Contact:
Name:
Prancevic, Jeff P.
Institution:
California Institute of Technology
contributor_email:
Laboratory experiments on initial sediment motion that cross the river to debris-flow sediment-transport transition. Results show that initial sediment motion by river processes requires heightened dimensionless bed shear stress (or critical Shields stress) with increasing channel-bed slope by as much as fivefold the conventional criterion established for lowland rivers.
Date Last Updated:
Friday, August 15, 2014
Image:
![prancevic](/sites/sedexp.umn.edu/files/2023-05/prancevic.png)
Language:
English
Rights management:
CC-BY
Coverage:
Location:
Geolocation is 34.1376576, -118.125269
Dates Collected:
Friday, August 15, 2014
Resource Type:
dataset
Degree of processing:
2: derived