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A polygenetic landform is a topographic feature shaped by multiple geomorphic processes over time. These processes can include tectonic movements, such as uplift and subsidence, as well as denudational processes like weathering, erosion, and deposition. Climate plays a significant role in determining the character of these denudational processes, leading to varied expressions such as forests, deserts, or glacial landscapes.12

Most landforms on Earth are polygenetic, meaning they are a result of a combination of these forces. For instance, a mountain range formed by tectonic uplift might be subsequently shaped by glacial erosion and river valleys. This interplay between internal Earth forces and external environmental factors creates the diverse and complex landforms we observe.3412

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