Chondrodite is a mineral belonging to the silicate family. The correct spelling of this word is pronounced as /ˈkɒndrədaɪt/. The first syllable, "chon," is pronounced with a short "o" sound followed by "d" and "r" sounds. The second syllable, "dro," is pronounced with a long "o" sound, followed by "d" and "r" sounds. The final syllable, "ite," is pronounced with a long "i" sound and a soft "t" sound. The spelling of this word follows the usual pronunciation of "ch" as "k" and "ti" as "tai."
Chondrodite is a mineral that belongs to the silicate group and the pyroxene family. It is typically found in medium to high-temperature metamorphic rocks, particularly in marbles and skarns. Chondrodite has a chemical formula of (Mg,Fe2+)5(PO4)2(SiO4)2(OH,F)2, where magnesium and iron are the dominant cations.
Chondrodite is characterized by its unique brown to reddish-brown color, often with a vitreous to resinous luster. It usually occurs in the form of granular aggregates, and its crystal structure is typically monoclinic.
This mineral has a hardness ranging from 5.5 to 6.5 on the Mohs scale, making it relatively durable. Its specific gravity falls between 2.9 and 3.2. Chondrodite also displays pleochroism, meaning that it can exhibit different colors when viewed from different angles, such as pale yellow to reddish-brown.
Chondrodite is most commonly associated with other minerals such as olivine, spinel, diopside, and tremolite. It is primarily found in regions with metamorphic activity, including Italy, the United States, England, and Sweden.
Due to its attractive color and rarity, chondrodite is sometimes sought after by collectors and used as a gemstone in jewelry. It also has various industrial uses, including its incorporation into refractory materials and as a source of phosphate and magnesium.
One of the gems, occurring in grains of various shades of yellow and red.
Etymological and pronouncing dictionary of the English language. By Stormonth, James, Phelp, P. H. Published 1874.
The word "chondrodite" has its origins in the Greek language. It is derived from the Greek words "chondros", meaning "grain" or "cartilage", and "dite", which is a suffix denoting a mineral species. The term "chondrodite" was coined in 1823 by the German mineralogist Friedrich Mohs to describe a specific type of mineral. Chondrodite is a silicate mineral belonging to the group of minerals called the pyroxenes. It is commonly found in metamorphic rocks and is known for its brown or yellow-brown color.