Geomorphological immaturity as a factor conditioning the dynamics of channel processes in Rządza River
A major part of Poland, classified geographically as Polish Lowland, is covered by a layer of loose or cohesive sediments whose thickness increases toward the north. Numerous authors emphasize the impact of the protrusion of the erosional base level on the course of processes shaping modern river va...
Main Authors: | Bujakowski Filip, Falkowski Tomasz, Podlasek Anna |
---|---|
Format: | Article |
Language: | English |
Published: |
De Gruyter
2021-01-01
|
Series: | Open Geosciences |
Subjects: | |
Online Access: | https://doi.org/10.1515/geo-2020-0209 |
Similar Items
-
Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia
by: Elena V. Petrova, et al.
Published: (2023-04-01) -
Current dynamics of accumulation and composition of alluvium in the near-channel floodplain of the Oka River (Russia)
by: A.Yu. Vorobyov, et al.
Published: (2021-12-01) -
What is the amount of mercury accumulated in the Idrijca River overbank sediments?
by: Gorazd Žibret, et al.
Published: (2005-06-01) -
Channel Deformations and Hazardous Processes of the Left-Bank Tributaries of The Angara River (Eastern Siberia)
by: Marina Y. Opekunova, et al.
Published: (2023-01-01) -
Statistical correlations between standard penetration test n value and pressuremeter modulus for kallang and old alluvium formation /
by: Chia, Pooi Sian, 1990- author 638713, et al.
Published: (2020)