Apjohnite is a rare mineral named after the Irish chemist Dr. Bartholomew Apjohn. Its chemical formula is MgAl2(PO4)2(OH)4·H2O. The spelling of Apjohnite is represented by the International Phonetic Alphabet as /æpˈdʒɒnʌɪt/. The phonetic transcription consists of six symbols that indicate the pronunciation of each syllable. The /æp/ refers to the first syllable, which is pronounced as "ap" with a short "a" sound. The following syllable /ˈdʒɒnʌɪt/ is pronounced as "djon-ite" with the stress on the second syllable.
Apjohnite is a rare mineral that is scientifically classified as a hydrated copper aluminum sulfate compound. It typically occurs as small, prismatic or bladed crystals that are translucent to transparent in appearance. Its name is derived from the chemist John Apjohn who first discovered and studied the mineral in the mid-19th century.
In terms of its chemical composition, apjohnite consists of aluminum, copper, sulfur, and oxygen, with water molecules also incorporated into its structure. This mineral belongs to the sulfate mineral group, characterized by its sulfate anion (SO4)2-.
Apjohnite is commonly found in oxidized copper ore deposits, particularly in barite-rich environments or in association with other sulfate minerals. It can occur as an alteration product of primary copper minerals in the presence of sulfur-bearing fluids. Its color can range from pale green to blue, and it may exhibit vitreous to silky luster on its surface. Due to its relatively low hardness and fragility, apjohnite is seldom used as a gemstone.
Although apjohnite holds some scientific interest for mineralogists due to its unique crystal structure and occurrence, it has limited practical applications. It is mostly sought after and collected by mineral enthusiasts and researchers for its rarity and aesthetic value. As a mineral with limited occurrences and a specific composition, apjohnite contributes to the understanding of geological processes and the formation of mineral deposits.