Obsidian is formed from rapidly cooled volcanic lava that solidifies before crystals can develop. As the molten rock cools quickly, the ions within it become randomly distributed, leading to a glassy texture without a crystalline structure. This rapid cooling occurs during volcanic eruptions or lava flows when the lava is exposed to air or water, preventing the orderly arrangement of atoms typical of crystalline minerals. The result is a natural glass that is typically dark in color and has a smooth, shiny surface.
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