In geography, folding refers to the bending and warping of rock layers due to tectonic forces. The stages of folding typically include the initial buildup of stress, leading to the formation of anticlines (upward folds) and synclines (downward folds). As stress continues, the rock layers may undergo further deformation, creating complex structures like domes and basins. Ultimately, if the stress exceeds the rock's elastic limit, it may lead to fracturing or faulting.
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