In scientific topics, uplift generally refers to the vertical elevation of Earth’s surface relative to a reference level, driven by tectonic, isostatic, or magmatic processes. Tectonic uplift occurs along convergent or transform boundaries through crustal shortening, faulting, and folding, whereas isostatic uplift reflects lithospheric adjustment to loading changes such as glaciation, erosion, or sedimentation. Uplift is quantified using geodetic measurements (e.g., GPS, InSAR), geomorphic markers (terraces, raised shorelines), and thermochronology to infer rates and timing. It plays a central role in mountain building, landscape evolution, crustal deformation studies, and coupling between tectonics, climate, and surface processes.