Further research concerned with possible correlation between type and color of mica and intensity of color of associated kyanite, as previously outlined by the writer (Dietrich, 1956), has been postponed indefinitely because of a shift in research objectives. The following data derived from already completed studies of chromium-bearing muscovite (“fuchsite”) from Baker Mountain, Prince Edward County, Virginia, are presented here because it is believed that possibly other workers may find them of value.

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