XX066 - Fluorite, Quartz with intermittent Phantoms Uruguay imprinting left over from early

imprinting left over from early generation Quartz

This phenomenon of delayed luminescence is powered by the radiative decay of its molecular triplet state

with multiple small faces on the surface

Locality: Peña Blanca Mine

but it has been theorized that it could be due to the underlying silica fossils

XX066 - Fluorite, Quartz with intermittent Phantoms Uruguay imprinting left over from earlyCluster of green stepped Fluorite in skeletal growth, forming an octahedral habit. The phantoms exhibited shows blue bandings intersecting at the Fluorite's tip in straight 90 degree angles, forming a cross. On the Fluorite tip, purple phantoms in spotty shapes can be observed. Accompanying the Fluorites are Quartz pointers with an unknown green coating, possibly Chlorite. The Fluorites show a milky white fluorescence under 395nm, and green under