Geomorphology refers to the study of the Earth's surface and the processes in which it is shaped, both in the present and in the past. Geomorphology has many sub-topics that refer to specific locations or areas of similar geomorphology. For instance, geomorphology in arid environments such as near the Tropics (of Capricorn and Cancer). The underlying features of all the sub-topics is that they contain similar core principles, which are most likely to be climatic or tectonic processes.
Geomorphology is studied under a number of different titles- most notably Physical Geography, but it can also be practised under the larger topics of archaeology or geology. The wide base of interest results in varying research methods, as well as different conclusions from the results of data collection.
They often aim to predict future changes in the Earth's surface through a number of methods including field observations, physical experiments and numerical observations. The latter known as Geomorphometry.
Such processes that may be included within the Geomorphology field include eolian processes such as wind erosion or fluvial erosion such as corrosion.
We should end with the name of a notable geomorphologist, William Morris Davis, who has been dubbed 'the father of American Geography' and he paid important attention to geomorphology as a key aspect to his research of Physical Geography. Thus proving the importance of this sub-field to the discipline as a whole.
References:
'International Conference Of Geomorphology', Europa Organisation.
Tinkler, Heith J. A short history of geomorphology. Page 4. 1985
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