Planform Change of River Networks and Their Drainage Basins
Planform Change of River Networks and Their Drainage Basins
Session ID#: 123003
Session Description:
River networks carve Earth’s surface into ridges and valleys and are conduits for sediment, water, nutrients, and organisms. Rivers can change in elevation by eroding their beds, but erosion can also generate planform change in river networks, with basins changing shape and size as divides move either through gradual migration or discrete river capture. The topology and geometry of river basins is shaped by external forcing (e.g., climate and tectonics) as well as internal dynamics such as lateral channel migration, landslides, or geological structures.
This session invites contributions that explore any aspect of river basin evolution, including studies that reconstruct paleo-river basins, investigate drivers of river basin evolution, or illustrate the implications of river basin dynamics for other Earth systems (e.g. sedimentary record, biological evolution). We welcome submissions from any disciplinary perspective, over any time and space scales, that use approaches ranging from field data to experimental or numerical modeling.
Index Terms:
1130 Geomorphological geochronology [GEOCHRONOLOGY]
1140 Thermochronology [GEOCHRONOLOGY]
1625 Geomorphology and weathering [GLOBAL CHANGE]
8175 Tectonics and landscape evolution [TECTONOPHYSICS]
Primary Convener: Helen Willemien Beeson, ETH Zurich, Department of Earth Sciences, Zurich, Switzerland
Convener: Maya F. F. Stokes, Massachusetts Institute of Technology, Cambridge, MA, United States
Primary Liaison: Helen Willemien Beeson, ETH Zurich, Department of Earth Sciences, Zurich, Switzerland
See more of: Earth and Planetary Surface Processes