Switzerite
Encyclopedia
Switzerite is a mineral with the chemical formula of (Mn)3(PO4)2·7H2O. Leavens, Peter B., White, John S. Jr., and Zanazzi, Pier F. (1986) Switzerite redefined as, Mn3(PO4)2·7H2O, and metaswitzerite, Mn3(PO4)2·4H2O. American Mineralogist, 71, 1221-1223. The mineral was named after George Switzer
, former Curator of Minerals at the US National Museum. Leavens, Peter B. and White, John S. Jr. (1967) Switzerite, (Mn,Fe)3(PO4)2·4H2O, A New Mineral. American Mineralogist, 52, 1595-1602..The mineral is monoclinic prismatic, meaning that it has one mirror plane, one 2-fold rotation axis which is perpendicular to the mirror plane and a center of symmetry. Switzerite is a part of the monoclinic space group P 21/a. Leavens, Peter B. and White, John S. Jr. (1967) Switzerite, (Mn,Fe)3(PO4)2·4H2O, A New Mineral. American Mineralogist, 52, 1595-1602.. For its optical properties, Switzerite is classified as anisotropic, has a low surface relief and birefringence of δ = 0.020. Leavens, Peter B. and White, John S. Jr. (1967) Switzerite, (Mn,Fe)3(PO4)2·4H2O, A New Mineral. American Mineralogist, 52, 1595-1602..
Switzerite was first discovered in the 1960's and the most important factor about this mineral is that it immediately dehydrates into metaswitzerite. Switzerite is a relatively uncommon mineral found in a few localities in Europe, North America, and Australia. This mineral is found in phosphate mines, along with other phosphate minerals. Alone, Switzerite does not have a huge significance due to its rarity and extremely small size. This mineral is found with other phosphate minerals thus, the importance of Switzerite is that it is used, along with the other phosphate minerals, for agricultural purposes.
George Switzer (mineralogist)
George Shirley Switzer was an American mineralogist who is credited with starting the Smithsonian Institution's famed National Gem and Mineral Collection by acquiring the Hope Diamond for the museum in 1958...
, former Curator of Minerals at the US National Museum. Leavens, Peter B. and White, John S. Jr. (1967) Switzerite, (Mn,Fe)3(PO4)2·4H2O, A New Mineral. American Mineralogist, 52, 1595-1602..The mineral is monoclinic prismatic, meaning that it has one mirror plane, one 2-fold rotation axis which is perpendicular to the mirror plane and a center of symmetry. Switzerite is a part of the monoclinic space group P 21/a. Leavens, Peter B. and White, John S. Jr. (1967) Switzerite, (Mn,Fe)3(PO4)2·4H2O, A New Mineral. American Mineralogist, 52, 1595-1602.. For its optical properties, Switzerite is classified as anisotropic, has a low surface relief and birefringence of δ = 0.020. Leavens, Peter B. and White, John S. Jr. (1967) Switzerite, (Mn,Fe)3(PO4)2·4H2O, A New Mineral. American Mineralogist, 52, 1595-1602..
Switzerite was first discovered in the 1960's and the most important factor about this mineral is that it immediately dehydrates into metaswitzerite. Switzerite is a relatively uncommon mineral found in a few localities in Europe, North America, and Australia. This mineral is found in phosphate mines, along with other phosphate minerals. Alone, Switzerite does not have a huge significance due to its rarity and extremely small size. This mineral is found with other phosphate minerals thus, the importance of Switzerite is that it is used, along with the other phosphate minerals, for agricultural purposes.