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5 x 2 x 6cm 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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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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4cm - 5cm 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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45mm - 50mm 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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30mm 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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4 x 1 x 5cm 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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4 x 2 x 6cm Celestite is a mineral consisting of strontium sulfate. The mineral is named for its periwinkle blue color. Celestite and the carbonate mineral strontianite are the main sources of the element strontium which is commonly used in fireworks and in various metal alloys. This mineral is found in Madagascar and Sicily, Italy. ***Due to natural variations in stones, appearance will vary***
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6cm - 7cm Chocolate calcite is a calcium carbonate mineral. It gets its name from its milky, chocolately appearance that comes from the different hues and banding. This mineral is often referred to as brown aragonite as they are both very similar in composition. Chocolate calcite can be found in calcium-rich environments. ***Due to natural variations in stones, the appearance will vary***
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6cm - 7cm Wide Clear quartz is made of Silicon dioxide and is one of Earth's hardest minerals on the Moh's hardness scale. It is found mixed in many types of minerals and also in bedrock, sand, and gravel. Quartz is naturally clear and opaque but can be found in many other colors. This mineral Earth's most abundant crystal and can be found in many different places but mostly in the Alps, Madagascar, and Brazil. ***Due to natural variations in stones, the appearance will vary***
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10cm - 11cm Tall 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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9cm Tall 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
