feijom thokpafelicitated

Feldspar (English) [ IPA: ˈfelˌspɑr ASM: ফেলস্পাৰ]
Contributed by: মৰ্ণিংকে ফাংচ` (Morningkeey Phangcho) on 2010-11-27
1. Geology(Common Noun-Common &/or Masculine) Feldspars (KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8) are a group of rock-forming tectosilicate minerals which make up as much as 60% of the Earth's crust.[1] Feldspars crystallize from magma in both intrusive and extrusive igneous rocks, as veins, and are also present in many types of metamorphic rock.[2] Rock formed almost entirely of calcic plagioclase feldspar (see below) is known as anorthosite.[3] Feldspars are also found in many types of sedimentary rock.[
English: Feldspar,
Karbi: chaplongbar