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6cm x 5cm x 8cm Carnelian is a part of the Chalcedony family. It is formed when two silica minerals with different crystal structures grow together such as quartz and moganite. The firey orange and red colors come from iron oxides in the mineral. Carnelian can be found in Brazil, India, and Uruguay. ***Due to natural variations in stones, the appearance will vary***
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13.5cm Tall Ocean jasper is a rare and colorful material exclusively from Madagascar. It is described as a variety of Orbicular Jasper due to its orb-like inclusions. Ocean jasper is a name for what is known to be a spherulitic chalcedony which is a cryptocrystalline variety of quartz. Cryptocrystalline is a term that means its crystals are too small to be seen with the naked eye. ***Due to natural variations in stones, appearance will vary***
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6cm x 4cm x 10cm Agate is a translucent form of microcrystalline quartz. These crystals form inside of igneous rocks over a long period of time and get their banding from years of siliceous groundwater building up in the cavities of these rocks. What makes this mineral so beautiful and unique is that the color variations and banding patterns are completely dependent on the environmental factors around them. This makes it so that every formation is different and there are no two formations that are the same! ***Due to natural variations in stones, the appearance will vary***
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50mm 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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60mm 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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8 x 8 x 9cm Calcite is a mineral when originally formed is colorless and opaque and can come in many different forms of translucency. It gets its beautiful colors and banding from impurities in the rocks the specimen is formed in. Calcite gets its name from the water within the mineral being rich in calcium. This soft mineral can be found all over the world; mainly in shallow marine settings such as hydrothermal veins and hot spring deposits. Many marine life species, such as crabs and coral, rely on calcite to form their shells. ***Due to natural variations in stones, the appearance will vary***
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8cm Wide Carnelian is a part of the Chalcedony family. It is formed when two silica minerals with different crystal structures grow together such as quartz and moganite. The fiery orange and red colors come from iron oxides in the mineral. Carnelian can be found in Brazil, India, and Uruguay. ***Due to natural variations in stones, the appearance will vary***
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5cm x 4.5cm x 7.5cm 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". ***Due to natural variations in stones, the appearance will vary***
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5cm x 5cm x 6cm Agate is a translucent form of microcrystalline quartz. These crystals form inside of igneous rocks over a long period of time and get their banding from years of siliceous groundwater building up in the cavities of these rocks. What makes this mineral so beautiful and unique is that the color variations and banding patterns are completely dependent on the environmental factors around them. This makes it so that every formation is different and there are no two formations that are the same! ***Due to natural variations in stones, the appearance will vary***
Shopwiredadmin2022-06-04T21:06:27-04:00
