On steady states in mountain belts

@article{Willett2002OnSS,
  title={On steady states in mountain belts},
  author={S. Willett and M. Brandon},
  journal={Geology},
  year={2002},
  volume={30},
  pages={175-178}
}
  • S. Willett, M. Brandon
  • Published 2002
  • Geology
  • Geology
  • The dynamic system of tectonics and erosion contains important feedback mechanisms such that orogenic systems tend toward a steady state. This concept is often invoked, but the nature of the steady state is commonly not specified. We identify four types of steady state that characterize the orogenic system and illustrate these cases by using numerical-model results and natural examples. These types are (1) flux steady state, (2) topographic steady state, (3) thermal steady state, and (4… CONTINUE READING
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    References

    SHOWING 1-10 OF 40 REFERENCES
    Uplift, shortening,and steady state topography in active mountain belts
    • 205
    • PDF
    FLUVIAL LANDSCAPE RESPONSE TIME: HOW PLAUSIBLE IS STEADY-STATE DENUDATION?
    • 343
    • PDF
    Orogeny and orography: The effects of erosion on the structure of mountain belts
    • 776
    Landsliding and the evolution of normal‐fault‐bounded mountains
    • 234
    • PDF
    Equilibrium and time scales in geomorphology: Application to sand-bed alluvial streams
    • 99
    • Highly Influential
    Large‐scale geomorphology: Classical concepts reconciled and integrated with contemporary ideas via a surface processes model
    • 241
    • Highly Influential
    • PDF
    Steady-state exhumation of the European Alps
    • 158
    • PDF