Frae Wikipedia
Jump to navigation Jump to search
Feldspar crystal (18×21×8.5 cm) frae Jequitinhonha valley, Minas Gerais, Sootheastren Brazil.
Category tectosilicate
(repeatin unit)
Creestal seestem triclinic or monoclinic
Colour pink, white, gray, broun
Twinnin tartan, carlsbad, etc
Cleavage twa or three
Fractur alang cleavage planes
Mohs scale haurdness 6.0-6.5
Skinkle Vitreous
Streak white
Diaphaneity opaque
Speceefic gravity 2.55 - 2.76
Density 2.56
Refractive index 1.518-1.526
Birefringence first order
Pleochroism none
Ither chairacteristics exsolution lamellae common
References [1]

Feldspars (KAlSi3O8NaAlSi3O8CaAl2Si2O8) are a group o rock-furmin tectosilicate meenerals that mak up as much as 60% o the Yird's crust.[2]

Feldspars crystallize frae magma as veins in baith intrusive an extrusive igneous rocks an are an aa present in mony types o metamorphic rock.[3] Rock furmed almaist entirely o calcic plagioclase feldspar is kent as anorthosite.[4] Feldspars are an aa foond in mony types o sedimentary rock.[5]

References[eedit | eedit soorce]

  1. "Feldspar". Gemology Online. Retrieved 8 November 2012. 
  2. Feldspar. What is Feldspar? Industrial Meenerals Association. Retrieved on July 18, 2007.
  3. "Metamorphic Rocks." Metamorphic Rocks Information. Retrieved on July 18, 2007
  4. Blatt, Harvey and Robert J. Tracy, Petrology, Freeman, 2nd ed., 1996, pp. 206–210 ISBN 0-7167-2438-3
  5. "Weathering and Sedimentary Rocks." Geology. Retrieved on July 18, 2007.