• Chemistry: Na(70-50%) Ca(30-50%) (Al, Si)AlSi2 O8, Sodium calcium aluminum silicate.
  • Class: Silicates
  • Subclass: Tectosilicates
  • Group: Feldspars
  • Uses: only as mineral specimens.
  • Specimens

Andesine is only a minor constituent in most granites and syenites. But is the dominant feldspar in certain igneous rocks called, appropriately andesites. It is also found in some metamorphic rocks as a minor constituent.

Andesine is a member of the Plagioclase Feldspar Group. The plagioclase series comprises minerals that range in chemical composition from pure NaAlSi3 O8, Albite to pure CaAl2 Si2 O8 , anorthite. Andesine by definition must contain 70-50% sodium to 30-50% calcium in the sodium/calcium position of the crystal structure. The various plagioclase feldspars are identified from each other by gradations in index of refraction and density in the absence of chemical analysis and/or optical measurements.

All plagioclase feldspars show a type of twinning that is named after albite. Albite Law twinning produces stacks of twin layers that are typically only fractions of millimeters to several millimeters thick. These twinned layers can be seen as striation like grooves on the surface of the crystal and unlike true striations these also appear on the cleavage surfaces. The Carlsbad Law twin produces what appears to be two intergrown crystals growing in opposite directions. Two different twin laws, the Manebach and Baveno laws, produce crystals with one prominant mirror plane and penetrant angles or notches into the crystal. Although twinned crystals are common, single crystals showing a perfect twin are rare and are often collected by twin fanciers.


  • Color is mostly white or gray
  • Luster is vitreous to dull if weathered..
  • Transparency crystals are translucent to transparent.
  • Crystal System is triclinic; bar 1
  • Crystal Habits include blocky, or tabular crystals. Crystals have a nearly rectangular or square cross-section with slightly slanted dome and pinacoid terminations. Twinning is almost universal in all plagioclases. Crystals can be twinned according to the Albite, Carlsbad, Manebach and Baveno laws.
  • Cleavage is perfect in one and good in another direction forming nearly right angled prisms.
  • Fracture is conchoidal.
  • Hardness is 6 - 6.5.
  • Specific Gravity is approximately 2.68-2.71 (average)
  • Streak is white.
  • Associated Minerals are biotite, hornblende, quartz and k-feldspars.
  • Other Characteristics: index of refraction is 1.545-1.562. Lamellar twinning may cause a grooved effect on cystal and cleavage surfaces that appear as striations.
  • Notable Occurrences include Greenland; Andes Mountains (hence the name Andesine) and Norway.
  • Best Field Indicators are occurence, twinning striations, density and index of refraction.
ANDESINE specimens:
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ANDESINE specimen ans-1
$ 25.00
Dims:0.9x0.8x0.1" (2.3x2.0x0.3 cm)
Wt: 0.1oz. (3g)
Sheridan, Montana
This specimen consists of a single crystal of andesine, with no matrix present. One edge shows an irregular termination, while the opposite edge shows a fair amount of damage. The pearly luster and vertical striations typical to this species are present. Andesine is named for the locality in the Andes mountains where it was first collected.
no photo
ans-1 ($ 25.00)
Sheridan, Montana


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