Feldspar is the name of an important group of rock-forming minerals which make up perhaps as much as 60% of the Earth's crust. Feldspars crystallize from magma in both intrusive and extrusive rocks; they occur as compact minerals, as veins, and are also present in many types of metamorphic rock. Rock formed entirely of plagioclase feldspar (see below) is known as anorthosite. Feldspars are also found in many types of sedimentary rock.
Feldspar is derived from the German Feld, field, and Spat, a rock that does not contain ore. Feldspathic refers to materials that contain feldspar. The alternative spelling, felspar, has now largely fallen out of use
This group of minerals consists of framework or tectosilicates:
Feldspat | Feldspat | Feldspat | Päevakivi | Feldespatos | Feldspato | فلدسپات | Feldspath | 장석 | Feldspat | Feldspato | פצלת השדה | Lauko špatas | Földpátok | Veldspaat | 長石 | Plagioklazy | Feldspato | Полевой шпат | Maasälpä | Fältspat
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"Feldspar".
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