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The formation of terraces and channel pattern changes in mountain rivers : findings from the upper Sava valley (Slovenia)
ID
Słowik, Marcin
(
Author
),
ID
Golob, Nejc
(
Author
),
ID
Grčman, Helena
(
Author
),
ID
Zupanc, Vesna
(
Author
)
PDF - Presentation file. The content of the document unavailable until 18.04.2028.
MD5: 6E867B9E34B85E0C8C3842BC245D2AA7
URL - Source URL, Visit
https://www.sciencedirect.com/science/article/pii/S034181622600305X
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Abstract
The evolution of many European mountain rivers was marked by the formation of terraces. Conditions influencing the formation of new floodplain levels and trajectories of channel pattern changes in montane settings remain understudied. The main goal of our research was to determine factors influencing a spatial and temporal formation of terraces and changes in channel planforms of the upper Sava River (Slovenia). We also reconstructed a trajectory of channel planform changes, the traces of which are preserved within the terrace levels. Our research was based on geophysical and geological surveys, analyses of digital terrain models and historical maps, and data from other studies in the upper Sava and other mountain rivers of Europe. Incisions to new floodplain levels commenced in interstadials characterized by glacier retreat. Stabilization of the floodplain levels took place in cold periods 50,000–40,000 BP (terrace I); 35,000–20,000 BP (terrace II); 15,000–10,000 BP (terrace III), and 5000 BP (modern floodplain). We identified traces of meandering and wandering channel planforms within the terraces. The Sava River evolved from braided (terrace I), through meandering with local traces of wandering river at terraces II-III, to a wandering planform preserved in the modern floodplain. The wandering pattern was active until constructions of dams in the 20th century. The formation time of the Sava terraces corresponds to the evolution of other mountain rivers situated in the Alps, Pyrenees, and Crete. The identified sequence of terraces formation can be connected with warm and cold climate phases. The influence of the climate changes was enhanced e.g. by the formation of glacial lakes causing sediment deficits in river valleys after 20,000 BP and meander cutoffs increasing valley slopes especially during the transition to the wandering planform in the Early and Middle Holocene.
Language:
English
Keywords:
terrace formation
,
meandering rivers
,
wandering rivers
,
incision
,
the Sava River valley
,
anthropogenic impact
Work type:
Article
Typology:
1.01 - Original Scientific Article
Organization:
BF - Biotechnical Faculty
Publication status:
Published
Publication version:
Version of Record
Year:
2026
Number of pages:
20 str.
Numbering:
Vol. 269, art.110095
PID:
20.500.12556/RUL-181948
UDC:
551.4
ISSN on article:
0341-8162
DOI:
10.1016/j.catena.2026.110095
COBISS.SI-ID:
275841795
Publication date in RUL:
20.04.2026
Views:
150
Downloads:
36
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Record is a part of a journal
Title:
Catena : an interdisciplinary journal of soil science, hydrology- geomorphology focusing on geology and landscape evolution
Shortened title:
Catena
Publisher:
Elsevier
ISSN:
0341-8162
COBISS.SI-ID:
25199104
Licences
License:
CC BY-NC-ND 4.0, Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
Link:
http://creativecommons.org/licenses/by-nc-nd/4.0/
Description:
The most restrictive Creative Commons license. This only allows people to download and share the work for no commercial gain and for no other purposes.
Secondary language
Language:
Slovenian
Keywords:
nastanek teras
,
gorske reke
,
Sava
Projects
Funder:
Other - Other funder or multiple funders
Funding programme:
Adam Mickiewicz University in Poznan, Poland
Name:
Initiative of Excellence - Research University grant 165/07/POB1/000
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
P4-0085
Name:
Agroekosistemi
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
J7-60124
Name:
Celostni pristop k preučevanju vplivov ekstremnih vremenskih dogodkov na procese na Zemljinem površju (ExtremEarth)
Funder:
ARIS - Slovenian Research and Innovation Agency
Funding programme:
Young Researcher Program
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