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Willow Spring is actually the result of Karst topography which is common for the North Georgia mountains. Springs may be formed in any sort of rock. Small springs are found in many places. In North Georgia, the largest springs are formed in limestone and dolomite in the karst topography of the Southern Appalachian Mountains. Both dolomite and limestone fracture relatively easily. When weak carbonic acid (formed by rainwater percolating through organic matter in the soil) enters these fractures it dissolves bedrock. When it reaches a horizontal crack or a layer of non-dissolving rock such as sandstone or shale, it begins to cut sideways, forming an underground stream. As the process continues, the water hollows out more rock, eventually admitting an airspace, at which point the spring stream can be considered a cave. This process is supposed to take tens to hundreds of thousands of years to complete.
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