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ArtistEnhance!!! Any gold present in the rocks being heated and squeezed is sweated out and goes into solution as complex ions. In this form, dissolved gold, along with other elements such as silicon, iron and sulphur, migrates wherever fractures in the rocks allow the fluids to pass. This direction is generally upwards, to cooler regions at lower pressures nearer the Earth’s surface. Under these conditions, the gold eventually becomes insoluble and begins to crystallise.
A close-up shot of a glowing geological formation, featuring a dark gray rock with a rough and layered surface, supported by a vibrant, translucent yellow crystalline structure. The crystalline formation appears to emit an internal light, casting a warm glow and exhibiting a textured, almost stalactite-like appearance with individual crystals forming jagged, vertical spikes. Small amounts of a translucent, honey-colored liquid drip from the base of the formation into shallow, murky water below, suggesting a wet environment. The background is softly blurred, showing hints of similar glowing formations and water, indicating this is likely a cave or a natural, underground setting.