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Feldspar

Silicate Minerals

A group of rock-forming silicate minerals, the single most abundant mineral group in the Earth's crust, and the source of the pale crystals that give granite its speckled look. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Kind
Mineral 2
Formation Class
Framework silicate, the most abundant mineral group in the Earth's crust 2
Chemical Formula
KAlSi3O8 - NaAlSi3O8 - CaAl2Si2O8 (end-member series) 1
Hardness (Mohs)
6 2
Standard reference value for the feldspar group generally; individual species vary slightly.
Classification
Classification
Silicate Mineral 1
Use
Ceramic and Glass Manufacture 1
Connections

Associated With

Amphibolite, Materials

Plagioclase feldspar is one of the two defining minerals of amphibolite, alongside amphibole.

Granite, Materials

Granite's own lead description names alkali feldspar as one of its main constituent minerals.

Source Granite (Wikipedia)
Migmatite, Materials

The pale leucosome bands of a migmatite are quartzofeldspathic melt segregations.

Monzonite, Materials

Monzonite is defined by roughly equal plagioclase and alkali feldspar with little quartz.

Pegmatite, Materials

Feldspar named as one of the three dominant minerals of most pegmatites.

Source Pegmatite (Wikipedia)
Rhyolite, Materials

Sanidine and plagioclase are both feldspar-group minerals; feldspar is a principal mineral of rhyolite.

Source Rhyolite (Wikipedia)
Trachyte, Materials

Trachyte is defined by its dominant alkali feldspar content.

Classified As

Entity-backed identity for the material classification this material already carries as an enum fact, pointing at the class subcategory of the same name. The enum fact itself stays on the entity unchanged.

In Discipline

Source Mineral (Wikipedia)
Sources
1. Feldspar (Wikipedia)
Wikimedia Foundation
  • Composition section
    orthoclase endmember KAlSi3O8, albite endmember NaAlSi3O8, anorthite endmember CaAl2Si2O8
  • Entity classification (SubLabel)
    A group of rock-forming silicate minerals, the single most abundant mineral group in the Earth's crust, and the source of the pale crystals that give granite its speckled look.
  • Feldspar (Wikipedia), Applications section
    Feldspar is a common raw material used in glassmaking, ceramics
View the Source
2. Mineral (Wikipedia)
Wikimedia FoundationView the Source
Wikidata: Feldspar
Wikidata Q170258
Quote, Wikidata Q170258
P279 subclass chain verified to reach rock (Q8063) or mineral (Q7946) within a few hops; identified via Wikipedia pageprops (article title match), PlaybookNote 38526.
Granite (Wikipedia)
Wikimedia FoundationAssociated With: Granite, Lead section
Quote, Associated With: Granite, Lead section
is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, mica and plagioclase.
View the Source
Rhyolite (Wikipedia)
Wikimedia FoundationAssociated With: Rhyolite, Mineralogy section
Quote, Associated With: Rhyolite, Mineralogy section
The mineral assemblage is predominantly quartz, sanidine, and plagioclase.
View the Source
Pegmatite (Wikipedia)
Wikimedia FoundationAssociated With: Pegmatite, Lead section
Quote, Associated With: Pegmatite, Lead section
Most pegmatites are composed of quartz, feldspar, and mica, having a similar silicic composition to granite.
View the Source
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