Pleochromism
Taking a quick break from describing the types of chromism, the topic of this post is pleochromism—which, despite the name, is not actually a form of chromism. Pleochromism is the optical phenomenon that results when a materials has a different appearance/color when viewed at different angles, or different angles of polarized light. It is not the process of a color change caused by an external stimuli, but rather the inherent property of a material.
Pleochromism results from anisotropy in crystal structures. Isotropic crystals do not exhibit pleochromism. Different crystal orientations in a material absorb and transmit different wavelengths of light, which can lead to both subtle or strong differences in visual appearances. This is most commonly seen in minerals, some exhibiting merely a change in the intensity of their coloration, others shifting colors entirely.
Some known pleochromic minerals include tourmaline, pictured above, alexandrite, corundum, and apatite. Commercial applications of pleochromism are rare, but scientists can use the effect to help identify minerals and gemstones.
Sources/Further Reading: (Image 1—Wikipedia) (Image 2—University of Granada) (GIA)













