Ammolite is a shimmering material that is both fossil and gemstone. It is a unique geologic stone that is found almost exclusively in the Bearpaw Formation in Alberta, Canada.

As you may be able to tell from the name, Ammolite is formed from the fossils of ammonite cephalopods. Like other mollusks, the shells of ammonites had an inner layer known as the nacre or "mother of pearl". The nacre is rich in aragonite, a crystal form of calcium carbonate, which produces an iridescent sheen.

Over tens of millions of years, aragonite tends to convert to calcite, the most stable form of calcium carbonate. However, in the Bearpaw Formation, the fossils have undergone a unique process of mineralization that both preserved and intensified the natural aragonite resulting in a colorful gemstone we call Ammolite.

This pendant is made from a piece of iridescent ammolite form the Bearpaw Formation in Alberta, Canada. These brilliant necklaces shine in a rainbow of different colors: greens, reds, blues, yellows, and oranges can all be found in the material.

The true spectrum is revealed as you move the piece through the light, making it an incredibly dynamic piece of jewelry.

Each pendant is set into a sterling silver backing and comes with an 18" chain. Pendants are also shipped with an informational card which serves as certificate of authenticity. All our currently available ammolite pendants are available in the collection below.

ESTIMATED AGE : c. 110,000,000 years old

Ammonites are an extinct group of cephalopods which entered the fossil record 400 million years ago. They survived several mass extinction events, including the Permian–Triassic "Great Dying" which wiped out 96% of all marine species. They finally succumbed during the Cretaceous-Paleogene extinction event 66 million years ago, which also wiped out the dinosaurs.

The size of ammonite shells range from sub-centimeter dwarf species to giants nearly three meters in diameter. Most iconic shells exhibit a nearly perfect logarithmic spiral.

How these creatures lived is of intense interest to science as ammonites likely played a vital role in the food chain in the ancient seas.  Evidence exists to suggest that ammonites were a prime food source for Mosasaurs and fishes, while other studies suggest the "bite marks" were created after death by limpets or even by other cephalopods.

The Late Cretaceous was a time during which the interior of North America was covered by the Western Interior Seaway which extended from the Arctic Ocean to the Gulf of Mexico. As mountains rose in the west, they were eroded, and rivers draining eastward deposited their sediments into this interior sea some 70 - 75 million years ago. 

These waters teamed with life, particularly Cretaceous ammonites, including the most common fossils: Placenticeras meeki and P. intercalare. Both of these species are important sources of Ammolite.

Today these predominantly dark-colored marine shales form the Bearpaw Formation of southern Alberta. Interspersed between layers of shale, silt and fine sand are specific layers containing concretions. These are formed as sediment surrounding a nucleus, such as an ammonite shell, are cemented by the eventual precipitation of calcium carbonate. The vast majority of commercial Ammolite is derived from such concretions. 

The Ammolite gemstone is formed as a result of alterations undergone by sediment following deposition, a process known as diagenesis. During this lengthy 70 million year process the aragonite of the ammonite shell was not converted to calcite as would be expected; the latter being the more stable form of calcium carbonate.

How these creatures lived is of intense interest to science, as ammonites likely played a vital role in the food chain in the ancient seas. Evidence exists to suggest that ammonites were a prime food source for Mosasaurs and fishes, while other studies suggest the bite marks on their remains were created after death by limpets or even by other cephalopods.

Many thousands of distinct species make up the long-lived ammonoid subclass.  Though most ammonite shells are the classic spiral, there are also straight and gastropod-like shells and even some shells that are partially uncoiled.  The surface of the shells also vary quite widely, from smooth to wildly thorny.

Ammonites were an incredibly diverse and plentiful group of animals that survived for hundreds of millions of years and lived all across the planet. Their rapid diversification and tough, rocky shells means there are many different and easily identifiable species in the fossil record. Because of this, scientists can use them to easily identify the age of other fossils and geologic deposits found in the same layer of the ammonites. They're a welcome sight to the eyes of any inquisitive geologist!

Aside from their complex shells, there is little direct evidence regarding the appearance of ammonites due to the absence of soft tissue fossils. However, many scientists believe ammonites had bodies similar to that of the present-day Nautilus.

Ammonite shells grew in a natural spiral and made a consistent, mathematically significant pattern. This special shape is known as a logarithmic spiral.

The main property of a logarithmic spiral is that the shape of the spiral is unaltered as it increases in size. Each turn is a pure geometrical progression of the last with a common ratio.  This form is found in many natural phenomena, from the shape of galaxies to patterns on sunflower heads.