“Epidote is a very typical and common regional mineral in the Western Gneiss Region of Norway and is often seen as a green colored fissure mineralization, like in the photo. From a small quarry, now overgrown, at Kjerringholmen, Runde, Møre og Romsdal, Norway. A closer look will sometimes, as here, reveal small cavities with microcrystals of epidote Photo taken 28.07.2020 ”