IPA: /ˌhɛmɪˈmɔːfɪzəm/
KK: /hɛməˈmɔrfɪzəm/
A property in crystallography where the two ends of a crystal are different from each other in their shapes or surfaces.
The mineral exhibits hemimorphism, showing distinct features at both ends of the crystal.
Hemimorphism is formed from "hemi-" (meaning half) and "morphe" (meaning form or shape). The term describes a condition where a crystal or mineral exhibits different forms on opposite sides, essentially having a 'half' form on each side.
Think of 'half' ('hemi-') and 'form' ('morphe') to remember that hemimorphism refers to a shape that has different forms on each side.