Amethyst: Geological Identity
Amethyst is part of the quartz family, one of the most common and abundant minerals on Earth. Its purple color comes from trace amounts of iron and natural irradiation that occur as the crystal forms. The deeper the purple, the higher the iron content or the greater the exposure to heat and light over time.
You’ll find Amethyst in geodes, clusters, and points that form in volcanic rock cavities when mineral-rich water cools slowly. Over thousands of years, these crystals grow layer by layer, creating the rich variety of shapes and shades we see today, from pale lavender to deep violet.
Major sources of Amethyst include Brazil, Uruguay, South Korea, Russia, and parts of North America. Each region’s environment gives its crystals slightly different hues and formations. For example, Brazilian Amethyst often has a soft, glowing purple tone, while stones from Uruguay are darker and more saturated.
Geologically, Amethyst reminds us that beauty often forms through pressure and time. It is a crystal shaped by the Earth’s movement, minerals, and heat, a natural record of transformation and patience.
🪶 Reflection Prompt: When you think about Amethyst forming deep within the Earth over thousands of years, what does that say about your own growth and the time it takes to transform?
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Dana Polledo
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Amethyst: Geological Identity
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