In Cyprus I saw sheeted dikes which were sometimes more or less greenish in color. It is mineral epidote that gives them this bright green tone.
Some dikes are almost apple-green which indicates that they are composed mostly of epidote and quartz. Original mafic minerals are completely replaced.
Weathered slope of an epidositic roadcut. I got a nice green sand sample for my sand collection from this place.
Greenest epidosite sample I found. The specimen is about 10 cm in width.
Epidosite is not an uncommon rock in certain conditions although it seems to me that its formation details are generally not well known. I’ve written about massive pyrite and umber which are characteristic rocks of complete ophiolites (like the Troodos Ophiolite in Cyprus). These rocks are enriched in metals (copper, zinc, manganese). Epidosite, on the other hand, is very much depleted in these elements although they are present in mafic dikes (parent rock of epidosite).
It seems logical to assume that seawater that circulates in the oceanic crust near the spreading zones heats up and alters the dikes by turning them into epidosite. By doing that it carries away not only metals but also sodium and magnesium and leaves behind rocks enriched in calcium and silicon. Hence, epidosite is an important piece of puzzle which helps to understand where is this material coming from that is carried to the seafloor by hydrothermal vents called black smokers.