Tectonic uplift is the geological process where sections of the Earth's crust are raised due to tectonic forces, primarily from the movement of the Earth's tectonic plates. This phenomenon often occurs at convergent boundaries, where plates collide, resulting in mountain formation and increased elevation. The interplay between isostasy and tectonic uplift helps shape the topography of the Earth, reflecting both ongoing tectonic activity and the response of the crust to changes in weight and pressure.
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