When tectonic plates meet, the intense pressure and stress can cause the rock layers at the boundaries to bend and deform. This bending can lead to the formation of folds, such as anticlines and synclines, in the Earth's crust. Additionally, if the stress exceeds the rock's strength, it may result in fractures or faults. These geological processes play a crucial role in shaping the Earth's landscape and are often associated with seismic activity.
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