Results 101 to 110 of about 18,588 (223)

KLIMONAS-Ch03-A03 – Description of the fluvial terraces profiles under study

open access: yes, 2023
Appendix of: Vigne J.-D., Briois F., Guilaine J. (eds.), « Klimonas, an Early Pre-Pottery Neolithic village in Cyprus », Gallia Préhistoire & Paléorient, International Supplement 1, CNRS Éditions, Paris, 2023.
DEVILLERS, Benoît, MYLONA, Pantelitsa
openaire   +2 more sources

Palaeoglacier reconstruction and dynamics of Cordillera Vilcanota in the tropical high Peruvian Andes

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 2, February 2026.
We provide a geomorphological analysis of Cordillera Vilcanota and use morphostratigraphic principles to reconstruct palaeo icefield extent and palaeoglacier readvances, likely during the Antarctic Cold Reversal and Younger Dryas. We find evidence of temperate and polythermal ice margins, with limited glaciofluvial landform generation.
Bethan Davies   +11 more
wiley   +1 more source

Fluvial terrace formation in a mountainous area (2): influence of eustatism, tectonics and altitudinal distribution of watersheds based on an allostratigraphic study (Albania)

open access: yesComptes Rendus. Géoscience
Terraces are highly developed along the Albanian rivers and eleven levels of terraces are recognized in the area, nine occurring during the last glacial cycle (MIS 5d to end of MIS 2).
Mugnier, Jean-Louis   +4 more
doaj   +1 more source

Erosive Response of Non-Glaciated Pyrenean Headwater Catchments to the Last Major Climate Transition and Establishing Interglacial Conditions

open access: yesQuaternary, 2019
Non-glaciated mountain headwater catchments feature high-resolution geomorphic archives, which provide important insight into erosive processes and sediment dynamics in mountain ranges.
Kurt Martin Stange   +7 more
doaj   +1 more source

Deformational behaviours of alluvial units detected by advanced radar interferometry in the Vega Media of the Segura River, southeast Spain [PDF]

open access: yes, 2016
It is widely known that differential land subsidence in a valley significantly controls its fluvial dynamics. Nevertheless, major uncertainty exists about the way in which alluvial forms respond to this process.
Cano, Miguel   +6 more
core   +2 more sources

Anastomosis and Low Flows Sustain Resilient Groundwater Dependent Riparian Floodplains in an Agricultural River Valley, New Mexico

open access: yesHydrological Processes, Volume 40, Issue 2, February 2026.
Groundwater‐dependent native riparian ecosystems of the Gila River floodplain (a) near the upstream end of the valley in winter 2014 and (b) near the downstream valley end in summer 2018. Topographically complex floodplains create favourable conditions across the full breadth of the valley bottom for a diversity of native groundwater‐dependent ...
Ellen Soles, Martha Cooper, Laurel Saito
wiley   +1 more source

Autogenic entrenchment patterns and terraces due to coupling with lateral erosion in incising alluvial channels [PDF]

open access: yes, 2017
The abandonment of terraces in incising alluvial rivers can be used to infer tectonic and climatic histories. A river incising into alluvium erodes both vertically and laterally as it abandons fill-cut terraces.
Avouac, Jean-Philippe   +2 more
core   +2 more sources

Evaluating the Interpretation Uncertainty From the Manual Streambank Delineation

open access: yesRiver Research and Applications, Volume 42, Issue 2, Page 495-506, February 2026.
ABSTRACT Streambank delineation enables the development of two important parameters: streambank position and channel width. For older aerial images that cannot be easily processed by automatic methods, manual interpretation of streambanks is a necessary task.
Megan M. Carr   +2 more
wiley   +1 more source

Fluvial terrace formation in mountainous areas: (1) Influence of climate changes during the last glacial cycle in Albania

open access: yesComptes Rendus. Géoscience
This work analyses terraces formation from the case of Albanian rivers. An allostratigraphy study of the fluvial terraces is combined with new numerical dating.
Guzmán, Oswaldo   +5 more
doaj   +1 more source

Textural and Lithologic Differences of Cretaceous, Tertiary, and Quaternary Gravels of South Arkansas [PDF]

open access: yes, 1987
Stream gravels have been derived from the Ouachita Mountains since at least Cretaceous times. Past studies have assigned ages to gravel deposits in the basins of the Saline and Little Missouri Rivers on the basis of altitude above local floodplains. This
Wood, Lesli
core   +2 more sources

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