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Compressional stress leads to the formation of reverse faults, small-scale mountain building, anticlines, and synclines.
Compressional stress results in transpressional features with reverse faults and small-scale mountain building, such as the San Gabriel Mountains in California. This type of stress leads to the formation of anticlines and synclines. Anticlines are upturned folds with the oldest rocks at the center, while synclines are down turned folds with the youngest rocks at the center.
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