Siderite and Sphalerite epimorphs after Calcite

Item Description

Outstanding pseudomorph of Siderite and Sphalerite replacing the original Calcite. The variety of replacement is an epimorph, where the later minerals have formed over and then casted the original crystal, which has now vanished and dissolved away leaving the hollow shell intact. The form is superb, and the color variations between terminations and faces, as well as the metallic luster on some of the crystals, creates a visual splendor and presence not often seen in something non-gemmy - especially in pseudomorphs! For the size, about the best you can ask for! These three crystals, the longest of which is about 4.5 cm long, are intergrown and sit nicely on matrix. There is good individuality, yet the cluster itself has good balance and great visual interest. Very aesthetic.