IPA: /ˈpleɪdʒiəˌkloʊs/
KK: /ˈplædʒiˌoʊkleɪs/
A type of mineral that is part of a group of feldspar minerals, commonly found in many types of rocks, and made up of sodium and calcium aluminum silicates.
Plagioclase is often used in geology to identify different types of igneous rocks.
Plagioclase → It is formed from "plagio-" (from Greek "plagios", meaning oblique) and "clase" (from Greek "klasis", meaning breaking). The word refers to a type of feldspar mineral that has an oblique cleavage pattern.
Think of the word 'oblique' ('plagio-') to remember that 'plagioclase' refers to a mineral that breaks in an oblique manner.
No commonly confused words.