|Crystal class||Hexoctahedral (m3m) |
H-M symbol: (4/m 3 2/m)
|Unit cell||a = 6.2931 Å; Z = 4|
|Formula mass||74.55 g/mol|
|Color||Colorless to white, pale gray, pale blue; may be yellowish red to red due to hematite inclusions|
|Crystal habit||As cubes and octahedra; columnar, in crusts, coarse granular, massive|
|Cleavage||Perfect on , , |
|Tenacity||Brittle to ductile|
|Mohs scale hardness||2|
|Diaphaneity||Transparent to translucent|
|Pleochroism||Visible in colored crystals|
|Solubility||Soluble in water|
|Other characteristics||salty to bitter taste|
Sylvite, or sylvine, is potassium chloride (KCl) in natural mineral form. It forms crystals in the isometric system very similar to normal rock salt, halite (NaCl). The two are, in fact, isomorphous. Sylvite is colorless to white with shades of yellow and red due to inclusions. It has a Mohs hardness of 2.5 and a specific gravity of 1.99. It has a refractive index of 1.4903. Sylvite has a salty taste with a distinct bitterness.
Sylvite is one of the last evaporite minerals to precipitate out of solution. As such, it is only found in very dry saline areas. Its principal use is as a potassium fertilizer.
Sylvite is found in many evaporite deposits worldwide. Massive bedded deposits occur in New Mexico and western Texas, and in Utah in the US, but the largest world source is in Saskatchewan, Canada. The vast deposits in Saskatchewan, Canada were formed by the evaporation of a Devonian seaway. Sylvite is the official mineral of Saskatchewan.
- Sylvite: Sylvite mineral information and data
- Sylvite Mineral Data
- Handbook of Mineralogy
- Klein, Cornelis and Cornelius S. Hurlbut, Jr. 1993. Manual of Mineralogy after J.D. Dana, 21st edition. New York: John Wiley & Sons, Inc.
- Deer, W.A., R.A. Howie, and J. Zussman. 1992. An Introduction to the Rock-Forming Minerals 2nd ed. New York: Prentice Hall.
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Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press..
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