Simple monoclinic refers to one of the seven crystal systems in crystallography, characterized by having three unequal axes with two axes intersecting at an angle of 90 degrees, while the third axis is inclined. This system has a specific symmetry and arrangement that is essential for understanding the properties of minerals within this classification. It is defined by its unique lattice structure, which significantly influences the physical properties and behaviors of the minerals that crystallize in this form.
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