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geomorphology: the study of landforms
1. Uniformitarianism
the present is the key to the past
2. W.M. Davis' Geographical Cycle
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3. Process Geomorphology
J.W. Powell
G.K. Gilbert
1. Process geomorphology & systems analysis
2. Applied geomorphology
3. Quantification in geomorphology
1. Equilibrium
driving framework: climate, gravity & internal heat
resisting framework: lithology & geologic structure
equilibrium
results from balance between driving and resisting forces
implies landforms exist in an unchanging condition
form remains constant provided fundamental controls don't change
2. Thresholds: the limits of equilibrium
what is temporary disequilibrium & what is geomorphologically significant disequilibrium?
complex responses
3. Equilibrium and time
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definition of equilibrium is time dependent
static equilibrium: landforms truly don't change (hours, days, months)
steady-state equilibrium: changes occur, but system maintains a constant average condition (100s to 1000s of years)
dynamic equilibrium: system changes progressively (millions of years)
4. Systems approach
a. morphological systems
b. cascading systems
c. process-response systems
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©
K.A. Lemke
(klemke@uwsp.edu)
Last modified September 6, 2006 |