Feldspath - significado y definición. Qué es Feldspath
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Qué (quién) es Feldspath - definición

MINERAL GROUP
Feldspars; Felspar; Feldspath; Feldspathic; Veldspar; Felspathic; Feltsparr; Alkali feldspar; Alkali Feldspar
  • Compositional phase diagram of the different minerals that constitute the feldspar solid solution.

Feldspath         
·noun A name given to a group of minerals, closely related in crystalline form, and all silicates of alumina with either potash, soda, lime, or, in one case, baryta. They occur in crystals and crystalline masses, vitreous in luster, and breaking rather easily in two directions at right angles to each other, or nearly so. The colors are usually white or nearly white, flesh-red, bluish, or greenish.
Feldspathic         
·adj ·Alt. of Feldspathose.
felspar         
['f?lsp?:]
¦ noun variant spelling of feldspar.

Wikipedia

Feldspar

Feldspars (sometimes spelled felspars) are a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the plagioclase (sodium-calcium) feldspars and the alkali (potassium-sodium) feldspars. Feldspars make up about 60% of the Earth's crust, and 41% of the Earth's continental crust by weight.

Feldspars crystallize from magma as both intrusive and extrusive igneous rocks and are also present in many types of metamorphic rock. Rock formed almost entirely of calcic plagioclase feldspar is known as anorthosite. Feldspars are also found in many types of sedimentary rocks.