TVALCHRELIDZEITE Meaning and
Definition
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Tvalchrelidzeite is a rare mineral that belongs to the mineral class of sulfates, specifically to the jarosite group. It was first discovered in the Udokan copper deposit, located in the Zabaikalsky Krai of Russia.
The mineral is named after G. Tvalchrelidze, a prominent Russian mineralogist, in recognition of his significant contributions to the field. Tvalchrelidzeite is characterized by its unique crystal structure and distinctive physical properties.
In terms of appearance, tvalchrelidzeite typically forms as small, elongated prismatic crystals, often occurring in aggregates or coatings. The mineral can exhibit various shades of yellow, ranging from light to dark hues.
Tvalchrelidzeite has a relatively high density and is non-magnetic. It is also known for its brittle nature and resistance to deformation. The mineral is insoluble in water and acidic solutions, and it has a moderate hardness on the Mohs scale, typically ranging between 2.5 and 3.
While tvalchrelidzeite is primarily found in the Udokan deposit, it has also been identified in a few other localities worldwide. Due to its limited occurrence and scarcity, the mineral holds more significance in the field of mineralogy and scientific research rather than commercial or industrial applications.
In conclusion, tvalchrelidzeite is a rare mineral with distinctive physical properties, including its prismatic crystal structure, yellowish coloration, and resistance to deformation.
Etymology of TVALCHRELIDZEITE
The word "tvalchrelidzeite" is a mineral name, specifically a type of arsenate mineral. It is named after its discoverer, Dr. Mikheil Tvalchrelidze, a Georgian mineralogist.
The name "tvalchrelidzeite" follows the convention of mineral nomenclature, where new minerals are often named after the scientist or mineralogist who first identified or described them. The suffix "-ite" is commonly used in mineral names to indicate that the term refers to a mineral species.
