geomorphology represent a significant movement away from classical geomorphology, which is concerned mostly with the evolutionary development of landforms.
Geomorphological phenomena depend on many different processes that operate on the surface of the planet, so the geomorphologist needs to integrate hydrology, climate, sedimentology, geology, forestry, pedology, and many other sciences. This type of research has relevant applications to everyday life—for example, the decomposition of bedrock and the development of soils relate to global climate systems and also can help local engineers solve problems such as determining slope stability for construction sites. other geomorphologists may study the development and evolution of drainage basins, along with the analysis of fluvial landforms such as flood-plains, terraces, and deltas. Desert geomorphology is concerned with the development of desert land-forms and climate, whereas glacial geomorphology analyzes the causes and effects of the movement of glaciers. Coastal processes including erosion, deposition, and longshore movement of sand are treated by coastal geomorphologists, whereas the development of various other types of landforms, such as karst, alpine, seafloor, and other terrains are treated by other specialists.
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