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Single Orthoclase Crystal

The Mineral orthoclase

Orthoclase is one of the most common minerals, and occurs in numerous mineral environments. It is polymorphous with the minerals Microcline and Sanidine. These three minerals form the Potassium Feldspar group. They are almost identical in physical properties, and it is sometimes impossible to distinguish one another without x-ray analysis. The only difference between them is their crystal structure. Microcline crystallizes in the triclinic system, and Orthoclase and Sanidine crystallize in the monoclinic system. Sanidine forms at high temperatures and has a disordered monoclinic symmetry, whereas Orthoclase forms at low temperatures and cools slowly, forming more ordered monoclinic crystals.

In some mineral reference guides, Microcline and Sanidine are wrongly categorized as variety of Orthoclase. Since it is so difficult to distinguish between Orthoclase, Sanidine, and Microcline, they may be simply called "Potassium Feldspar".
Chemical Formula KAlSi3O8
Composition Potassium aluminum silicate
Color White, yellow, colorless, pink, orange, light blue, light green, brown, gray
Streak White
Hardness 6
Crystal System Monoclinic
3D Crystal Atlas
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Crystal Forms
and Aggregates
Occurs in well shaped prismatic and tabular crystals, which are sometimes striated. Crystals often form penetration twins and repeated twins, in the form of Carlsbad twins, Baveno twins, and Manbach twins. Also occurs massive, grainy, and as rounded, waterworn stones.

Click here for more detailed information on the crystal structure of the Feldspars.
Transparency Transparent to opaque
Specific Gravity 2.6
Luster Vitreous to pearly
Cleavage 2,1 - basal ; 2,1 - prismatic ; 3,1 - pinacoidal. The cleavage angle is about 90º.
Fracture Conchoidal to uneven
Tenacity Brittle
In Group Silicates; Tectosilicates; Feldspar Group
Striking Features Crystal habits, cleavage, and hardness
Environment A major constituent of low-temperature metamorphic rocks. Also in igneous environments such as pegmatites, as well as sedimentary conglomerates.
Rock Type Igneous, Sedimentary, Metamorphic
Popularity (1-4) 2
Prevalence (1-3) 1
Demand (1-3) 2

Orthoclase AUCTIONS
Potassium Feldspar Name used to describe the minerals belonging to the potassium feldspar group, specifically Orthoclase, Microcline, and Sanidine.

 -  White or colorless, transparent to translucent variety of Orthoclase (or Sanidine).
 -  Form of feldspar that displays a color sheen known as adularescence. Depending on the locality, Moonstone may be Orthoclase feldspar (Adularia), or it may be the Plagioclase feldspar Oligoclase.
 -  Describes a transparent, yellow variety of Orthoclase from Madagascar.
 -  White form of bladed or platy Adularia from the Valenciana Mine in Guanajuato, Mexico.
Microcline, Sanidine

Orthoclase is industrially important in the manufacture of glass and ceramics. Orthoclase crystals and twins provide information on the formation of minerals and environmental factors. Well shaped crystals and twins are highly sought after by mineral collectors, and the Moonstone variety is used as a gemstone.

For additional information, see the gemstone section on Orthoclase and Moonstone.

Orthoclase is one of the most common minerals, and is found worldwide. Only a select few localities are mentioned. The original Carlsbad twins were described from Karlovy Vary (Carlsbad), Bohemia, Czech Republic. Some of the best crystals come from Baveno, Piedmont, Italy, especially the famous Baveno twins. Good crystals come from San Piero in Campo on the Island of Elba, Italy; and Zarzalejo, Madrid, Spain; Switzerland contains numerous good localities in the pegmatites of Uri.

Light blue crystals came from the the Lake Baikal area in Russia, and large masses from Mt. Kilimanjaro, Tanzania. Transparent gemmy yellow crystals that have recently become very popular come from a pegmatite in Madagascar, at Itrongay, Tulear Province.

In the U.S., enormous crystals were found on Sandia Mountain, Bernalillo Co, New Mexico. Good collector specimens have come from the Organ Mountains, Dona Ana Co., New Mexico; Robinson Gulch, Jefferson Co., Colorado; and Goodsprings, Clark Co., Nevada. Orthoclase has also come from the French Creek mine, St. Peters, Chester Co., Pennsylvania.

Quartz, Muscovite, Plagioclase Feldspars, Biotite, Tourmaline, Garnet

Sanidine - Indistinguishable without complex methods. Sanidine, however, is never opaque.
Microcline - Indistinguishable without complex methods. However, Microcline can have a deep green color that Orthoclase cannot achieve.
Plagioclase Feldspars - May exhibit striations on twinned crystal surfaces, otherwise difficult to distinguish.
Spodumene - Has a splintery fracture.
Calcite - much softer (3).

orthoclase PHOTOS
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