Siderite and Sphalerite Epimorphs after Calcite

Item Description

Superb pseudomorph of a combination 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 fantastic, and the slight color variations between terminations and faces, as well as the near-metallic luster on all of the crystals, creates a visual splendor and presence not often seen in something non-gemmy - especially in pseudomorphs! This reminds one of the great oldtime, Hemimorphite pseudomorphs from Missouri, but with sharper crystals yet. The largest crystal in this magnificent plate is an amazing 5.2 cm long, and they are nearly all complete. A fabulous specimen, dramatic in appearance and aesthetic when displayed either horizontally or vertically, from a major find. In my opinion, one of the best I have seen for overall composition.