Geomorphology

'noun Geol. the scientific study of the nature and history of the landforms on the surface
of the Earth and other planets, and of the processes that create them.'

- Chambers Combined Dictionary Thesaurus (1997, Edinburgh)


  Geomorphology is an academic discipline. It attempts to explain features found and processes operating upon the surface of the earth. It is scientific in approach. Formal research in geomorphology is mostly carried out within the rational, empirical and analytical traditions of modern science. The approach includes information gathering in the field and testing of hypotheses. Efforts are taken to replicate and to generalise results. Other disciplines and human endeavours make use of the results of geomorphology.

Many universities teach
geomorphology (it is generally offered as a group of subjects). At schools in Australia it is usually covered as a part of geography, although aspects of landform studies are often included in geology, a branch of science. Perhaps geomorphology could best be regarded as a disciplinary 'bridge' (i.e. link) between geography and geology.

While geomorphology is primarily concerned with landforms and their processes of change, in a broader sense it is important to see that there is an environmental conservation imperative shared between geomorphology, geology and soil studies. The approach of looking to reserve, preserve and conserve representative elements of bedrock, landform and soil is now referred to as geoconservation. Reasons for doing so go beyond economic forces such as ecotourism benefit, and include arguments of 'intrinsic worth'. This approach is well explained in a series of articles on geoconservation produced by the Tasmanian Government.  

 
 


The detailed field sites examined in Matthew FLINDERS & the Coastal LANDFORMS of SE Australia
are found along or near the coast of southeastern Australia (Spencer Gulf, SA, to Bargara Beach, Qld).
While the majority of sites illustrate coastal geomorphic processes, some coastal and near-coastal
sites included are primarily the result of other processes (eg. volcanic and glacial) - they have been
included for interest and as their locations place them where they were visited/charted/passed by
Matthew Flinders on at least one of his expeditions.


Matthew Flinders & Landform Study

 
 

 

 



Main
Page


C.Grant  2002, 2003