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Thalweg

  • Lesson 4: Sediment Deposition and River Structures

    Lesson 4: Sediment Deposition and River Structures

  • Geomorphic Classification of Rivers

    Geomorphic Classification of Rivers

  • Stream Restoration, a Natural Channel Design

    Stream Restoration, a Natural Channel Design

  • Channel Aggradation by Beaver Dams on a Small Agricultural Stream in Eastern Nebraska

    Channel Aggradation by Beaver Dams on a Small Agricultural Stream in Eastern Nebraska

  • Seasonal Controls on Meteoric 7Be in Coarse‐Grained River Channels

    Seasonal Controls on Meteoric 7Be in Coarse‐Grained River Channels

  • Introduction to Morphodynamics of Sedimentary Patterns

    Introduction to Morphodynamics of Sedimentary Patterns

  • Channel Aggradation by Beaver Darns on a Small Agricultural Stream In

    Channel Aggradation by Beaver Darns on a Small Agricultural Stream In

  • 6.6.4 Bank Angle and Channel Cross-Section

    6.6.4 Bank Angle and Channel Cross-Section

  • Channel Morphology of the Shag River, North Otago 2

    Channel Morphology of the Shag River, North Otago 2

  • Three Dimensional Mobile Bed Dynamics for Sediment Transport Modeling

    Three Dimensional Mobile Bed Dynamics for Sediment Transport Modeling

  • Physical Stream Assessment: a Review of Selected Protocols for Use in the Clean Water Act Section 404 Program

    Physical Stream Assessment: a Review of Selected Protocols for Use in the Clean Water Act Section 404 Program

  • Hydraulic Drag: a Meander-Initiating Mechanism

    Hydraulic Drag: a Meander-Initiating Mechanism

  • Chapter 4. Sediment Transport and Deposition

    Chapter 4. Sediment Transport and Deposition

  • Geomorphic Process Fingerprints in Submarine Canyons

    Geomorphic Process Fingerprints in Submarine Canyons

  • Flux Or Entrainment Form for Sediment Mass Conservation?

    Flux Or Entrainment Form for Sediment Mass Conservation?

  • Grade Control

    Grade Control

  • Stream Dynamics Are Demonstrated Through Dis- Cussion of Processes and Process Indicators; Theory Is Included Only Where Helpful to Explain Concepts

    Stream Dynamics Are Demonstrated Through Dis- Cussion of Processes and Process Indicators; Theory Is Included Only Where Helpful to Explain Concepts

  • Stabilization of a Gravel Channel by Large Streamside Obstructions and Bedrock Bends, Jacoby Creek, Northwestern California

    Stabilization of a Gravel Channel by Large Streamside Obstructions and Bedrock Bends, Jacoby Creek, Northwestern California

Top View
  • Fluvial Requirements for Gravel Bar Formation in Northwestern California
  • Thalweg Detection for River Network Cartography in Forest from High-Resolution Lidar Data
  • Extraction of Thalweg Networks from Dtms: Application to Badlands N
  • Controls on Submarine Canyon Activity During Sea-Level Highstands: the Biobío Canyon System Offshore Chile GEOSPHERE; V
  • Patterns of Alluvial Rivers
  • Download Article (PDF)
  • Channel Dimensions
  • Cedar Rapids Post-Project Channel Change Evaluation King County Water and Land Resources Division
  • Section 2 Standard Methods for Identifying Bankfull Channel Features and Channel Migration Zones
  • Human Elevated Floodplain (IRHEF) Vs. Abandoned Floodplain (IRRAF)
  • Appendix D: Glossary
  • Interpreting Terms Used in River Boundary Definition
  • Developing Hydraulic Relationships at the Riffle Crest
  • Submarine Canyon Systems Focusing Sub-Surface Fluid in the Canterbury
  • Geomorphometry of Drainage Basins: a Global View from the Shuttle
  • River Meanders Theory of Minimum Variance
  • Path of Gravel Movement in a Coarse Stream Channel
  • Effects of Aggradation and Degradation on Riffle-Pool Morphology in Natural Gravel Channels, Northwestern California


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