulfates in volcanic environments. Additionally, its presence can indicate the occurrence of specific geological processes, such as hydrothermal activity.
Due to its rarity, alumoklyuchevskite does not have significant industrial or commercial applications. However, it is sought after by mineral collectors and enthusiasts for its unique aesthetic value and scientific significance.
Etymology of ALUMOKLYUCHEVSKITE
The word "alumoklyuchevskite" is a scientific name for a mineral, and its etymology can be broken down as follows:
"Alumo" refers to aluminum, which comes from the Latin word "alumen", meaning "alum". Alum is a compound used in various chemical processes.
"Klyuchevskite" is derived from the Klyuchevskaya Sopka volcano in Kamchatka, Russia. This volcano is known for its volcanic activity and the formation of various minerals, including alumoklyuchevskite.
Therefore, "alumoklyuchevskite" is named after the presence of aluminum and its association with the Klyuchevskaya Sopka volcano in Kamchatka.
