CHROMOLEUCITE Meaning and
Definition
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Chromoleucite is a mineral that belongs to the tectosilicate group and has the chemical formula (K,Na)AlSi2O6. It crystallizes in the tetragonal system and is usually found in the form of small, prismatic crystals or grainy masses. Chromoleucite is typically transparent or translucent and has a vitreous to silky luster.
Physically, chromoleucite can range in color from white to grayish-white, and it often exhibits a greasy or waxy appearance. It has a Mohs hardness of 5 to 6, which means it is relatively hard and can resist scratching and abrasion. Its specific gravity varies between 2.60 and 2.65.
Chromoleucite is primarily composed of potassium, sodium, aluminum, and silicon. It is commonly found in alkaline pegmatites and nepheline syenites, as well as in contact metamorphic zones. It forms as a result of the crystallization of magma and undergoes the process of hydrothermal alteration.
This mineral is of interest to collectors due to its unique crystal habit, as well as its association with other rare minerals like leucite, nepheline, and sodalite. It is primarily found in a few localities worldwide, including Greenland, Russia, and the United States.
Chromoleucite is not widely known for any significant industrial or commercial applications. Its main significance lies in its presence as a collecting specimen for mineral enthusiasts, who value its rarity and aesthetic qualities.
Common Misspellings for CHROMOLEUCITE
- xhromoleucite
- vhromoleucite
- fhromoleucite
- dhromoleucite
- cgromoleucite
- cbromoleucite
- cnromoleucite
- cjromoleucite
- curomoleucite
- cyromoleucite
- cheomoleucite
- chdomoleucite
- chfomoleucite
- chtomoleucite
- ch5omoleucite
- ch4omoleucite
- chrimoleucite
- chrkmoleucite
- chrlmoleucite
Etymology of CHROMOLEUCITE
The word "chromoleucite" is derived from the Greek words "chroma" meaning "color" and "leukos" meaning "white". The combination of the two words refers to the characteristic color and appearance of the mineral. The suffix "-ite" is commonly used in mineralogy to indicate that it is a mineral.
