Geomorphology is the scientific discipline that investigates the origin, evolution, and spatial distribution of landforms and the processes that shape Earth’s surface across a range of temporal and spatial scales. It integrates principles from geology, hydrology, climatology, soil science, and geophysics to analyze fluvial, glacial, aeolian, coastal, tectonic, and mass-wasting processes. Quantitative geomorphology employs field measurements, remote sensing, numerical modeling, and geochronological techniques to constrain rates of erosion, sediment transport, and landscape adjustment, providing a mechanistic framework for understanding surface dynamics, surface–climate–tectonics interactions, and the development of topography on Earth and other planetary bodies.
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