The word "chlorophoenicite" is a mouthful, but its spelling can be explained with phonetic transcription. The first syllable "chloro-" is pronounced as /ˈklɔːroʊ/, indicating the presence of chlorine. The second syllable "-phoeni-" is pronounced as /fiːnaɪ/, referencing the coloring of a deep reddish-purple found in phoenician glass. The final syllable "-cite" is pronounced as /saɪt/, indicating a mineral or rock. Chlorophoenicite is a rare mineral consisting of manganese, zinc, and iron, found in Norway and Mexico.
Chlorophoenicite is a mineral that belongs to the family of carbonates. It is characterized by its complex chemical composition, with the formula (Zn,Mn2+)2Mn3+(CO3)4·3H2O. The name "chlorophoenicite" originates from the Greek words "chloros," meaning green, and "phoinix," signifying dark red or brown. This name denotes the mineral's distinctive color range, which often displays shades of green and reddish-brown.
Chlorophoenicite commonly occurs as tabular or prismatic crystals, and its crystal structure is monoclinic. It is typically found in association with other minerals like rhodochrosite and hyalophane. This mineral has a relatively low hardness, ranging between 3 and 4 on the Mohs scale, making it susceptible to scratches.
Chlorophoenicite's specific gravity falls approximately around 3.5, and it has a transparent to translucent appearance. Due to its composition, this mineral exhibits weak double refraction, causing light rays to split when passing through it.
When it comes to its occurrence, chlorophoenicite has been discovered in various locations worldwide, including Germany, Scotland, Hungary, Russia, and the United States. It is often found in hydrothermal veins, granite pegmatites, and oxidized zinc-manganese deposits.
Although chlorophoenicite is not a particularly well-known mineral, its striking colors and occurrence alongside other notable minerals make it of interest to collectors and geologists alike. Its unique blend of green and reddish-brown hues adds aesthetic value to mineral collections, while further exploration of its properties contributes to our understanding of the geological processes behind its formation.
The word "chlorophoenicite" is derived from Ancient Greek roots.
- "Chloro-" is derived from the Greek word "khlōros", meaning "green". This prefix is commonly used in scientific terminology to refer to the color green or any compounds or elements associated with green coloration.
- "Phoenici-" stems from the Greek word "Phoinix", which refers to the color purple, vibrant red, or dark red. It also has associations with the Phoenicians, an ancient seafaring civilization known for their production of purple dye from the murex snail.
- "-ite" is a suffix used in mineralogy to indicate a mineral or compound. It is derived from the Greek suffix "-ites", which simply means "of or pertaining to". It is commonly used to form the names of minerals.