CLARAITE Meaning and
Definition
-
Claraite is a term used in geology to refer to a rare mineral that belongs to the zeolite group. It is a hydrated sodium-calcium-iron silicate that forms in hydrothermal veins, which are cracks or fractures in rocks filled with minerals due to the circulation of hot fluids. The mineral typically occurs in association with other zeolites, such as stilbite and heulandite.
In terms of its physical properties, claraite usually appears as small, blocky crystals or fibrous aggregates that are translucent to transparent. Its color ranges from white to pale grey or yellowish-white. Claraite has a vitreous to pearly luster and exhibits a perfect cleavage along one direction. It is a relatively soft mineral with a Mohs hardness of around 4 to 5, meaning it can be easily scratched by common minerals like fluorite or apatite.
The chemical composition of claraite consists of sodium, calcium, iron, silicon, oxygen, and water molecules. Its precise formula is Na4(Ca,Na)3FeSi8O22(OH)2·H2O. This mineral has been found in various locations worldwide, most notably in the Apuan Alps of Italy and the Khibiny Massif in Russia.
Due to its rarity, claraite primarily holds significance among mineral collectors and researchers studying the geological processes that lead to its formation. Its unique combination of chemical composition and physical properties make it an intriguing mineral deserving of further study and appreciation.
