highly variable Chalcedony spheres are almost geode-like in appearance and one can clearly see the process of geode or agate formation in progress in each specimen
These high quality and exceptional color Chiapan Amber originated in Mexico during the Oligocene
and is one of the more common gems although pieces of exceptional hue and clarity are considered fairly rare and can be extremely valuable
The spectacular display of colors these specimens display can be formed by two different geological processes: the oxidation of pyrite causing ultra-thin layers of iron oxide to form on the surface
or the formation of equally thin layers of secondary minerals due to hydrothermal or other alteration
Fluorite Cubes on Matrix Tanzanite highly variable Chalcedony spheres areFluorite is one of the most variable of all crystalline minerals, occurring in shades of blue, green, purple, red and many other colors corresponding to their physical makeup and conditions when the mineral was formed. The name fluorite comes from its use as a flux, or chemical cleaning agent, in iron smelting and other metallurgy. Pure fluorite is clear, but most specimens have vivid color due to various impurities and are often fluorescent. With a