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Plagioclase

/ˈpleɪdʒioʊkleɪs/noun

The group of feldspar minerals whose two cleavage planes meet at an angle slightly off ninety degrees.

The Greek roots

πλάγιος
plágios
slanting, oblique
+
κλάσις
klásis
breaking, fracture

Literally: oblique breaking

The story of the word

Johann Breithaupt named it in 1847 for a geometric fault: its cleavages meet obliquely rather than square. The name was built as the answer to orthoclase, the right-angled feldspar he had named twenty-four years earlier, so the pair still divides the feldspars in every mineralogy course. Plagioclase makes up a large share of the Earth's crust and most of the pale lunar highlands.

How it travelled
Ancient Greek → German → English
First recorded
19th century

Same family

orthoclasemicroclineiconoclastplagiarism

In a sentence

The thin section showed plagioclase laths in a dark groundmass.

Plagioclase composition tracks the temperature the magma cooled at.

Built on the same root

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