Abstract
Using the unique data of long-term hydrological observations and detailed topographic survey of river bed in 1946 author evaluated the rate of vertical and lateral channel deformations, the influence of log gorges, icings, and landslides on channel forms development, the features of small river floodplain-terrace complex formation.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
