pleokrooppisia

Pleokrooppisia, also known as pleochroism, is a property exhibited by certain minerals and crystals. It refers to the phenomenon where a mineral displays different colors when viewed from different angles. This effect is due to the mineral's optical properties, specifically its birefringence, which is the ability to split light into two rays that travel at different speeds. The two rays then interfere with each other, creating the observed color changes.

Pleochroism is most commonly observed in anisotropic minerals, which have different optical properties in different directions. The colors seen in pleochroic minerals can vary widely, ranging from subtle shades to vibrant hues. For example, tourmaline is a well-known pleochroic mineral, exhibiting colors such as brown, green, or blue depending on the viewing angle.

The study of pleochroism is important in mineralogy and crystallography, as it provides insights into the internal structure and optical properties of minerals. It is also utilized in gemology to identify and classify gemstones. Pleochroism is typically observed using a polarizing microscope, which allows for the controlled viewing of minerals from different angles.