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Birefringence is another crucial property, describing the difference in refractive indices for light traveling through the mineral in different directions. When you observe a mineral under **cross-polarized light (XPL)**, you can see interference colors. Cordierite typically shows low-order interference colors, which means pale grays and yellows. It does not display strong, vibrant colors. Keep this in mind when you are observing your used sporty cars for sale thin sections. The typical birefringence values range from 0.009 to 0.012, so the interference colors are usually quite subtle. These are often the first-order greys and whites. If you see high-order interference colors, then you probably aren't looking at cordierite. Cordierite’s subtle interference colors can be a great clue, especially when combined with its pleochroism and relief. Do not overlook the details.
