![]() ![]() Ammonites were cephalopods, that thrived in tropical seas until becoming extinct along with the dinosaurs at the end of the Mesozoic era. ![]() Significant deposits of gem-quality ammolite are only found in the Bearpaw Formation that extends from Alberta to Saskatchewan in Canada and south to Montana in the USA.Īmmolite comes from the fossil shells of the Upper Cretaceous disk-shaped ammonites Placenticeras meeki and Placenticeras intercalare, and (to a lesser degree) the cylindrical baculite, Baculites compressus. The iridescence is due to the microstructure of the aragonite: unlike most other gems, whose colors come from light absorption, the iridescent color of ammolite comes from interference with the light that rebounds from stacked layers of thin platelets that make up the aragonite. An iridescent opal-like play of color is shown in fine specimens, mostly in shades of green and red all the spectral colors are possible, however. Its hardness is 4.5–5.5, and its specific gravity is 2.60–2.85. The shell itself may contain a number of trace elements, including: aluminium barium chromium copper iron magnesium manganese strontium titanium and vanadium. The chemical composition of ammolite is variable, and aside from aragonite may include calcite, silica, pyrite, or other minerals. Rare Giant Natural Ammolite From Alberta, Canada. It is one of few biogenic gemstones others include amber and pearl. Giant, human-sized ammonites extinct relatives of cuttlefish and squid with coiled shells and tentacles lived on both sides of the Atlantic 80 million years ago. It is made of the fossilized shells of ammonites, which in turn are composed primarily of aragonite, the same mineral contained in nacre, with a microstructure inherited from the shell. Ammolite is an opal-like organic gemstone found primarily along the eastern slopes of the Rocky Mountains of North America.
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