Fluorite Root Point Crystal Tower
3”
68g
💎
Fluorite is a mineral known for its wide range of colors and often forms beautiful crystals with various geometric shapes.
•
Fluorite comes in a spectrum of colors, including purple, green, blue, yellow, pink, and more. The colors are often vibrant and can even appear in multiple bands within a single crystal.
•
The crystal structure of fluorite is typically cubic, but it can also form octahedral or dodecahedral crystals. Cleavage in fluorite is well-defined, and it often forms transparent to translucent crystals.
•
Fluorite can range from transparent to translucent, allowing light to pass through, showcasing its internal coloration.
•
Some fluorite specimens exhibit fluorescence under ultraviolet (UV) light. This property is one reason why fluorite is sometimes referred to as the “most colorful mineral in the world.”
•
Fluorite is found in various geological environments, including hydrothermal veins, sedimentary rocks, and as a gangue mineral in ore deposits. Significant deposits are located in China, Mexico, Mongolia, and other regions.
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3”
68g
💎
Fluorite is a mineral known for its wide range of colors and often forms beautiful crystals with various geometric shapes.
•
Fluorite comes in a spectrum of colors, including purple, green, blue, yellow, pink, and more. The colors are often vibrant and can even appear in multiple bands within a single crystal.
•
The crystal structure of fluorite is typically cubic, but it can also form octahedral or dodecahedral crystals. Cleavage in fluorite is well-defined, and it often forms transparent to translucent crystals.
•
Fluorite can range from transparent to translucent, allowing light to pass through, showcasing its internal coloration.
•
Some fluorite specimens exhibit fluorescence under ultraviolet (UV) light. This property is one reason why fluorite is sometimes referred to as the “most colorful mineral in the world.”
•
Fluorite is found in various geological environments, including hydrothermal veins, sedimentary rocks, and as a gangue mineral in ore deposits. Significant deposits are located in China, Mexico, Mongolia, and other regions.
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