Pronunciation: [ˈɛsvˈa͡ɪɐʒˌɪna͡ɪt] (IPA)

Svyazhinite is a rare mineral that has a complex chemical composition of calcium, vanadium, titanium, and silicon. Its name is derived from the Russian word "svyazh," which means "related" or "connected." It is pronounced as /svɪˈæʒɪnaɪt/ using the International Phonetic Alphabet (IPA). The spelling of "svyazhinite" reflects the mineral's unique chemical structure and is a testament to the importance of accurate and precise scientific language. The study of minerals such as svyazhinite helps us better understand the history, evolution, and makeup of our planet.

SVYAZHINITE Meaning and Definition

Svyazhinite is a rare mineral that belongs to the complex sulfide group. It is classified as a telluride and is known for its unique crystal structure and distinctive chemical composition. The word "svyazhinite" originates from the Russian word "связь" (svyaz), which means "connection" or "bond."

In terms of its physical properties, svyazhinite has a metallic silver-gray color and generally appears in granular aggregates or as fine needles within other minerals. It possesses a high density and can exhibit a metallic luster. Its hardness on the Mohs scale is relatively low, ranging from 2 to 2.5.

Chemically, svyazhinite is composed of various elements, including lead, antimony, tellurium, and sulfur. Its chemical formula is typically expressed as Pb6Bi2S9(TeO6), illustrating the specific arrangement of atoms within its crystal lattice.

Svyazhinite is found in hydrothermal ore deposits associated with other minerals like galena, sphalerite, and chalcopyrite. It is primarily discovered in localized occurrences, making it quite rare and sought after by mineral collectors and researchers.

Due to its unique crystal structure and elemental composition, svyazhinite holds significance in the field of mineralogy and geology. It provides insights into the formation processes of ore deposits and the geochemical conditions that led to its specific formation. The study of svyazhinite contributes to a deeper understanding of mineral diversity and Earth's geological history.