CAMEROLAITE Meaning and
Definition
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Camerolaite is a rare mineral that belongs to the vanadium iron oxide hydroxide group. This mineral has a chemical formula of Fe^3+V^4+2O4(OH)2 and typically occurs in the form of green or brownish-green crystalline masses. The name camerolaite was derived from its first discovered location, the Camerola mine in Tuscany, Italy.
As a mineral, camerolaite is often found in hydrothermal veins or as part of the oxidation zone of ore deposits. It commonly forms alongside other vanadium-bearing minerals and compounds. The crystal structure of camerolaite consists of octahedral layers of linked oxygen and hydrogen atoms, with vanadium and iron atoms occupying the octahedral sites in this structure.
Physically, camerolaite exhibits high birefringence, which means that it can split light into two different polarized rays, resulting in a colorful interference pattern when viewed under a polarizing microscope. The mineral is known for its sub-adamantine to vitreous luster and can have a translucent to transparent appearance.
Camerolaite is not of significant industrial importance due to its rarity and limited occurrence. It is mainly sought after by mineral collectors, researchers, and those with an interest in the study of rare minerals and their crystal structures. As a vanadium-bearing mineral, camerolaite can provide insight into geochemical processes and help in the understanding of vanadium ore formation.
