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Rose Quartz is an anhedral crystal. It is found in the cores of pegmatites and gets its color from microscopic inclusions of a pink variety of the mineral dumortierite . Rose Quartz is naturally a pink hue but can have more hues of grey/purple or red. This mineral Earth's can be found in many places including South Africa, Madagascar, and Brazil.
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Rose Quartz is an anhedral crystal. It is found in the cores of pegmatites and gets its color from microscopic inclusions of a pink variety of the mineral dumortierite . Rose Quartz is naturally a pink hue but can have more hues of grey/purple or red. This mineral Earth's can be found in many places including South Africa, Madagascar, and Brazil.
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Sardonyx is a chalcedony crystal who's banding is formed when Silica-rich waters seep into cracks in rocks at low temperatures. Quartz then grows from the deposited silica. These crystals vary in color from a light orange/red to a dark brown color. These crystals are usually found near volcanic activity; In Brazil, India, Germany, Madagascar, and in the US.
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Sardonyx is a chalcedony crystal who's banding is formed when Silica-rich waters seep into cracks in rocks at low temperatures. Quartz then grows from the deposited silica. These crystals vary in color from a light orange/red to a dark brown color. These crystals are usually found near volcanic activity; In Brazil, India, Germany, Madagascar, and in the US.
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Sardonyx is a chalcedony crystal who's banding is formed when Silica-rich waters seep into cracks in rocks at low temperatures. Quartz then grows from the deposited silica. These crystals vary in color from a light orange/red to a dark brown color. These crystals are usually found near volcanic activity; In Brazil, India, Germany, Madagascar, and in the US.
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Serpentine is primarily composed of one or more of the three magnesium silicate minerals: lizardite, chrysotile, and antigorite. This mineral comes from the Earth's mantle which is just under the Earth's crust. This mineral is the state rock of California but can also be found in Russia, Greece, New Zealand, and many other places.
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Sodalite is a rare mineral formed inside igneous rocks crystalized as a result of sodium-rich magma. The blue color comes from the rock that Sodalite is formed in; nepheline syenite, trachyte, and phonolite. Although the sodalite-bearing rock is rare, it can most commonly be found in the US, Canada, and Africa.
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Stichtite is a secondary mineral that forms as a result of the interaction between Serpentine and chromium. This is a hyrdothermal interaction where the chromium and other fluids infiltrate the Serpentine and create Stichtite. This crystal is famously found in the Dundas mineral field in Tasmania, Australia.
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Labradorite is a type of feldspar that gets it's flashy colors from intergrowths within the mineral. Light then travels through these intergrowths and displays its beautiful colors. These colors can range from purples and blues to greens and yellows. This mineral gets its name from where it was originally discovered, in Labrador, Canada. This mineral was also found in Finland during WWII and was also known as "Falcon's Eye".
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Tiger's eye is a semiprecious stone that is formed when parallel veins of crocidolite fibers are first altered to iron oxides and then replaced by silica. As a result it is more opaque, and creates a rich yellow to brown color. Tiger Eye can be found in Australia, Burma, United States, Brazil, China, and many other countries.
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Sale!11cm Wide Fluorite is composed of fluorine and calcium and is formed in hydrothermal veins in the Earth's crust. This mineral can be found in all colors of the rainbow with different hues. The different colors in Fluorite are caused by impurities within the mineral. The deeper colors are found in well-formed crystals. Fluorite was originally discovered in Illinois in 1842 but is no longer mined in the US. It can be found in China, South Africa, Mongolia, France, and Russia. ***Due to natural variations in stones, the appearance will vary***
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