SANIDINE
Feldspar
Group
sanidine - mineral 76.1.1.2
| Chemical Formula | KAlSi3O8 | |
| Composition | Potassium aluminum silicate. Forms a series with Albite (NaAlSi3O8), in which the intermediary member is Anorthoclase. | |
| Variable Formula | (K,Na)AlSi3O8 | |
| Color | Colorless, white, cream, yellow, gray, light brown | |
| Streak | White | |
| Hardness | 6 | |
| Crystal Forms and Aggregates |
(Monoclinic) Most commonly as tabular crystals, but occasionally in prismatic form. Crystals frequently form penetration and repeated twins, and they are often striated. Also occurs massive and grainy. | |
| Transparency | Transparent to translucent | |
| Specific Gravity | 2.5 - 2.6 | |
| Luster | Vitreous | |
| Cleavage | 1,1 - basal ; 2,1 - prismatic The cleavage angle is about 90º |
|
| Fracture | Conchoidal to uneven | |
| Tenacity | Brittle | |
| Varieties | ||
| Polymorphs | Orthoclase, Microcline | |
| In Group | Silicates ; Tectosilicates ; Feldspar group ; Potassium feldspars | |
| All About | Sanidine is polymorphous with Orthoclase and Microcline. These three minerals form the Potassium
Feldspar group.They
are almost identical in physical properties, and
sometimes it is 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. [For more information on the crystal structure of the feldspars, see "All about" in the mineral Anorthite.] In many 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". Moonstone is a form of Adularia (or several other feldspars) that displays adularescence, exhibiting a color sheen on its surface. This phenomenon gives Moonstone important status and recognition on the gem market. |
|
| Uses | Sanidine crystals and twins are studied by scientists, as they provide information on the formation of minerals and environmental factors. Well shaped crystals and twins are highly sought after by mineral collectors, and the variety Moonstone is an important gem. | |
| Striking Features | Crystal habits, cleavage, and hardness | |
| Complex Tests | Soluble in hydrofluoric acid | |
| Popularity (1-4) | 2 | |
| Prevalence (1-3) | 2 | |
| Demand (1-3) | 2 | |
| Distinguishing Similar Minerals |
Orthoclase - Indistinguishable without
complex methods. Sanidine, however, is never opaque,
whereas Orthoclase may be. Microcline - Indistinguishable without complex methods. However, Microcline can be a deep green color that Sanidine cannot achieve. Plagioclase feldspars - exhibit striations on twinned crystal surfaces Spodumene - has a splintery cleavage Calcite - much softer (3) |
|
| Commonly Occurs With |
Quartz, Muscovite, Plagioclase feldspars | |
| Noteworthy Localities |
Some famous localities are the Island of Elba, Italy; the Caucasus Mountains, Russia; Ragged Mountain, Gunnison Co., Colorado; the Black Range, Grant Co., New Mexico; and Bisbee, Cochise Co., Arizona. | |
| Picture Icon Links |
Sorry. No Images currently available. | |
| Picture Links | Sorry. No Images currently available. |
Additional references
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