Halite has perfect cleavage in 3 planes or axes at right angles, meaning halite often forms nearly perfect cubes.
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Halite typically exhibits perfect cubic cleavage, meaning it breaks into perfect cubes or square shapes along its crystal planes. This cleavage is a defining characteristic of halite and can be observed by examining the broken surfaces of the mineral.
This tendency of halite to break apart in one of three directions is called cleavage. Cleavage is a property of minerals where they break along specific planes of weakness due to their crystal structure. In the case of halite, it exhibits cubic cleavage, which means it breaks into cube-shaped fragments when struck.
Halite crystals break into smaller crystals of the same shape due to the crystal structure and cleavage of the mineral. Halite has a cubic crystal structure and perfect cubic cleavage, which means it breaks along planes that are parallel to the faces of the cube, resulting in smaller crystals with the same cubic shape.
Halite typically displays cleavage along three planes at right angles to each other. However, if halite is subjected to mechanical stress, it can also exhibit a conchoidal fracture pattern due to its brittle nature.
An example of rhombic cleavage would be siderite and rhodochrosite. Remember that this is basically a "partically squashed box." Essentially, the direction of deformation in a rhombohedron occurs in one of the three diagonals that run from one corner of the cube to the other. Calcite is not a particularly fabulous example of a rhombohedron, because it is considered to be cubed.
Halite has a cubic crystal structure, which makes it naturally form into perfect cubes. When broken repeatedly along its natural cleavage planes, halite will continue to fragment into smaller cubes due to its internal molecular arrangement. This phenomenon is a result of the crystal structure of halite and its tendency to break along specific planes.