Epidote
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“Monoclinic. Crystals are often much elongated parallel to the ortho-axis with a prominent development of the faces of the orthodome zone, giving them a prismatic aspect. Striated parallel to the ortho-axis. Terminated usually at one end of the ortho-axis and most commonly by the two faces of a pyramid.” — Ford, 1912
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William E. Ford Dana's Manual of Mineralogy (New York: John Wiley and Sons, Inc, 1912) 259
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