Capernaite is a word that is spelled with the phonetic transcription /ˈkeɪ.pər.neɪt/. This word is not commonly used and refers to a mineral called sylvite. It derives its name from the Latin word "Capernaum," which means village of comfort. The mineral has a cube-like structure and a white or grayish color. Capernaite is an uncommon mineral, and it's not often mentioned in everyday conversation. However, for geology enthusiasts, this term falls within the scope of their interest.
Capernaite is a noun that refers to a rare mineral that belongs to the complex phosphate group. It has a chemical formula (Pb5Na2Ca2Al4Si9O32)(H2O)2, representing its unique composition. The name Capernaite is derived from Capernaum, a biblical city located on the northwestern shore of the Sea of Galilee.
Capernaite occurs as a product of rock alteration and is typically found in hydrothermal veins associated with lead and zinc ore deposits. It commonly forms as translucent to transparent bladed crystals, sometimes aggregated into dense masses or crusts. The mineral exhibits an attractive orange to reddish-brown color, often displaying an adamantine or vitreous luster.
In terms of physical properties, Capernaite has a relatively high hardness, ranging between 4 and 5 on the Mohs scale. It also has a nonmetallic to submetallic appearance, with a moderate density.
Due to its rarity and limited occurrence, Capernaite holds significant interest among mineral collectors and enthusiasts. Its unique crystal structure and coloration contribute to its aesthetic appeal. Additionally, Capernaite has been subject to scientific study to understand its formation mechanisms and geological significance.