Omavektorite

Omavektorite is a mineral species belonging to the group of borate minerals. It was discovered in 2013 by a team of geologists and crystallographers in the mountains of Tibet, China. The mineral is characterized by its distinctive chemical composition and physical properties.

Omavektorite is a sodium and magnesium borate mineral, with the chemical formula Na7MgB5O10(OH)5·5H2O. It typically forms in hydrothermal veins as a secondary mineral, often associated with other borate minerals such as tsilaisite and paraskoliasite. Omavektorite has a distinct crystal habit, consisting of tabular to prismatic crystals that can reach up to several centimeters in length.

Omavektorite has a relatively high hardness, ranging from 5 to 6 on the Mohs scale, and exhibits a vitreous to pearly luster. It is relatively brittle and tends to form cleavage planes, which makes it prone to breakage. The mineral is colored by its impurities, often presenting shades of pink, yellow, or white.

Omavektorite is of interest to geologists and scientists due to its unique chemical structure and crystallization habits. Its discovery has contributed to a better understanding of the geological processes that shape the Earth's crust. The mineral is rare and usually obtained through specialized mining techniques, making it a valuable specimen for collectors and researchers.