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- Q182264 subject Q7318333.
- Q182264 subject Q8445686.
- Q182264 subject Q8833492.
- Q182264 abstract "Albite is a plagioclase feldspar mineral. It is the sodium endmember of the plagioclase solid solution series. As such it represents a plagioclase with less than 10% anorthite content. The pure albite endmember has the formula NaAlSi3O8. It is a tectosilicate. Its color is usually pure white, hence its name from Latin albus. It is a common constituent in felsic rocks.Albite crystallizes with triclinic pinacoidal forms. Its specific gravity is about 2.62 and it has a Mohs hardness of 6 - 6.5. Albite almost always exhibits crystal twinning often as minute parallel striations on the crystal face. Albite often occurs as fine parallel segregations alternating with pink microcline in perthite as a result of exolution on cooling.There are two variants of albite, which are referred to as low albite and high albite; the latter is also known as analbite. Although both variants are triclinic, they differ in the volume of their unit cell, which is slightly larger for the high form. The high form can be produced from the low form by heating above c. 750 °C (1382 °F). Upon further heating to more than c. 1050 °C the crystal symmetry changes from triclinic to monoclinic; this variant is also known as monalbite.It occurs in granitic and pegmatite masses, in some hydrothermal vein deposits and forms part of the typical greenschist metamorphic facies for rocks of originally basaltic composition.It was first reported in 1815 for an occurrence in Finnbo, Falun, Dalarna, Sweden.".
- Q182264 colour Q1068275.
- Q182264 thumbnail Albite_-_Crete_(Kriti)_Island,_Greece.jpg?width=300.
- Q182264 wikiPageExternalLink Albite.
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- Q182264 wikiPageWikiLink Q7318333.
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- Q182264 wikiPageWikiLink Q7946.
- Q182264 wikiPageWikiLink Q8445686.
- Q182264 wikiPageWikiLink Q847257.
- Q182264 wikiPageWikiLink Q8833492.
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- Q182264 color "White to gray, blueish, greenish, reddish; may be chatoyant".
- Q182264 name "Albite".
- Q182264 type ChemicalSubstance.
- Q182264 type Mineral.
- Q182264 type ChemicalObject.
- Q182264 type Thing.
- Q182264 type Q7946.
- Q182264 comment "Albite is a plagioclase feldspar mineral. It is the sodium endmember of the plagioclase solid solution series. As such it represents a plagioclase with less than 10% anorthite content. The pure albite endmember has the formula NaAlSi3O8. It is a tectosilicate. Its color is usually pure white, hence its name from Latin albus. It is a common constituent in felsic rocks.Albite crystallizes with triclinic pinacoidal forms. Its specific gravity is about 2.62 and it has a Mohs hardness of 6 - 6.5.".
- Q182264 label "Albite".
- Q182264 depiction Albite_-_Crete_(Kriti)_Island,_Greece.jpg.
- Q182264 name "Albite".