Feldspar, sometimes spelled felspar, is 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 kinds of sedimentary rocks.

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