IPA: /ˈɒlɪɡəʊkleɪz/
KK: /ˈɑlɪɡoʊˌkleɪs/
A type of mineral that is part of the plagioclase series, commonly found in igneous rocks.
Oligoclase is often used in the study of geological formations due to its unique properties.
Oligoclase → It is formed from "oligo-" (from Greek "oligos", meaning few or little) and "clase" (from Greek "klasis", meaning breaking or fracture). The word refers to a mineral that has a few distinct cleavage planes, indicating its crystalline structure.
Think of 'few' ('oligo-') and 'breaking' ('clase') to remember that oligoclase is a mineral with few distinct breakage patterns.