- Geomorphology
- the systematic description and analysis of landforms and the processes that create/modify them
- Landform
- an element of the landscape that can be observed in its entirety and has consistence of form
- Landscape
- earth surfaces composed of an assemblage of subjectively defined, lesser surfaces
- Geomorphic system
- a set of related landforms and processes, usually defined in terms of a dominant agent of geomorphic activity (water, gravity, ice, wind, waves, or organisms)
BASIC CONCEPTS AND APPROACHES
- Physical geomorphology
- explanatory description, analysis of process mechanics, modelling, geological and engineering oriented
- Environmental geomorphology
- regional description, geographical, relationship of unique landscapes to environmental variables
- Climatic geomorphology
- regional landscapes (morphogenic regions) are related to distinctive climates and geomorphic processes
- Climatogenetic geomorphology
- recognizing successive periods of relief development; explaining historical development of landscapes in terms of past and present processes
- Quantitative and process geomorphology
- focus on rates and mechanics of contemporary exogenous processes, experimentation, and the evolving modern landscape
- Theoretical geomorphology
- mathematical expression of processes; deduction of form and landscape evolution from physical principles
STRUCTURE, PROCESS AND TIME
- Structure
- the physical and chemical properties of rocks and sediments, the geological framework, determines resistance to forces generated by geomorphic agents
- Process
- a distinctive mechanism for the transfer of rock and sediment, and thereby the creation of modification of landforms; represent a force acting on the landscape (work) in response to the availability of energy (solar, gravitational, molecular and geothermal)
- Time
- the interval over which driving and resisting forces interact to alter the landscape to a definable extent (stage)
- Frequency and magnitude of geomorphic processes
- which processes do the most work, high frequency/low magnitude (quasi-continuous) or low frequency/high magnitude (discrete, episodic); uniformitarianism versus catastrophism
- Geomorphic thresholds
- limits of equilibrium states, the landscape does not yield continuously and stresses do not act continuously
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