Steven Dutch, Professor Emeritus, Natural and Applied Sciences, Universityof Wisconsin - Green Bay
High relief. Can occur as colorless irregular grains (A) or be tinted yellowish orgreenish (B). Common alteration or metamorphic mineral derived from plagioclase, and smalleuhedral crystals in plagioclase are common (C).
Piemontite, an uncommon manganese-bearing epidote, is one of the showpieces ofgeology. It has a dazzling pleochroism in yellow, orange, red and magenta (D). It cannotbe mistaken for anything else.
Moderately high birefringence resulting in vivid second- and third- order colors.Anomalous interference colors are common in the variety zoisite (A). Piemontite'sbright colors totally dominate its interference colors.
The euhedral light-green crystals below, seen in plane-polarized light, are epidote.Note the rather high relief.
Same field in crossed polarizers. The bright interference colors are typical.
The brightly-colored mass in the center of this view in crossed polarizers is epidote.Variegated bright interference colors like these are typical of epidote.
Created 10 Oct 1997, Last Update 16 December 1999