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Mineral group · Silicate

Plagioclase

(Na,Ca)(Al,Si)₄O₈

Albite–anorthite solid-solution series, the most abundant mineral on Earth's surface.

Hardness6–6.5
Crystal systemTriclinic
ClassSilicate
Plagioclase specimen

corundum var. ruby, garnet var. almandin, mica var. biotite, feldspar var. plagioclase : Khit Ostrov (Khit, Island), Northern Karelia, Karelia Republic, Norther — Photo: Géry PARENT · Public domain

Plagioclase

Also known as: Soda-lime feldspar.

The continuous feldspar series from albite to anorthite — the most abundant minerals in Earth's crust.

Intro adapted from Wikipedia (CC BY-SA).

Plagioclase is a mineral group, with the chemical formula (Na,Ca)(Al,Si)₄O₈.

It crystallizes in the triclinic crystal system.

Key properties: Mohs hardness 6–6.5; typically white or gray or colorless.

Collections: Everyday Minerals.

Index entry. This entry combines official IMA/RRUFF species data with published physical-property data and a Wikipedia introduction — a full written entry hasn’t been published yet. Browse more P minerals or help write this entry.