Page 20 - Fundamentals of Geomorphology
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                          WHAT IS GEOMORPHOLOGY?




















              Geomorphology is the study of landforms and the processes that create them. This chapter covers:


                  historical, process, applied, and other geomorphologies
                  the form of the land
                  land-forming processes and geomorphic systems
                  the history of landforms
                  methodological isms




              INTRODUCING GEOMORPHOLOGY                 to major tectonic plates, and their ‘lifespans’ range from
                                                        days to millennia to aeons (Figure 1.1).
              The word geomorphology derives from three Greek  Geomorphology was first used as a term to describe the
                                                        morphology of the Earth’s surface in the 1870s and 1880s
              words: gew (the Earth), morfh (form), and logoV
              (discourse). Geomorphology is therefore ‘a discourse on  (e.g. de Margerie 1886, 315). It was originally defined as
              Earth forms’. It is the study of Earth’s physical land-  ‘the genetic study of topographic forms’ (McGee 1888,
              surface features, its landforms – rivers, hills, plains,  547), and was used in popular parlance by 1896. Despite
              beaches, sand dunes, and myriad others. Some work-  the modern acquisition of its name, geomorphology is a
              ers include submarine landforms within the scope of  venerable discipline (Box 1.1). It investigates landforms
              geomorphology. And some would add the landforms of  and the processes that fashion them. A large corpus of
              other terrestrial-type planets and satellites in the Solar  geomorphologists expends much sweat in researching
              System – Mars, the Moon, Venus, and so on. Landforms  relationships between landforms and the processes act-
              are conspicuous features of the Earth and occur every-  ing on them now. These are the process or functional
              where. They range in size from molehills to mountains  geomorphologists. Many geomorphic processes affect,
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