Landscape response to tectonic forcing: Digital elevation model analysis of stream profiles in the Mendocino triple junction region, northern California

@article{Snyder2000LandscapeRT,
  title={Landscape response to tectonic forcing: Digital elevation model analysis of stream profiles in the Mendocino triple junction region, northern California},
  author={N. Snyder and K. Whipple and G. Tucker and D. Merritts},
  journal={Geological Society of America Bulletin},
  year={2000},
  volume={112},
  pages={1250-1263}
}
The topographic evolution of orogens is fundamentally dictated by rates and patterns of bedrock-channel incision. Quantitative field assessments of process-based laws are needed to accurately describe landscape uplift and denudation in response to tectonics and climate. We evaluate and calibrate the shear stress (or similar unit stream-power) bedrock-incision model by studying stream profiles in a tectonically active mountain range. Previous work on emergent marine terraces in the Mendocino… Expand
Channel response to tectonic forcing: field analysis of stream morphology and hydrology in the Mendocino triple junction region, northern California
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