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N. J. Finnegan Interpretation and downstream correlation of bedrock river terrace treads created from propagating knickpoints Journal of Geophysical Research: Earth Surface 118

Article first published online: 27 JAN 2013 | DOI: 10.1029/2012JF002534

Key Points

  • Time-transgressive terraces constrain incision rate dependence on channel slope
  • Time-transgressive terraces do not record the rock uplift field in a simple way
  • A process of incision with a slope threshold best explains terrace gradients

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