Roger Weller, geology instructor
email@example.com copyright 2010-R.Weller
epidote as slickensides-1
Huachuca Mountains, southeastern Arizona
In this specimen, epidote replaced the minerals in the fault-produced slickenside
structure. The massive epidote displays its typical peas soup green color.
Photo is copyright free only for non-commercial educational uses.
Just credit photo to R.Weller/Cochise College.