The monoclinic system is one of the seven crystal systems characterized by three unequal axes, where two axes intersect at an angle that is not 90 degrees, while the third axis is perpendicular to the plane formed by the other two. This unique arrangement allows for a variety of crystal shapes and forms, making it significant in the study of crystal structures and symmetry. The monoclinic system includes specific lattice types that play a critical role in crystallography, influencing properties such as symmetry and packing arrangements in solids.
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