Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

River sinuosity describes a continuum between randomness and ordered growth

Journal Article · · Geology
DOI:https://doi.org/10.1130/g49153.1· OSTI ID:1822814
 [1];  [2];  [1];  [3]
  1. Univ. of Virginia, Charlottesville, VA (United States)
  2. Univ. of Southampton (United Kingdom)
  3. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

River channels are among the most common landscape features on Earth. An essential characteristic of channels is sinuosity: their tendency to take a circuitous path, which is quantified as along-stream length divided by straight-line length. River sinuosity is interpreted as a characteristic that either forms randomly at channel inception or develops over time as meander bends migrate. Studies tend to assume the latter and thus have used river sinuosity as a proxy for both modern and ancient environmental factors including climate, tectonics, vegetation, and geologic structure. But no quantitative criterion for planform expression has distinguished between random, initial sinuosity and that developed by ordered growth through channel migration. This ambiguity calls into question the utility of river sinuosity for understanding Earth’s history. We propose a quantitative framework to reconcile these competing explanations for river sinuosity. Using a coupled analysis of modeled and natural channels, we show that while a majority of observed sinuosity is consistent with randomness and limited channel migration, rivers with sinuosity ≥1.5 likely formed their geometry through sustained, ordered growth due to channel migration. This criterion frames a null hypothesis for river sinuosity that can be applied to evaluate the significance of environmental interpretations in landscapes shaped by rivers. The quantitative link between sinuosity and channel migration further informs strategies for preservation and restoration of riparian habitat and guides predictions of fluvial deposits in the rock record and in remotely sensed environments from the seafloor to planetary surfaces.

Research Organization:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Organization:
USDOE Laboratory Directed Research and Development (LDRD) Program; National Science Foundation (NSF)
Grant/Contract Number:
89233218CNA000001
OSTI ID:
1822814
Report Number(s):
LA-UR--21-26455
Journal Information:
Geology, Journal Name: Geology Journal Issue: 12 Vol. 49; ISSN 0091-7613
Publisher:
Geological Society of AmericaCopyright Statement
Country of Publication:
United States
Language:
English

References (12)

Cambrian to Devonian evolution of alluvial systems: The sedimentological impact of the earliest land plants journal February 2010
Reconstruction of turbidity currents in Amazon Channel journal June 2003
Hierarchy of models for meandering rivers and related morphodynamic processes: HIERARCHY OF MODELS FOR MEANDERING RIVERS journal February 2007
River dynamics and the diversity of Amazon lowland forest journal July 1986
Downstream changes in river avulsion style are related to channel morphology journal April 2020
Experimental evidence for the conditions necessary to sustain meandering in coarse-bedded rivers journal September 2009
Global extent of rivers and streams journal June 2018
The Osage River and Its Meanders journal July 1893
Controlling factors in the distribution and development of incised meanders in the central Colorado Plateau journal February 1990
A lithologic control on active meandering in bedrock channels journal June 2015
Comparing submarine and fluvial channel kinematics: Implications for stratigraphic architecture journal October 2016
River Restoration and Meanders journal January 2006

Similar Records