Cleavage in minerals can result in distinctive shapes like cubes or rhombs, dictated by the number of directions and angles of cleavage.
Cleavage in minerals refers to their tendency to break along certain planes. Some minerals, like halite and calcite, exhibit cubic cleavage with three directions of cleavage intersecting at 90-degree angles. For example, halite cleaves at 90° angles producing cubic shapes, while calcite cleaves in three directions forming rhomb shapes with approximately 75° cleavage angles.
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