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switzerite

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Also known as IMA1966-042

Switzerite is a mineral with the chemical formula of (Mn)3(PO4)2·7H2O. The mineral was named after George Switzer, former Curator of Minerals at the US National Museum. 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. For its optical properties, Switzerite is classified as anisotropic, has a low surface relief and birefringence of δ = 0.020.

Key facts

Mineral.name
Switzerite
Mineral.category
Phosphate minerals
Mineral.image
Metaswitzerite-177958.jpg
Mineral.caption
Switzerite (metaswitzerite) from Foote Lithium County Mine, Kings Mountain District, Cleveland County, North Carolina, US
Mineral.formula
(Mn,Fe)3(PO4)2·7H2O
Mineral.molweight
481.55 g/mol
Mineral.strunz
8.CE.25
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P21/a
Mineral.unit cell
a = 8.528 Å b = 13.166 Å c = 11.812 Å; β = 110.05° Z = 4; V = 1,245.87 Å3
Mineral.color
Pale pink, Pinkish brown
Mineral.cleavage
Perfect (001) Cleavage
Mineral.mohs
2
Mineral.luster
Pearly
Mineral.opticalprop
Biaxial (-)
Mineral.streak
White
Mineral.density
2.535

via Wikipedia infobox

Wikidata facts

Image
Metaswitzerite-177958.jpg
Show 8 more facts
Commons category
Switzerite
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
8.CE.25
Nickel-Strunz 9th edition (updated 2009)
8.CE.25
streak color
white
IMA Mineral Symbol
Swt
chemical formula
Mn²⁺₃(PO₄)₂ * 7H₂O
Strunz 8th edition (series ID, updated)
VII/C.07
Sources (2)

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Encyclopedic overview

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Contents
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Switzerite is a mineral with the chemical formula of (Mn)3(PO4)2·7H2O. The mineral was named after George Switzer, former Curator of Minerals at the US National Museum. 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. For its optical properties, Switzerite is classified as anisotropic, has a low surface relief and birefringence of δ = 0.020.

Switzerite was first discovered in the 1960s and 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. It is unstable and immediately dehydrates into metaswitzerite on exposure to the atmosphere.

Excerpted from Wikipedia’s “switzerite” article, available under the CC BY-SA 4.0 licence.

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