KAMBALDAITE Meaning and
Definition
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Kambaldaite refers to a rare mineral that falls under the category of sulfide minerals. It is a member of the nickeline group and is primarily composed of nickel and sulfur. The name "kambaldaite" derives from the town of Kambalda in Western Australia, where it was first discovered.
In terms of physical characteristics, kambaldaite typically appears as opaque and metallic, exhibiting a silver-white to pale pink coloration. It possesses a relatively high hardness and density, making it somewhat durable. The crystal structure of kambaldaite is notably complicated and often characterized by a hexagonal form.
Chemically, kambaldaite contains significant proportions of nickel and sulfur, forming the main constituents of its composition. This mineral may also contain small traces of other elements such as cobalt, iron, and arsenic. Kambaldaite forms in hydrothermal vents and is usually associated with other sulfide minerals such as pentlandite and chalcopyrite.
Due to its rarity and limited occurrence, kambaldaite holds little significance in terms of practical applications. However, it serves as an intriguing subject for scientific research and mineral collectors. Its unique crystal structure and composition contribute to its scientific importance, allowing for a deeper understanding of geological processes and the formation of sulfide minerals.
In summary, kambaldaite is a rare nickel-sulfur mineral with a complex hexagonal crystal structure. Though not commercially valuable, it holds scientific significance and is sought after by mineral enthusiasts.
Etymology of KAMBALDAITE
The word "kambaldaite" is derived from the name of the town Kambalda, located in Western Australia. Kambalda is known for its significant nickel deposits, and the mineral kambaldaite was named after the town to acknowledge its discovery in that region. The suffix "-ite" is commonly used in mineralogy to indicate a mineral species. Hence, the term "kambaldaite" refers to a specific mineral found in Kambalda.
