Cyanophyllite is a rare mineral that is also known as "cyanophyll." The word is spelled with the /saɪənoʊfɪlaɪt/ phonetic transcription, which signifies the pronunciation of the word. This distinctive mineral is a beautiful hue of deep blue-green, with a metallic luster that makes it unique. Cyanophyllite is commonly found in metamorphic rocks and is primarily composed of aluminum, magnesium, and iron. The word "cyanophyllite" may be difficult to pronounce at first, but once you get the hang of it, it's a fascinating mineral worthy of exploration.
Cyanophyllite is a rare mineral that belongs to the phyllosilicate family. It typically occurs in metamorphic rocks, especially those derived from manganese ores. The name cyanophyllite is derived from the Greek words "cyanos," meaning blue, and "phyllon," meaning leaf, due to its characteristic blue color and leaf-like crystal morphology.
Chemically, cyanophyllite is a hydrated potassium calcium manganese aluminum silicate. Its formula can be expressed as K3Ca2(Mn2+4Al)(Si4O10)2(OH)4·nH2O, where n represents the variable amount of water molecules in its structure. This mineral forms in the hydrothermal alteration of primary manganese ore deposits, often in association with other manganese-bearing minerals such as rhodonite, hausmannite, and braunite.
Physically, cyanophyllite typically appears as bluish-green to blue crystalline aggregates or compact masses. Its hardness ranges between 4 and 4.5 on the Mohs scale, indicating a relatively moderate hardness. Cyanophyllite exhibits perfect cleavage in one direction and has a sub-vitreous to pearly luster. Its density varies between 2.85 and 3.1 g/cm³.
Although cyanophyllite is not widely known or commercially used, its distinct blue color and attractive crystal habit make it a sought-after specimen among mineral collectors and enthusiasts. Due to its rarity, it is not widely available, and fine specimens are often found in specialized mineral collections or museums dedicated to minerals and gemstones.
The word "cyanophyllite" is derived from two components: "cyano-" and "-phyllite".
1. "Cyano-" is derived from the Greek word "kuanos", meaning "dark blue". This prefix is often used to refer to the color blue.
2. "-Phyllite" is derived from the Greek word "phyllon", meaning "leaf". It is commonly used as a suffix to describe a natural color resemblance to a leaf or leaf-like structure.
Therefore, the term "cyanophyllite" combines these elements to indicate a substance or mineral resembling a dark blue leaf or having a dark blue coloration similar to a leaf.