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Formation and Structure of Landforms
The collision, separation, sliding of tectonic plates, and magmatic activity directly convert underground energy into surface features such as elevations and depressions, fault zones, fold belts, mountains, and basins through mechanical processes like compression, tension, and shearing. Different types of plate boundaries often correspond to different landform products: at convergent boundaries, continental plates push against each other, producing folds and continental upheaval, resulting in a landscape where high mountain ranges coexist with deep basins; at divergent boundaries, plates move apart, thinning and fracturing the crust, forming vast basins and rift valleys; at transform boundaries, plates slide horizontally, and the displaced fault zones divide the region into alternating highlands and lowlands.

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