Amazonite, also called amazonstone, is a type of microcline feldspar which is translucent to opaque blue-green in color. It was named in 1847 by Johann Friedrich August Breithaupt. Even though the name implies a locality close to the Amazon, no deposits have yet been found nearby. Instead, it has been found in Ontario, Quebec, Italy, Russia, and Colorado. The color comes from traces of lead, not copper.
Teredo-bored petrified wood is North Dakota’s state fossil. It is found in 60 million year old Paleocene deposits, found in the southwestern area of the state. These are areas that were covered by the Cannonball Sea, now exposed at the surface. Before fossilizing, it was drift wood (ginkgo, bald cypress, metasequoia, etc.) that had been drilled (bored) into by small worm-like clams (Teredo), creating a Swiss-cheese effect.
Part of the fossilization included filling the borings with sediment or crystals, often seen as a different color or texture. If slabbed, the tiny clams can even be seen in cross section as little white crescents. The clams, also called shipworms, still pose a problem for wooden boats or docks today.
Teredo-bored petrified wood was adopted in 1967, and added to the Smithsonian Institution’s mineral collection. The selection was brought to the legislature by R. W. Carlson of Bismarck, former present of the Central Dakota Gem and Mineral Society, and H. A. Brady of Mandan. State Represenative W. G. Sanstead of Minot proposed the state fossil selection in House Bill 933.
https://www.dmr.nd.gov/ndgs/outofprint/NewsLetters/1993Spring.pdf (publication page 4 & 5)
Gold is an element (atomic number 79), rather than a rock or mineral. A precious metal used in coins, jewelry, and more recently electronics, it has been coveted by humans for thousands of years. On the periodic table, gold is written as “Au”, which comes from the Latin word for gold: aurum. It is highly malleable, and can be beaten into thin sheets of leaf for artistic purposes such as illumination, or as a protective coating in industry. It is
often alloyed with copper or nickel, but in its pure state is non-reactive and does not tarnish upon exposure to air. By adding copper a more red color is achieved (rose gold). Blue with iron, purple with aluminum, and white with palladium, silver, or nickel. Along with the more obvious nuggets, gold is often found naturally as dust or flakes, embedded in rock or quartz.
Rhodochrosite is a translucent to transparent, ranging in colors from white, to pink, to red. It is a manganese carbonate, found in hydrothermal veins alongside copper, silver, and lead, and can be used as a manganese ore. When exposed to air, rhodochrosite tends to form a dark rind as it oxidizes. It is generally a massive, nodular, or botryoidal form, however the rare transparent rhombohedral crystals can also be found. It has a hardness of 3.5-4 on the Mohs scale, has a white streak, and is soluble in warm hydrochloric acid. Due to its soft nature, and beautiful commonly banded colors, this mineral is often used as a carving medium, but rarely faceted. Its chemical composition is MnCO3. Its name comes from Greek, literally meaning rose-colored.
Pellant, Chris. Rocks And Minerals. New York, Dorling Kindersley, Inc., 2000. Pg 100.
Busbey III, Arthur B. Rocks & Fossils. Time Life Books, 1997. Pg 170.
Ammolite is both fossil and gemstone. It comes from the aragonite mother-of-pearl surrounding ammonites – jokingly called “grandmother-pearl”. Many ammonites still exhibit an iridescent sheen to them, however the ones from mines in southern Alberta exhibit a rainbow spectrum of gem-quality colors. Aragonite in life is an unstable organic crystal form of carbonate, and generally when a shell fossilizes, as it’s already a mineral, simply reverts to a more stable form of calcite. With Ammolite, the aragonite layers haven’t reverted – and the more layers there are, the more colors are refracted.
It was given gem status in 1981 by the World Jewelry Confederation. It is one of three organic gemstones – the other two being amber and pearls. If used in jewelry, because of the soft nature of the stone (only a 3.5-4 on the Mohs scale), it should only be set in earrings or pendants – not rings.
Group: Halide. Chemical formula is CaF2.
Fluorite is a translucent mineral that covers a rainbow of colors, yet has a clear streak. The crystal structure is cubic to octahedral, often with twinning. Like chalcopyrite, fluorite is found in hydrothermic veins, and hot springs, often alongside sulfides. It is fluorescent under ultraviolet light.
The mineral has been used as lenses in telescopes and microscopes, a flux for smelting, and even as a source of fluoride for hydrofluoric acid. It was named in 1797 by Carlo Antonio Geleani Napione, from Latin – “fluor” meaning stream, or to flow – for its use as a flux. Fluorspar is also a common name. Fluorite is also used in carving and jewelry, however with a hardness of 4 on the Mohs scale, heavy wear is not recommended.
Pellant, Chris. Rocks And Minerals. New York, Dorling Kindersley, Inc., 2000. Pg 74.
Chalcopyrite is a brassy-colored, copper iron sulfide. It was named by Johann Friedrich Henckel in 1725, from the Greek “chalkos” meaning copper, and “pyrites” meaning to strike fire. It has a green-black streak, yet tarnishes in a variety of iridescent purple, blue, and red. It sometimes goes by the term “peacock rock”. It is often mistaken for pyrite, but is a softer 3.5-4 on the Mohs scale. It is brittle, and can shatter if struck. It has poor cleavage, and fractures unevenly. It can be found in tetragonal crystal form, massive, and even botryoidal.
This mineral has been mined as a copper ore for thousands of years. Copper mixed with zinc creates brass, but mixed with tin creates bronze – a metal used in tools for ages. It is very common in sulfide veins, high-temperature hydrothermal veins, igneous dikes, and more. When oxidized, or weathered, chalcopyrite may form malachite, azurite, cuprite, and other minerals.
Group: Sulfide. The chemical formula is CuFeS2.
Klein, Cornelis and Cornelius S. Hurlbut, Jr., Manual of Mineralogy, Wiley, 20th ed., 1985, pp. 277 – 278
Discovered in 1967 in Tanzania, tanzanite (named by Tiffany & Co.) is one of the more recent birthstones for December (as of 2002, via the American Gem Trade Association). While the stone may be light violet in some cases, darker shades of periwinkle with hints of purple are sought after for higher gem quality. A blue variety of the gemstone zoisite, tanzanite has a Mohs harness of 6.5-7 – not particularly tough for a gemstone. Corundum (rubies and sapphires) sit at a healthy 9.0 on the Mohs scale.
The blue color is caused by trace amounts of vanadium within the ziosite – much like trace elements can also cause various colors of diamonds. The blue can be enhanced and brought out in the stone by careful addition of heat. Tanzanite crystals are also pleochroic – meaning from different angles they exhibit different colors. The same crystal from one direction may look blue, and another direction look red or brown – thus faceting the stone can be challenging.
The chemical composition of tanzanite is: Ca2Al3(SiO4)3(OH)
Newman, Renee. Exotic Gems: How to Identify and Buy Tanzanite, Ammolite, Rhodochrosite, Zultanite, Moonstone & Other Feldspars. International Jewelry Publications, 2010.