Results 21 to 30 of about 2,074 (117)

Characteristics of loess seismic subsidence and corresponding micro-zonation for the Fuping Country, Shaanxi

open access: yesZhongguo dizhi zaihai yu fangzhi xuebao, 2023
Typical loess generally shows the property of strong seismic subsidence due to its special microstructure characteristics. Fuping County which is located in the connection zone of Weihe Basin and Ordos Platform possesses complex seismic tectonic settings,
Sen REN   +4 more
doaj   +1 more source

Analysis tectonic role in river terraces geomorphologic evolution Ghezel Owzan [PDF]

open access: yesنشریه جغرافیا و برنامه‌ریزی, 2018
Review of river terraces is main issues related to river geomorphology. They are areas with low slope that is parallel to the axis of the river valley and are in the higher levels of the river bed and created through cutting the river bed and response to
gholam hassan jafari, Mahdei Abbasei
doaj  

The impact of informal irrigation practices on soil drainage condition, soil pollution and land suitability for agriculture in El Saf area of El Giza Governorate

open access: yesEgyptian Journal of Remote Sensing and Space Sciences, 2015
The study area was selected in El Saf District of El Giza Governorate in Egypt, covering 21461.4 ha of Nile sediments and their outskirts of alluvial higher and lower terraces.
Hanan E.M. El Azab   +2 more
doaj   +1 more source

Terrace formation linked to outburst floods at the Diexi palaeo-landslide dam, upper Minjiang River, eastern Tibetan Plateau [PDF]

open access: yesEarth Surface Dynamics
River terraces are frequently investigated with the aim of extracting information regarding tectonic or climate forcing on the evolution of landscapes.
J. Li   +5 more
doaj   +1 more source

Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift

open access: yesOpen Geosciences, 2020
Along the lower reaches of the Yarlung Zangbo River, scattered alluvium sections appear on T1 and T2 terraces. The alluvial deposits on the T1 terrace in Linduo and Ximogou and the T2 terrace in Guoguotang are composed principally of coarse-grained sand ...
Xie Chao   +5 more
doaj   +1 more source

Chemical weathering as a tool for distinguishing river terraces of varying ages: a case study of the Qingyi River on the eastern Tibetan Plateau

open access: yesFrontiers in Earth Science
River terraces are essential objects for studying Quaternary landforms and active tectonics. Previous researchers often identified river terraces formed in different eras by height and landmark strata.
Diwei Hua   +4 more
doaj   +1 more source

Mapping of River Terraces with Low-Cost UAS Based Structure-from-Motion Photogrammetry in a Complex Terrain Setting

open access: yesRemote Sensing, 2019
River terraces are the principal geomorphic features for unraveling tectonics, sea level, and climate conditions during the evolutionary history of a river.
Hui Li   +3 more
doaj   +1 more source

Late Quaternary fluvial terrace formation in the Luan River drainage basin, north China and its possible linkages with climate change and tectonic activation

open access: yesChina Geology, 2023
: The Luan River is the most important water system in north-eastern Hebei Province, China and is located in the transitional zone of the Eastern Yan Mountains, North China Plain and Songliao Plain. The well-developed river terraces of its tributary, the
Yu-chen Tian   +7 more
doaj   +1 more source

Quartz Electron Spin Resonance (ESR) Dating of River Terraces in the Zhenjiang River of the Upper Beijiang River

open access: yesRedai dili
River terraces are important geomorphic indicators that reveal the evolution of rivers, and their climatic and tectonic responses. Dating is key to studying terrace evolution.
Cheng Ziye   +6 more
doaj   +1 more source

Hillslope Sediment Supply Limits Alluvial Valley Width

open access: yesAGU Advances, 2022
River‐valley morphology preserves information on tectonic and climatic conditions that shape landscapes. Observations suggest that river discharge and valley‐wall lithology are the main controls on valley width.
Stefanie Tofelde   +2 more
doaj   +1 more source

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