In crystallography, describing a crystal system with two unequal oblique angles, specifically relating to the monoclinic system's variations.
From Greek 'di-' (two) and 'clinic' from 'clinein' (to lean or incline). The term was developed in the 19th century by mineralogists describing crystal angles and symmetry.
Crystallographers can identify minerals in seconds by recognizing which crystal system they belong to—diclinic crystals form some of the most beautifully intricate geometric patterns in nature, and understanding their angles helps miners find valuable deposits!
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