Logjams are not jammed: measurements of log motions in Big Creek, Idaho
Nakul S. Deshpande, Benjamin T. Crosby

TL;DR
This study uses in-situ measurements to demonstrate that natural logjams in rivers are not actually jammed but exhibit continuous, slow deformation influenced by water flow, offering insights into their dynamics and hazards.
Contribution
First in-situ field measurements of natural logjam dynamics revealing continuous deformation rather than complete arrest, bridging environmental observations with soft matter physics.
Findings
Logjams are not fully jammed but deform continuously.
Log motion correlates with water flow and hydrograph stages.
Deformation patterns resemble creep and clogging behaviors.
Abstract
Colloquially, a "logjam" indicates a kinematic arrest of movement. Taken literally, it refers to a type of dense accumulation of wood in rivers widely recognized as bestowing numerous biological and physical benefits to the system but also present serious hazards to infrastructure. Despite this, no in-situ field measurements have assessed the degree of arrest in a naturally-formed logjam. Using time-lapse photography, repeat total station surveys and water level loggers, we provide an unprecedented perspective on the evolution of a logjam in central Idaho. Despite the namesake, we find that the logjam is not jammed. The ensemble of logs progressively deforms in response to shear and buoyant lift of flowing water, modulated by the rising limb, peak and falling limb of the snowmelt hydrograph. As water rises and log drag against the bed and banks decreases, they collectively translate…
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Taxonomy
TopicsHydrology and Sediment Transport Processes · Geological formations and processes · Soil erosion and sediment transport
